Abstract
Energy levels and Lande g-factors for the configurations 3dn4p+3dn−14s4p+3dn−24s24p in the first spectra of the iron group were calculated and compared with experimental values, in both general and individual treatments. The calculations were done in intermediate coupling taking into account explicity the interactions between configurations, as well as complete effective interactions of the core, and effective interactions d − p. Due to a successful starting point based on Hartree-Fock calculations for the Slater parameters, as well as the insertion of the effective interactions, considerable improvement was obtained compared to previous results.
On fitting 1537 levels using 67 free interaction parameters a mean error of 182 cm−1 was obtained. Altogether 3652 energy levels were calculated including all the levels for the configurations 3dn−24s24p across the sequence. It was shown that all interaction parameters could be expressed either as linear functions, or linear functions with small quadratic corrections, of the atomic number. There was general qualitative agreement between the values of the parameters calculated using the semi-empirical method and those calculated using Hartree-Fock methods. There remained some isolated terms with large deviations. These are attributed to be due to the interactions with the configurations (3d+4s)n5p, that were not considered explicitly in this analysis.
Tables comparing the experimental and calculated energy levels and Lande g-factors, as well as detailed analyses for each spectrum are given in another paper.
Keywords: Iron group elements, least squares optimization, theoretical spectroscopy
1. Introduction.
Traditionally, theoretical spectroscopists consider the radial Slater integrals as unknown parameters, obtaining their values empirically by fitting the experimental data to the calculated energy levels, and then performing least-squares optimization calculations.
For the even configurations 3dn + 3dn−14s, and the odd configurations 3dn4p in the second and third spectra of the iron group, the results were excellent, [1–4].1 Furthermore, it was shown that the radial parameters are either linear functions, or linear functions with small quadratic corrections, of the atomic number. For the odd configurations in neutral atoms, the interactions between configurations are very strong. Thus the algebraic matrices of the configurations (d + s)np were calculated and checked by the author, [5–9]. Theoretical investigations were then performed for the configurations (3d + 4s)n4p in neutral atoms of calcium, scandium, titanium, vanadium, chromium, manganese, iron, cobalt and nickel, [10–16].
Although the results were good (average r.m.s. error of 210cm−1); a very disturbing feature of the results was the fact that the behavior of the final values of the radial parameters was generally far from linear.
It would be highly anomalous to have the radial parameters behave so irregularly in the first spectra. Thus, in order to overcome this discrepancy it was essential to have improved initial values of the radial parameters. Hence the radial parameters were first calculated using the Hartree-Fock method. Least-squares optimization calculations were then performed on these parameters forcing them to behave linearly, with possibly at most small quadratic corrections, as functions of the atomic number. The values thus computed were then compared with those obtained previously in individual treatments by the author, [10–16]. Whenever the Hartree-Fock values were uniformly higher or lower than those of the previous results, [10–16], appropriate scaling factors were utilized on the linearized Hartree-Fock values, and the latter were than used as initial parameters for this investigation.
In this project were included the electrostatic and spin-orbit interactions of the individual configurations 3dn4p, 3dn−14s4p and 3dn−24s24p; the explicit electrostatic interactions between configurations 3dn4p−3dn−14s4p, 3dn−14s4p−3dn−24s24p and 3dn4p−3dn−24s24p; and the complete two- and three-body effective interactions of the core d electrons, as well as two-body mixed effective interactions between the 3d and 4p electrons.
The initial values of the radial parameters were then used to multiply the algebraic matrices on tape and the resulting matrices were diagonalized. Besides the eigenvalues, the diagonalization routine also yields the derivatives of the eigenvalues with respect to the parameters, the squares of the eigenvectors (percentage compositions) and the calculated Lande g values. The appropriate experimental levels were then fitted to the eigenvalues, and using the derivatives obtained in the diagonalization, least squares optimization calculations were performed. In these calculations, the improved values of the theoretical energy levels, the corrected values of the parameters including their statistical deviations and the sum of the squares of the differences between the observed and the calculated levels, were obtained. The rms error is then defined as
where the Δi are the differences between the observed and calculated levels, n is the number of known levels and m is the number of free parameters. The mean error is quite different from the mean deviation
as the former takes into account the statistical effect of the number of free parameters. Hence in order for a new parameter to have physical significance, it should cause an essential decrease in the rms error, and not simply a decrease in the mean deviation.
The value of Δ is also given by the least-squares routine. The same derivatives can be used for several variations in the least squares, either imposing different conditions on the parameters, inserting the experimental levels with different assignments, or even rejecting some levels from consideration. The parameters of that variation which yielded the best results were used to perform new diagonalizations. This iterative process was continued until mathematical convergence was attained. In the present project four complete iterations were required.
The use of the same assumptions and the same approximations in all the spectra made it possible to obtain a consistent set of interaction parameters and compare the results obtained from the spectra of different elements. Due to a successful choice of the initial values of the radial parameters, it was shown that the final values can indeed be expressed as simple functions of the atomic number. A consistent use of such interpolation formulas for all parameters, combined eleven problems, formerly independent, into one problem. This result, which is significant by itself, very much improved the reliability of the results for those spectra where the experimental data is still scarce, and which are thus most in need of reliable predictions of the unknown levels.
This is particularly true for the configurations 3dn−24s24p. For each individual element there in not a sufficient number of experimental levels in order to predict even approximately the remaining levels. However, by considering a general treatment ALL the levels of the configurations 3dn−24s24p for the entire sequence were calculated.
For completeness and comparison, individual least squares (ILS) were also performed for each element.
The procedures followed, a description of the various interactions considered, and an analysis of the results and significance of the different parameters are contained in this work. The tables comparing the experimental and calculated energy levels, values for all the theoretical levels specifying their percentage compositions, as well as detailed analyses for each spectrum are given in another paper, [17].
2. Effective electrostatic interactions
For the odd configurations in the first spectra of the iron group, both strong and weak configuration interactions are significant. The former arise when the perturbing and perturbed configurations are energetically close to each other and there is strong coupling of the configurations by the Coulomb field. These were taken into account by explicitly considering the configurations 3dn4p, 3dn−14s4p, 3dn−24s24p and the electrostatic interactions between them. Weak interactions occur when the perturbing configurations are well separated from the perturbed configuration, and the coupling of the Coulomb field is weak.
The individual weak interactions may not be significant, but their cumulative influence may be quite large, due to the increasing density of states as the continuum is approached. As it would be completely futile to consider each of these effects individually, the aim should be to modify the energy matrices of the principal configurations so that the major part of all the weakly perturbing configurations be included.
By first order perturbation theory, different configurations do not interact. In second order only those configurations interact that differ in the quantum numbers of at most two electrons. Bacher and Goudsmit, [18], have shown that the terms of the configuration ln may be expressed as linear combinations of the terms of l2, so that the perturbation of ln by all the configurations differing from it by the state of two electrons, and being distant from it, can be accounted for by suitably modifying the terms of l2. Hence these perturbations can be described by two-body effective interactions.
The first correction of this kind for the configurations dn was the αL(L+1) correction introduced by Trees, [19–20], in the configurations 3d54s of MnII and FeIII. Trees introduced his correction empirically, but Racah, [21], showed that the above effects can be described by a model or effective interaction of the form
where q12 is the seniority operator, [22]. For the configuration dn this becomes
where
| (1) |
is the total seniority operator. Here n is the number of d electrons in the configurations dnp, v is the seniority of the dn core term, and l is 2 as we are dealing with d electrons. The constant −6nα is usually incorporated into the height of the configuration. Racah, [21], showed that the αL(L +1) and the βQ corrections form a complete set of two-body effective interactions for the dn configurations. This is due to the fact that together with the Slater integrals F0(d2), F2(d2) and F4(d2), they form a set of five independent parameters that can represent the five terms of d2.
Bacher and Goudsmit, [18], also showed that if the far-lying perturbing configuration differs from ln by the state of only one electron, its effect can be described by expressing the terms of ln as linear combinations of l3, and modifying the values of these terms. Hence in the linear theory, the Hamiltonian in this case must be augmented by additional three-body interactions.
Rajnak and Wybourne, [23], obtained explicit formulas for the effective interactions representing the perturbation of an ln configuration by far-lying configurations differing from it by one or two electrons or holes. Racah and Stein, [24], subsequently, developed an elegant method that considerably simplified the calculations of Rajnak and Wybourne.
If A and B represent the perturbed and perturbing configurations, respectively, and if G is the operator representing the Coulomb energy of repulsion between the electrons, , then the matrix elements of the second-order perturbation produced by B on A are given approximately by
| (2) |
where ΔE is the distance between the centers of gravity of the two configurations, which are assumed to be well separated. According to Racah and Stein, [24], the operator G in the first factor is replaced by a “curtailed” operator g, whose matrix elements (A′ψ∣g∣B′ψ″) are equal to those of G if A′ = A and B′ = B, and vanish otherwise. Similarly, the operator G in the second factor is replaced by , defined analogously to g. Then
| (3) |
where the summation is over the complete set B′Ψ″. Thus,
| (4) |
and hence the electrostatic interaction between the configuration A and all the other distant configurations may be simply expressed as an effective interaction within the configuration A given by
| (5) |
Then using either the above method or that of Rajnak and Wybourne, [23], we obtain that the correction term W2, that must be added to the Hamiltonian of ℓn caused by the perturbation of ℓn by ℓn−1 ℓ′ configurations is given by
| (6) |
where
| (7) |
and
| (8) |
ΔE is the distance between the perturbing configuration and ℓn,
| (9) |
For the perturbation of ℓn by ℓ′ (4ℓ′+1)ℓn+1 we similarly obtain
| (10) |
where
| (11) |
The P are radial parameters; the ϕ and ϕ′ are their coefficient operators.
The matrix elements of ℓn can be calculated by Racah algebra. The variables k and k′ are even and nonzero integers that must satisfy the usual triangular conditions of the 6-j symbols. The variables k″ can assume all integral values consistent with the triangular conditions for the 6-j symbols.
The parameter T represents the perturbation of the configuration 3dn by the configuration 3s3dn+1. It was first considered by Trees, [25], when he investigated the configuration 3s23p63d6, and took into account its interaction with the configuration 3s3p63d7. Shadmi, [26] extended the work of Trees to all configurations 3dn + 3dn−14s + 3dn−24s2 in the sequence of the second spectra of the iron group by introducing a three-body effective interaction between 3d electrons which represented the perturbation of a configuration of the type 3s23dn by the configuration 3s3dn+1. Roth [3–4] included the parameters α, β and T in the configurations 3dn4p in the second and third spectra of the iron group, as well as for the configurations 3d34p + 3d24s4p in V II, [27].
Further important investigations were carried out by Shadmi, Stein, Oreg, Caspi, Goldschmidt and Starkand [28–30].
Now from (10) with k = k′ =2 here, we have .
where we used according to Racah, [22]. However, in order to be consistant with the definition of
used in a previous work by the author, [7], we get for the coefficient operator of T the expression
| (12) |
The parameters Tx, Ty, Tz represent the perturbation of the configuration 3dn by a configuration of the type 3dn−1n′d, where n′ ⩾4. Similarly, to the above result for t their coefficient operators tx, ty, tz are
| (13a) |
| (13b) |
| (13c) |
In terms of the P, the parameters are given by
| (14a) |
| (14b) |
| (14c) |
| (14d) |
Only the parameters T and Tx were used as Ty and Tz depend upon the other parameters.
2.1. Effective interactions in the configuration ℓnℓ′
First we define the tensor operators u(k), v(k), w(k), , y(k), , z(k) and as the tensor operators of order k whose only non-vanishing reduced matrix elements are
| (15a) |
| (15b) |
| (15c) |
| (15d) |
| (15e) |
Then in terms of the quantities P and X defined in (7) and (8), the curtailed operators g and representing the effective interactions of the configuration ℓnℓ′, may be written as
| (16) |
and
| (17) |
Upon substituting (16) and (17) into (5) we obtain after considerable manipulation
| (18) |
where
| (19) |
| (20) |
| (21) |
| (22) |
WB represents a two-body interaction and for even values of t is a linear combination of the coefficients of the Slater parameters Ft (ℓℓ′). However, new parameters are obtained for odd values of t. The second term of Wc, also representing a two-body interaction, yields new parameters with t equal to ℓ + ℓ′ + 1. Hence a Hamiltonian , containing the two-body contribution to W2 may be written
| (23) |
The two terms are referred to as the direct and exchange effective Slater parameters. The matrix elements of are diagonal in S and L, and are independent of J and M.
WA represents a three-body interaction if i ≠ j ≠ s. Otherwise, it contains mixtures of one and two-body terms which either vanish or have been previously considered. Hence taking this term and the first term of Wc, the Hamiltonian representing the three-body effective electrostatic direct and exchange interactions, may be written
| (24) |
The coefficients of Ft in the configuration are found by calculating the matrix elements
Since this involves the reduced matrix element (p∥v(t)∥p), t may take only the values 0, 1 and 2 because of the triangular relationship δ(1,t,1) between the two p angular momenta and t. For t equal to 0 and 2 the Slater parameters F0 and F2 are included elsewhere (see sec. 3). Thus, the only new direct effective parameter for dnp as well as for dn−1sp and dn−2s2p is F1.
Similarly for Gt, the calculation of the matrix elements
is required. Due to the reduced matrix element (p∥z(t)∥p) with the triangular relation δ(2,t,1), t may take on the values 1, 2 or 3. Since G1 and G3 are already included elsewhere, the only new exchange effective parameter is G2.
The three-body effective interactions involve 9 independent parameters. They were not included in this investigation as their contributions are not expected to be significant (see sec. 4).
3. Parameters
The algebraic matrices of (d + s)np comprise the electrostatic and spin orbit interaction matrices of the configurations dnp, dn−1sp and dn−2s2p; the electrostatic interactions between configurations dnp − dn−1sp, dn−1sp − dn−2s2p, dnp − dn−2s2p; the complete two and three-body effective interactions of the core d electrons, as well as two-body mixed effective interactions between the d and p electrons. The energy matrix (for a particular n) is then a linear combination of these matrices, the coefficients of which are parameters to be discussed below. Unprimed quantities denote the configuration dnp, primes denote dn−1sp and double primes denote dn−2s2p.
A, A′, A″—the heights of the configurations,
B, B′, B″—linear combinations of the Slater parameters F2(dtd) and F4(d,d):
C, C′, C″—multiples of the Slater parameter F4(d,d):
Gds—the parameter of the d − s interaction in the configuration dn−1sp:
F2, , —parameters of the direct part of the d-p interaction:
G1, , —parameters of the exchange part of the d-p interaction:
G3, , —parameters of the exchange part of the d-p interaction:
Gps—the parameter of the p − s interaction in the configuration dn−1sp:
H—the parameter of the dn − dn−1s interaction:
H′—the parameter of the dn−1s − dn−2s2 interaction, defined the same as H.
J—the parameter of the direct part of the dnp − dn−1sp interaction:
J′—the parameter of the direct part of the dn−1sp − dn−2s2p interaction, defined the same as J.
K—the parameter of the exchange part of the dnp − dn−1sp interaction:
K′— the parameter of the exchange part of the dn−1sp − dn−2s2p interaction, defined the same as K.
G*—the parameter of the dnp − dn−2s2p interaction:
The spin-orbit contribution to the Hamiltonian has the form (p. 120, TAS, [32],)
where ri is the distance of the i th electron from the nucleus,
∪(ri) is the potential in which the i th electron moves and μ is the reduced mass of the electron. Then,
where is the radial part of the wave function. Then ζd, , —parameters of the spin-orbit interaction of the d-electrons. ζp, , —parameters of the spin-orbit interaction of the p-electron.
The following parameters were discussed in detail in the previous section:
α, α′, α″—parameters of the L(L + 1) correction.
β, β′, β″—parameters of the Q correction.
T, T′, T″ parameters of the three-body effective
Tx, , interactions of the core d-electrons.
F1, ,—parameters of the direct part of the effective interactions.
G2, ,—parameters of the exchange part of the effective interactions.
The calculated Lande g-factors given by
were also computed. Whenever observed g-values exist, they provide very useful information to help fit the experimental levels.
Racah and Shadmi [1,2,9] have shown that if M(dn), M′(dn−1s) and M″(dn−2s2) are the centers of gravity of dn, dn−1s and dn−2s2, i.e., the weighted averages of the terms of these configurations, then the parameters
and
are linear functions with small quadratic corrections of n for the configurations (3d + 4s)n in the second spectra of the iron group.
Now in dnp we must consider n interactions d − p, n(n − 1)/2 interactions d − d. From page 200, TAS, [32], the center of gravity of dp is
| (25) |
From equation (78) of Racah [31], the center of gravity of d2 is
| (26) |
Also, (p.197, TAS, [32],)
| (27) |
| (28) |
Since H, H′, J, J′, K, K′ and G* don’t have diagonal elements, they need not be considered for the centers of gravity.
Now, by taking into account α, we have
| (29) |
As explained in the previous section, the L(L + 1) correction has to be considered in the form [L(L + 1) − 6n) α. Thus, write
| (30) |
For the βQ correction we note that since Q is a two-body operator, and for d2 we have a contribution of 1/9, the net contribution to dn will be . Since T represents a three-body interaction, its contribution will involve a cubic in n. Since there is no interaction of s2dn with sdn+1 for n = 0,9,10, the polynomial must vanish for those n. For n = 1 the contribution is easily seen to be 70, and thus the contribution to dn is (35/36) n (9 − n) (10 − n). Directly from the algebraic matrices of the parameters Tx, and it was seen that these parameters do not contribute to the center of gravity.
Finally, the direct part of the effective interaction for dnp has no contribution to the center of gravity, whereas the exchange part gives nG2.
Thus, we obtain
| (31) |
| (32) |
Since for dn−2s2p the interactions d − s and s − p are constant and thus can be incorporated into the height of the configuration, we have
| (33) |
The above expressions must be modified for complementary configurations (n > 5). The matrices of B, C, α, and β for the configurations dnp, dn−1sp, and dn−2s2p are equal to the corresponding matrices of the complementary configurations d10−ns2p, d11−nsp, and d12−np, respectively, [7]. Also, the matrices of Gds and Gps for dn−1sp are equal to the corresponding matrices of d11−nsp. The matrices of T and G2 must be replaced for complementary configurations by those of Tc and G2c, respectively, [7]. Since the weighted average of the terms of d9p is given by
we obtain
| (34) |
| (35) |
| (36) |
The checks of the algebraic matrices were described previously by the author, [8,9]. In section 5, [9], we had
| (37) |
In analogy to the above result we obtain
| (38) |
where t, tc, tx, txc, b, and c are the algebraic matrices of the parameters T, Tc, Tx, Txc, B, and C, respectively, and k is a numerical constant. The checks are possible because the sum of either t and tc, or tx and txc, gives rise only to two-body and one-body terms, that may be expressed as linear combinations of the algebraic matrices associated with the two and one-body parameters β, α, B, and C of the configuration dn. The algebraic matrices of the parameters T, T′, T″, Tc, , , Tx, , , Txc, and were added to the previously calculated matrices and the above checks utilized.
In the general treatment, with the exception of the centers of gravity M(dnp), the parameters are required to satisfy the interpolation formula
| (39) |
where P0, P1, and P2 are the general parameters and replace the individual parameter P for all the spectra of the sequence; n is the number of 3d and 4s electrons for each spectrum. As an example, in table 42, B0, , refer to the constant terms; B1, , to the linear terms; B2, , to effectively the quadratic terms, for the configurations dnp, dn−1sp and dn−2s2p, respectively, in the general treatment.
Table 42.
General interpolation parameters preliminary iterations
| PAR. | INITIAL | GLS 1 | GLS 1a | GLS 2 | GLS 2a | GLS 2b | GLS 3 | GLS 3 | GLS 3b | GLS 3c |
|---|---|---|---|---|---|---|---|---|---|---|
| 1610.69 | 860 ± 31 | 543 ± 108 | 773 ± 32 | 713 ± 67 | 795 ± 40 | 948 ± 37 | 585 ± 79 | 906 ± 38 | 974 ± 39 | |
| 28623.08 | 28482 ± 62 | 26086 ± 236 | 28746 ± 81 | 28674 ± 107 | 28350 ± 92 | 28682 ± 81 | 28723 ± 101 | 28665 ± 87 | 28527 ± 110 | |
| 3892.39 | 3641 ± 16 | 3550 ± 42 | 3673 ± 16 | 3614 ± 22 | 3661 ± 16 | 3688 ± 16 | 3487 ± 29 | 3703 ± 18 | 3709 ± 16 | |
| 5951.37 | 5719 ± 21 | 5278 ± 164 | 5711 ± 20 | 5898 ± 44 | 5738 ± 27 | 5738 ± 20 | 5832 ± 80 | 5731 ± 29 | 5740 ± 30 | |
| 0 | −123 ± 4 | −133 ± 5 | −128 ± 5 | −130 ± 5 | −123 ± 5 | −117 ± 5 | −135 ± 9 | −120 ± 5 | −115 ± 5 | |
| 0 | −123 | −238 ± 67 | −128 | −127 ± 13 | −123 | −117 | −94 ± 12 | −120 | −115 | |
| B 0 | 769 | 734 ± 8 | 745 ± 13 | 727 ± 6 | 734 ± 6 | 731 ± 5 | 717 ± 5 | 735 ± 8 | 712 ± 6 | 719 ± 5 |
| 853 | 863 ± 6 | 854 ± 7 | 849 ± 4 | 849 ± 4 | 852 ± 3 | 848 ± 3 | 840 ± 5 | 845 ± 4 | 848 ± 3 | |
| 937 | 992 | 963 | 971 | 964 | 973 | 979 | 945 | 978 | 977 | |
| B 1 | 67 | 52 ± 2 | 57 ± 3 | 53 ± 2 | 57 ± 2 | 55 ± 2 | 52 ± 2 | 60 ± 3 | 52 ± 2 | 52 ± 2 |
| 61 | 62 ± 2 | 59 ± 2 | 60 ± 2 | 57 ± 2 | 59 ± 2 | 61 ± 2 | 57 ± 2 | 61 ± 2 | 60 ± 2 | |
| 55 | 72 | 61 | 67 | 57 | 63 | 70 | 54 | 70 | 68 | |
| C 0 | 2802 | 2898 ± 31 | 2889 ± 50 | 2954 ± 30 | 2896 ± 42 | 2935 ± 25 | 2988 ± 21 | 2919 ± 42 | 2998 ± 25 | 2988 ± 26 |
| 3133 | 3255 ± 28 | 3258 ± 49 | 3319 ± 26 | 3325 ± 22 | 3306 ± 20 | 3338 ± 19 | 3361 ± 37 | 3340 ± 19 | 3332 ± 20 | |
| 3464 | 3612 | 3627 | 3684 | 3754 | 3677 | 3688 | 3803 | 3682 | 3676 | |
| C 1 | 244 | 408 ± 8 | 402 ± 14 | 433 ± 7 | 419 ± 13 | 429 ± 8 | 437 ± 8 | 413 ± 11 | 429 ± 9 | 438 ± 9 |
| 220 | 304 ± 7 | 317 ± 12 | 354 ± 7 | 353 ± 11 | 347 ± 9 | 351 ± 8 | 357 ± 11 | 351 ± 9 | 352 ± 9 | |
| 196 | 200 | 232 | 275 | 287 | 265 | 265 | 301 | 273 | 266 | |
| (G3)1 | −1.54 | −7.0 ± 2.0 | 0.1 ± 2.2 | 2.2 ± 0.7 | 1.8 ± 1.1 | 0.3 ± 0.5 | 0 (FIX) | −0.8 ± 1.1 | 0.8 ± 0.6 | 0 (FIX) |
| −0.97 | −7.0 ± 1.8 | −2.2 ± 2.0 | 2.2 | −2.8 ± 0.8 | 0.3 | 0 | −3.5 ± 1.2 | 0.8 | 0 | |
| −0.40 | −7.0 | −4.3 | 2.2 | −7.4 | 0.3 | 0 | −6.2 | 0.8 | 0 | |
| (G3)2 | 0.44 | 1.4 ± 2.0 | −0.9 ± 0.3 | 0 (FIX) | −1.2 ± 0.3 | 1.4 ± 0.2 | 0 (FIX) | −1.1 ± 03 | 0 (FIX) | 0 (FIX) |
| 0.20 | −1.4 | −1.1 ± 0.3 | 0 | −1.0 ± 0.3 | −1.4 | 0 | −1.1 | 0 | 0 | |
| −0.04 | −1.4 | −1.3 | 0 | −0.8 | −1.4 | 0 | −1.1 | 0 | 0 | |
| (Gps)0 | 6295.11 | 6516 ± 37 | 6451 ± 76 | 6406 ± 36 | 6517 ± 42 | 6494 ± 33 | 6469 ± 33 | 6597 ± 46 | 6443 ± 34 | 6515 ± 33 |
| (Gps)1 | 149.80 | 238 ± 13 | 244 ± 38 | 244 ± 12 | 258 ± 16 | 292 ± 13 | 228 ± 9 | 287 ± 20 | 230 ± 10 | 259 ± 11 |
| (Gps)2 | −10.78 | −2 ± 3 | −24 ± 5 | −33 ± 5 | −24 ± 5 | −11 ± 4 | −18 ± 4 | −16 ± 6 | −19 ± 4 | −15 ± 4 |
| (Gds)0 | 1622.01 | 1654 ± 28 | 1626 ± 45 | 1599 ± 28 | 1647 ± 30 | 1724 ± 25 | 1589 ± 22 | 1641 ± 34 | 1580 ± 23 | 1589 ± 24 |
| (G*)0 | 2420.66 | 2362 (F.D.) | 3030 ± 425 | 1985 ± 76 | 2350 ± 183 | 2432 (F.D.) | 1664 ± 68 | 4913 ± 365 | 1707 ± 72 | 1767 ± 71 |
| (Gds)1 | −39.05 | 44 ± 8 | 24 ± 27 | −11 ± 7 | 16 ± 8 | 6.5 ± 4.2 | −10 (FIX) | 13 ± 8 | −10 ± 5 | −5.5 ± 3.3 |
| (G*)1 | −93.02 | 44 | 430 ± 86 | −11 | 148 ± 83 | 179 ± 45 | −10 | 373 ± 94 | −10 | −5.5 |
| (Gds)2 | 10.42 | 16 ± 3 | 9.1 ± 4.0 | 5.0 ± 3.2 | 12 ± 3 | 17 ± 3 | 8.7 ± 2.1 | 13.5 ± 3.8 | 6.6 ± 2.5 | 8.2 ± 2.7 |
| (G*)2 | 10.42 | 16 | 9 | 5.0 | 12 | 17 | 8.7 | 216 ± 70 | 6.6 | 8.2 |
| H 0 | 187.37 | 102 ± 9 | 120 ± 9 | 140 ± 9 | 136 ± 7 | 139 ± 7 | 144 ± 3 | 122 ± 10 | 119 ± 7 | 144 ± 3 |
| 119.65 | 68 (F.D.) | −117 ± 47 | 106 (F.D.) | −54 ± 21 | 105 (F.D.) | 88 (F.D.) | 43 ± 54 | 84 (FIX) | 51 ± 12 | |
| H 1 | −27.53 | −14 ± 5 | −23 ± 5 | −20 ± 2 | −21 ± 2 | −22 ± 2 | −20 ± 2 | −21 ± 2 | −22 ± 2 | −20 ± 2 |
| −27.53 | −14 | −78 ± 11 | −20 | −48 ± 9 | −5.6 ± 4.0 | −20 | −30 ± 16 | −22 | −20 | |
| H 2 | 2.61 | 1.0 ± 0.8 | −0.7 ± 0.8 | 3.2 ± 1.1 | 1.8 ± 0.9 | 3.0 ± 0.9 | 3 (FIX) | −0.1 ± 1.2 | −0.2 ± 1.0 | 3 (FIX) |
| 2.61 | 1.0 | −0.7 | 3.2 | 1.8 | 3.0 | 3 | 10 ± 6 | −0.2 | 3 | |
| J 0 | 1098.80 | 1328 ± 48 | 981 ± 80 | 1058 ± 47 | 1047 ± 50 | 1076 ± 47 | 1125 ± 39 | 1021 ± 68 | 1118 ± 41 | 1063 ± 42 |
| 1204.32 | 1612 ± 67 | 832 ± 307 | 1362 ± 62 | 583 ± 172 | 1356 (F.D.) | 1702 ± 60 | 784 ± 229 | 1676 ± 70 | 1687 ± 72 | |
| J 1 | −57.21 | 30 ± 9 | 29 ± 41 | 55 ± 9 | 37 ± 13 | 45 ± 10 | 9.3 ± 5.8 | −11 ± 18 | 6.4 ± 5.1 | −10 ± 6 |
| −31.67 | 38 ± 12 | −322 ± 70 | 55 | −319 ± 54 | −46 ± 21 | 9.3 | −308 ± 78 | 6.4 | −10 | |
| J 2 | 6.72 | 20 ± 5 | 4 ± 5 | 59 ± 9 | 7.6 ± 5.6 | 6.7 ± 5.1 | 5.5 ± 3.2 | 5.2 ± 7.0 | 5.1 ± 4.7 | 0.6 ± 4.9 |
| 6.72 | 20 | 4 | 59 | 7.6 | 6.7 | 5.5 | −53 ± 29 | 5.1 | 0.6 | |
| K 0 | 2509.57 | 2485 ± 53 | 2563 ± 76 | 2497 ± 50 | 2451 ± 46 | 2412 ± 35 | 2491 ± 39 | 2336 ± 73 | 2449 ± 41 | 2437 ± 42 |
| 3190.04 | 3506 ± 88 | 2788 ± 213 | 3288 ± 73 | 2839 ± 110 | 3432 (F.D.) | 3489 ± 58 | 2696 ± 190 | 3426 ± 62 | 3525 ± 61 | |
| K 1 | −147.70 | 30 ± 7 | −46 ± 37 | −18 ± 7 | −44 ± 13 | −59 ± 10 | −57 ± 10 | −96 ± 22 | −53 ± 11 | −85 ± 11 |
| − 86.74 | 34 ± 11 | −185 ± 98 | −18 | −138 ± 36 | 39 ± 14 | −57 | −193 ± 75 | −53 | 17 ± 7 | |
| K 2 | 19.15 | 26 ± 4 | 34 ± 5 | 18 ± 5 | 17 ± 5 | 11 ± 4 | 13 ± 4 | 7.6 ± 6.9 | 9.0 ± 4.2 | 9.4 ± 4.3 |
| 22.29 | 26 | −54 ± 11 | 18 | −31 ± 9 | 11 | 13 | −43 ± 19 | 9.0 | 9.4 | |
| (F2)0 | 205.11 | 200 ± 7 | 175 ± 10 | 176 ± 5 | 173 ± 5 | 181 ± 4 | 188 ± 4 | 181 ± 5 | 189 ± 5 | 187 ± 4 |
| 275.06 | 299 ± 4 | 292.5 ± 6 | 289 ± 4 | 288 ± 4 | 299 ± 3 | 299 ± 3 | 289 ± 4 | 301 ± 3 | 301 ± 3 | |
| 345.01 | 398 | 410 | 402 | 403 | 417 | 410 | 397 | 413 | 415 | |
| (F2)1 | −13.65 | 5.9 ± 2.1 | 5.2 ± 4.0 | 5.7 ± 1.9 | 7.3 ± 1.4 | 7.6 ± 1.6 | 1.9 ± 1.0 | 6.4 ± 2.0 | 7.5 ± 1.7 | 3.7 ± 1.1 |
| −7.68 | 4.1 ± 1.5 | 2.9 ± 3.1 | 2.3 ± 1.4 | −2.9 ± 1.3 | 1.7 ± 1.2 | 1.9 | −3.4 ± 2.1 | −0.4 ± 1.1 | 3.7 | |
| −1.71 | 2.3 | 0.6 | −1.1 | −13.1 | −4.2 | 1.9 | −13.2 | −8.3 | 3.7 | |
| 0 | 0 (FIX) | 0 ± 0.4 | 0 (FIX) | −2.1 ± 1.6 | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | |
| (G1)0 | 254.21 | 205 ± 7 | 241 ± 9 | 225 ± 4 | 237 ± 5 | 229 ± 4 | 233 ± 4 | 233 ± 6 | 229 ± 4 | 230 ± 4 |
| 267.65 | 254 ± 5 | 265 ± 7 | 259 ± 3 | 271 ± 4 | 261 ± 4 | 260 ± 3 | 259 ± 4 | 258 ± 3 | 262 ± 3 | |
| 281.09 | 303 | 289 | 293 | 305 | 293 | 287 | 285 | 287 | 294 | |
| (G1)1 | −25.98 | −5 ± 2 | −17 ± 5 | −19 ± 2 | −15 ± 2 | −17 ± 2 | −19 ± 1 | −17 ± 2 | −16 ± 1 | −18 ± 1 |
| −15.07 | −19 ± 2 | −14 ± 2 | −16 ± 2 | −19 ± 1 | −19 | −17 ± 2 | −16 | −18 | ||
| −4.16 | −33 | −15 | −9 | −17 | −21 | −19 | −17 | −16 | −18 | |
| (G1)2 | 7.83 | 0 (FIX) | 2.5 ± 0.6 | 0 (FIX) | 1.8 ± 0.6 | 1.1 ± 0.4 | 0 (FIX) | 0.9 ± 0.3 | 0 (FIX) | 0 (FIX) |
| 3.54 | 0 | 0.6 ± 0.7 | 0 | 1.2 ± 0.5 | 1.1 | 0 | 0 (FIX) | 0 | 0 | |
| −0.75 | 0 | −1.3 | 0 | 0.6 | 1.1 | 0 | 0 | 0 | 0 | |
| (G3)0 | 16.22 | 26 ± 3 | 4.1 ± 5.9 | 10 ± 1 | −2.0 ± 3.2 | 2.5 ± 1.7 | 15 ± 2 | 1.9 ± 3.1 | 13 ± 2 | 14 ± 2 |
| 18.96 | 32 ± 3 | 11 ± 3 | 10 | 11 ± 3 | 2.5 | 23 ± 1 | 11 ± 3 | 24 ± 2 | 24 ± 1 | |
| 21.70 | 38 ± 2 | 18 | 10 | 24 | 2.5 | 31 | 20 | 35 | 34 | |
| (ζd)0 | 356.97 | 360 ± 39 | 337 ± 45 | 331 ± 26 | 352 ± 24 | 339 ± 21 | 322 ± 24 | 354 ± 31 | 326 ± 26 | 332 ± 25 |
| 401.94 | 421 ± 20 | 367 ± 19 | 369 ± 18 | 368 ± 15 | 370 ± 14 | 358 ± 16 | 363 ± 21 | 372 ± 17 | 368 ± 17 | |
| 446.92 | 482 | 397 | 407 | 384 | 401 | 394 | 372 | 418 | 404 | |
| (ζd)1 | 86.24 | 70 ± 12 | 73 ± 26 | 78 ± 10 | 81 ± 8 | 76 ± 8 | 84 ± 8 | 87 ± 11 | 82 ± 9 | 85 ± 9 |
| 92.53 | 79 ± 11 | 96 ± 15 | 89 ± 6 | 90 ± 4 | 89 ± 5 | 87 ± 5 | 90 ± 6 | 91 ± 6 | 90 ± 6 | |
| 98.81 | 88 | 119 | 100 | 99 | 102 | 90 | 93 | 100 | 95 | |
| (ζd)2 | 8.14 | 2.3 ± 1.8 | 2.2 ± 3.1 | 2.7 ± 1.6 | 6.9 ± 2.9 | 2.8 ± 1.9 | 3.7 ± 1.4 | 8.5 ± 4.0 | 4.8 ± 2.4 | 4.9 ± 2.4 |
| 8.14 | 2.3 | 3.3 ± 2.3 | 2.7 | 2.3 ± 2.3 | 2.8 | 3.7 | 2.5 ± 3.0 | 4.8 | 4.9 | |
| 8.14 | 2.3 | 4.4 | 2.7 | −2.3 | 2.8 | 3.7 | −3.5 | 4.8 | 4.9 | |
| (ζp)0 | 89.03 | 190 ± 61 | 127 ± 68 | 129 ± 49 | 123 ± 39 | 103 ± 38 | 142 ± 38 | 123 ± 51 | 137 ± 40 | 125 ± 41 |
| 199.19 | 252 ± 39 | 281 ± 39 | 284 ± 38 | 273 ± 29 | 279 ± 30 | 298 ± 30 | 280 ± 38 | 298 ± 32 | 305 ± 32 | |
| 309.34 | 314 | 435 | 439 | 423 | 455 | 454 | 437 | 459 | 485 | |
| (ζp)1 | 8.67 | 31 ± 11 | 37 ± 35 | 19 ± 10 | 20 ± 14 | 16 ± 9 | 11 ± 8 | 18 ± 16 | 9.5 ± 7.1 | 10 ± 7 |
| 24.32 | 31 | 21 ± 20 | 23 ± 9 | 24 ± 11 | 23 ± 10 | 11 | 22 ± 14 | 19 ± 8 | 10 | |
| 39.97 | 31 | 5 | 27 | 28 | 30 | 11 | 26 | 29 | 10 | |
| (ζp)2 | 0 | 0 (FÍX) | 8.3 ± 4.3 | 5.0 ± 4.0 | 5.0 ± 4.3 | 3.2 ± 2.8 | 6.2 ± 2.7 | 7.2 ± 5.6 | 4.0 ± 2.6 | 4.6 ± 2.5 |
| 0 | 0 | 3.9 ± 3.2 | 5.0 | 2.4 ± 3.2 | 3.2 | 6.2 | 4.0 ± 4.2 | 4.0 | 4.6 | |
| 0 | 0 | 0 | 5.0 | −0.2 | 3.2 | 6.2 | 0.8 | 4.0 | 4.6 | |
| α 0 | 60 | 47 ± 5 | 42 ± 10 | 39 ± 3 | 45 ± 6 | 42 ± 3 | 36 ± 3 | 40 ± 7 | 37 ± 3 | 37 ± 3 |
| 60 | 47 | 48 ± 6 | 39 | 39 ± 3 | 42 | 36 | 35 ± 4 | 37 | 37 | |
| 60 | 47 | 54 | 39 | 33 | 42 | 36 | 30 | 37 | 37 | |
| α 1 | 0 | 7.6 ± 1.2 | 8.5 ± 2.0 | 1.3 ± 1.1 | 2.0 ± 1.9 | 1.2 ± 1.1 | 1.7 ± 1.1 | 4.4 ± 2.5 | 2.8 ± 1.0 | 1.1 ± 1.2 |
| 0 | 7.6 | 5.8 ± 1.7 | 1.3 | 1.1 ± 1.6 | 1.2 | 1.7 | 1.4 ± 2.2 | 2.8 | 1.1 | |
| 0 | 7.6 | 3.1 | 1.3 | 0.2 | 1.2 | 1.7 | −1.6 | 2.8 | 1.1 | |
| β 0 | 0 | −253 ± 41 | −247 ± 196 | −381 ± 66 | −299 ± 100 | −321 ± 52 | −476 ± 48 | −280 ± 115 | −476 ± 51 | −460 ± 50 |
| 0 | −253 | −301 ± 138 | −381 | −365 ± 57 | −321 | −476 | −507 ± 73 | −476 | −460 | |
| 0 | −253 | −355 | −381 | −431 | −321 | −476 | −734 | −476 | −460 | |
| 0 | 0 (FIX) | −28 ± 39 | −122 ± 43 | −121 ± 38 | −115 ± 34 | −42 ± 22 | −24 ± 39 | −21 ± 16 | −53 ± 19 | |
| T 0 | 0 | −2.9 ± 0.6 | −22 ± 0.9 | −3.1 ± 0.3 | −2.3 ± 0.5 | −2.7 ± 0.4 | −3.3 ± 0.3 | −3.2 ± 0.7 | −3.2 ± 0.3 | −3.3 ± 0.3 |
| 0 | −2.9 | −1.7 ± 0.6 | −3.1 | −3.4 ± 0.3 | −3.2 ± 0.3 | −3.3 | −3.5 ± 0.4 | −3.2 | −3.3 | |
| 0 | −2.9 | −1.2 | −3.1 | −4.5 | −3.7 | −3.3 | −3.8 | −3.2 | −3.3 | |
| 0 | 0.4 ± 0.2 | 0.3 ± 0.2 | −0.4 ± 0.2 | −0.3 ± 0.2 | −0.3 ± 0.2 | −0.4 ± 0.2 | −0.2 ± 0.2 | −0.3 ± 0.2 | −0.4 ± 0.2 | |
| (T2)0 | 0 | −3.1 ± 0.9 | −4.7 ± 1.2 | −2.6 ± 0.6 | −3.1 ± 0.8 | −2.4 ± 0.5 | −2.8 ± 0.6 | −3.5 ± 1.0 | −2.6 ± 0.6 | −2.7 ± 0.6 |
| 0 | −3.1 | −3.2 ± 0.9 | −2.6 | −2.1 ± 0.6 | −2.4 | −2.8 | −1.9 ± 0.7 | −2.6 | −2.7 | |
| 0 | −3.1 | −1.7 | −2.6 | −1.1 | −2.4 | −2.8 | −0.3 | −2.6 | −2.7 | |
| 0 | −0.3 ± 0.2 | −0.3 ± 0.2 | −0.3 ± 0.2 | −0.3 ± 0.2 | −0.3 ± 0.2 | 0 (FIX) | 0.1 ± 0.3 | 0.1 ± 0.3 | 0 (FIX) | |
| (F1)0 | 0 | −12 ± 4 | −40 ± 11 | −35 ± 5 | −38 ± 9 | −18 ± 5 | −6.2 ± 4.1 | −28 ± 8 | −8.1 ± 3.7 | −7.0 ± 3.8 |
| 0 | −12 | −18 ± 3 | −35 | −33 ± 8 | −18 | −6.2 | −27 ± 9 | −8.1 | −7.0 | |
| 0 | −12 | 4 | −35 | −28 | −18 | −6.2 | −26 | −8.1 | −7.0 | |
| (F1)1 | 0 | 0 (FIX) | 2.8 ± 3.8 | 2.6 ± 1.9 | 7.8 ± 4.2 | 3.1 ± 2.3 | 2 (FIX) | −1.6 ± 2.8 | −5.0 ± 1.6 | −3.9 ± 2.0 |
| 0 | 0 | −7.6 ± 2.6 | 2.6 | −9.1 ± 2.8 | 3.1 | 2 | −12 ± 4 | −5.0 | −3.9 | |
| 0 | 0 | −18 | 2.6 | −26 | 3.1 | 2 | −22 | −5.0 | −3.9 | |
| (G2)0 | 0 | 21 ± 5 | −4.2 ± 10 | −6.6 ± 5.1 | −7.4 ± 5.3 | 2.8 ± 4.0 | 13 ± 3 | −5.4 ± 6.9 | 3.2 ± 3.0 | 5.9 ± 3.1 |
| 0 | 21 | 29 ± 9 | −6.6 | 25.2 ± 4.8 | 23 ± 4 | 13 | 19 ± 6 | 3.2 | 5.9 | |
| 0 | 21 | 62 | −6.6 | 57.8 | 43 | 13 | 43 | 2.3 | 5.9 | |
| (G2)1 | 0 | 4.7 ± 1.2 | −0.2 ± 2.1 | 0.8 ± 1.1 | 4.3 ± 2.2 | 2.0 ± 1.6 | 0 (FIX) | −0.4 ± 1.7 | 1.3 ± 1.1 | 0 (FIX) |
| 0 | 4.7 | 6.0 ± 2.0 | 0.8 | −0.1 ± 2.2 | 2.0 | 0 | −1.9 ± 1.8 | 1.3 | 0 | |
| 0 | 4.7 | 12 | 0.8 | −4.5 | 2.0 | 0 | −3.4 | 1.3 | 0 | |
| M 0 | 13020 | 13030 ± 159 | 13049 ± 170 | 13051 ± 180 | 13048 ± 179 | 13037 ± 161 | 13073 ± 126 | 13065 ± 172 | 13060 ± 131 | 13061 ± 131 |
| M 1 | 35800 | 37641 ± 96 | 37643 ± 119 | 37840 ± 98 | 37580 ± 127 | 37600 ± 89 | 37651 ± 88 | 37700 ± 174 | 37682 ± 94 | 37655 ± 95 |
| M 2 | 35070 | 35281 ± 86 | 35278 ± 109 | 35332 ± 86 | 35252 ± 120 | 35298 ± 80 | 35333 ± 83 | 35304 ± 96 | 35339 ± 87 | 35344 ± 86 |
| M 3 | 38690 | 38515 ± 84 | 38486 ± 108 | 38552 ± 84 | 38504 ± 116 | 38571 ± 80 | 38521 ± 82 | 38467 ± 96 | 38514 ± 84 | 38545 ± 85 |
| M 4 | 43540 | 43757 ± 88 | 43807 ± 102 | 43798 ± 82 | 43796 ± 110 | 43863 ± 80 | 43724 ± 83 | 43721 ± 98 | 43722 ± 87 | 43748 ± 86 |
| M 5 | 59160 | 58916 ± 83 | 59013 ± 90 | 58888 ± 79 | 58911 ± 100 | 58978 ± 77 | 58794 ± 78 | 58878 ± 96 | 58798 ± 86 | 58820 ± 84 |
| M 6 | 70910 | 67536 ± 78 | 67669 ± 77 | 67465 ± 72 | 67504 ± 87 | 67551 ± 71 | 67382 ± 70 | 67607 ± 92 | 67390 ± 75 | 67400 ± 68 |
| M 7 | 51750 | 51974 ± 67 | 52177 ± 61 | 51869 ± 74 | 51934 ± 69 | 51930 ± 60 | 51779 ± 58 | 51936 ± 79 | 51792 ± 67 | 51786 ± 65 |
| M 8 | 42130 | 42285 ± 51 | 42548 ± 42 | 42158 ± 54 | 42230 ± 47 | 42183 ± 43 | 42071 ± 47 | 42481 ± 69 | 42085 ± 48 | 42065 ± 49 |
| M 9 | 31370 | 31914 ± 73 | 32269 ± 103 | 31784 ± 88 | 31865 ± 113 | 31766 ± 67 | 31639 ± 71 | 31970 ± 102 | 31642 ± 74 | 31618 ± 75 |
| M 10 | 30700 | 32238 ± 75 | 32681 ± 65 | 32118 ± 84 | 32189 ± 71 | 32039 ± 68 | 31857 ± 70 | 32227 ± 91 | 31846 ± 78 | 31812 ± 77 |
| 94502 | 92090 ± 183 | 91674 ± 310 | 92033 ± 191 | 92430 ± 239 | 91861 ± 164 | 92261 ± 120 | 92580 ± 118 | 92142 ± 128 | 92166 ± 127 | |
| 551 | 570 ± 160 | 527 ± 173 | 597 ± 180 | 561 ± 181 | 594 ± 162 | 583 ± 108 | 566 ± 171 | 598 ± 116 | 591 ± 119 | |
| Δ | 205.0 | 193.9 | 200.3 | 188.2 | 203.1 | 196.7 | 187.8 | 198.1 | 194.5 |
The above form of accounting for linearity with a quadratic correction, was chosen in order to make the parameters as nearly orthogonal as possible.
Since the parameter M(dnp) incorporates setting the value of the lowest energy level to zero, it is not expected to behave regularly as a function of n. Consequently, when M, M′, and M″ were replaced with
the latter were compelled to satisfy the relation (39).
4. Results
The source of the experimental data for all the elements with the exception of manganese is “Atomic Energy Levels”, Vols. I and II by C.E. Moore, referred to as AEL, [35]. For manganese, the experimental results of Catalan, Meggers and Garcia-Riquelme, [36] were used. Details indicating the levels included, as well as those that were rejected, are provided in another paper, [17]. On fitting 1537 levels using 67 free interaction parameters a mean error of 182cm−1 was obtained. Altogether 3652 energy levels were calculated including all the levels for the configurations 3dn−24s24p across the sequence.
Tables 1–412 yield the results for each of the parameters individually, whereas tables 42 and 43 give the results of the general interpolation formulas, together with the centers of gravity M(dnp), (0 ⩽ n ⩽ 10), M11(d9s2p) and M12(d10s2p), for the various significant stages of this project.
Table 1.
Results for the parameter D′
| EL. | Previous results | DIACON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | Final GLS |
|---|---|---|---|---|---|---|
| Ca | −18902 | −17851.26 | −19140 | −19497 | −19247 | −19252 |
| Sc | −14492 | −13958.87 | −14420 | −14681 | −14506 | −14525 |
| Ti | −10511 | −10066.48 | −9940 | −10119 | −9999 | −10026 |
| V | −5504 | −6174.09 | −5700 | −5811 | −5726 | −5755 |
| Cr | −2275 | −2281.70 | −1700 | −1757 | −1687 | −1712 |
| Mn | 1554 | 1610.69 | 2060 | 2043 | 2118 | 2103 |
| Fe | 6185 | 5503.08 | 5580 | 5589 | 5689 | 5690 |
| Co | 8939 | 9395.47 | 8860 | 8881 | 9026 | 9049 |
| Ni | 12367 | 13287.85 | 11900 | 11919 | 12129 | 12180 |
| Cu | 17180.24 | 14700 | 14703 | 14998 | 15083 |
Table 41.
Results for the mean error Δ in the ILS.
| EL. | Previous results | ILS 3 | FINAL ILS |
|---|---|---|---|
| Ca | 22.8 | 52.7 | 45.6 |
| Sc | 126.4 | 112.3 | 108.7 |
| Ti | 261.4 | 129.8 | 124.0 |
| V | 215.8 | 164.2 | 161.1 |
| Cr | 183.1 | 137.6 | 132.4 |
| Mn | 169.9 | 161.2 | 157.6 |
| Fe | 213.4 | 159.2 | 152.8 |
| Co | 164.2 | 146.3 | 140.2 |
| Ni | 131.1 | 112.5 | 106.3 |
| Cu | 12a | 89.2b | 82.8b |
Based on 18 levels.
Based on 23 levels.
Table 43.
General Interpolation Parameters Final Iteration
| PAR. | GLS 4 | GLS 4a | GLS 4b | GLS 4c | GLS 4d | GLS 4e | GLS 4f | GLS 4g | GLS 4h | GLS 4i |
|---|---|---|---|---|---|---|---|---|---|---|
| 963 ± 31 | 612 ± 105 | 920 ± 36 | 895 ± 38 | 929 ± 36 | 965 ± 32 | 968 ± 33 | 1007 ± 34 | 1039 ± 35 | 1041 ± ;37 | |
| 28770 ± 72 | 28599 ± 98 | 28689 ± 82 | 28745 ± 81 | 28683 ± 74 | 2873 ± 77 | 28739 ± 78 | 28784 ± 77 | 28704 ± 79 | 28703 ± 83 | |
| 3701 ± 15 | 3592 ± 46 | 3691 ± 17 | 3690 ± 17 | 3699 ± 17 | 3706 ± 17 | 3706 ± 16 | 3723 ± 17 | 3720 ± 19 | 3724 ± 19 | |
| 5784 ± 32 | 5818 ± 58 | 5736 ± 35 | 5754 ± 32 | 5748 ± 31 | 5791 ± 33 | 5794 ± 32 | 5814 ± 31 | 5813 ± 33 | 5822 ± 35 | |
| −114 ± 4 | −126 ± 10 | −116 ± 5 | −114 ± 5 | −116 ± 5 | −115 ± 5 | −117 ± 5 | ± 120 ± 5 | −120 ± 6 | −121 ± 6 | |
| −114 | −100 ± 15 | −116 | −114 | −116 | −115 | −117 | −120 | −120 | −121 | |
| B 0 | 714 ± 4 | 727 ± 7 | 714 ± 5 | 716 ± 5 | 714 ± 5 | 712 ± 5 | 700 ± 4 | 705 ± 4 | 714 ± 4 | 712 ± 4 |
| 844 ± 3 | 839 ± 4 | 842 ± 3 | 841 ± 3 | 842 ± 3 | 844 ± 3 | 839 ± 3 | 843 ± 3 | 855 ± 3 | 855 ± 3 | |
| 974 | 951 | 970 | 966 | 970 | 976 | 978 | 981 | 996 | 998 | |
| B 1 | 51 ± 2 | 57 ± 3 | 51 ± 2 | 51 ± 2 | 51 ± 2 | 51 ± 2 | 45 ± 2 | 51 ± 2 | 52 ± 2 | 52 ± 2 |
| 60 ± l | 57 ± 2 | 60 ± 2 | 58 ± 2 | 59 ± 2 | 61 ± 2 | 55 ± 2 | 63 ± 1 | 63 ± 1 | 63 ± 1 | |
| 69 | 57 | 69 | 65 | 67 | 71 | 65 | 75 | 74 | 74 | |
| C 0 | 3013 ± 19 | 2938 ± 46 | 3005 ± 27 | 3010 ± 26 | 3005 ± 22 | 3016 ± 22 | 3099 ± 20 | 2916 ± 15 | 2839 ± 15 | 2843 ± 13 |
| 3362 ± 16 | 3376 ± 26 | 3359 ± 23 | 3364 ± 23 | 3359 ± 21 | 3361 ± 18 | 3433 ± 17 | 3267 ± 12 | 3190 ± 10 | 3191 ± 9 | |
| 3711 | 3814 | 3713 | 3718 | 3713 | 3706 | 3767 | 3618 | 3541 | 3539 | |
| C 1 | 433 ± 7 | 426 ± 15 | 441 ± 11 | 448 ± 11 | 440 ± 8 | 437 ± 8 | 450 ± 8 | 413 ± 7 | 412 ± 7 | 414 ± 8 |
| 348 ± 7 | 362 ± 13 | 358 ± 10 | 362 ± 10 | 358 ± 8 | 350 ± 8 | 362 ± 8 | 322 ± 7 | 319 ± 6 | 320 ± 6 | |
| 263 | 298 | 275 | 276 | 276 | 263 | 274 | 231 | 226 | 226 | |
| (F2)0 | 183 ± 3 | 190 ± 5 | 187 ± 4 | 186 ± 4 | 186 ± 4 | 180 ± 4 | 179 ± 4 | 180 ± 4 | 181 ± 5 | 178 ± 4 |
| 299 ± 3 | 293 ± 4 | 298 ± 3 | 290 ± 3 | 298 ± 3 | 299 ± 3 | 298 ± 3 | 298 ± 3 | 297 ± 4 | 297 ± 3 | |
| 415 | 396 | 410 | 394 | 410 | 418 | 417 | 416 | 413 | 416 | |
| (F2)1 | 2.5 ± 1.1 | 7.7 ± 1.8 | 2.5 ± 1 | 2.0 ± 1.0 | 2.1 ± 1.1 | 2.3 ± 1.1 | 2.2 ± 1.1 | 2.3 ± 1.1 | 2.5 ± 1.2 | 2.4 ± 1.2 |
| 2.5 | −2.2 ± 2.0 | 2.5 | 2.0 | 2.1 | 2.3 | 22 | 2.3 | 2.5 | 2.4 | |
| 2.5 | −12.1 | 2.5 | 2.0 | 2.1 | 2.3 | 2.2 | 2.3 | 2.5 | 2.4 | |
| 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | |
| (G1)0 | 235 ± 3 | 236 ± 5 | 233 ± 4 | 237 ± 4 | 234 ± 4 | 228 ± 4 | 229 ± 4 | 230 ± 4 | 237 ± 4 | 231 ± 4 |
| 261 ± 3 | 260 ± 4 | 251 ± 3 | 259 ± 3 | 261 ± 3 | 256 ± 3 | 256 ± 3 | 256 ± 3 | 260 ± 3 | 256 ± 3 | |
| 287 | 284 | 269 | 281 | 288 | 284 | 283 | 282 | 283 | 281 | |
| (G1)1 | −19 ± 1 | −17 ± 2 | −19 ± 1 | −18 ± 1 | −17 ± 1 | −19 ± 1 | −18 ± 1 | −18 ± 1 | −19 ± 1 | −19 ± 1 |
| −19 | −18 ± 2 | −19 | −18 | −17 | −19 | −18 | −18 | −19 | −19 | |
| −19 | −19 | −19 | −18 | −17 | −19 | −18 | −18 | −19 | −19 | |
| (G1)2 | 0 (FIX) | 0.7 ± 0.3 | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) |
| 0 | 0.7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| 0 | 0.7 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| (G3)0 | 13 ± 1 | 4.6 ± 2.8 | 14 ± 2 | 14 ± 1 | 14 ± 1 | 13 ± 1 | 13 ± 1 | 13 ± 1 | 14 ± 2 | 14 ± 1 |
| 21 ± 1 | 11.1 ± 2.6 | 22 ± 1 | 19 ± 2 | 22 ± 1 | 22 ± 1 | 22 ± 1 | 22 ± 1 | 20 ± 2 | 21 ± 1 | |
| 29 | 17.6 | 30 | 24 | 30 | 31 | 31 | 31 | 26 | 28 | |
| (G3)1 | 0 (FIX) | −0.5 ± 1.0 | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) |
| 0 | −3.5 ± 1.1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| 0 | −6.5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| (G3)2 | 0 (FIX) | −1.1 ± 0.2 | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) |
| 0 | −1.1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| 0 | −1.1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| (Gps)0 | 6454 ± 20 | 6601 ± 49 | 6447 ± 34 | 6555 ± 37 | 6445 ± 23 | 6446 ± 23 | 6463 ± 22 | 6462 ± 23 | 6458 ± 24 | 6469 ± 26 |
| (Gps)1 | 220 ± 10 | 257 ± 18 | 222 ± 10 | 280 ± 13 | 221 ± 10 | 222 ± 10 | 221 ± 10 | 219 ± 11 | 217 ± 11 | 219 ± l1 |
| (Gps)2 | −15 ± 3 | −4.6 ± 5.6 | −14 ± 4 | −10 ± 4 | −15 ± 4 | −17 ± 4 | −17 ± 4 | −19 ± 4 | −14 ± 4 | −16 ± 4 |
| (Gds)0 | 1595 ± 14 | 1660 ± 30 | 1593 ± 26 | 1587 ± 25 | 1592 ± 15 | 1579 ± 17 | 1583 ± 15 | 1584 ± 15 | 1616 ± 16 | 1601 ± 18 |
| (G*)0 | 1826 (F.D.) | 3107 ± 801 | 1649 ± 83 | 1674 ± 81 | 1829 (F.D.) | 1810 (F.D.) | 1814 (F.D.) | 1815 (F.D.) | 1847 (F.D.) | 1832 (F.D.) |
| (Gds)1 | 0 (FIX) | 14 ± 9 | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) |
| (G*)1 | 0 | 544 ± 241 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 |
| (Gds)2 | 8.7 ± 1.2 | 15 ± 3 | 8.1 ± 2,9 | 6.8 ± 2.6 | 8.1 ± 1.9 | 9.0 ± 1.7 | 9.0 ± 1.6 | 8.7 ± 1.8 | 9.0 ± 1.7 | 9.2 ± 1.8 |
| (G*)2 | 8.7 | 82 ± 62 | 8.1 | 6.8 | 8.1 | 9.0 | 9.0 | 8.7 | 9.0 | 9.2 |
| H 0 | 123 ± 2 | 114 ± 8 | 123 ± 3 | 124 ± 3 | 123 ± 2 | 124 ± 3 | 124 ± 3 | 122 ± 3 | 123 ± 3 | 124 ± 3 |
| 84 (FIX) | 88 ± 47 | 84 (FIX) | 42 ± 15 | 84 (FIX) | 84 (FIX) | 84 (FIX) | 84 (FIX) | 84 (FIX) | 84 (FIX) | |
| H 1 | −23 ± 1 | −24 ± 2 | −22 ± 1 | −23 ± 1 | −22 ± 1 | −23 ± 1 | − 24 ± 1 | −24 ± 1 | −24 ± 1 | −24 ± 2 |
| −23 | − 11 ± 14 | −22 | −23 | −22 | −23 | −24 | −24 | −24 | −24 | |
| H 2 | 0 (FIX) | −1.3 ± 1.1 | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) |
| 0 | 9.0 ± 5.0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| J 0 | 1122 ± 21 | 1090 ± 61 | 1134 ± 47 | 1039 ± 41 | 1123 ± 25 | 1126 ± 25 | 1127 ± 24 | 1118 ± 23 | 1126 ± 24 | 1129 ± 26 |
| 1652 ± 38 | 598 ± 271 | 1693 ± 70 | 975 ± 74 | 1666 ± 39 | 1695 ± 36 | 1708 ± 37 | 1685 ± 40 | 1645 ± 42 | 1689 ± 43 | |
| J 1 | 26 ± 3 | −15 ± 17 | 14 ± 9 | −2.8 ± 1.9 | 19 ± 6 | 11 ± 6 | 15 ± 5 | −1.8 ± 5.2 | 7.0 ± 5.3 | 6.7 ± 5.2 |
| 26 | −376 ± 127 | 14 | −231 ± 37 | 19 | 11 | 15 | −1.8 | 7.0 | 6.7 | |
| J 2 | 8.4 ± 2.1 | 8.2 ± 6.2 | 7.2 ± 5 | −1.4 ± 3.1 | 6.1 ± 3.0 | 6.9 ± 3.2 | 7.5 ± 3.1 | 5.0 ± 3.2 | 8.1 ± 3.1 | 6.6 ± 4.2 |
| 8.4 | −32 ± 27 | 7.2 | −1.4 | 6.1 | 6.9 | 7.5 | 5.0 | 8.1 | 6.6 | |
| K 0 | 2474 ± 29 | 2404 ± 66 | 2508 ± 36 | 2468 ± 40 | 2485 ± 28 | 2468 ± 29 | 2467 ± 28 | 2445 ± 29 | 2476 ± 30 | 2470 ± 31 |
| 3421 ± 38 | 2984 ± 209 | 3446 ± 46 | 3182 ± 51 | 3426 ± 34 | 3463 ± 38 | 3467 ± 39 | 3435 ± 37 | 3426 ± 39 | 3467 ± 41 | |
| K 1 | −62 ± 6 | −93 ± 20 | −54 ± 13 | −76 ± 13 | −60 ± 7 | −61 ± 8 | −61 ± 7 | −67 ± 7 | −63 ± 8 | −62 ± 9 |
| −62 | −167 ± 70 | −54 | −76 | −60 | −61 | −61 | −67 | −63 | −62 | |
| K 2 | 15 ± 3 | 12 ± 6 | 17 ± 5 | 14 ± 5 | 14 ± 3 | 12 ± 4 | 13 ± 4 | 7.9 ± 4.1 | 15 ± 5 | 12 ± 5 |
| 15 | −5.6 ± 19 | 17 | 14 | 14 | 12 | 13 | 7.9 | 15 | 12 | |
| (ζd)0 | 310 ± 19 | 343 ± 28 | 319 ± 25 | 327 ± 24 | 323 ± 18 | 311 ± 17 | 308 ± 18 | 315 ± 19 | 314 ± 20 | 315 ± 21 |
| 364 ± 16 | 360 ± 19 | 355 ± 17 | 367 ± 17 | 359 ± 14 | 365 ± 15 | 367 ± 16 | 365 ± 17 | 366 ± 16 | 366 ± 19 | |
| 418 | 377 | 391 | 407 | 395 | 419 | 426 | 415 | 418 | 417 | |
| (ζd)1 | 78 ± 5 | 82 ± 10 | 82 ± 9 | 84 ± 9 | 82 ± 6 | 77 ± 7 | 77 ± 8 | 78 ± 8 | 77 ± 9 | 76 ± 10 |
| 91 ± 4 | 90 ± 5 | 87 ± 6 | 89 ± 5 | 87 ± 5 | 90 ± 6 | 91 ± 6 | 92 ± 6 | 92 ± 6 | 91 ± 6 | |
| 104 | 98 | 92 | 94 | 92 | 103 | 105 | 106 | 107 | 106 | |
| (ζd)2 | 2.6 ± 1.2 | 5.5 ± 3.5 | 1.9 ± 1.6 | 3.2 ± 2.1 | 2.4 ± 1.5 | 2.5 ± 1.8 | 2.3 ± 1.7 | 3.0 ± 1.5 | 2.8 ± 1.6 | 2.7 ± 1.4 |
| 2.6 | 1.8 ± 2.8 | 1.9 | 3.2 | 2.4 | 2.5 | 2.3 | 3.0 | 2.8 | 2.7 | |
| 2.6 | −1.9 | 1.9 | 3.2 | 2.4 | 2.5 | 2.3 | 3.0 | 2.8 | 2.7 | |
| (ζp)0 | 143 ± 26 | 139 ± 46 | 149 ± 43 | 135 ± 42 | 150 ± 26 | 137 ± 28 | 140 ± 25 | 135 ± 27 | 130 ± 29 | 123 ± 30 |
| 284 ± 19 | 278 ± 34 | 290 ± 34 | 279 ± 33 | 290 ± 19 | 269 ± 24 | 269 ± 21 | 269 ± 22 | 279 ± 25 | 164 ± 27 | |
| 425 | 417 | 431 | 423 | 430 | 401 | 398 | 403 | 428 | 405 | |
| (ζp)1 | 13 ± 5 | 17 ± 17 | 15 ± 8 | 13 ± 8 | 18 ± 6 | 14 ± 6 | 15 ± 5 | 16 ± 6 | 15 ± 7 | 16 ± 7 |
| 13 | 19 ± 13 | 15 | 13 | 18 | 14 | 15 | 16 | 15 | 16 | |
| 13 | 21 | 15 | 13 | 18 | 14 | 15 | 16 | 15 | 16 | |
| (ζp)2 | 5.2 ± 1.7 | 5.4 ± 5.0 | 5.6 ± 3.2 | 5.3 ± 3.0 | 5.6 ± 1.9 | 5.3 ± 2.1 | 5.5 ± 2.0 | 5.4 + 1.9 | 5.4 ± 2.0 | 5.5 ± 2.1 |
| 5.2 | 3.6 ± 3.8 | 5.6 | 5.3 | 5.6 | 5.3 | 5.5 | 5.4 | 5.4 | 5.5 | |
| 5.2 | 1.8 | 5.6 | 5.3 | 5.6 | 5.3 | 5.5 | 5.4 | 5.4 | 5.5 | |
| α 0 | 33 ± 2 | 42 ± 6 | 34 ± 3 | 33 ± 3 | 34 ± 3 | 34 ± 3 | 30 ± 3 | 61 ± 2 | 71 ± 1 | 72 ± 1 |
| 33 | 32 ± 3 | 34 | 33 | 34 | 34 | 30 | 61 | 71 | 72 | |
| 33 | 22 | 34 | 33 | 34 | 34 | 30 | 61 | 71 | 72 | |
| α 1 | 3.7 ± 0.9 | 3.0 ± 2.3 | 1.6 ± 1.2 | 0.7 ± 1.1 | 1.5 ± 1.2 | 3.1 ± 1.1 | 2.9 ± 1.2 | 6.8 ± 1.1 | 7.1 ± 0.8 | 6.9 ± 0.7 |
| 3.7 | 0.8 ± 2.0 | 1.6 | 0.7 | 1.5 | 3.1 | 2.9 | 6.8 | 7.1 | 6.9 | |
| 3.7 | −1.4 | 1.6 | 0.7 | 1.5 | 3.1 | 2.9 | 6.8 | 7.1 | 6.9 | |
| β 0 | −527 ± 28 | −380 ± 102 | −523 ± 37 | −534 ± 38 | −526 ± 31 | −521 ± 30 | −673 ± 31 | −336 ± 32 | 0 (FIX) | 0(FIX) |
| −527 | −549 ± 65 | −523 | −534 | −526 | −521 | −673 | −336 | 0 | 0 | |
| −527 | −718 | −523 | −534 | −526 | −521 | −673 | −336 | 0 | 0 | |
| −23 ± 11 | −59 ± 44 | −65 ± 29 | −89 ± 31 | −40 ± 13 | −22 ± 12 | −51 ± 18 | −7.2 ± 8.1 | 0 (FIX) | 0 (FIX) | |
| T 0 | −3.5 ± 0.3 | −2.6 ± 0.7 | −3.4 ± 0.3 | −3.5 ± 0.3 | −3.4 ± 0.3 | −3.5 ± 0.3 | −3.8 ± 0.3 | 0 (FIX) | 0 (FIX) | 0 (FIX) |
| −3.5 | −3.7 ± 0.4 | −3.4 | −3.5 | −3.4 | −3.5 | −3.8 | 0 | 0 | 0 | |
| −3.5 | −4.8 | −3.4 | −3.5 | −3.4 | −3.5 | −3.8 | 0 | 0 | 0 | |
| −0.2 ± 0.1 | −0.3 ± 0.2 | −0.4 ± 0.2 | −0.4 ± 0.2 | −0.4 ± 0.2 | −0.3 ± 0.2 | −0.3 ± 0.2 | 0 (FIX) | 0 (FIX) | 0 (FIX) | |
| (T2)0 | −2.6 ± 0.6 | −3.1 ± 0.9 | −2.6 ± 0.6 | −2.5 ± 0.5 | −2.6 ± 0.5 | −2.7 ± 0.6 | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) |
| −2.6 | −2.0 ± 0.6 | −2.6 | −2.5 | −2.6 | −2.7 | 0 | 0 | 0 | 0 | |
| −2.6 | −0.9 | −2.6 | −2.5 | −2.6 | −2.7 | 0 | 0 | 0 | 0 | |
| 0 (FIX) | 0.1 ± 0.3 | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0(FIX) | 0(FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | |
| (F1)0 | −13 ± 3 | −14 ± 9 | −8.6 ± 4.1 | −21 ± 5 | −11 ± 4 | 0 (FIX) | 0 (FIX) | 0 (FIX) | −13 ± 5 | 0 (FIX) |
| −13 | −26 ± 9 | −8.6 | −21 | −11 | 0 | 0 | 0 | −13 | 0 | |
| −13 | −38 | −8.6 | −21 | −11 | 0 | 0 | 0 | −13 | 0 | |
| (F1)1 | 0 (FIX) | −1.9 ± 4.3 | 0 (FIX) | −4.0 ± 2.1 | 0 (FIX) | 0 (FIX) | 0(FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) |
| 0 | −11 ± 4 | 0 | −4.0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| 0 | −20 | 0 | −4.0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| (G2)0 | 9 ± 3 | 4.2 ± 4.0 | 12 ± 3 | 10 ± 3 | 12 ± 3 | 0 (FIX) | 0 (FIX) | 0 (FIX) | 9 ± 4 | 0 (FIX) |
| 9 | 19 ± 4 | 12 | 10 | 12 | 0 | 0 | 0 | 9 | 0 | |
| 9 | 34 | 12 | 10 | 12 | 0 | 0 | 0 | 9 | 0 | |
| (G2)1 | 0 (FIX) | 0.6 ± 2.4 | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0 (FIX) | 0(FIX) | 0(FIX) |
| 0 | −2.0 ± 2.9 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| 0 | −4.6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | |
| M 0 | 13065 ± 99 | 13057 ± 156 | 13066 ± 113 | 13062 ± 109 | 13060 ± 101 | 13062 ± 103 | 13061 ± 101 | 13060 ± 102 | 13059 ± 107 | 13057 ± 106 |
| M 1 | 37650 ± 69 | 37629 ± 161 | 37646 ± 79 | 37644 ± 80 | 31647 ± 66 | 37652 ± 68 | 37658 ± 66 | 37681 ± 68 | 37678 ± 71 | 37681 ± 72 |
| M 2 | 35331 ± 72 | 35300 ± 151 | 35337 ± 81 | 35332 ± 76 | 35339 ± 71 | 35332 ± 72 | 35343 ± 71 | 35356 ± 73 | 35365 ± 76 | 39230 ± 75 |
| M 3 | 38522 ± 70 | 38524 ± 136 | 38533 ± 80 | 38539 ± 79 | 38533 ± 69 | 38524 ± 68 | 38544 ± 69 | 38538 ± 70 | 38566 ± 73 | 38569 ± 74 |
| M 4 | 43725 ± 71 | 43773 ± 105 | 43738 ± 80 | 43750 ± 76 | 43732 ± 70 | 43722 ± 72 | 43742 ± 71 | 43719 ± 73 | 43771 ± 75 | 43770 ± 76 |
| M 5 | 58792 ± 59 | 58887 ± 126 | 58808 ± 75 | 58819 ± 72 | 58798 ± 58 | 58789 ± 64 | 58786 ± 63 | 58764 ± 62 | 58837 ± 63 | 58836 ± 63 |
| M 6 | 67352 ± 54 | 67506 ± 98 | 67367 ± 69 | 67364 ± 68 | 67355 ± 56 | 67347 ± 57 | 67330 ± 56 | 67302 ± 57 | 67379 ± 56 | 67374 ± 55 |
| M 7 | 51757 ± 49 | 52013 ± 91 | 51772 ± 67 | 51761 ± 61 | 51756 ± 51 | 51754 ± 52 | 51720 ± 51 | 51701 ± 52 | 51789 ± 52 | 51783 ± 53 |
| M 8 | 42032 ± 47 | 42398 ± 88 | 42063 ± 50 | 42042 ± 48 | 42042 ± 42 | 42027 ± 48 | 41994 ± 49 | 41961 ± 47 | 42016 ± 48 | 42008 ± 48 |
| M 9 | 31585 ± 55 | 32095 ± 102 | 31644 ± 78 | 31619 ± 74 | 31614 ± 56 | 31580 ± 59 | 31558 ± 60 | 31493 ± 59 | 31511 ± 61 | 31504 ± 61 |
| M 10 | 31759 ± 59 | 32429 ± 91 | 31868 ± 79 | 31829 ± 76 | 31823 ± 60 | 31752 ± 62 | 31758 ± 63 | 31652 ± 61 | 31653 ± 63 | 31646 ± 64 |
| 92641 ± 94 | 92492 ± 146 | 92289 ± 103 | 92306 ± 102 | 93322 ± 96 | 92668 ± 102 | 92631 ± 101 | 92697 ± 103 | 92640 ± 101 | 92664 ± 99 | |
| 572 ± 102 | 559 ± 153 | 579 ± 105 | 573 ± 103 | 583 ± 101 | 569 ± 104 | 571 ± 103 | 573 ± 102 | 577 ± 104 | 574 ± 102 | |
| Δ | 182.2 | 171.3 | 180.2 | 176.1 | 199.7 | 183.5 | 189.1 | 203.7 | 210.8 | 211.4 |
The error attributed to a parameter defines the range within which it may vary without the mean error increasing. In particular, if zero lies within the range of the value of a parameter and ± its error, then that particular parameter may be fixed at zero, which is equivalent to excluding it in the first place.
In this project, Hartree-Fock calculations were performed for all the configurations 3dn4p, 3dn−14s4p and 3dn−24s24p. Details of these calculations and results are given in another paper, [38].
With the exception of the results obtained from the Hartree-Fock calculations, the values of particular parameters pertaining to the three configurations 3dn4p, 3dn−14s4p and 3dn−24s24p are in arithmetic progression, since there is insufficient experimental data for 3dn−24s24p to determine parameters pertaining only to those configurations. Hence even in results arising from the least-squares computations these parameters do not have attached a ± error value. Furthermore, also in those cases where a parameter has a value in the least-squares either equal to the one directly preceding it (denoted, specifically, for the sake of clarity by EQ.), or if it is maintained at a fixed difference (unless specified otherwise, the differences that appears in the diagonalization, and denoted by F.D.), there is no ± error attached to the value of the parameter. In those cases where a parameter either changes sign or is ill-defined in the least-squares, it is fixed at either its value in the diagonalization, or at a value of zero (denoted by FIX). This procedure may also be followed if one is interested to study the effect of a particular parameter either on other parameters or in reducing the mean error, by considering two variations, one with the parameter left intact and in the other maintained at a value of zero.
The column PREVIOUS RESULTS refers to individual treatments without two- and three-body effective interactions, performed by the author for calcium-nickel, [10–16]. For the case of copper, the excellent results of Martin and Sugar, [38], for the configurations 3d94s4p + 3d84s24p of CuI, were considered.
Results for the following parameters were obtained by the Hartree-Fock calculations: B, B′, B″, C, C′, C″, F2, ,, G1, , , G3, , , Gps, Gds, G*, H, H′, J, J′, K, K′, ζd, ,, ζp, , and as indicated in Tables 3–32. Very interesting and important conclusions from these results, not known or anticipated previously, were that G* is significantly larger than Gds, whereas H′ is appreciably smaller than H. The Hartree-Fock results for J′ and K′ in ZnI 3d104s4p + 3d94s24p were anomalous to the other values, and thus excluded from consideration.
Table 3.
Results for the parameter B
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 529 ± 6 | 615.95 | 501 | 526 | 515 | 509 | 536 ± 7 | 518 ± 4 | 510 |
| Ti | 554 ± 7 | 724.20 | 568 | 578 | 568 | 561 | 555 ± 6 | 549 ± 6 | 561 |
| V | 579 ± 12 | 816.61 | 635 | 630 | 621 | 613 | 547 ± 12 | 570 ± 10 | 612 |
| Cr | 677 ± 7 | 900.84 | 702 | 682 | 674 | 665 | 652 ± 8 | 666 ± 7 | 663 |
| Mn | 800 ± 14 | 980.13 | 769 | 734 | 727 | 717 | 722 ± 15 | 739 ± 14 | 714 |
| Fe | 738 ± 9 | 1056.03 | 836 | 786 | 780 | 769 | 768 ± 11 | 759 ± 4 | 765 |
| Co | 833 ± 8 | 1129.51 | 903 | 838 | 833 | 821 | 841 ± 16 | 842 ± 10 | 816 |
Table 32.
Results for the parameter
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 105 | 131.98 | 149.95 | 190 | 361 | 446 | 333 | 245 | 401 |
| Ti | 114 | 157.90 | 189.42 | 220 | 353 | 415 | 259 | 302 | 379 |
| V | 140 | 185.31 | 229.40 | 250 | 355 | 396 | 216 | 179 | 367 |
| Cr | 184 | 214.35 | 269.36 | 280 | 367 | 389 | 342 | 418 | 365 |
| Mn | 212 | 245.08 | 309.34 | 310 | 389 | 394 | 740 | 772 | 373 |
| Fe | 200 | 277.51 | 349.30 | 340 | 421 | 411 | 521 | 450 | 391 |
| Co | 236 | 311.61 | 389.28 | 370 | 463 | 440 | 429 | 305 | 419 |
| Ni | 255 | 347.35 | 429.25 | 400 | 515 | 481 | 385 | 376 | 457 |
| Cu | 375 | 384.69 | 469.22 | 430 | 577 | 534 | 608 | 575 | 505 |
| Zn | 423.56 | 509.19 | 460 | 649 | 599 | 563 | |||
| Ga | 463.94 | 549.16 | 490 | 731 | 676 | 631 |
All entries of the parameters are in cm−1.
4.1. Initial values
These entries appear in DIAGON 1 in Tables 1–40, and in the column INITIAL in table 42 for the general interpolation parameters.
Table 40.
Results for the parameter
| EL. | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | FINAL ILS | FINAL GLS |
|---|---|---|---|---|---|---|---|
| Ti | 0 | 9 | 30 | 13 | 30 (FIX) | 0 (FIX) | 9 |
| V | 0 | 13 | 30 | 13 | 21 | 11 | 9 |
| Cr | 0 | 17 | 30 | 13 | 30 (FIX) | 4 | 9 |
| Mn | 0 | 21 | 30 | 13 | 24 | 3 | 9 |
| Fe | 0 | 25 | 30 | 13 | 30 | 28 | 9 |
| Co | 0 | 29 | 30 | 13 | 30 (FIX) | 5 | 9 |
| Ni | 0 | 33 | 30 | 13 | 30 (FIX) | 9 | 9 |
| Cu | 0 | 37 | 30 | 13 | 30 (FIX) | 13 (FIX) | 9 |
| Zn | 0 | 41 | 30 | 13 | 9 |
For the parameters D′ and D″, least-squares optimization calculations were performed on those values obtained in the columns PREVIOUS RESULTS. Even when allowing for quadratic corrections, the deviations were quite large, especially near the center of the period, where the elements have the largest number of levels. Consequently, least-squares were performed, weighing the entry of each element proportionally to the number of its levels. When (D′)2 and (D″)2, the quadratic corrections were allowed to be free, their values were very different with both assuming large errors. When they were restricted to be equal the common value was −87 ± 95. Consequently, initially D′ and D″ were taken to be linear functions of the atomic number, as indicated in tables 1, 2, 42, and 43. Entries are given to two decimal places to ascertain that the interpolation relation, (39), for the parameters be satisfied.
Table 2.
Results for the parameter D″
| EL. | Previous results | DIACON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | Final GLS |
|---|---|---|---|---|---|---|
| Sc | 4833 | 4817.60 | 4880 | 5140 | 5028 | 4950 |
| Ti | 12010 | 10768.97 | 11440 | 11740 | 11585 | 11532 |
| V | 17228 | 16720.34 | 17760 | 18086 | 17908 | 17886 |
| Cr | 20565 | 22671.71 | 23840 | 24178 | 23997 | 24012 |
| Mn | 27138 | 28623.08 | 29680 | 30016 | 29852 | 29910 |
| Fe | 36419 | 34574.45 | 35280 | 35600 | 35473 | 35580 |
| Co | 41960 | 40525.82 | 40640 | 40930 | 40860 | 41022 |
| Ni | 47690 | 46477.18 | 45760 | 46006 | 46013 | 46236 |
| Cu | 51395 | 52428.55 | 50640 | 50828 | 50932 | 55980 |
| Zn | 58379.92 | 55280 | 55396 | 55617 | 55980 |
From previous results obtained for the even configurations in the iron group by Racah, Shadmi, Oreg, Stein and Caspi, [1,2,28,29], and for the odd configurations by the author, [3,4], the parameters B and C behaved as linear functions of the atomic number.
For the parameters B, B′, and B″ using the values obtained from the Hartree-Fock calculations, and demanding that they be in arithmetic progression, the best straight lines yielded
| (40a) |
| (40b) |
| (40c) |
The Hartree-Fock results were on the average greater by a factor of 1.27 from the spectroscopic results. Hence the initial values given in tables 3–5, and 42 are the above values divided by 1.27.
Table 5.
Results for the parameter B″
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| V | 881 | 1041.24 | 827 | 848 | 837 | 839 | 899 | 860 | 833 |
| Cr | 833 | 1116.47 | 882 | 920 | 904 | 909 | 886 | 886 | 903 |
| Mn | 922 | 1189.31 | 937 | 992 | 971 | 979 | 964 | 948 | 973 |
| Fe | 1148 | 1260.59 | 992 | 1064 | 1038 | 1049 | 1034 | 1049 | 1043 |
| Co | 1079 | 1330.49 | 1047 | 1136 | 1105 | 1119 | 1135 | 1160 | 1113 |
| Ni | 1109 (FIX) | 1399.33 | 1102 | 1208 | 1172 | 1189 | 1164 | 1175 | 1183 |
| Cu | 1000 (FIX) | 1467.33 | 1157 | 1280 | 1239 | 1259 | 1239 (FIX) | 1259 (FIX) | 1253 |
Table 4.
Results for the parameter B′
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ti | 651 ± 7 | 850.52 | 670 | 677 | 669 | 665 | 655 ± 7 | 655 ± 6 | 664 |
| V | 730 ± 5 | 934.80 | 731 | 739 | 729 | 726 | 723 ± 6 | 715 ± 5 | 724 |
| Cr | 755 ± 5 | 1013.87 | 792 | 801 | 789 | 787 | 769 ± 8 | 776 ± 7 | 784 |
| Mn | 861 ± 4 | 1089.50 | 853 | 863 | 849 | 848 | 843 ± 6 | 843 ± 7 | 844 |
| Fe | 943 ± 7 | 1162.72 | 914 | 925 | 909 | 909 | 901 ± 5 | 904 ± 3 | 904 |
| Co | 956 ± 6 | 1234.15 | 975 | 987 | 969 | 970 | 983 ± 10 | 1001 ± 12 | 964 |
| Ni | 1024 ± 7 | 1304.17 | 1036 | 1049 | 1029 | 1031 | 1021 ± 7 | 1017 ± 7 | 1024 |
Exactly as for the B, s, we obtain, using the Hartree-Fock results
| (41a) |
| (41b) |
| (41c) |
Again, the initial values for these parameters given in Tables 6–8, and 42 are the above values divided by the same factor of 1.27.
Table 6.
Results for the parameter C
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 714 ± 69 | 2221.17 | 1826 | 1266 | 1222 | 1240 | 762 ± 69 | 866 ± 47 | 1281 |
| Ti | 1661 ± 33 | 2623.15 | 2070 | 1674 | 1655 | 1677 | 1741 ± 31 | 1747 ± 30 | 1714 |
| V | 2084 ± 23 | 2965.90 | 2314 | 2082 | 2088 | 2114 | 2204 ± 42 | 2228 ± 38 | 2147 |
| Cr | 2445 ± 15 | 3277.50 | 2558 | 2490 | 2521 | 2551 | 2596 ± 51 | 2535 ± 48 | 2580 |
| Mn | 2772 ± 17 | 3569.86 | 2802 | 2898 | 2954 | 2988 | 3121 ± 71 | 3108 ± 63 | 3013 |
| Fe | 3310 ± 29 | 3849.30 | 3046 | 3306 | 3387 | 3425 | 3404 ± 31 | 3435 ± 25 | 3446 |
| Co | 3744 ± 63 | 4119.39 | 3290 | 3714 | 3820 | 3862 | 3852 ± 84 | 3797 ± 70 | 3879 |
Table 8.
Results for the parameter C″
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| V | 3090 | 3878.88 | 3072 | 3212 | 3134 | 3158 | 3112 | 3216 | 3185 |
| Cr | 3391 | 4155.83 | 3268 | 3412 | 3409 | 3423 | 3462 | 3463 | 3448 |
| Mn | 3508 | 4423.76 | 3464 | 3612 | 3684 | 3688 | 3699 | 3718 | 3711 |
| Fe | 3708 | 4685.03 | 3660 | 3812 | 3959 | 3953 | 3970 | 3940 | 3974 |
| Co | 4006 | 4941.20 | 3856 | 4012 | 4234 | 4218 | 4136 | 4111 | 4237 |
| Ni | 4287 | 5193.31 | 4052 | 4212 | 4509 | 4483 | 4522 | 4531 | 4500 |
| Cu | 4500 (FIX) | 5442.15 | 4248 | 4412 | 4784 | 4748 | 4784 (FIX) | 4748 (FIX) | 4763 |
Table 7.
Results for the parameter C′.
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ti | 2319 ± 57 | 3131.03 | 2473 | 2343 | 2257 | 2285 | 2380 ± 38 | 2354 ± 38 | 2318 |
| V | 2587 ± 19 | 3443.16 | 2693 | 2647 | 2611 | 2636 | 2658 ± 29 | 2722 ± 30 | 2666 |
| Cr | 2918 ± 12 | 3735.06 | 2913 | 2951 | 2965 | 2987 | 3029 ± 39 | 2999 ± 37 | 3014 |
| Mn | 3140 ± 9 | 4013.59 | 3133 | 3255 | 3319 | 3338 | 3410 ± 57 | 3413 ± 50 | 3362 |
| Fe | 3509 ± 14 | 4282.74 | 3353 | 3559 | 3673 | 3689 | 3687 ± 18 | 3688 ± 16 | 3710 |
| Co | 3875 ± 18 | 4545.00 | 3573 | 3863 | 4027 | 4040 | 3994 ± 35 | 3954 ± 34 | 4058 |
| Ni | 4187 ± 54 | 4801.79 | 3793 | 4167 | 4381 | 4391 | 4394 ± 45 | 4439 ± 43 | 4406 |
For F2, , , least-squares were performed on the Hartree-Fock results demanding that they be in arithmetic progression. When quadratic corrections were allowed, the mean error was 5.0cm−1, with values of 1.2 ± 0.3cm−1 and 0.7 ± 0.2cm−1 for (F2)2 and , respectively. When (F2)2 and were set equal, they had a common value of 1.0 ± 0.3cm−1, with the mean error rising to 7.9cm−1. When both were zero, the mean error only rose to 9.0cm−1. Hence this variation was adopted, the parameters were restricted to be linear with initial values given in tables 9–11 and 42. However, the possibility of allowing for quadratic corrections in subsequent iterations and variations was permitted.
Table 9.
Results for the parameter F 2
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ca | 128 ± 2 | 306.13 | 273.34 | 200 | 151 | 178 | 171 ± 24 | 190 ± 27 | 170.5 |
| Sc | 201 ± 8 | 258.97 | 259.70 | 200 | 156 | 180 | 212 ± 9 | 200 ± ll | 173 |
| Ti | 153 ± 9 | 235.96 | 246.05 | 200 | 161 | 182 | 163 ± 6 | 167 ± 5 | 175.5 |
| V | 160 ± 8 | 220.50 | 232.40 | 200 | 166 | 184 | 182 ± 7 | 168 ± 6 | 178 |
| Cr | 187 ± 10 | 208.61 | 218.75 | 200 | 171 | 186 | 196 ± 8 | 189 ± 5 | 180.5 |
| Mn | 193 ± 7 | 198.79 | 205.10 | 200 | 176 | 188 | 206 ± 9 | 178 ± 8 | 183 |
| Fe | 173 ± 10 | 190.32 | 191.45 | 200 | 181 | 190 | 205 ± 7 | 202 ± 7 | 185.5 |
| Co | 218 ± 10 | 182.79 | 177.80 | 200 | 186 | 192 | 221 ± 10 | 226 ± 9 | 188 |
| Ni | 166 ± 13 | 175.92 | 164.15 | 200 | 191 | 194 | 167 ± 21 | 170 ± 15 | 190.5 |
Table 11.
Results for the parameter
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ti | 419 | 354.97 | 350.13 | 400 | 402 | 404 | 473 | 468 | 407.5 |
| V | 404 | 352.41 | 348.42 | 400 | 402 | 406 | 390 | 380 | 410 |
| Cr | 363 | 349.86 | 346.71 | 400 | 402 | 408 | 378 | 405 | 412.5 |
| Mn | 435 | 347.26 | 345.01 | 400 | 402 | 410 | 410 | 402 | 415 |
| Fe | 437 | 344.57 | 343.31 | 400 | 402 | 412 | 425 | 442 | 417.5 |
| Co | 388 | 341.77 | 341.60 | 400 | 402 | 414 | 389 | 396 | 420 |
| Ni | 456 | 338.86 | 339.89 | 400 | 402 | 416 | 433 | 434 | 422.5 |
| Cu | 480 (FIX) | 335.82 | 338.18 | 400 | 402 | 418 | 422 | 432 | 425 |
| Zn | 332.70 | 400 | 402 | 420 | 427.5 |
For the parameters G1, , and , when least-squares were performed on the Hartree-Fock results, the quadratic corrections were significant. When the parameters were forced to be linear, the mean error was 68 cm−1, whereas with (G1)2 assuming a value of 7.8 ± 1.0cm−1 and a value of 3.5 ± 0.6cm−1 the mean error was reduced to 21 cm−1. The initial values are given in tables 12–14 and 42. As for the F2 parameters no scaling factor was used between the spectroscopic and the Hartree-Fock results.
Table 12.
Results for the parameter G 1
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ca | 394 ± 2 | 559.20 | 501.60 | 231 | 305 | 328 | 419 ± 29 | 423 ± 32 | 327.5 |
| Sc | 335 ± 9 | 367.63 | 405.13 | 226 | 289 | 309 | 344 ± 10 | 347 ± 11 | 309 |
| Ti | 283 ± 10 | 290.99 | 324.32 | 221 | 273 | 290 | 287 ± 5 | 288 ± 5 | 290.5 |
| V | 229 ± 8 | 247.17 | 259.17 | 216 | 257 | 271 | 251 ± 7 | 251 ± 7 | 272 |
| Cr | 224 ± 7 | 217.86 | 209.69 | 211 | 241 | 252 | 243 ± 8 | 241 ± 7 | 253.5 |
| Mn | 227 ± 7 | 196.41 | 175.88 | 206 | 225 | 233 | 220 ± 8 | 230 ± 9 | 235 |
| Fe | 202 ± 8 | 179.74 | 157.73 | 201 | 209 | 214 | 237 ± 7 | 238 ± 5 | 216.5 |
| Co | 196 ± 9 | 166.21 | 155.25 | 196 | 193 | 195 | 199 ± 9 | 199 ± 10 | 198 |
| Ni | 165 ± 9 | 154.84 | 168.43 | 191 | 177 | 176 | 172 ± 11 | 171 ± 10 | 179.5 |
Table 14.
Results for the parameter
| EL. | Previous results | Hartree− Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ti | 293 | 311.36 | 294.28 | 401 | 341 | 344 | 369 | 362 | 342.5 |
| V | 333 | 300.52 | 293.93 | 368 | 325 | 325 | 351 | 337 | 324 |
| Cr | 248 | 292.02 | 292.05 | 335 | 309 | 306 | 235 | 283 | 305.5 |
| Mn | 263 | 284.95 | 288.64 | 302 | 293 | 287 | 244 | 264 | 287 |
| Fe | 288 | 278.81 | 283.73 | 269 | 277 | 268 | 259 | 272 | 268.5 |
| Co | 202 | 273.28 | 277.31 | 236 | 261 | 249 | 221 | 227 | 250 |
| Ni | 281 | 268.19 | 269.37 | 203 | 245 | 230 | 282 | 281 | 231.5 |
| Cu | 284 (EQ.) | 263.39 | 259.91 | 170 | 229 | 211 | 240 | 235 | 213 |
| Zn | 258.81 | 248.94 | 137 | 213 | 192 | 194.5 |
From the definition of the G3 parameters, it is clear that they should be allowed the same degree of freedom as the G1 parameters. Hence the initial values given in tables 15–17 and 42, were obtained by allowing quadratic corrections in the least squares of the Hartree-Fock results, and then using a scale factor of 2 to divide the latter. This common factor was obtained by comparing the Hartree-Fock and spectroscopic results.
Table 15.
Results for the parameter G 3
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ca | 0 (FIX) | 66.67 | 30.42 | 62 | 5 | 15 | 5 (FIX) | 15 (FIX) | 13 |
| Sc | 5 ± 3 | 45.84 | 24.96 | 55 | 5 | 15 | 8 ± 6 | 4 ± 5 | 13 |
| Tí | 10 ± 3 | 37.21 | 20.38 | 48 | 5 | 15 | 8 ± 3 | 7 ± 3 | 13 |
| V | 13 ± 2 | 32.11 | 16.67 | 41 | 5 | 15 | 18 ± 3 | 14 ± 3 | 13 |
| Cr | 16 ± 1 | 28.61 | 13.82 | 34 | 5 | 15 | 10 ± 3 | 7 ± 2 | 13 |
| Mn | 18 ± 1 | 25.98 | 11.85 | 27 | 5 | 15 | 24 ± 3 | 14 ± 3 | 13 |
| Fe | 20 ± 2 | 23.90 | 10.75 | 20 | 5 | 15 | 17 ± 3 | 18 ± 2 | 13 |
| Co | 14 ± 2 | 22.18 | 10.52 | 13 | 5 | 15 | 13 ± 4 | 13 ± 3 | 13 |
| Ni | 14 ± 4 | 20.70 | 11.16 | 6 | 5 | 15 | 7 ± 5 | 6 ± 5 | 13 |
Table 17.
Results for the parameter
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ti | 10 | 47.75 | 22.98 | 58 | 25 | 31 | 34 | 37 | 29 |
| V | 13 | 46.23 | 22.77 | 51 | 25 | 31 | 30 | 20 | 29 |
| Cr | 16 | 44.98 | 22.49 | 44 | 25 | 31 | 48 | 53 | 29 |
| Mn | 18 | 43.89 | 22.12 | 37 | 25 | 31 | 36 | 30 | 29 |
| Fe | 20 | 42.90 | 21.67 | 30 | 25 | 31 | 23 | 24 | 29 |
| Co | 14 | 42.00 | 21.13 | 23 | 25 | 31 | 15 | 17 | 29 |
| Ni | 14 | 41.14 | 20.52 | 16 | 25 | 31 | 15 | 18 | 29 |
| Cu | 51 (EQ.) | 40.32 | 19.82 | 9 | 25 | 31 | 41 | 43 | 29 |
| Zn | 39.53 | 19.03 | 2 | 25 | 31 | 29 |
For the parameter Gps the quadratic correction was very significant, reducing the mean error in the least-squares of the Hartree-Fock results from 79cm−1 to 27cm−1. The values given in tables 18 and 42 are those obtained after dividing the least squares results by a common factor of 1.58.
Table 18.
Results for the parameter Gps
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ca | 4977 ± 19 | 8451.47 | 5384.41 | 5326 | 4736 | 5059 | 5135 ± 89 | 4917 ± 86 | 5129 |
| Sc | 5970 ± 82 | 8924.04 | 5631.23 | 5564 | 5250 | 5449 | 5906 ± 76 | 5850 ± 71 | 5484 |
| Ti | 5395 ± 97 | 9294.41 | 5856.49 | 5802 | 5704 | 5803 | 5873 ± 63 | 5900 ± 66 | 5809 |
| V | 6022 ± 80 | 9605.22 | 6060.20 | 6040 | 6098 | 6121 | 6000 ± 66 | 5936 ± 67 | 6104 |
| Cr | 6155 ± 45 | 9873.36 | 6242.34 | 6278 | 6432 | 6403 | 6479 ± 55 | 6493 ± 52 | 6369 |
| Mn | 6631 ± 60 | 10107.40 | 6402.92 | 6516 | 6706 | 6649 | 6641 ± 61 | 6498 ± 54 | 6604 |
| Fe | 7116 ± 58 | 10313.14 | 6541.94 | 6754 | 6920 | 6859 | 6726 ± 37 | 6746 ± 36 | 6809 |
| Co | 7038 ± 56 | 10493.43 | 6659.39 | 6992 | 7074 | 7033 | 6991 ± 51 | 7005 ± 50 | 6984 |
| Ni | 7027 ± 60 | 10651.78 | 6755.28 | 7230 | 7168 | 7171 | 7011 ± 76 | 7011 ± 72 | 7129 |
| Cu | 8425 ± 17 | 10789.03 | 6829.62 | 7468 | 7202 | 7273 | 7994 ± 96 | 8003 ± 92 | 7244 |
| Zn | 10908.11 | 6882.39 | 7706 | 7176 | 7339 | 7329 |
For Gds and G*, least-squares calculations on the Hartree-Fock results decreased the value of the mean error from 91cm−1 to 38cm−1, after allowing a quadratic correction. However, the values of (Gds)2 and (G*)2 were sufficiently close to each other, 7.3 ± 1.5cm−1 and 8.9 ± 1.6cm−1, respectively, that these were compelled to be equal in the initial computations. The latter were obtained by dividing the results from the least-squares by a common factor of 1.1.
For H and H′, in the least-squares of the Hartee-Fock results, the values of H1 and were −11.5 ± 1.6cm−1 and −13.5 ± 1.2cm−1, respectively, whereas H2 and were 2.9 ± 0.2cm−1 and 2.5 ± 0.2cm−1, respectively. Consequently, both pairs of parameters were set equal. Then the mean error was only 5.8cm−1 and the results, without a scaling factor, are given in tables 21, 22, and 42.
Table 21.
Results for the parameter H
| EL. | Previous results | Hartree· Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 275 ± 18 | 323.61 | 313.20 | 158 | 238 | 224 | 331 ± 27 | 310 ± 31 | 215 |
| Ti | 175 ± 7 | 267.45 | 267.36 | 144 | 197 | 204 | 184 ± 5 | 184 ± 4 | 192 |
| V | 150 ± 6 | 224.55 | 226.76 | 130 | 162 | 184 | 165 ± 6 | 166 ± 5 | 169 |
| Cr | 157 ± 4 | 190.00 | 191.38 | 116 | 133 | 164 | 166 ± 5 | 161 ± 5 | 146 |
| Mn | 70 ± 6 | 161.19 | 161.23 | 102 | 110 | 144 | 100 ± 8 | 121 ± 9 | 123 |
| Fe | 85 ± 6 | 136.54 | 136.31 | 88 | 93 | 124 | 92 ± 5 | 90 ± 5 | 100 |
| Co | 72 ± 6 | 115.04 | 116.61 | 74 | 82 | 104 | 82 ± 6 | 81 ± 6 | 77 |
| Ni | 154 ± 33 | 95.99 | 102.15 | 60 | 77 | 84 | 118 ± 22 | 123 ± 18 | 54 |
Table 22.
Results for the parameter H′
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ti | 175 (EQ.) | 189.71 | 199.65 | 104 | 141 | 144 | 141 (FIX) | 124 (F.D.) | 153 |
| V | 150 (EQ.) | 152.87 | 159.04 | 90 | 106 | 124 | 35 ± 18 | 106 (F.D.) | 130 |
| Cr | 157 (EQ.) | 122.62 | 123.66 | 76 | 77 | 104 | 84 ± 15 | 61 ± 13 | 107 |
| Mn | 70 (EQ.) | 97.00 | 93.51 | 62 | 54 | 84 | 54 (FIX) | 61 (F.D.) | 84 |
| Fe | 85 (EQ.) | 74.76 | 68.59 | 48 | 37 | 64 | 37 (FIX) | 30 (F.D.) | 61 |
| Co | 72 (EQ.) | 55.13 | 48.90 | 34 | 26 | 44 | 26 (FIX) | 21 (F.D.) | 38 |
| Ni | 154 (EQ.) | 37.58 | 34.44 | 20 | 21 | 24 | 21 (FIX) | 63 (F.D.) | 15 |
| Cu | 0 (FIX) | 21.65 | 25.20 | 6 | 22 | 4 | 22 (FIX) | 4 (FIX) | 0 (FIX) |
Unlike the case of the H parameters, in the least-squares calculations of the Hartree-Fock results, J1 and had to be different, as their values were −28 ± 8cm−1 and 14 ± 7 cm−1, respectively. However, J2 and were sufficiently close to have a common value of 11 ± 2cm−1. This quadratic correction was important in reducing the mean error from 98cm−1 to 41 cm−1. The initial values in tables 23,24, and 42 are the least-square values divided by a common factor of 1.67 for both J and J′.
Table 23.
Results for the parameter J
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ca | 575 ± 20 | 2607.28 | 1485.69 | 1480 | 1260 | 1237 | 1260 (FIX) | 1237 (FIX) | 1112 |
| Sc | 1877 ± 96 | 2239.09 | 1367.98 | 1330 | 1040 | 1088 | 1668 ± 91 | 1579 ± 85 | 1066 |
| Ti | 1251 ± 53 | 2041.11 | 1263.71 | 1220 | 880 | 979 | 1326 ± 44 | 1313 ± 44 | 1036 |
| V | 972 ± 48 | 1907.24 | 1172.89 | 1150 | 780 | 910 | 992 ± 46 | 946 ± 40 | 1022 |
| Cr | 954 ± 32 | 1806.73 | 1095.51 | 1120 | 740 | 881 | 1061 ± 35 | 990 ± 31 | 1024 |
| Mn | 1294 ± 34 | 1726.42 | 1031.57 | 1130 | 760 | 892 | 1292 ± 56 | 1016 ± 55 | 1042 |
| Fe | 1183 ± 41 | 1659.47 | 981.08 | 1180 | 840 | 943 | 1004 ± 39 | 1025 ± 37 | 1076 |
| Co | 1245 ± 50 | 1601.79 | 944.02 | 1270 | 980 | 1034 | 1224 ± 55 | 1210 ± 55 | 1126 |
| Ni | 1144 ± 134 | 1550.86 | 920.42 | 1400 | 1180 | 1165 | 906 ± 89 | 913 ± 81 | 1192 |
| Cu | (2446 ± 365) | 1505.08 | 910.25 | 1570 | 1440 | 1336 | 1440 (FIX) | 1336 (FIX) | 1274 |
Table 24.
Results for the parameter J′
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 1877 (EQ.) | 2250.32 | 1371.30 | 1610 | 1380 | 1540 | 2008 (F.D.) | 2031 (F.D.) | 1596 |
| Ti | 1251 (EQ.) | 2134.09 | 1292.59 | 1500 | 1220 | 1431 | 1666 (F.D.) | 1765 (F.D.) | 1566 |
| V | 972 (EQ.) | 2052.61 | 1227.31 | 1430 | 1120 | 1362 | 1675 (F.D.) | 1337 ± 89 | 1552 |
| Cr | 954 (EQ.) | 1990.63 | 1175.48 | 1400 | 1080 | 1333 | 1401 (F.D.) | 1442 (F.D.) | 1554 |
| Mn | 1294 (EQ.) | 1940.85 | 1137.10 | 1410 | 1100 | 1344 | 1632 (F.D.) | 1468 (F.D.) | 1572 |
| Fe | 1183 (EQ.) | 1899.24 | 1112.15 | 1460 | 1180 | 1395 | 1344 (F.D.) | 1477 (F.D.) | 1606 |
| Co | 1245 (EQ.) | 1863.20 | 1100.65 | 1550 | 1320 | 1486 | 1564 (F.D.) | 1662 (F.D.) | 1656 |
| Ni | 1144(EQ.) | 1831.30 | 1102.59 | 1680 | 1520 | 1617 | 1246 (F.D.) | 1365 (F.D.) | 1722 |
| Cu | (2446 (EQ.)) | 1802.11 | 1117.97 | 1850 | 1780 | 1788 | 1780 (FIX) | 1788 (FIX) | 1804 |
| Zn | (1393.74) | 1146.79 | 2060 | 2100 | 1999 | 1902 |
For K and K′ the situation was very similar as that for J and J′—linearity with a common quadratic correction—here 24.5 ± cm−1, yielded a mean error of 62cm−1 compared with 142cm−1, when the parameters were forced to be linear. The initial values for K were obtained by using a scale factor of 1.28, whereas for K′ the scale factor was 1.10. Hence, initally K2 had a value of 19.15cm−1 and , a value of 22.29cm−1 in the tables 25, 26 and 42.
Table 25.
Results for the parameter K.
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ca | 3795 ± 32 | 4824.07 | 3535.35 | 2710 | 2875 | 2930 | 2922 ± 98 | 2571 ± 83 | 3009 |
| Sc | 2551 ± 95 | 4001.34 | 3215.28 | 2515 | 2680 | 2741 | 2743 ± 85 | 2638 ± 82 | 2812 |
| Ti | 2415 ± 48 | 3590.97 | 2933.52 | 2370 | 2525 | 2586 | 2613 ± 30 | 2611 ± 29 | 2645 |
| V | 2468 ± 48 | 3324.70 | 2690.06 | 2275 | 2410 | 2465 | 2555 ± 42 | 2520 ± 39 | 2508 |
| Cr | 2311 ± 30 | 3130.26 | 2484.91 | 2230 | 2335 | 2378 | 2423 ± 33 | 2350 ± 29 | 2401 |
| Mn | 2599 ± 36 | 2977.82 | 2318.05 | 2235 | 2300 | 2325 | 2597 ± 46 | 2358 ± 52 | 2324 |
| Fe | 2459 ± 45 | 2852.49 | 2189.51 | 2290 | 2305 | 2306 | 2211 ± 51 | 2236 ± 36 | 2277 |
| Co | 2331 ± 55 | 2745.36 | 2099.27 | 2395 | 2350 | 2321 | 2328 ± 63 | 2323 ± 53 | 2260 |
| Ni | 2072 ± 135 | 2651.31 | 2047.34 | 2550 | 2435 | 2370 | 1980 ± 96 | 1982 ± 89 | 2273 |
| Cu | (5090 ± 125) | 2566.78 | 2033.70 | 2755 | 2560 | 2453 | 4122 ± 97 | 3864 ± 90 | 2316 |
Table 26.
Results for the parameter K′
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 3059 (F.D.) | 3944.13 | 3670.74 | 3535 | 3480 | 3639 | 3543 (F.D.) | 3536 (F.D.) | 3759 |
| Ti | 2987 (F.D.) | 3715.02 | 3427.99 | 3390 | 3325 | 3484 | 3413 (F.D.) | 3509 (F.D.) | 3592 |
| V | 3104 (RD.) | 3561.34 | 3229.81 | 3295 | 3210 | 3363 | 3342 ± 73 | 2828 ± 89 | 3455 |
| Cr | 3011 (F.D.) | 3448.62 | 3076.21 | 3250 | 3135 | 3276 | 3353 ± 88 | 3458 ± 87 | 3348 |
| Mn | 3363 (F.D.) | 3360.71 | 2967.18 | 3255 | 3100 | 3223 | 3397 ± 74 | 3256 (F.D.) | 3271 |
| Fe | 3287 (F.D.) | 3288.84 | 2902.72 | 3310 | 3105 | 3204 | 3011 ± 79 | 3134 (F.D.) | 3224 |
| Co | 3223 (F.D.) | 3227.54 | 2882.84 | 3415 | 3150 | 3219 | 3128 ± 87 | 3221 (F.D.) | 3207 |
| Ni | 3028 (F.D.) | 3173.85 | 2907.54 | 3570 | 3235 | 3268 | 2780 (F.D.) | 2880 (F.D.) | 3220 |
| Cu | (5090 (EQ.)) | 3124.84 | 2976.79 | 3775 | 3360 | 3351 | 4922 (F.D.) | 4762 (F.D.) | 3263 |
| Zn | (2275.24) | 3090.63 | 4030 | 3525 | 3468 | 3336 |
In previous general treatments dealing with the spectra of the iron group [1–4,27,28], the parameters of the spin-orbit interaction generally required a quadratic correction. After performing several variations in the least-squares of the Hartree-Fock results, it was seen that the parameters ζd, , were required to have a quadratic correction, whereas the parameters ζp, , and could, initially, be linear.
The values of (ζd)2 and in the least-squares of the Hartree-Fock results were 6.9 ± 0.2 cm−1 and 8.1 ± 0.2cm−1, respectively. Hence they were set equal.
The mean error was then only 8.7cm−1, reduced from 32cm−1 when the ζd parameters were linear. The values obtained from those least-squares calculations were used directly without a scaling factor and are given in Tables 60–62, and 75.
When least squares were performed on the Hartree-Fock results of ζp,, and , demanding that they be in arithmetic progression, the value of (ζp)2 was −0.2 ± 0.3cm−1 and that of () was 0.3 ± 0.2cm−1. Thus, these parameters were fixed at zero, and initially ζp, , and were linear. Then, the mean error only increased from 7.9cm−1 to 8.2cm−1. By comparing the Hartree-Fock and spectroscopic results, a common scale factor of 0.8 was used to divide the values of the least-squares, in order to obtain the initial values given in tables 30–32 and 42.
Table 30.
Results for the parameter ζp
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Fina! GLS |
|---|---|---|---|---|---|---|---|---|---|
| K | 37.03 | 10 | 145 | 232 | 197 | ||||
| Ca | 87 ± 16 | 36.66 | 45.69 | 40 | 109 | 177 | 141 ± 67 | 139 ± 65 | 155 |
| Sc | 105 ± 56 | 44.52 | 54.35 | 70 | 83 | 134 | 147 ± 55 | 125 ± 53 | 123 |
| Ti | 114 ± 94 | 52.28 | 63.02 | 100 | 67 | 103 | 93 ± 51 | 82 ± 48 | 101 |
| V | 140 ± 78 | 60.06 | 71.70 | 130 | 61 | 84 | 96 ± 70 | 95 ± 60 | 89 |
| Cr | 184 ± 51 | 67.91 | 80.36 | 160 | 65 | 77 | 118 ± 56 | 118 ± 51 | 87 |
| Mn | 212 ± 60 | 75.88 | 89.04 | 190 | 79 | 82 | 0 (FIX) | 82 (FIX) | 95 |
| Fe | 200 ± 68 | 83.96 | 97.70 | 220 | 103 | 99 | 157 ± 57 | 106 ± 52 | 113 |
| Co | 236 ± 53 | 92.14 | 106.38 | 250 | 137 | 128 | 111 ± 58 | 187 ± 54 | 141 |
| Ni | 255 ± 51 | 100.38 | 115.05 | 280 | 181 | 169 | 263 ± 71 | 270 ± 71 | 179 |
| Cu | 375 ± 8 | 108.71 | 123.71 | 310 | 235 | 222 | 208 ± 94 | 201 ± 82 | 227 |
From the parameters of the effective interactions, previous values were available only for the α’s. As this parameter behaved irregularly, a common average value of 60 was taken as the initial value of α, α′, and α″ for all elements in the period. The initial values of β, β′, β″, T, T′, T″, Tx, , , F1,, , G2, , and were zero for all elements.
4.2. Preliminary iterations
For the general least-squares routine a maximum capacity for 101 parameters could be achieved.
In the first two iterations the parameters D′, D″, G1, , G3, , Gps, K, K′, ζd, , ζp, and were allowed independent quadratic variations as functions of the atomic number.
The parameters F2, , Gds, G*, H, H′, J, and J′ were permitted a quadratic variation with the restrictions
The parameters B, B′, C, C′, α, α′, F1, , G2, and were allowed to vary linearly.
The parameters β, β′, T, T′, Tx, and varied linearly with the restrictions
The remaining 13 places were reserved for the centers of gravity M0 − M12.
In the third iteration the restrictions
were not included. Thus, all the parameters for the interactions between configurations were permitted independent quadratic variations. The required places were obtained by realizing from the first two iterations that F2 need vary only linearly and it was also possible to impose the restrictions
The initial parameters of the first variation are given in the column DIAGON 1, (tables 1–40), whereas the final values are given in the column GLS1, (table 42). These parameters, with some modifications, were used for the second iteration and given in the column DIAGON 2. The results of the most successful of many variations in the general least-squares are given in the column GLS2, which are essentially the ones used in the next iteration and given in the column DIAGON 3. Again the results of the best variation are given in the columns GLS3, and then used with some modifications for the next iteration.
The values of the least-squares where all 101 parameters are allowed to be free are given in the columns GLS 1a, GLS 2a, and GLS 3a.
From the results of GLS1a it is clear that we should have
which can be seen either directly from the results or by noting that otherwise the parameters are ill-defined. With the above restrictions there then remained 78 free parameters in that variation which was used for the next stage of the computations, GLS 1. In GLS 1, the sum of the squares of the deviations decreased from 2.83879 × 109 to 5.97895 × 107. Besides the changes in the M’s, the parameter that had the greatest effect was C1; while changing from 244cm−1 to 408 ± 8cm−1 it reduced the sum of the squares of the deviations from 3.29325 × 108 to 2.57289 × 108.
In a variation where , , were free, but in addition to the restriction of GLS 1, there were the conditions
the parameters β0, T0, , , and H2 were badly defined. In each case the ± error of the parameter exceeded its actual value.
In another variation, with the same restrictions as in GLS 1, but leaving β1, (F1)1 and free, the values of these parameters were
As (G2)0 had the value of 24 ± 8 it is clear that β1 and (F1)1 should be zero whereas
In the second iteration when all 101 parameters are left free, GLS 2a, the G3, F1, and G2 parameters behave erratically, whereas ,, , and change sign. From these results and many other variations it became apparent that for the final variation in this iteration we should have
with 77 free parameters remaining.
The sum of the squares of the deviations is decreased from 2.06466 × 108 to 5.71710 × 107. The parameters having the greatest effect were (G3)0, in changing from 27 cm−1 to 10 ± 1 cm−1 it reduced the sum of the deviations from 1.47723 × 108 to 1.14285 × 108; (G3)1 from −7 cm−1 to 2.2 ± 0.7 cm−1 and reduced from 1.14285 × 108 to 8.71367 × 107, and (Gps)2, from 0 to −33 ± 5 cm−1, and reduced from 5.97160 × 107 to 5.75448 × 107.
In the variation with parameters given in the column GLS 2b, the values of , ,,,, (G1)2, and (G3)2 are allowed to be free, whereas
The results clearly show that can’t vary independently. and H1 are too far apart with not well-defined, J1 and , as well as K1 and , have opposite signs, which is unacceptable. is well-defined but need not be different from T0. Allowing (G1)2 and (G3)2 to vary has no significant effect. The reduction of the mean error from 203.1 cm−1 to 200.3 cm−1, certainly does not justify allowing the increase in the number of parameters as then they do not behave reasonably.
In a variation identical to GLS 2, except that , the values of these two parameters were −120±5 cm−1 and −127 ± 11 cm−1, respectively, showing clearly that they should be equal.
A variation in which ,, , are free, and all other conditions the same as in GLS 2, indicated that none of these parameters should be free, as they were either of different sign than the corresponding values G1, H1, J1, and K1, or were ill-defined.
In GLS 3a, with all 101 parameters free, the sum of the squares of the deviations was reduced from 9.62040 × 107 to 5.79187 × 107. However, several parameters such as , , , , , and were badly defined.
From the results of GLS 3a, as well as many other variations wherein only a smal number of restrictions are imposed in each case, the following restrictions were imposed in the final variation of the third iteration, GLS 3, yielding 68 free parameters:
The sum of the squares of the deviations was reduced from 8.28089 × 107 to 5.12809 × 107. The only parameter that had a very significant effect was J0, which changed from 1600 cm−1 to 1125 ± 39 cm−1, thereby reducing the sum of the squares of the deviations from 7.63469 × 107 to 6.39959 × 107. Although all the parameters had reasonable well-defined values, the change in the sum of the squares of the deviations was such that a further iteration was required.
In GLS 3b, there are 76 free parameters. The same conditions apply as for GLS 3a, with the exception of (F2)1, , (Tx)1, (F1)1, (G2)1 being free; , but not fixed at −10 cm−1; , but not fixed at 0; , but not fixed at 3 cm−1.
Although the parameters are very reasonable, the mean error actually increased from 196.7 cm−1 to 198.1 cm−1, indicating that the improvement caused by these parameters was more than counterbalanced by the fact that their number increased.
In GLS 3c there are 72 free parameters. The same conditions apply as for GLS 3a, with the exception of , and (F1)1 being free; , but not forced at −10 cm−1. Although the mean error decreases to 194.5 cm−1, the parameters and (F1)1 change sign, while the value of 51 ± 12 cm−1 is definitely too small for .
In a variation where was allowed to vary freely, although its value changed from 50 cm−1 to the unreasonable value of −304 ± 44 cm−1, the sum of the squares of the deviations only decreased as a consequence from 6.74632 × 107 to 6.67194 × 107. Furthermore, such a value for would cause J′ to become negative for Cu I. Clearly, then should equal J1 as in GLS 3.
In a variation where was not equal and (F1)0 not equal to , the resulting values were
and thus as in GLS 3 these parameters should be respectively equal to each other.
The values of the parameters of the individual least squares of the third iteration are given in tables 3–40.
4.3. Final iteration.
For this iteration the 101 places for the parameters were the same as for the previous iteration.
From the final results of that iteration, GLS 3, as well as several different variations in this iteration, it became evident that 67 parameters should be free in the final results, GLS 4. Thus, the following 34 restrictions were imposed:
Hence in the final results the parameters D′, D″, Gps, Gds, G*, J, J′, K, K′, ζd, , , ζp, , and required quadratic corrections, with the restrictions noted above. In particular, Gds and G* did not have linear terms. All the other parameters were linear functions of the atomic number. Furthermore, Tx, ,, F1, ,, G2, , and were constant for all spectra across the entire period.
The sum of the squares of the deviations only decreased from 5.83692 × 107 to 4.87994 × 107 for all the parameters. In each case the change in a parameter from the value in the diagonalization to its value in the least squares was less than the statistical error associated with the parameter. All the parameters have very reasonable values and are well-defined. The comparisons between these final results and those obtained from the Hartree-Fock calculations as well as those of previous results, are indicated graphically at the end of this section.
In GLS4a, where all the 101 parameters are free, although the mean error is only 171.3cm−1, the parameters are not nearly as well defined as those of GLS4. Furthermore, the values of at 598 ± 271cm−1, at −376 ± 127 cm−1, t at −11 ± 4cm−1, at −20cm−1 (causing both F′ and F″ to assume positive and negative values for different elements of the period), are not reasonable.
In GLS4b, the parameter is allowed to be free and changes from 1820cm−1 to a value of 1649 ± 83cm−1, thereby decreasing the sum of the squares of the deviations only from 5.40826 × 107 to 5.38969 × 107. Hence G* is then uniformly higher than Gds by only 56cm−l. Thus, the significant difference between G* and Gds obtained in the Hartree-Fock calculations and the initial iterations becomes considerably less pronounced here. Nevertheless, in view of the other considerations above, was maintained in the final variation at 1826cm−1, a fixed difference of 231cm−1 above the value of (Gds)0.
In GLS4c, there are 71 free parameters, the same restrictions are imposed as in GLS4, with the exception that , , , and (F1)1 are left free. Although the mean error is reduced from 182.2cm−1 to 176.1cm−1 and the values for of 1674 ± 81cm−1 and (F1)1 of −4 ± 2cm−1 are reasonable, the value for of 42 ± 15 cm−1 is much too low, whereas the value for of −231 ±37 cm−1 is definitely unacceptable.
In another variation, with the same restrictions as in GLS4, but (F1)1 free, the value of this parameter was −5 ± 2cm−1. Coupled with a value of (F1)0 of −11 ± 4cm−1, the parameter F1 assumes negative and positive values for different spectra of the period, which is unacceptable.
In GLS4d, the following additional 26 levels, which although having deviations exceeding the maximum tolerated for the other iterations (∿ 600cm−1), had deviations below 1000cm−1 when inserted into the least squares.
Ti
The level 3d24s(b2P)4py3S at 35439.43 cm−1.
The three levels 3d3(a2G)4pt3F2,3,4 at 38451.29cm−1, 38544.38cm−1 and 38670.73cm−1.
The level 3d3(a2G)4px1G at 38959.53cm−1.
The level 3d3(a2P)4pw1D at 39265.80cm−1.
The three levels 3d3(a2P)4pr3D at 40556.70cm−1, 40670.60cm−1, and 40844.19cm−1.
V
The level 1° at 34019.12cm−1.
The four levels of 3d4(a3G)4pt4F at 41389.49cm−1, 41428.93cm−1, 41492.29cm−1, and 41599.36cm−1.
Cr
The level 3d44s(a2P)4px3S at 60084.09cm−1.
Mn
The four levels 3d6(3G)4pw4H at 63395.45cm−1, 63444.61cm−1, 63457.85cm−1, and 63363.54cm−1.
Fe
The five levels 3d44s(a4D)4px5H at 39625.829cm−1, 39969.880cm−1, 40231.365cm−1, 40404.544cm−1, and 40491.32cm−1.
Cu
The two levels 3d94s(1D)4p″2P at 56343.74cm−1 and 58364.73cm−1.
The restrictions are the same as in the case of GLS4, and as expected, the parameters are well-defined and reasonable. However, the mean error increases substantially from 182.2cm−1 to 199.7cm−1.
In GLS4e there are 65 parameters. In addition to the restrictions of GLS4, the conditions
are imposed. As a consequence, the parameters of the two-body effective interactions d − p: F1, , , G2, , and are eliminated. Surprisingly, the mean error only increases from 182.2cm−1 to 183.5cm−1. The elimination of these parameters also affects very slightly the values of the other parameters, and thus their overall effects are minimal indeed. Consequently, the higher order three-body effective interactions d − p were not included (see the end of sec. 2).
In the variation GLS4f, there are 64 free parameters. In addition to the elimination of the F1 and G2 parameters, as in GLS4e, the condition
was imposed. Hence the three-body effective interaction parameters of the d-electrons, Tx, , and were eliminated. The mean error rose to 189.1cm−1, indicating that the Tx parameters have a considerably greater effect than the F2 and G1 parameters combined. The significant increase in the value of
from −527 ± 28cm−1 in GLS4 to the present value of −673 ± 31cm−1, should be noted.
In GLS4g, there are 62 parameters. In addition to the elimination of the F1, G2, and Tx parameters, as in GLSf, the conditions
are imposed. Hence both parameters of the effective interactions of the d-electrons are eliminated. As expected, the effects here are very pronounced, the mean error rising from 189.1cm−1 to 203.7cm−1. Thus the effect of T is twice as great as Tx, and 11 times as large as F2 and G1 combined! As expected, the elimination of T has profound effects on the other remaining effective intersection parameters:
increases from 30 ± 3cm−1 to 61 ± 2cm−1, whereas
changes from −673 ± 31 cm−1 to −336 ± 32 cm−1.
In GLS 4h there are also 62 free parameters. The F2 and G1 parameters are included, but instead the restrictions
are imposed.
Hence, β, β′, and β″ are eliminated. The results again deteriorate, the mean error rising from 203.7cm−1 to 210.8cm−1. As expected, the F1 and G2 parameters have similar values as in GLS4 and GLS4d.
has the higher value of 71 ± 1cm−1, incorporating partially the other effective parameters.
In GLS4i, there are only 60 free parameters. Here, in addition to the restrictions of GLS4, the parameters β, β′, β″, T, T′, T″, Tx, , , F1, , , G2, and are eliminated. The mean error rises to 211.4cm−1. Comparing this value with that of GLS4h (Δ of 210.8cm−1) emphasizes again the minimal effects of the parameters F2 and G1. α0 again has the high value of 72 ± 1cm−1.
In conclusion, starting from the 67 parameters in GLS4, the elimination of F2 and G1 increases the mean error by only 1.3cm−1, Tx by a further 5.6cm−1, T by an additional 14.6cm−1, and β by an additional 7.7cm−1.
The values of the parameters of the individual least squares of the final iteration are given in tables 3–40. More detailed discussions of the individual least squares are given in the paper dealing with the correspondence of the energy levels of the various configurations (3d + 4s)n4p, [17].
4.4. Plots of parameters
Figures 1–17 describe graphically the variation of the parameters as functions of the atomic number for the cases of the previous results, Hartree-Fock computations and the final general least-squares (GLS4). In the case of the previous results, PR, the entries are from individual least squares and are indicated by a dot, ●; whenever a particular parameter varied freely the ± value of the error is also given. For the case of Hartree-Fock computations, HF, the entries are given by a solid triangle, ▲; whereas a solid square, ■, denotes the results of the final GLS.
Figure 1.

Plots of D′ versus atomic number.
Figure 17.

Plots of T = T′ = T″ versus atomic number.
Since Tx, , , F1, , , G2, ,, are constant in the final results, their graphs clearly need not be drawn. Graphs of all the other parameters are given.
The sets of parameters B, B′, B″; C, C′, C″; F2, ,; G1, , ; G3, , ; ζd, ,;; ζp, , ; are in arithmetic progression in the least squares. Consequently, in order to indicate explicitly this interdependence, separate graphs were drawn where each set of three parameters appears together.
The graphs vividly illustrate and contrast the often irregular behavior of the parameters in the previous results, with the smooth, regular and very reasonable variations obtained in the present project for both the Hartree-Fock computations and, of course, for the general least squares. The contrasts are particularly prominent for the parameters of the interactions between configurations. There is general qualitative agreement between the Hartree-Fock results and those of the GLS. The only notable exceptions are the parameters F2, , and , as they increase slowly in the GLS as functions of the atomic number, whereas in the Hartree-Fock computations they decrease.
Figure 2.

Plots of D″ versus atomic number.
Figure 3.

Plots of B, B′, and B″ versus atomic number.
Figure 4.

Plots of C, C′, and C″ versus atomic number.
Figure 5.

Plots of F2, , and versus atomic number.
Figure 6.

Plots of G1, , and versus atomic number.
Figure 7.

Plots of G3, , and versus atomic number.
Figure 8.

Plots of Gps versus atomic number.
Figure 9.

Plots of Gds and G* versus atomic number.
Figure 10.

Plots of H and H′ versus atomic number.
Figure 11.

Plots of J and J′ versus atomic number.
Figure 12.

Plots of K and K′ versus atomic number.
Figure 13.

Plots of ζd, , and versus atomic number.
Figure 14.

Plots of ζp, , and versus atomic number.
Figure 15.

Plots of α = α′ = α″ versus atomic number.
Figure 16.

Plots of β = β′ = β″ versus atomic number.
Table 10.
Results for the parameter
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 284 ± 8 | 300.16 | 305.77 | 300 | 279 | 291 | 297 ± 11 | 285 ± 12 | 289 |
| Ti | 286 ± 8 | 290.88 | 298.09 | 300 | 281.5 | 293 | 318 ± 5 | 317 ± 5 | 291.5 |
| V | 282 ± 6 | 283.55 | 290.41 | 300 | 284 | 295 | 286 ± 6 | 274 ± 6 | 294 |
| Cr | 275 ± 5 | 277.22 | 282.73 | 300 | 286.5 | 297 | 287 ± 5 | 297 ± 5 | 296.5 |
| Mn | 314 ± 4 | 271.46 | 275.06 | 300 | 289 | 299 | 308 ± 10 | 290 ± 10 | 299 |
| Fe | 305 ± 5 | 266.08 | 267.38 | 300 | 291.5 | 301 | 315 ± 4 | 322 ± 5 | 301.5 |
| Co | 303 ± 7 | 260.91 | 259.70 | 300 | 294 | 303 | 305 ± 8 | 311 ± 7 | 304 |
| Ni | 311 ± 7 | 255.92 | 252.02 | 300 | 269.5 | 305 | 300 ± 9 | 304 ± 8 | 306.5 |
| Cu | 329 ± 12 | 251.02 | 244.35 | 300 | 299 | 307 | 319 ± 7 | 319 ± 9 | 309 |
Table 13.
Results for the parameter G′ 1
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 327 ± 12 | 328.91 | 349.14 | 330 | 323 | 336 | 354 ± 13 | 344 ± 16 | 335 |
| Ti | 288 ± 10 | 293.92 | 309.30 | 311 | 307 | 317 | 328 ± 6 | 325 ± 6 | 316.5 |
| V | 281 ± 8 | 271.04 | 276.55 | 292 | 291 | 298 | 301 ± 6 | 294 ± 7 | 298 |
| Cr | 236 ± 5 | 254.27 | 250.87 | 273 | 275 | 279 | 239 ± 7 | 262 ± 5 | 279.5 |
| Mn | 245 ± 6 | 241.08 | 232.26 | 254 | 259 | 260 | 232 ± 9 | 247 ± 8 | 261 |
| Fe | 245 ± 7 | 230.18 | 220.73 | 235 | 243 | 241 | 248 ± 6 | 255 ± 5 | 242.5 |
| Co | 199 ± 7 | 220.78 | 216.28 | 216 | 227 | 222 | 210 ± 8 | 213 ± 7 | 224 |
| Ni | 223 ± 9 | 212.51 | 218.90 | 197 | 211 | 203 | 227 ± 12 | 226 ± 12 | 205.5 |
| Cu | 284 ± 2 | 205.00 | 228.59 | 178 | 195 | 184 | 206 ± 13 | 208 ± 16 | 187 |
Table 16.
Results for the parameter
| EL | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 5 (EQ.) | 45.63 | 24.04 | 60 | 15 | 23 | 18 ± 6 | 4 (EQ.) | 21 |
| Ti | 10 (EQ.) | 41.50 | 21.68 | 53 | 15 | 23 | 21 ± 3 | 22 ± 3 | 21 |
| V | 13 (EQ.) | 38.66 | 19.72 | 46 | 15 | 23 | 24 ± 3 | 17 ± 3 | 21 |
| Cr | 16 (EQ.) | 36.50 | 18.16 | 39 | 15 | 23 | 29 ± 3 | 30 ± 2 | 21 |
| Mn | 18 (EQ,) | 34.73 | 16.99 | 32 | 15 | 23 | 30 ± 4 | 22 ± 4 | 21 |
| Fe | 20 (EQ.) | 33.23 | 16.21 | 25 | 15 | 23 | 20 ± 2 | 21 ± 4 | 21 |
| Co | 14 (EQ.) | 31.90 | 15.82 | 18 | 15 | 23 | 14 ± 3 | 15 ± 2 | 21 |
| Ni | 14 (EQ.) | 30.71 | 15.84 | 11 | 15 | 23 | 11 ± 6 | 12 ± 6 | 21 |
| Cu | 51 ± 1 | 29.62 | 16.24 | 4 | 15 | 23 | 31 ± 6 | 35 ± 7 | 21 |
Table 19.
Results for the parameter Gds
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 1943 ± 68 | 2007.15 | 1840.72 | 1574 | 1670 | 1637 | 1787 ± 62 | 1930 ± 65 | 1649 |
| Ti | 1719 ± 56 | 1876.97 | 1728.73 | 1506 | 1625 | 1581 | 1538 ± 37 | 1560 ± 66 | 1590 |
| V | 1584 ± 33 | 1795.01 | 1637.57 | 1470 | 1590 | 1541 | 1531 ± 29 | 1563 ± 30 | 1541 |
| Cr | 1590 ± 19 | 1739.54 | 1567.26 | 1466 | 1565 | 1517 | 1513 ± 24 | 1474 ± 24 | 1514 |
| Mn | 1532 ± 22 | 1700.66 | 1517.80 | 1494 | 1550 | 1509 | 1515 ± 34 | 1501 ± 37 | 1505 |
| Fe | 1536 ± 24 | 1672.86 | 1489.17 | 1554 | 1545 | 1517 | 1561 ± 19 | 1556 ± 18 | 1514 |
| Co | 1607 ± 33 | 1652.90 | 1481.39 | 1646 | 1550 | 1541 | 1554 ± 46 | 1557 ± 41 | 1541 |
| Ni | 1626 ± 53 | 1638.76 | 1494.45 | 1770 | 1565 | 1581 | 1590 ± 68 | 1589 ± 65 | 1590 |
| Cu | 1550 (FIX) | 1629.02 | 1528.35 | 1926 | 1590 | 1637 | 1274 ± 86 | 1250 ± 83 | 1649 |
Table 20.
Results for the parameter G*
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 1943 (EQ.) | 3223.33 | 2855.34 | 2282 | 2070 | 1868 | 2187 ± 62 | 2161 (F.D.) | 1880 |
| Ti | 1719 (EQ.) | 2936.23 | 2689.36 | 2214 | 2025 | 1812 | 1938 ± 37 | 1789 (F.D.) | 1821 |
| V | 1584 (EQ.) | 2751.21 | 2544.23 | 2178 | 1990 | 1772 | 2233 ± 91 | 1794 (F.D.) | 1772 |
| Cr | 1590 (EQ.) | 2622.68 | 2419.94 | 2174 | 1965 | 1748 | 1784 ± 87 | 1882 ± 82 | 1745 |
| Mn | 1532 (EQ.) | 2529.16 | 2316.48 | 2202 | 1950 | 1740 | 1915 ± 34 | 1732 (F.D.) | 1736 |
| Fe | 1536 (EQ.) | 2458.99 | 2233.87 | 2262 | 1945 | 1748 | 1961 ± 19 | 1787 (F.D.) | 1745 |
| Co | 1607 (EQ.) | 2405.28 | 2172.11 | 2354 | 1950 | 1772 | 1954 ± 46 | 1788 (F.D.) | 1772 |
| Ni | 1626 EQ.) | 2363.57 | 2131.18 | 2478 | 1965 | 1812 | 1990 ± 88 | 1820 (F.D.) | 1821 |
| Cu | 2330.91 | 2111.11 | 2634 | 1990 | 1868 | 1674 ± 101 | 1481 (F.D.) | 1880 |
Table 27.
Results for the parameter ζd
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ca | 18 ± 9 | 27.94 | 47.87 | 10 | 1 | 0 | 1 (FIX) | 0 (FIX) | 0 (FIX) |
| Sc | 58 ± 21 | 59.25 | 60.81 | 80 | 49 | 41 | 53 ± 26 | 34 ± 28 | 13 |
| Ti | 114 ± 29 | 97.59 | 90.04 | 150 | 103 | 90 | 99 ± 25 | 97 ± 24 | 73.5 |
| V | 141 ± 22 | 145.93 | 135.56 | 220 | 163 | 147 | 148 ± 34 | 172 ± 33 | 139 |
| Cr | 247 ± 24 | 206.17 | 197.37 | 290 | 229 | 212 | 235 ± 26 | 238 ± 25 | 209.5 |
| Mn | 321 ± 28 | 280.14 | 275.46 | 360 | 301 | 285 | 215 ± 41 | 228 ± 41 | 285 |
| Fe | 410 ± 23 | 369.69 | 369.85 | 430 | 379 | 366 | 367 ± 38 | 341 ± 23 | 365.5 |
| Co | 517 ± 17 | 476.79 | 480.52 | 500 | 463 | 455 | 447 ± 48 | 461 ± 45 | 451 |
| Ni | 603 ± 19 | 603.50 | 607.48 | 570 | 553 | 552 | 582 ± 52 | 580 ± 50 | 541.5 |
Table 28.
Results for the parameter
| EL | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Sc | 58 (EQ.) | 79.12 | 80.69 | 100 | 35 | 42 | 78 ± 42 | 79 ± 35 | 15 |
| Ti | 114(EQ.) | 121.83 | 116.21 | 180 | 102 | 99 | 108 ± 23 | 99 ± 22 | 88.5 |
| V | 141 (EQ.) | 174.62 | 168.01 | 260 | 175 | 164 | 149 ± 19 | 160 ± 20 | 167 |
| Cr | 247 (EQ.) | 239.97 | 236.11 | 340 | 254 | 237 | 296 ± 75 | 223 ± 52 | 250.5 |
| Mn | 328 (EQ.) | 319.65 | 320.49 | 420 | 339 | 318 | 368 ± 51 | 343 ± 55 | 339 |
| Fe | 410 (EQ.) | 415.55 | 421.16 | 500 | 430 | 407 | 446 ± 24 | 439 ± 30 | 432.5 |
| Co | 517 (EQ.) | 529.64 | 538.12 | 580 | 527 | 504 | 535 ± 21 | 541 ± 20 | 531 |
| Ni | 603 (EQ.) | 663.96 | 671.37 | 660 | 630 | 609 | 639 ± 22 | 640 ± 22 | 634.5 |
| Cu | 836 ± 3 | 820.74 | 820.91 | 740 | 739 | 722 | 860 ± 48 | 847 ± 42 | 743 |
Table 29.
Results for the parameter
| EL. | Previous results | Hartree· Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ti | 114 | 146.57 | 142.38 | 210 | 101 | 108 | 117 | 101 | 103.5 |
| V | 141 | 205.25 | 200.46 | 300 | 187 | 181 | 150 | 148 | 195 |
| Cr | 247 | 275.91 | 274.85 | 390 | 279 | 262 | 357 | 208 | 291.5 |
| Mn | 328 | 361.53 | 365.52 | 480 | 377 | 351 | 521 | 458 | 393 |
| Fe | 410 | 464.00 | 472.48 | 570 | 481 | 448 | 525 | 537 | 499.5 |
| Co | 517 | 585.31 | 595.72 | 660 | 591 | 553 | 623 | 621 | 611 |
| Ni | 603 | 727.55 | 735.26 | 750 | 707 | 666 | 696 | 700 | 727.5 |
| Cu | 836 (EQ.) | 892.91 | 891.09 | 840 | 829 | 787 | 950 | 912 | 849 |
| Zn | 1083.68 | 1063.20 | 930 | 957 | 916 | 975.5 |
Table 31.
Results for the parameter
| EL. | Previous results | Hartree-Fock | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|---|
| Ca | 89 (EQ.) | 63.40 | 77.59 | 100 | 244 | 333 | 277 (F.D.) | 295(F.D.) | 294 |
| Sc | 105 (EQ.) | 79.93 | 101.90 | 130 | 222 | 290 | 190 ± 55 | 185 ± 52 | 262 |
| Ti | 114 (EQ.) | 96.20 | 126.22 | 160 | 210 | 259 | 176 ± 59 | 192 ± 57 | 240 |
| V | 140 (EQ.) | 112.88 | 150.55 | 190 | 208 | 240 | 156 ± 57 | 137 ± 51 | 228 |
| Cr | 184 (EQ.) | 130.15 | 174.86 | 220 | 216 | 223 | 230 ± 49 | 268 ± 40 | 226 |
| Mn | 212 (EQ.) | 148.07 | 199.19 | 250 | 234 | 238 | 370 ± 52 | 377 ± 46 | 234 |
| Fe | 200 (EQ.) | 166.68 | 223.50 | 280 | 262 | 255 | 339 ± 56 | 278 ± 52 | 252 |
| Co | 236 (EQ.) | 185.90 | 247.82 | 310 | 300 | 284 | 270 ± 62 | 246 ± 61 | 280 |
| Ni | 255 (EQ.) | 205.76 | 272.15 | 340 | 348 | 325 | 324 ± 63 | 323 ± 62 | 318 |
| Cu | 375 (EQ.) | 226.17 | 296.46 | 370 | 406 | 378 | 408 ± 74 | 388 ± 68 | 366 |
| Zn | 247.11 | 320.79 | 400 | 474 | 443 | 424 |
Table 33.
Results for the parameter α = α′ = α″
| EL. | Previous results | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | Final ILS | Final GLS |
|---|---|---|---|---|---|---|---|---|
| Se | 50 (FIX) | 60 | 23 | 31 | 28 | 54 ± 9 | 28 (FIX) | 19 |
| Ti | 43 ± 4 | 60 | 29 | 33 | 30 | 19 ± 6 | 18 ± 5 | 22.5 |
| V | 54 ± 2 | 60 | 35 | 35 | 32 | 37 ± 6 | 24 ± 5 | 26 |
| Cr | 63 ± 1 | 60 | 41 | 37 | 34 | 37 ± 6 | 32 ± 4 | 29.5 |
| Mn | 73 ± 2 | 60 | 47 | 39 | 36 | 16 ± 6 | 15 ± 5 | 33 |
| Fe | 74 ± 2 | 60 | 53 | 41 | 38 | 40 ± 3 | 39 ± 3 | 36.5 |
| Co | 71 ± 3 | 60 | 59 | 43 | 40 | 39 ± 5 | 37 ± 5 | 40 |
| Ni | 83 ± 7 | 60 | 65 | 45 | 42 | 55 ± 7 | 52 ± 7 | 43.5 |
| Cu | 60 | 71 | 47 | 44 | 44 (FIX) | 47 |
Table 34.
Results for the parameter β = β′ = β″
| EL. | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | FINAL ILS | FINAL GLS |
|---|---|---|---|---|---|---|---|
| Sc | 0 | −250 | −20 | −308 | −20 (FIX) | − 308 (FIX) | −435 |
| Ti | 0 | −250 | −110 | −350 | −173 ± 76 | − 243 ± 69 | −458 |
| V | 0 | −250 | −200 | −392 | −507 ± 67 | −740 ± 68 | −481 |
| Cr | 0 | −250 | −290 | −434 | −506 ± 68 | −426 ± 62 | −504 |
| Mn | 0 | −250 | −380 | −476 | −634 ± 72 | −637 ± 68 | −527 |
| Fe | 0 | −250 | −470 | −518 | −470 (FIX) | −518 (FIX) | −550 |
| Co | 0 | −250 | −560 | −560 | −560 (FIX) | −560 (FIX) | −573 |
| Ni | 0 | −250 | −650 | −602 | −650 (FIX) | −602 (FIX) | −596 |
| Cu | 0 | −250 | −740 | −644 | −740 (FIX) | −644 (FIX) | −619 |
Table 35.
Results for the parameter T = T′ = T″
| EL. | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | FINAL ILS | FINAL GLS |
|---|---|---|---|---|---|---|---|
| Sc | 0 | −4.5 | −1.9 | −1.7 | −1.9 (FIX) | −1.7 (FIX) | −2.7 |
| Ti | 0 | −4.1 | −2.2 | −2.1 | −2.7 ± 0.8 | −2.6 ± 0.7 | −2.9 |
| V | 0 | −3.7 | −2.5 | −2.5 | −1.9 ± 0.6 | −2.7 ± 0.6 | −3.1 |
| Cr | 0 | −3.3 | −2.8 | −2.9 | −2.6 ± 0.6 | −3.2 ± 0.5 | −3.3 |
| Mn | 0 | −2.9 | −3.1 | −3.3 | −5.6 ± 0.9 | −5.6 ± 0.7 | −3.5 |
| Fe | 0 | −2.5 | −3.4 | −3.7 | −3.3 ± 0.4 | −3.1 ± 0.3 | −3.7 |
| Co | 0 | −2.1 | −3.7 | −4.1 | −4.0 ± 0.8 | −4.3 ± 0.6 | −3.9 |
| Ni | 0 | −1.7 | −4.0 | −4.5 | −4 (FIX) | −4.5 (FIX) | −4.1 |
| Cu | 0 | −1.3 | −4.3 | −4.9 | −4.3 (FIX) | −4.9 (FIX) | −4.3 |
Table 36.
Results for the parameter
| EL. | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | FINAL ILS | FINAL GLS |
|---|---|---|---|---|---|---|---|
| Sc | 0 | −1.8 | −1.4 | −2.8 | −1.4 (FIX) | −1.4 (FIX) | −2.6 |
| Ti | 0 | −2.1 | −1.7 | −2.8 | −1.7 (FIX) | −2.8 (FIX) | −2.6 |
| V | 0 | −2.4 | −2.0 | −2.8 | −2.0 (FIX) | −2.8 (FIX) | −2.6 |
| Cr | 0 | −2.7 | −2.3 | −2.8 | −2.3 (FIX) | −4.0 ± 0.8 | −2.6 |
| Mn | 0 | −3.0 | −2.6 | −2.8 | −2.6 (FIX) | −2.8 (FIX) | −2.6 |
| Fe | 0 | −3.3 | −2.9 | −2.8 | −2.9 (FIX) | −2.8 (FIX) | −2.6 |
| Co | 0 | −3.6 | −3.2 | −2.8 | −3.2 (FIX) | −6.0 ± 0.8 | −2.6 |
| Ni | 0 | −3.9 | −3.5 | −2.8 | −3.5 (FIX) | −2.8 (FIX) | −2.6 |
| Cu | 0 | −4.2 | −3.8 | −2.8 | −3.8 (FIX) | −2.8 (FIX) | −2.6 |
Table 37.
Results for the parameter
| EL. | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | FINAL ILS | FINAL GLS |
|---|---|---|---|---|---|---|---|
| Ca | 0 | −10 | −45 | −6 | −45 (FIX) | −6 (FIX) | −13 |
| Sc | 0 | −10 | −43 | −6 | −43 (FIX) | −46 ± 3 | −13 |
| Ti | 0 | −10 | −41 | −6 | −12 ± 4 | −11 ± 4 | −13 |
| V | 0 | −10 | −39 | −6 | −10 ± 3 | −13 ± 4 | −13 |
| Cr | 0 | −10 | −37 | −6 | −19 ± 4 | −6 (FIX) | −13 |
| Mn | 0 | −10 | −35 | −6 | −30 ± 5 | −14 ± 4 | −13 |
| Fe | 0 | −10 | −33 | −6 | −30 ± 4 | −30 ± 3 | −13 |
| Co | 0 | −10 | −31 | −6 | −19 ± 6 | −14 ± 6 | −13 |
| Ni | 0 | −10 | −29 | −6 | −42 ± 6 | −38 ± 6 | −13 |
| Cu | 0 | −10 | −27 | −6 | −27 (FIX) | −6 (FIX) | −13 |
| Zn | 0 | −10 | −25 | −6 | −13 |
Table 38.
Results for the parameter G 2
| EL. | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | FINAL ILS | FINAL GLS |
|---|---|---|---|---|---|---|---|
| Ca | 0 | 1 | 0 | 13 | 0 (FIX) | 9 | |
| Sc | 0 | 5 | 0 | 13 | 27 ± 9 | 14 ± 4 | 9 |
| Ti | 0 | 9 | 0 | 13 | 0 (FIX) | 0 (FIX) | 9 |
| V | 0 | 13 | 0 | 13 | 21 ± 6 | 11 ± 3 | 9 |
| Cr | 0 | 17 | 0 | 13 | 0 (FIX) | 4 ± 3 | 9 |
| Mn | 0 | 21 | 0 | 13 | 24+9 | 3 ± 3 | 9 |
| Fe | 0 | 25 | 0 | 13 | 30 ± 6 | 28 ± 4 | 9 |
| Co | 0 | 29 | 0 | 13 | 0 (FIX) | 5 ± 3 | 9 |
| Ni | 0 | 33 | 0 | 13 | 0 (FIX) | 9 ± 4 | 9 |
Table 39.
Results for the parameter
| EL. | DIAGON 1 | DIAGON 2 | DIAGON 3 | DIAGON 4 | ILS 3 | FINAL ILS | FINAL GLS |
|---|---|---|---|---|---|---|---|
| Sc | 0 | 5 | 15 | 13 | 27 (EQ.) | 14 (EQ.) | 9 |
| Ti | 0 | 9 | 15 | 13 | 15 (FIX) | 0 (FIX) | 9 |
| V | 0 | 13 | 15 | 13 | 21 (EQ.) | 11 (EQ.) | 9 |
| Cr | 0 | 17 | 15 | 13 | 15 (FIX) | 4 (EQ.) | 9 |
| Mn | 0 | 21 | 15 | 13 | 24 (EQ.) | 3 (EQ.) | 9 |
| Fe | 0 | 25 | 15 | 13 | 30 (EQ.) | 28 (EQ.) | 9 |
| Co | 0 | 29 | 15 | 13 | 15 (FIX) | 5 (EQ.) | 9 |
| Ni | 0 | 33 | 15 | 13 | 15 (FIX) | 9 (EQ.) | 9 |
| Cu | 0 | 37 | 15 | 13 | 15 (FIX) | 13 (FIX) | 9 |
Acknowledgments
This work was supported in part by the National Bureau of Standards, Washington, D.C.
The author wishes to acknowledge helpful comments and suggestions from E. Caspi, Z. Goldschmidt and Y. Shadmi of the Hebrew University, Jerusalem.
Footnotes
Figures in brackets indicate literature references at the end of this paper.
All tables and figures are placed at the end of this paper, beginning on page 54.
5. References
- [1].Racah G., and Shadmi Y., Bull. Res. Council Israel, 8F, No. 1, 15(1959). [Google Scholar]
- [2].Shadmi Y., Bull. Res. Council Israel, 10F, No. 3, 109(1962). [Google Scholar]
- [3].Roth C., J. Res. Nat. Bur. Std., 72A (Phys. and Chem.) No. 5, 505(1968). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [4].Roth C., J. Res. Nat. Bur. Std., 73A (Phys. and Chem.) No. 2, 125(1968). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [5].Roth C., J. Math. Phys. 9, 686(1968). [Google Scholar]
- [6].Roth C., J. Math. Phys. 9, 1832(1968). [Google Scholar]
- [7].Roth C., J. Math. Phys. 10, 1038(1969). [Google Scholar]
- [8].Roth C., J. Res. Nat. Bur. Stand., 75B(Math. Sci.) Nos. 1 & 2, 31 (Jan-Jun 1971). [Google Scholar]
- [9].Roth C., J. Res. Nat. Bur. Stand., 76B(Math. Sci.) Nos. 1 & 2, 61 (Jan-Jun 1972). [Google Scholar]
- [10].Roth C., J. Res. Nat. Bur. Stand., 73A(Phys. and Chem.) No. 5, 497 (Sep-Oct. 1969). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [11].Roth C., J. Res. Nat. Bur. Stand., 74A(Phys. and Chem.) No. 2, 141(Mar-Apr. 1970). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [12].Roth C., J. Res. Nat. Bur. Stand., 74A(Phys. and Chem.) No. 2, 157(Mar-Apr. 1970). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [13].Roth C., J. Res. Nat. Bur. Stand., 74A(Phys. and Chem.) No. 4, 507(Jul-Aug. 1970). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [14].Roth C., J. Res. Nat. Bur. Stand., 74A(Phys. and Chem.) No. 2, 181 (Mar-Apr. 1970). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [15].Roth C., J. Res. Nat. Bur. Stand., 74A(Phys. and Chem.) No. 5, 703 (Sep-Oct. 1970). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [16].Roth C., J. Res. Nat. Bur. Stand., 74A(Phys. and Chem.) No. 5, 715 (Sep-Oct. 1970). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [17].Roth C., Atomic Data and Nuclear Data Tables. (In press).
- [18].Bacher R.F., and Goudsmit S., Phys. Rev. 46, 948(1934). [Google Scholar]
- [19].Trees R.E., Phys. Rev. 83, 756(1951). [Google Scholar]
- [20].Trees R.E., Phys. Rev. 84, 1089(1951). [Google Scholar]
- [21].Racah G., Phys. Rev. 85, 381(1952). [Google Scholar]
- [22].Racah G., Phys. Rev. 63, 367(1943). [Google Scholar]
- [23].Rajnak K., and Wybourne B.G., Phys. Rev. 132, 280(1963). [Google Scholar]
- [24].Racah G., and Stein J., Phys. Rev. 156, 58(1967). [Google Scholar]
- [25].Trees R.E., Phys. Rev. 129, 1220(1963). [Google Scholar]
- [26].Shadmi Y., Phys. Rev. 139, A43(1965). [Google Scholar]
- [27].Roth C., Res J., Nat. Bur. Stand., 73A(Phys. and Chem.) No. 2, 159(1969). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [28].Shadmi Y., Oreg J., and Stein J., J. Opt. Soc. Am 58, 909(1968). [Google Scholar]
- [29].Shadmi Y., Caspi E., and Oreg J., J. Res. Nat. Bur. Stand., 73A(Phys. and Chem.) No. 2, 173(1969). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [30].Goldschmidt Z.B., and Starkand J., J. Phys. B, L141(1970). [Google Scholar]
- [31].Racah G., Phys. Rev. 62, 438(1942). [Google Scholar]
- [32].Condon E.U., and Shortley G.H., The Theory of Atomic Spectra (Cambridge University Press, 1935), referred to as TAS. [Google Scholar]
- [33].Rosenzweig N., Phys. Rev. 88, 580(1952). [Google Scholar]
- [34].Racah G., Bull. Res. Council Israel 3, 290(1954). [Google Scholar]
- [35].Moore C.E., Atomic Energy Levels NBS Circ. 467, 1(1949) ibid, II(1952). [Google Scholar]
- [36].Catalan M.A., Meggers W.F., and Garcia-Riquelme J. Res. Nat. Bur. Stands. (U.S.) 68A(Phys. and Chem.) No. 1, 9(1964). [DOI] [PMC free article] [PubMed] [Google Scholar]
- [37].Roth C. (To be published).
- [38].Martin W.C., and Sugar J., J. Opt. Soc. Am. 59, 1266(1969). [Google Scholar]
