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Journal of Research of the National Bureau of Standards logoLink to Journal of Research of the National Bureau of Standards
. 1981 Jan-Feb;86(1):33–77. doi: 10.6028/jres.086.003

The Configurations 3dn4p+3dn−14s4p+3dn−24s24p in the First Spectra of the Iron Group

Charles Roth 1
PMCID: PMC6756267  PMID: 34566038

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, [14].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, [59]. 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, [1016].

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, [1016]. Whenever the Hartree-Fock values were uniformly higher or lower than those of the previous results, [1016], 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

Δ=i=1nΔi2nm

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

δ=i=1nΔi2n

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, [1920], 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

2α(l1l2)+βq12

where q12 is the seniority operator, [22]. For the configuration dn this becomes

α[L(L+1)6n]+βQ

where

Q(n, v)=1/4(nv)(4 l+4nv)=1/4(nv)(12nv) (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, i<je2rij, then the matrix elements of the second-order perturbation produced by B on A are given approximately by

(Aψ|W2|Aψ)=1ΔEψ(Aψ|G|Bψ)(Bψ|G|Aψ), (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′ψgB′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 g˜, defined analogously to g. Then

(Aψ|W2|Aψ)=1ΔEBψ(Aψ|g|Bψ)(Bψ|g˜|Aψ), (3)

where the summation is over the complete set B′Ψ″. Thus,

(Aψ|W2|Aψ)=1ΔE(Aψ|g˜g|Aψ), (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

W2=g˜gΔE (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 n caused by the perturbation of n by n−1 ℓ′ configurations is given by

W2=kKP(kk;ll,ll)ϕ(kk;ll,ll) (6)

where

P(kk;lalb,lcld)=X(k;lalb,lcld)X(k;lalb,lcld)/ΔE, (7)

and

X(k;lalb,lcld)=(laC(k)lc)(lbC(k)ld)Rk(lalb,lcld), (8)

ΔE is the distance between the perturbing configuration and n,

ϕ(kk,ll,ll)=K(2k+1){kkklll}[U(k)×U(k)×U(k)](0)..+[δll/(2l+1)][(U(k)U(k))+(U(k)U(k))n/(2l+1)]. (9)

For the perturbation W2 of n by (4′+1)n+1 we similarly obtain

W2=kKP(kk;ll,ll)ϕ(kk;ll,ll), (10)

where

ϕ(kk;ll,ll)=K(1)(k+1)(2k+1){kkklll}[U(k)×U(k)×U(k)](0)[2δkk/(2k+1)](U(k)U(k)). (11)

The P are radial parameters; the ϕ and ϕ′ are their coefficient operators.

The matrix elements of n 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 [34] 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 [2830].

Now from (10) with k = k′ =2 here, we have W2=P(22;3d3d,3d3s)ϕ(22;dd,ds).

P(22;3d3d,3d3s)=X(2;22,20)2[R2(dd,ds)]2ΔE=(2C(2)2)2(2C(2)0)2[R2(dd,ds)]2ΔE=107[R2(dd,ds)]2ΔE Thus, W2=107[R2(dd,ds)]2ΔEϕ(22;dd,ds)=107(35)2H2ΔEϕ(22;dd,ds)=1750H2ΔEϕ(22;dd,ds),

where we used H=R2(dd,ds)35 according to Racah, [22]. However, in order to be consistant with the definition of

T=H2ΔE

used in a previous work by the author, [7], we get for the coefficient operator of T the expression

t=1750ϕ(22;dd,ds). (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

tx=1750ϕ(22;dd,dd), (13a)
ty=1750[ϕ(24;dd,dd)+ϕ(42;dd,dd)], (13b)
tx=1750ϕ(44;dd,dd). (13c)

In terms of the P, the parameters are given by

T=(1 / 1750) P(22;3d3d, 3d3s), (14a)
Tx=(1/1750)P(22;3d3d,3dnd), (14b)
Ty=(1/1750)P(24;3d3d,3dnd), (14c)
Tz=(1/1750)P(44;3d3d,3dnd). (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 n

First we define the tensor operators u(k), v(k), w(k), w˜(k), y(k), y˜(k), z(k) and z˜(k) as the tensor operators of order k whose only non-vanishing reduced matrix elements are

(nlu(k)nl)=1, (15a)
(nlv(k)nl)=1, (15b)
(nlw(k)nl)=(nlw˜(k)nl)=1, (15c)
(nly(k)|nl)=(nly˜(k)nl)=1, (15d)
(nlz(k)nl)=(nl|z˜(k)nl)=1. (15e)

Then in terms of the quantities P and X defined in (7) and (8), the curtailed operators g and g˜ representing the effective interactions of the configuration nℓ′, may be written as

g=k[X(k;ll,ll)ij(uj(k)wi(k))+X(k;ll,ll)ij(yi(k)z˜j(k))], (16)

and

g˜=k[X(k;ll,ll)ij(uj(k)·w˜i(k))+X(k;ll,ll)ij(y˜i(k)·zj(k))]. (17)

Upon substituting (16) and (17) into (5) we obtain after considerable manipulation

W2=WA+WB+WC, (18)

where

WA=kktP(kk;ll,ll)(2t+1){kktlll}ijs[ui(k)×(uj(k)×vs(t))](0), (19)
WB=kktP(kk;ll,ll)(2t+1){{kk,t}lll}{kktlll}ij(ui(t)vj(t)), (20)
Wc=kktQ(kk;ll,lll)(2t+l){kktlll}{ijs(1)k+k+t[ui(k)×([zj(k)×z˜s(t)](k)++[zj(t)× z˜s(k)](k))](0)+2ij{kktlll}(zi(t)z˜j(t))}, (21)
Q(kk;ll,ll)=X(k;ll,ll)X(k;ll,ll)ΔE. (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′ + 1. Hence a Hamiltonian Heff2, containing the two-body contribution to W2 may be written

Heff.2=iFtij(ui(t)vj(t))tGiij(zi(i)z˜j(i)). (23)

The two terms are referred to as the direct and exchange effective Slater parameters. The matrix elements of Heff.2 are diagonal in S and L, and are independent of J and M.

WA represents a three-body interaction if ij ≠ 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

Heff3=kkt(kkt)ijs[ui(k)×uj(k)×vs(t)](0)kkiV(kkt)ijs(1)k+k+t[ui(k)×{(zj(k)×z˜s(i))(k)+(zj(t)×z˜s(k))(k)}]. (24)

The coefficients of Ft in the configuration dpn are found by calculating the matrix elements

(dn(α1S1L1)pSLJM|ij(ui(t)vj(t))|dn(α1S1Li)pSLJM).

Since this involves the reduced matrix element (pv(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

(dn(α1S1L1)pSLJM|ij(zi(t)z˜j(i))|dn(α1S1Li)pSLJM)

is required. Due to the reduced matrix element (pz(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,

S=AA,S=AA.

B, B′, B″—linear combinations of the Slater parameters F2(dtd) and F4(d,d):

B=1441[9F2(dd)5F4(dd)]=F2(dd)5F4(dd),[31].

C, C′, C″—multiples of the Slater parameter F4(d,d):

C=563F4(dd)=35F4(dd),[31].

Gds—the parameter of the ds interaction in the configuration dn−1sp:

Gds=15G2(ds),[22].

F2, F2, F2parameters of the direct part of the d-p interaction:

F2=135F2(dp),[31].

G1, G1, G1—parameters of the exchange part of the d-p interaction:

G1=115G1(dp),[31].

G3, G1, G1—parameters of the exchange part of the d-p interaction:

G3=3245G3(dp),[31].

Gps—the parameter of the ps interaction in the configuration dn−1sp:

Gps=13G1(ps),[32].

H—the parameter of the dndn−1s interaction:

H=R2(dd,ds)35,[22].

H′—the parameter of the dn−1sdn−2s2 interaction, defined the same as H.

J—the parameter of the direct part of the dnpdn−1sp interaction:

J=R2(dp,sp)5,[33].

J′—the parameter of the direct part of the dn−1spdn−2s2p interaction, defined the same as J.

K—the parameter of the exchange part of the dnpdn−1sp interaction:

K=R1(dp,ps)3,[33].

K′— the parameter of the exchange part of the dn−1spdn−2s2p interaction, defined the same as K.

G*—the parameter of the dnpdn−2s2p interaction:

G*=R2(dd,ss)5,[22].

The spin-orbit contribution to the Hamiltonian has the form (p. 120, TAS, [32],)

iξ(ri)(lisi)

where ri is the distance of the i th electron from the nucleus,

ξ(ri)=12μ2c21r1U(ri)ri, where 

∪(ri) is the potential in which the i th electron moves and μ is the reduced mass of the electron. Then,

ζnl=20R2(nl)ξ(r)dr,

where R(nl)r is the radial part of the wave function. Then ζd, ζd, ζd—parameters of the spin-orbit interaction of the d-electrons. ζp, ζp, 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, Tx, Tx interactions of the core d-electrons.

F1, F1,F1—parameters of the direct part of the effective interactions.

G2, G2,G2—parameters of the exchange part of the effective interactions.

The calculated Lande g-factors given by

g=32+S(S+1)L(L+1)2J(J+1),[31]

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

D=M(dn1s)M(dn)

and

D=M(dn2s2)M(dn1s)

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

M(dp)=F0(dp)(G1+72G3). (25)

From equation (78) of Racah [31], the center of gravity of d2 is

M(d2)=A+79(C2B). (26)

Also, (p.197, TAS, [32],)

M(ds)=Fo(ds)Gds2, (27)
M(ps)=F0(ps)Fps2. (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

M(d2)=A+79(C2B)+323α. (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

M(d2)=A+79(C2B)+12α43α. (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 n(n1)2(19). 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,Tx and Tx 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

M(dnp)=A+7n(n1)18(C2B)n(G1+72G3)+2n3(10n)α+n(n1)18β+3536n(9n)(10n)T+nG2. (31)
M(dn1sp)=A+718(n1)(n2)(C2B)(n1)(G1+72G3)(n1)2Gds12Gps+23(n1)(11n)α+(n1)(n2)18β+3536(n1)(10n)(11n)T+(n1)G2. (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

M(dn1s2p)=A+718(n2)(n3)(C2B)(n2)(G1+72G3)23(n2)(12n)α+(n2)(n3)18β+3536(n2)(11n)(12n)T+(n2)G2. (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

M(d9p)=M(d9s2p)=F0+(G1+72G3),[32,p.200]

we obtain

M(d12np)=A+718(n2)(n3)(C2B)+(n2)(G1+72G3)+23(n2)(12n)α+(n2)(n3)18β+3536(12n)(n2)(n3)Tc+(12n)G2c. (34)
M(d11nsp)=A+718(n1)(n2)(C2B)+(n1)(G1+72G3)(n1)2Gds12Gps+23(n1)(11n)α+(n1)(n2)18β+3536(11n)(n1)(n2)TC+(11n)G2c. (35)
M(d102s2p)=A+718n(n1)(C2B)+n(G1+72G3)23n(10n)α+n(n1)18β+3536(10n)n(n1)TC+(10n)G2c. (36)

The checks of the algebraic matrices were described previously by the author, [8,9]. In section 5, [9], we had

t+tc+160Q+15L(L+1)80c=24040(n2)(n3). (37)

In analogy to the above result we obtain

14tx+14txc1280Q15L(L+1)60b+640c=320n21180n+k, (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, Tc, Tc, Tx, Tx, Tx, Txc, Txc and Txc 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

P=P0+P1(n6)+P2[(n6)210], (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, B0,B0 refer to the constant terms; B1, B1, B1 to the linear terms; B2, B2,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
D0 1610.69 860 ± 31 543 ± 108 773 ± 32 713 ± 67 795 ± 40 948 ± 37 585 ± 79 906 ± 38 974 ± 39
D0 28623.08 28482 ± 62 26086 ± 236 28746 ± 81 28674 ± 107 28350 ± 92 28682 ± 81 28723 ± 101 28665 ± 87 28527 ± 110
D1 3892.39 3641 ± 16 3550 ± 42 3673 ± 16 3614 ± 22 3661 ± 16 3688 ± 16 3487 ± 29 3703 ± 18 3709 ± 16
D1 5951.37 5719 ± 21 5278 ± 164 5711 ± 20 5898 ± 44 5738 ± 27 5738 ± 20 5832 ± 80 5731 ± 29 5740 ± 30
D2 0 −123 ± 4 −133 ± 5 −128 ± 5 −130 ± 5 −123 ± 5 −117 ± 5 −135 ± 9 −120 ± 5 −115 ± 5
D2 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
B0 853 863 ± 6 854 ± 7 849 ± 4 849 ± 4 852 ± 3 848 ± 3 840 ± 5 845 ± 4 848 ± 3
B0 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
B1 61 62 ± 2 59 ± 2 60 ± 2 57 ± 2 59 ± 2 61 ± 2 57 ± 2 61 ± 2 60 ± 2
B1 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
C0 3133 3255 ± 28 3258 ± 49 3319 ± 26 3325 ± 22 3306 ± 20 3338 ± 19 3361 ± 37 3340 ± 19 3332 ± 20
C0 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
C1 220 304 ± 7 317 ± 12 354 ± 7 353 ± 11 347 ± 9 351 ± 8 357 ± 11 351 ± 9 352 ± 9
C1 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)
(G3)1 −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
(G3)1 −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)
(G3)2 0.20 −1.4 −1.1 ± 0.3 0 −1.0 ± 0.3 −1.4 0 −1.1 0 0
(G3)2 −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
H0 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
H1 −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)
H2 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
J0 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
J1 −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
J2 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
K0 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
K1 − 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
K2 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
(F2)0 275.06 299 ± 4 292.5 ± 6 289 ± 4 288 ± 4 299 ± 3 299 ± 3 289 ± 4 301 ± 3 301 ± 3
(F2)0 345.01 398 410 402 403 417 410 397 413 415
(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
(F2)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
(F2)1 −1.71 2.3 0.6 −1.1 −13.1 −4.2 1.9 −13.2 −8.3 3.7
(F2)2=(F2)2=(F2)2 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
(G1)0 267.65 254 ± 5 265 ± 7 259 ± 3 271 ± 4 261 ± 4 260 ± 3 259 ± 4 258 ± 3 262 ± 3
(G1)0 281.09 303 289 293 305 293 287 285 287 294
(G1)1 −25.98 −5 ± 2 −17 ± 5 −19 ± 2 −15 ± 2 −17 ± 2 −19 ± 1 −17 ± 2 −16 ± 1 −18 ± 1
(G1)1 −15.07 −19 ± 2 −14 ± 2 −16 ± 2 −19 ± 1 −19 −17 ± 2 −16 −18
(G1)1 −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)
(G1)2 3.54 0 0.6 ± 0.7 0 1.2 ± 0.5 1.1 0 0 (FIX) 0 0
(G1)2 −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
(G3)0 18.96 32 ± 3 11 ± 3 10 11 ± 3 2.5 23 ± 1 11 ± 3 24 ± 2 24 ± 1
(G3)0 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
(ζd)0 401.94 421 ± 20 367 ± 19 369 ± 18 368 ± 15 370 ± 14 358 ± 16 363 ± 21 372 ± 17 368 ± 17
(ζd)0 446.92 482 397 407 384 401 394 372 418 404
(ζd)1 86.24 70 ± 12 73 ± 26 78 ± 10 81 ± 8 76 ± 8 84 ± 8 87 ± 11 82 ± 9 85 ± 9
(ζd)1 92.53 79 ± 11 96 ± 15 89 ± 6 90 ± 4 89 ± 5 87 ± 5 90 ± 6 91 ± 6 90 ± 6
(ζd)1 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
(ζd)2 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
(ζd)2 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
(ζp)0 199.19 252 ± 39 281 ± 39 284 ± 38 273 ± 29 279 ± 30 298 ± 30 280 ± 38 298 ± 32 305 ± 32
(ζp)0 309.34 314 435 439 423 455 454 437 459 485
(ζp)1 8.67 31 ± 11 37 ± 35 19 ± 10 20 ± 14 16 ± 9 11 ± 8 18 ± 16 9.5 ± 7.1 10 ± 7
(ζp)1 24.32 31 21 ± 20 23 ± 9 24 ± 11 23 ± 10 11 22 ± 14 19 ± 8 10
(ζp)1 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
(ζp)2 0 0 3.9 ± 3.2 5.0 2.4 ± 3.2 3.2 6.2 4.0 ± 4.2 4.0 4.6
(ζp)2 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
α0 60 47 48 ± 6 39 39 ± 3 42 36 35 ± 4 37 37
α0 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
α1 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
α1 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
β0 0 −253 −301 ± 138 −381 −365 ± 57 −321 −476 −507 ± 73 −476 −460
β0 0 −253 −355 −381 −431 −321 −476 −734 −476 −460
β1=β1=β1 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
T0 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
T0 0 −2.9 −1.2 −3.1 −4.5 −3.7 −3.3 −3.8 −3.2 −3.3
T1=T1=T1 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
(T2)0 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
(T2)0 0 −3.1 −1.7 −2.6 −1.1 −2.4 −2.8 −0.3 −2.6 −2.7
(T2)1=(T2)1=(T2)1 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
(F1)0 0 −12 −18 ± 3 −35 −33 ± 8 −18 −6.2 −27 ± 9 −8.1 −7.0
(F1)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
(F1)1 0 0 −7.6 ± 2.6 2.6 −9.1 ± 2.8 3.1 2 −12 ± 4 −5.0 −3.9
(F1)1 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
(G2)0 0 21 29 ± 9 −6.6 25.2 ± 4.8 23 ± 4 13 19 ± 6 3.2 5.9
(G2)0 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)
(G2)1 0 4.7 6.0 ± 2.0 0.8 −0.1 ± 2.2 2.0 0 −1.9 ± 1.8 1.3 0
(G2)1 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
M11 94502 92090 ± 183 91674 ± 310 92033 ± 191 92430 ± 239 91861 ± 164 92261 ± 120 92580 ± 118 92142 ± 128 92166 ± 127
M12 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

D=M(dn1sp)M(dnp)
D=M(dn2s2p)M(dn1sp),

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 1412 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
a

Based on 18 levels.

b

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
D0 963 ± 31 612 ± 105 920 ± 36 895 ± 38 929 ± 36 965 ± 32 968 ± 33 1007 ± 34 1039 ± 35 1041 ± ;37
D0 28770 ± 72 28599 ± 98 28689 ± 82 28745 ± 81 28683 ± 74 2873 ± 77 28739 ± 78 28784 ± 77 28704 ± 79 28703 ± 83
D1 3701 ± 15 3592 ± 46 3691 ± 17 3690 ± 17 3699 ± 17 3706 ± 17 3706 ± 16 3723 ± 17 3720 ± 19 3724 ± 19
D1 5784 ± 32 5818 ± 58 5736 ± 35 5754 ± 32 5748 ± 31 5791 ± 33 5794 ± 32 5814 ± 31 5813 ± 33 5822 ± 35
D2 −114 ± 4 −126 ± 10 −116 ± 5 −114 ± 5 −116 ± 5 −115 ± 5 −117 ± 5 ± 120 ± 5 −120 ± 6 −121 ± 6
D2 −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
B0 844 ± 3 839 ± 4 842 ± 3 841 ± 3 842 ± 3 844 ± 3 839 ± 3 843 ± 3 855 ± 3 855 ± 3
B0 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
B1 60 ± l 57 ± 2 60 ± 2 58 ± 2 59 ± 2 61 ± 2 55 ± 2 63 ± 1 63 ± 1 63 ± 1
B1 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
C0 3362 ± 16 3376 ± 26 3359 ± 23 3364 ± 23 3359 ± 21 3361 ± 18 3433 ± 17 3267 ± 12 3190 ± 10 3191 ± 9
C0 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
C1 348 ± 7 362 ± 13 358 ± 10 362 ± 10 358 ± 8 350 ± 8 362 ± 8 322 ± 7 319 ± 6 320 ± 6
C1 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
(F2)0 299 ± 3 293 ± 4 298 ± 3 290 ± 3 298 ± 3 299 ± 3 298 ± 3 298 ± 3 297 ± 4 297 ± 3
(F2)0 415 396 410 394 410 418 417 416 413 416
(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
(F2)1 2.5 −2.2 ± 2.0 2.5 2.0 2.1 2.3 22 2.3 2.5 2.4
(F2)1 2.5 −12.1 2.5 2.0 2.1 2.3 2.2 2.3 2.5 2.4
(F2)2=(F2)2=(F2)2 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
(G1)0 261 ± 3 260 ± 4 251 ± 3 259 ± 3 261 ± 3 256 ± 3 256 ± 3 256 ± 3 260 ± 3 256 ± 3
(G1)0 287 284 269 281 288 284 283 282 283 281
(G1)1 −19 ± 1 −17 ± 2 −19 ± 1 −18 ± 1 −17 ± 1 −19 ± 1 −18 ± 1 −18 ± 1 −19 ± 1 −19 ± 1
(G1)1 −19 −18 ± 2 −19 −18 −17 −19 −18 −18 −19 −19
(G1)1 −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)
(G1)2 0 0.7 0 0 0 0 0 0 0 0
(G1)2 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
(G3)0 21 ± 1 11.1 ± 2.6 22 ± 1 19 ± 2 22 ± 1 22 ± 1 22 ± 1 22 ± 1 20 ± 2 21 ± 1
(G3)0 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)
(G3)1 0 −3.5 ± 1.1 0 0 0 0 0 0 0 0
(G3)1 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)
(G3)2 0 −1.1 0 0 0 0 0 0 0 0
(G3)2 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
H0 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
H1 −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)
H2 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
J0 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
J1 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
J2 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
K0 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
K1 −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
K2 15 −5.6 ± 19 17 14 14 12 13 7.9 15 12
d)0 310 ± 19 343 ± 28 319 ± 25 327 ± 24 323 ± 18 311 ± 17 308 ± 18 315 ± 19 314 ± 20 315 ± 21
(ζd)0 364 ± 16 360 ± 19 355 ± 17 367 ± 17 359 ± 14 365 ± 15 367 ± 16 365 ± 17 366 ± 16 366 ± 19
(ζd)0 418 377 391 407 395 419 426 415 418 417
d)1 78 ± 5 82 ± 10 82 ± 9 84 ± 9 82 ± 6 77 ± 7 77 ± 8 78 ± 8 77 ± 9 76 ± 10
(ζd)1 91 ± 4 90 ± 5 87 ± 6 89 ± 5 87 ± 5 90 ± 6 91 ± 6 92 ± 6 92 ± 6 91 ± 6
(ζd)1 104 98 92 94 92 103 105 106 107 106
d)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
(ζd)2 2.6 1.8 ± 2.8 1.9 3.2 2.4 2.5 2.3 3.0 2.8 2.7
(ζd)2 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
(ζp)0 284 ± 19 278 ± 34 290 ± 34 279 ± 33 290 ± 19 269 ± 24 269 ± 21 269 ± 22 279 ± 25 164 ± 27
(ζp)0 425 417 431 423 430 401 398 403 428 405
(ζp)1 13 ± 5 17 ± 17 15 ± 8 13 ± 8 18 ± 6 14 ± 6 15 ± 5 16 ± 6 15 ± 7 16 ± 7
(ζp)1 13 19 ± 13 15 13 18 14 15 16 15 16
(ζp)1 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
(ζp)2 5.2 3.6 ± 3.8 5.6 5.3 5.6 5.3 5.5 5.4 5.4 5.5
(ζp)2 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
α0 33 32 ± 3 34 33 34 34 30 61 71 72
α0 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
α1 3.7 0.8 ± 2.0 1.6 0.7 1.5 3.1 2.9 6.8 7.1 6.9
α1 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)
β0 −527 −549 ± 65 −523 −534 −526 −521 −673 −336 0 0
β0 −527 −718 −523 −534 −526 −521 −673 −336 0 0
β1=β1=β1 −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)
T0 −3.5 −3.7 ± 0.4 −3.4 −3.5 −3.4 −3.5 −3.8 0 0 0
T0 −3.5 −4.8 −3.4 −3.5 −3.4 −3.5 −3.8 0 0 0
T1=T1=T1 −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)
(T2)0 −2.6 −2.0 ± 0.6 −2.6 −2.5 −2.6 −2.7 0 0 0 0
(T2)0 −2.6 −0.9 −2.6 −2.5 −2.6 −2.7 0 0 0 0
(T2)1=(T2)1=(T2)1 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)
(F1)0 −13 −26 ± 9 −8.6 −21 −11 0 0 0 −13 0
(F1)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)
(F1)1 0 −11 ± 4 0 −4.0 0 0 0 0 0 0
(F1)1 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)
(G2)0 9 19 ± 4 12 10 12 0 0 0 9 0
(G2)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)
(G2)1 0 −2.0 ± 2.9 0 0 0 0 0 0 0 0
(G2)1 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
M11 92641 ± 94 92492 ± 146 92289 ± 103 92306 ± 102 93322 ± 96 92668 ± 102 92631 ± 101 92697 ± 103 92640 ± 101 92664 ± 99
M12 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, [1016]. 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, F2,F2, G1, G1, G1, G3, G3, G3, Gps, Gds, G*, H, H′, J, J′, K, K′, ζd, ζd,ζd, ζp, ζp, and ζp as indicated in Tables 332. 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 ζp

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 140, and in the column INITIAL in table 42 for the general interpolation parameters.

Table 40.

Results for the parameter G2

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

B=976+84(n6) (40a)
B=1083+77(n6) (40b)
B=1190+70(n6). (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 35, 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

C=3558+310(n-6) (41a)
C=3980+280(n6) (41b)
C=4402+250(n6). (41c)

Again, the initial values for these parameters given in Tables 68, 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, F2, 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 (F2)2, respectively. When (F2)2 and (F2)2 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 911 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 F2

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, G1, and G1, 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 (G1)2 a value of 3.5 ± 0.6cm−1 the mean error was reduced to 21 cm−1. The initial values are given in tables 1214 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 G1

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 1517 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
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 G3

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 H1 were −11.5 ± 1.6cm−1 and −13.5 ± 1.2cm−1, respectively, whereas H2 and H2 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 J1 had to be different, as their values were −28 ± 8cm−1 and 14 ± 7 cm−1, respectively. However, J2 and J2 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 K2, 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 [14,27,28], 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, ζd, ζd were required to have a quadratic correction, whereas the parameters ζp, ζp, and ζp could, initially, be linear.

The values of (ζd)2 and (ζd)2 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,ζp, and ζp, demanding that they be in arithmetic progression, the value of (ζp)2 was −0.2 ± 0.3cm−1 and that of (ζp) was 0.3 ± 0.2cm−1. Thus, these parameters were fixed at zero, and initially ζp, ζp, and ζp 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 3032 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, Tx, Tx, F1,F1, F1, G2, G2, and G2 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, G1, G3, G3, Gps, K, K′, ζd, ζd, ζp, and ζp were allowed independent quadratic variations as functions of the atomic number.

The parameters F2, F2, Gds, G*, H, H′, J, and J′ were permitted a quadratic variation with the restrictions

(F2)2=(F2)2,(Gds)2=G2*,H2=H2,J2=J2.

The parameters B, B′, C, C′, α, α′, F1, F1, G2, and G2 were allowed to vary linearly.

The parameters β, β′, T, T′, Tx, and Tx varied linearly with the restrictions

β1=β1
T1=T1,
(Tx)1(Tx)1.

The remaining 13 places were reserved for the centers of gravity M0M12.

In the third iteration the restrictions

(Gds)2=G2*,
H2=H2,
J2=J2,

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

(G1)2=(G1)2 and (G3)2=(G3)2.

The initial parameters of the first variation are given in the column DIAGON 1, (tables 140), 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

D2=D2(F2)2=0(FIX)(G1)2=(G1)2=0(FIX)(G3)2=(G3)2G0*(Gds)0=708(F.D.)G1*=(Gds)1H0H0=34(F.D.)K2=K2(ζd)2=(ζd)2(ξp)1=(ζp)1(ξp)2=(ξp)2=0(FIX)α0=α0α1=α1β0=β0T0=T0(Tx)0=(Tx)0(F1)0=(F1)0(F1)1=(F1)1=0(FIX)(G2)0=(G2)0(G2)1=(G2)1,

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 G0*, J0,K0 were free, but in addition to the restriction of GLS 1, there were the conditions

Gi*=(Gds)1H1=H1J1=J1K1=K1

the parameters β0, T0, (G1)2, (Gps)2, 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(G2)0 free, the values of these parameters were

β1=29±37(F1)1=0.8±2.2(G2)0=36±7.

As (G2)0 had the value of 24 ± 8 it is clear that β1 and (F1)1 should be zero whereas

(G2)0=(G2)0.

In the second iteration when all 101 parameters are left free, GLS 2a, the G3, F1, and G2 parameters behave erratically, whereas H0,J1, K2, and (ζd)2 change sign. From these results and many other variations it became apparent that for the final variation in this iteration we should have

D2=D2(F2)2=0(FIX)(G1)2=(G1)2=0(FIX)(G3)0=(G3)0(G3)1=(G3)1(G3)2=(G3)2=0(FIX)G1*=(Gds)1H0H0=40(F.D.)H1=H1J1=J1K1=K1K2=K2(ζd)2=(ζd)2(ζp)2=(ζp)2α0=α0α1=α1β0=β0T0=T0(Tx)0=(Tx)0(F1)0=(F1)0(Ft)1=(F1)1(G2)1=(G2)1

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 i(Δi)2 from 1.14285 × 108 to 8.71367 × 107, and (Gps)2, from 0 to −33 ± 5 cm−1, and reduced i(Δi)2 from 5.97160 × 107 to 5.75448 × 107.

In the variation with parameters given in the column GLS 2b, the values of G1*, H1,J1,K1,T0, (G1)2, and (G3)2 are allowed to be free, whereas

G0*(Gds)0=708(F.D.)
J0J0=280(F.D.)
K0K0=1020(F.D.).

The results clearly show that G1* can’t vary independently. H1 and H1 are too far apart with H1 not well-defined, J1 and J1, as well as K1 and K1, have opposite signs, which is unacceptable. T0 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 D2D2, 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 G1*,Ht, J1,K1 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 G0*, G1*, G2*, H0, J0, J1 and J2 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:

D2=D2(F2)1=(F2)1(G1)1=(G1)1(G1)2=0(FIX)(G1)2=0(FIX)(G3)1=(G3)1=0(FIX)(G3)2=0(FIX)G1*=(Gds)1=10(FIX)G2*=(Gd2)2H0=84(FIX)H1=H1H2=H2=3(FIX)J1=J1J2=J2K1=K1K2=K2(ζp)1=(ξp)1(ζp)2=(ζp)2(ζd)2=(ζd)2α0=α0α1=α1β0=β0T0=T0(Tx)0=(Tx)0(Tx)1=0.3(FIX)(F1)0=(F1)0(F1)1=(F1)1=2(FIX)(G2)0=(G2)0(G2)1=(G2)1=0(FIX)

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, (ξp)1, (Tx)1, (F1)1, (G2)1 being free; G1*=(Gd)1, but not fixed at −10 cm−1; (G3)1=(G3)1, but not fixed at 0; H2=H2, 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 H0,K1 and (F1)1 being free; G1*=(Gds)1, but not forced at −10 cm−1. Although the mean error decreases to 194.5 cm−1, the parameters K1 and (F1)1 change sign, while the value of 51 ± 12 cm−1 is definitely too small for H0.

In a variation where J0 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 J1 would cause J′ to become negative for Cu I. Clearly, then J1 should equal J1 as in GLS 3.

In a variation where D2 was not equal D2 and (F1)0 not equal to (F1)0, the resulting values were

D2=117±5cm1D2=109±11cm1(F1)0=13±6cm1(F1)0=9±6cm1,

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 340.

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:

D2=D2(F2)1=(F2)1(G1)1=(G1)1(G1)2=0(FIX)(G3)1=(G3)1=0(FIX)(G3)2=0(FIX)G0*(Gds)0=231(F.D.)G1*=(Gds)1=0(FIX)G2*=(GdS)2H0=84(FIX)Ht=H1H2=H2=0(FIX)J1=J1J2=J2K1=K2K2=K2(ζp)1=(ζp)1(ζp)2=(ζp)2(ζd)2=(ζd)2α0=α0α1=α1β0=β0T0=T0(Tx)0=(Tx)0(Tx)1=0(FIX)(F1)0=(F1)0(F1)1=(F1)1=0(FIX)(G2)0=(G2)0(G2)1=(G2)1=0(FIX)

Hence in the final results the parameters D′, D″, Gps, Gds, G*, J, J′, K, K′, ζd, ζd, ζd, ζp, ζp, and ζp 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, Tx,Tx, F1, F1,F1, G2, G2, and 957263MC 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 J0 at 598 ± 271cm−1, J1 at −376 ± 127 cm−1, (F1)1t at −11 ± 4cm−1, (F1)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 G0* 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, G0* 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 G0*, H0, J1, and (F1)1 are left free. Although the mean error is reduced from 182.2cm−1 to 176.1cm−1 and the values for H0 of 1674 ± 81cm−1 and (F1)1 of −4 ± 2cm−1 are reasonable, the value for H0 of 42 ± 15 cm−1 is much too low, whereas the value for J1 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

  1. The level 3d24s(b2P)4py3S at 35439.43 cm−1.

  2. The three levels 3d3(a2G)4pt3F2,3,4 at 38451.29cm−1, 38544.38cm−1 and 38670.73cm−1.

  3. The level 3d3(a2G)4px1G at 38959.53cm−1.

  4. The level 3d3(a2P)4pw1D at 39265.80cm−1.

  5. The three levels 3d3(a2P)4pr3D at 40556.70cm−1, 40670.60cm−1, and 40844.19cm−1.

V

  1. The level 1° at 34019.12cm−1.

  2. The four levels of 3d4(a3G)4pt4F at 41389.49cm−1, 41428.93cm−1, 41492.29cm−1, and 41599.36cm−1.

Cr

  1. The level 3d44s(a2P)4px3S at 60084.09cm−1.

Mn

  1. The four levels 3d6(3G)4pw4H at 63395.45cm−1, 63444.61cm−1, 63457.85cm−1, and 63363.54cm−1.

Fe

  1. The five levels 3d44s(a4D)4px5H at 39625.829cm−1, 39969.880cm−1, 40231.365cm−1, 40404.544cm−1, and 40491.32cm−1.

Cu

  1. 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

(F1)0=(F1)0=(F1)0=0(FIX)
(G2)0=(G2)0=(G2)0=0(FIX)

are imposed. As a consequence, the parameters of the two-body effective interactions d − p: F1, F1, F1, G2, G2, and G2 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

(Tx)0=(Tx)0=(Tx)0=0(FIX)

was imposed. Hence the three-body effective interaction parameters of the d-electrons, Tx, Tx, and Tx 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

β0=β0=β0

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

T0=T0=T0=0(FIX)
T1=T1=T1=0(FIX)

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:

α0=α1=α0

increases from 30 ± 3cm−1 to 61 ± 2cm−1, whereas

β0=β0=β0

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

β0=β0=β0=0(FIX)
β1=β1 β1=0(FIX)

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.

α0=α0=α0

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, Tx, Tx, F1, F1, F1, G2,G2 and G2 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 340. 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 117 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.

Figure 1.

Plots of D′ versus atomic number.

Figure 17.

Figure 17.

Plots of T = T′ = T″ versus atomic number.

Since Tx, Tx, Tx, F1, F1, F1, G2, G2,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, F2,F2; G1, G1, G1; G3, G3, G3; ζd, ,ζd;; ζp, ζp, 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, F2, and F2, as they increase slowly in the GLS as functions of the atomic number, whereas in the Hartree-Fock computations they decrease.

Figure 2.

Figure 2.

Plots of D″ versus atomic number.

Figure 3.

Figure 3.

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

Figure 4.

Figure 4.

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

Figure 5.

Figure 5.

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

Figure 6.

Figure 6.

Plots of G1, Gt, and Gt versus atomic number.

Figure 7.

Figure 7.

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

Figure 8.

Figure 8.

Plots of Gps versus atomic number.

Figure 9.

Figure 9.

Plots of Gds and G* versus atomic number.

Figure 10.

Figure 10.

Plots of H and H′ versus atomic number.

Figure 11.

Figure 11.

Plots of J and J′ versus atomic number.

Figure 12.

Figure 12.

Plots of K and K′ versus atomic number.

Figure 13.

Figure 13.

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

Figure 14.

Figure 14.

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

Figure 15.

Figure 15.

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

Figure 16.

Figure 16.

Plots of β = β′ = β″ versus atomic number.

Table 10.

Results for the parameter F2

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 G3

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 ζd

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 ζd

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 ζp

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 Tx=Tx=Tx

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 F1=F1=F1

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 G2

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

1

Figures in brackets indicate literature references at the end of this paper.

2

All tables and figures are placed at the end of this paper, beginning on page 54.

5. References


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