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. 2025 Nov 26;21(23):12094–12109. doi: 10.1021/acs.jctc.5c01616

Multireference Equation-of-Motion-Driven Similarity Renormalization Group for X‑ray Photoelectron Spectra

Shuhang Li 1, Zijun Zhao 1, Francesco A Evangelista 1,*
PMCID: PMC12874376  PMID: 41296653

Abstract

We formulate and implement the core–valence separated multireference equation-of-motion-driven similarity renormalization group method (CVS-IP-EOM-DSRG) for simulating X-ray photoelectron spectra (XPS) of strongly correlated molecular systems. This method is numerically robust and computationally efficient, delivering accurate core-ionization energies with O(N 4) scaling relative to basis set size N in the EOM step. To ensure rigorous core intensivity, we propose a simple modification of the ground-state MR-DSRG formalism. We develop and compare three variants of the theory based on different approximations of the effective Hamiltonian: two derived from low-order perturbative methods (DSRG-MRPT2 and DSRG-MRPT3) and one from a nonperturbative scheme truncated to 1- and 2-body operators [MR-LDSRG(2)]. We benchmark the CVS-IP-EOM-DSRG methods by computing vertical core-ionization energies for a representative molecular test set and comparing the results against the established single-reference and multireference methods. To demonstrate the applicability of CVS-IP-EOM-DSRG to strongly correlated systems, we compute the potential energy curves and vibrationally resolved XPS of N2 and CO and the XPS of ozone. Comparison with experimental data and other high-level theoretical results shows that all three CVS-IP-EOM-DSRG variants accurately predict vertical ionization energies but only those based on the DSRG-MRPT3 and MR-LDSRG(2) levels of theory reliably capture the full dissociation behavior and reproduce the experimental vibrational structure.


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1. Introduction

Time-resolved X-ray photoelectron spectroscopy (TR-XPS) provides element- and site-specific access to ultrafast electronic dynamics. By tracking core-level ionizations, TR-XPS reports on oxidation state, local charge redistribution, and spin changes during photochemical and catalytic processes. Theory in support of experimental analysis must deliver core-ionization energies and reliable relative intensities along nonequilibrium geometries, often in the presence of strong static correlation and near-degeneracies.

Electronic-structure strategies for core ionization fall into two classes. The first consists of approaches that optimize orbitals and optional variational parameters for each core-ionized state. This category includes the delta-Hartree–Fock method, delta-density-functional-theory, delta-restricted-active-space self-consistent-field (ΔRASSCF), the static exchange (STEX) method, , nonorthogonal configuration interaction singles (NOCIS), and recently developed approaches based on the generalized-active-space self-consistent field (GASSCF) framework. These methods capture large core-hole relaxation but incur high cost when many states or geometries are needed; moreover, evaluation of transition properties is complicated by the lack of orthogonality of the underlying basis set. ,

A second category of methods includes response methods such as the equation-of-motion coupled-cluster theory (EOM-CC) ,− and the algebraic diagrammatic construction (ADC), which are particularly well suited for computing many excited states starting from a correlated ground state. This feature makes them very attractive for predicting pump–probe signals. However, methods in this second category lack explicit orbital relaxation; for core holes, this typically forces the inclusion of triples or transition-potential constructs that compromise ground-state accuracy. ,,, To obviate this limitation, Simons and Matthews proposed the transition potential CC (TP-CC) theory, which can accurately describe core-hole states at a purely singles and doubles level. , Moreover, EOM and ADC methods have been, for the most part, formulated on the assumption that a single mean-field state dominates the correlated ground state; such an assumption fails to capture the distinctive features of many open-shell systems and transient species, motivating multireference (MR) formulations such as MR-ADC for simulating various spectroscopic processes including XPS.

In this work, we build on a Hermitian MR equation-of-motion framework derived from the multireference-driven similarity renormalization group (DSRG), recently proposed and validated for valence ionization energies (IP-EOM-DSRG). A significant challenge in computing core-ionization energies is the fact that X-ray transitions lie deep within the spectrum, while conventional eigenvalue solvers focus mostly on extremal eigenvalues. Here, we extend IP-EOM-DSRG to core-ionized states using core–valence separation (CVS), , yielding the CVS-IP-EOM-DSRG approach. The CVS helps target core levels directly, avoiding the costly convergence of many lower-energy valence states and mixing with unphysical states in the continuum. ,,, We assess the CVS-IP-EOM-DSRG approach in combination with both perturbative and nonperturbative approximations to the DSRG transformed Hamiltonian and introduce a modified MR-DSRG scheme that enforces rigorous core intensivity.

The review is organized as follows. Section presents the IP-EOM-DSRG framework, the core-intensive extension of the MR-DSRG, and two CVS schemes. Section details the implementation, and Section reports benchmarks and numerical tests of this new approach. Finally, Section summarizes the findings of this work .

2. Theory

2.1. EOM-DSRG Formalism for Photoelectron Spectra

In this section, we briefly recapitulate the salient features of the IP-EOM-DSRG formalism. For detailed derivations, we refer the reader to our previous work. The IP-EOM-DSRG formalism is an equation-of-motion formulation built on the ground-state multireference DSRG theory. In DSRG, the ground state is modeled with a zeroth-order reference state (|Φ0⟩), chosen to be a complete- or generalized-active-space (CAS/GAS) wave function:

|Φ0=μ=1d|ϕμcμ 1

The set of determinants M={|ϕμ,μ=1,...,d} defines the model space, which accounts for the dominant electron configurations relevant to the description of the ground state for a set of molecular geometries, e.g., along a bond-breaking reaction path. The determinant coefficients c μ are normalized to one. The determinants are formed from a set of spin orbitals {ψp}p=1N that have been partitioned into core (C, indices m, n), active (A, indices u, v, w, x, y, z), and virtual (V, indices e, f) subsets of size N C , N A , and N V , respectively. We also introduce two composite orbital subsets: the hole spin orbitals (H = CA, indices i, j, k, l) and the particle spin orbitals (P = AV, indices a, b, c, and d). General spin orbitals (G) are designated as p, q, r, and s. We use the notation {ârs···pq···}={âpâq···âsâr} to represent creation ( â ) and annihilation â operator strings normal-ordered with respect to the correlated vacuum |Φ0⟩.

In the MR-DSRG, internally contracted excited configurations are decoupled from the reference |Φ0⟩ via a unitary transformation of the Hamiltonian:

Ĥ(s)=eÂ(s)ĤeÂ(s) 2

where (s) is the MR-DSRG similarity-transformed Hamiltonian, and Â(s)=(s)(s) is an anti-Hermitian combination of the cluster operator (s). The flow parameter s ∈ [0, ∞) that enters into the definition of (s) plays the role of a regularization parameter responsible for suppressing low-energy excited configurations that lead to numerical issues. Values of s > 0 suppress those excitations with energy denominators larger than the energy cutoff Λ = s –1/2. The amplitudes are determined by the regularized many-body condition:

[(s)]N=[eÂ(s)ĤeÂ(s)]N=(s) 3

where the superscript “N” indicates the nondiagonal (excitation rank changing) components of we seek to remove, and (s) is a regularizer that smoothly drives the original Hamiltonian to the one with no coupling between the reference and its excited configurations, i.e., lims[(s)]N=0 , when all energy denominators are nonzero. For clarity, in the following text, we omit the symbol “(s)” from all s-dependent quantities.

The EOM-DSRG approach defines the α-th excited state |Ψα⟩ as

|Ψα=α|Ψ0 4

where α is a state-transfer operator that delivers the α-th excited state wave function from the ground-state wave function |Ψ0=eÂ(s)|Φ0 . Excited states can be computed by variational minimization of an energy functional augmented with orthonormality constraints:

L=αNΨ0|αĤα|Ψ0αβNλαβ(Ψ0|βα|Ψ0δαβ) 5

Due to its formal advantages, we employ self-consistent excitation operators introduced by Mukherjee and co-workers, , which express α as a similarity-transformation of a bare excitation operator α :

αeÂαe 6

The bare excitation operator is expanded over a set of excitation operators ρ̂p , with corresponding amplitudes r α :

α=p=1neomrαpρ̂p 7

With this choice of α , the energy functional can be expressed in terms of the similarity-transformed Hamiltonian as

L=αNΦ0|αα|Φ0αβNλαβ(Φ0|βα|Φ0δαβ) 8

By requiring that all partial derivatives with respect to the excitation amplitudes r α (assumed to be real) and the Lagrange multipliers λαβ to be zero, we arrive at the following generalized eigenvalue problem:

q=1neomΦ0|ρ̂pρ̂q|Φ0rαq=Eαq=1neomΦ0|ρ̂pρ̂q|Φ0rαq 9

where E α is the excited-state energy. The excitation energy is then given by ωα = E αE 0, where E0=Φ0||Φ0 is the ground-state energy.

In this work, we truncate the IP-EOM-DSRG excitation operator to one-hole (1h) and two-hole-one-particle (2h1p) operators:

α=iHri{âi}+12ijHaPraij{âija} 10

The IP-EOM-DSRG formalism is compatible with any choice of the underlying MR-DSRG method. We investigate the performance of IP-EOM-DSRG-PT2, IP-EOM-DSRG-PT3, and IP-EOM-LDSRG(2), which are based on second- and third-order perturbative MR-DSRG methods (DSRG-MRPT2/3) , and an iterative MR-LDSRG(2) formalism.

2.2. Ensuring Rigorous Core Intensivity in IP-EOM-DSRG

A basic formal requirement for all excited-state theories is that excitation energies for localized excitations of a fragment A are unchanged in the presence of other fragments that do not interact with A (size intensivity). It is common to distinguish between full intensivity and core intensivity. The former requires the invariance of excitation energies when the additional noninteracting fragments increase the number of core, active, and virtual orbitals, while the latter only requires invariance with respect to the addition of noninteracting core and virtual orbitals, for a fixed set of active orbitals.

The conditions that guarantee full size intensivity of EOM excitation energies for multireference unitary coupled cluster theory have been discussed in ref . Since DSRG relies on the same transformation used in unitary coupled cluster theory, these formal results also find application in the case of EOM-DSRG. In particular, following Appendix B of ref , the necessary condition for full intensivity of IP-EOM-DSRG with up to 2h1p excitations is that matrix elements of between singly excited configurations ( {âia}|Φ0 ) and the reference (the projective residuals Sai ) are equal to zero, i.e.,

Sai=Φ0|{âai}|Φ0=0iHandaP 11

We can evaluate the residuals Sai using Wick’s theorem to obtain

Sai=jHbPγjiηabHbj12jHuxyAγjiλauxyHxyju+···16jHuvxyzAγjiλauvxyzxyzjuv+··· 12

All terms in eq are multiplied by nondiagonal components of , which are null for untruncated MR-DSRG theory in the limit of lims[(s)]N=0 . Therefore, in this case, Sai=0 , and size intensivity is guaranteed. For truncated theories at finite s values, the operator [(s)]N is not null, and consequently, the singles projective conditions Sai=0 are not satisfied, implying that size intensivity is violated. As shown in ref , full intensivity errors for IP-EOM-DSRG are small for valence ionization energies of realistic systems.

A possible solution to the size intensivity problem is modifying the ground-state formalism by directly enforcing the projective condition for singles ( Sai=0 ), with the remaining double excitation amplitudes solved using the regularized many-body approach (eq ). This approach would be similar to the pIC-MRCC formalism, except for retaining the Hermiticity of the transformed Hamiltonian and the presence of a source operator for double excitations (see eq ). One potential disadvantage is the potential for reintroducing numerical instabilities due to small energy denominators.

We propose an alternative approach that aims to rigorously satisfy the core intensivity of the ionization energies while retaining the numerical stability of the parent MR-DSRG theory. In most applications, it is paramount that this property is satisfied to guarantee that the ionization energies remain constant as the system of interest is studied in a variety of larger, weakly interacting environments that contribute only additional core and virtual orbitals. Core intensivity can be satisfied by imposing eq only onto the subset of equations that involve core and virtual orbitals, namely, Sem=0 , ∀mC, and eV. The structure of the core-virtual block Sem is also simple, since only the first term on the r.h.s. of eq survives. The remaining terms are zero because they contain contributions from blocks of that are contracted with null density cumulants (since m, eA, at least one index of the cumulants does not belong to the active orbital set). Consequently, the condition Sem=0 is satisfied if the one-body components em are null. To rigorously restore core intensivity in IP-EOM-DSRG, we solve for the condition em=0 for core-virtual singles and impose the MR-DSRG equations (eq ) using a finite s value for all other blocks. Note that one may equivalently view this approach as taking the s → ∞ limit of the single core-virtual block of the original MR-DSRG equations. This approach is expected to be intruder-free, as long as core and virtual orbitals are energetically well-separated, which is typically ensured by appropriate active space selection. In addition, this approach is anticipated to introduce only negligible changes to the ground-state energy. This aspect will be investigated numerically in Section .

2.3. IP-EOM-DSRG with Core–Valence Separation for X-ray Photoelectron Spectra

IP-EOM-DSRG theories can simulate electron ionization involving nonactive molecular orbitals, including core-ionized states. However, core-ionized states are numerically challenging to access, as they are deeply embedded in the autodetaching continuum. To address this issue, we adopt the core–valence separation (CVS) scheme, where the continuum is projected out and the core-ionized states are stabilized. We refer to this combination of methods as CVS-IP-EOM-DSRG. First proposed by Cederbaum et al., the CVS approximation was later used for simulating core-level excitation and ionization with a variety of electronic structure theories, including coupled-cluster theory, ,− single reference and multireference ADC theory, ,,,,− second-order excited-state perturbation theory, linear-response CASSCF, and linear-response density cumulant theory.

Figure shows the orbital spaces and definitions of the cluster operator and the EOM excitation operator used in the MR-DSRG and CVS-IP-EOM-DSRG schemes. In this work, we test two different CVS approaches that differ in the treatment of core orbitals in the ground-state MR-DSRG step. We distinguish (1) a CVS set I (indices M, N) that is used to restrict the EOM excitation operator and (2) a frozen set that is excluded from both the ground- and excited-state computations. In the full-CVS scheme, all electrons in I are correlated in the ground-state MR-DSRG. This is equivalent to the approach of Coriani and Koch. In the fc-CVS scheme, the ground-state MR-DSRG computation is performed by keeping the orbitals in I doubly occupied. This follows the idea of Cederbaum et al. and matches the approach of Vidal et al. In both schemes, the EOM operator is restricted to excitations involving at least one orbital from I. To target a specific element and shell, the EOM operator is restricted to a subset of CVS orbitals. For example, for CO2, we choose I = {C 1s, O1 1s, and O2 1s}. For the C K-edge spectrum, the EOM operator only excites from the C 1s-like orbital, while for the O K-edge, it excites from the two O 1s-like orbitals. This ensures that both edges are computed from the same ground-state reference wave function, while the EOM step targets only the desired edge.

1.

1

Orbital spaces and schematic definitions of the cluster operator (, left) and the EOM excitation operator ( , right) used in the MR-DSRG and CVS-IP-EOM-DSRG schemes. Curved arrows represent electron excitations, while wavy arrows denote electron ionizations. Crossed-out terms are excluded from the definition of an operator. Core orbitals probed in the ionization process are shown in green.

The intensity of a photoelectron transition to the α-th state with excitation energy ωα can be approximated using the spectroscopic factor S α, ,, which is given by

Sα=M|ΨαN1|âM|Ψ0N|2=M|Φ0|αM|Φ0|2 13

where M=eÂâMe is a similarity-transformed operator, and M runs over the targeted CVS orbitals. In the fc-CVS scheme, where  does not contain excitation operators involving CVS orbitals, âM and  commute, and this expression simplifies to

Sα=M|Φ0|αâM|Φ0|2 14

In the full-CVS scheme, eq serves as a zeroth-order approximation of the spectroscopic factor. In this work, we employ eq for both CVS schemes.

Comparing to the IP-EOM-DSRG formalism, major computational savings are achieved by neglecting excitations that include only active orbitals. In the scenario where N V > N C N A , the dominant computational cost of CVS-IP-EOM-DSRG scales as O(NINC2NV2) (quartic overall in basis size). This scaling arises from contracting the CVCV block of the similarity-transformed Hamiltonian with the operator âICV . Additionally, the cost associated with the active space scales as O(NINA8) , arising from the contraction between the AAAA block of the with the operator âIAA . For brevity, we will remove the “CVS-IP” prefix in the abbreviations of CVS-IP-EOM-DSRG theories henceforth.

3. Implementation

All EOM-DSRG computations are performed using NiuPy, an open-source Python library of multireference electronic structure theories for simulating excited states. The underlying CASSCF and MR-DSRG ground-state computations are carried out with a development version of the Forte quantum chemistry package. NiuPy serves as a general-purpose MR-EOM solver that is agnostic to the ground-state method, requiring only the effective Hamiltonian and reduced density matrices to solve eq . To speed up both the derivation and implementation of EOM-DSRG, we use a development version of the Wick&d software package, which generates working equations and executable code at runtime.

In our implementation, the generalized eigenvalue problem in eq is transformed into a standard eigenvalue problem, =E , where =S1/2S1/2 and =S1/2r . The matrix square root S 1/2 is computed efficiently by exploiting the block-diagonal structure of S. For each diagonal block, we apply a threshold ηd = 10–10 to eliminate linear dependencies, except for the block corresponding to spectator excitations, where operators âM and âMuv are known to exhibit strong linear dependence. For this block, we adopt the sequential orthogonalization procedure developed by Hanauer and Köhn, where âM operators are first orthogonalized and then projected out from the âMuv operator space. Subsequently, the âMuv operators are orthogonalized using a larger threshold of ηs = 10–5. This orthogonalization strategy has also been used in the implementation of MR-ADC. , The resulting eigenvalue problem is solved using a multiroot implementation of the Davidson algorithm, , which avoids the explicit storage of .

4. Results and Discussion

4.1. CVS-IP Scheme and Flow Parameter Choice

To calibrate the EOM-DSRG methods, we first examined the sensitivity of the vertical K-edge ionization energies with respect to the choice of the CVS scheme. For this purpose, in Table , we report eight ionization energies for HF, CO, N2, F2, and H2O computed using different levels of EOM-DSRG theory and the two CVS schemes. Results are benchmarked against highly accurate CVS-EOMIP-CCSDTQ reference data. All EOM-DSRG computations use s=0.5Eh2 and the core-intensive modification of the MR-DSRG formalism. To enable a direct comparison, our EOM-DSRG computations adopt the same geometries, basis sets, and exact two-component relativistic treatment as those in the CVS-EOMIP-CCSDTQ study. CVS-EOMIP-CCSDTQ calculations were carried out by using the full-CVS scheme. For each method, we summarize the error statistics by computing the mean absolute error (MAE) and standard deviation (STD).

1. K-Edge Ionization Energy Errors (in eV) for EOM-DSRG Methods [PT2 = DSRG-MRPT2, PT3 = DSRG-MRPT3, and LDSRG(2) = MR-LDSRG(2)] Computed Using Two CVS Schemes: Full-CVS (full) and Fc-CVS (fc) .

  CCSDTQ
PT2
PT3
LDSRG(2)
    fc full fc full fc full
HF 694.45 –1.21 0.19 0.41 1.86 –0.96 0.39
CO 296.30 0.14 1.93 –0.14 1.22 –0.16 1.21
CO 542.68 –1.24 1.93 –0.09 1.29 –0.45 0.91
N 2 (2Σ g ) 410.03 0.05 1.38 0.43 1.72 0.32 1.61
N 2 (2Σ u ) 409.95 0.03 1.37 0.41 1.70 0.30 1.59
F 2 (2Σ g ) 696.82 –1.00 0.42 1.73 3.08 0.98 2.31
F 2 (2Σ u ) 696.81 –1.01 0.43 1.72 3.08 0.97 2.31
H2O 539.99 –0.97 0.42 0.90 2.23 0.52 1.84
MAE 0.71 1.01 0.73 2.02 0.58 1.52
STD 0.61 0.72 0.73 0.73 0.68 0.67
a

All results are reported relative to the CVS-EOMIP-CCSDTQ (CCSDTQ) reference values taken from ref . The element symbols in bold indicate the atom from which the core electron is ionized. For homonuclear diatomics, we distinguish ionization from symmetric (g) and antisymmetric (u) linear combinations of the atomic 1s orbitals

As shown in Table , computations using the full-CVS scheme consistently overestimate the ionization energy for all truncation levels by more than 1 eV. Within the full-CVS scheme, the DSRG-MRPT2 level of theory yields the smallest MAE (1.01 eV), whereas MRPT3 and MR-LDSRG(2) give MAEs of 2.02 and 1.52 eV, respectively. This behavior is consistent with error cancellation: an incomplete treatment of dynamical electron correlation in DSRG-MRPT2 in the ground state likely offsets the missing explicit orbital relaxation in the EOM step. Higher-level ground-state treatments reduce that cancellation and expose the intrinsic bias of full CVS (to inflate excitation energies), which suppresses core–valence relaxation/screening. In contrast, the standard deviation is comparable across the methods, ranging from 0.73 eV for EOM-DSRG-PT3 to 0.67 eV for EOM-LDSRG(2).

Imposing the frozen-core approximation systematically reduces the ionization energy, leading to improved agreement with the CVS-EOMIP-CCSDTQ reference across all levels of theory, consistent with the error cancellation pointed out by Vidal et al. Under the fc-CVS scheme, the highest-level EOM-LDSRG(2) method yields the smallest MAE of 0.58 eV, while EOM-DSRG-PT2 and EOM-DSRG-PT3 yield MAEs of 0.71 and 0.73 eV, respectively. Notably, within the fc-CVS scheme, EOM-DSRG-PT2 and EOM-DSRG-PT3 exhibit large errors for F2, a notoriously challenging diatomic; however, these errors are reduced by EOM-LDSRG(2). This trend is consistent with our earlier observations, indicating that a higher-level treatment of dynamic correlation is needed for this system. Due to the lower statistical errors of the fc-CVS for this benchmark set, all subsequent EOM-DSRG computations employ this scheme.

Another aspect that we examine is the sensitivity of the ionization energy and spectroscopic factor to the DSRG flow parameter s. As an example, in Table , we report the carbon K-edge ionization energy and spectroscopic factor of CO, computed using various levels of EOM-DSRG theory with s values ranging from 0.25 to 4 E h , employing the cc-pCVTZ-DK basis set and the 1e-sf-X2C relativistic correction. Across all levels of theory, the ionization energy and spectroscopic factor exhibit weak dependence on s until it reaches a relatively large value ( s=2.0Eh2 ), beyond which the MR-LDSRG(2) ground-state amplitude equations fail to converge. An analysis of the double substitution amplitudes involving both α and β electrons at large s values shows amplitudes as large as 0.6, indicating the presence of intruder states, while for s1.0Eh2 , all amplitudes are less than 0.1. Within the recommended range of s[0.5,1.0]Eh2 , the EOM-DSRG ionization energy remains nearly constant at the MR-LDSRG(2) level, varying by only 0.02 eV. At the DSRG-MRPT2 and DSRG-MRPT3 levels, the ionization energy shows weak dependence, with maximum variations of 0.09 and 0.08 eV, respectively. Based on these findings and prior studies that suggest an optimal s value in the range [0.5, 1.0] E h , ,− we adopt the value s=0.5Eh2 for all subsequent EOM-DSRG computations.

2. Carbon K-Edge Core-Ionization Energy (ω, in eV) and Spectroscopic Factor (S) of CO Computed with Various Levels of EOM-DSRG Theory [PT2 = DSRG-MRPT2, PT3 = DSRG-MRPT3, and LDSRG(2) = MR-LDSRG(2)] Using Different Flow Parameter Values (s, in E h ).

s
PT2
PT3
LDSRG(2)
  ω S ω S ω S
0.25 296.08 1.5477 296.02 1.5522 296.04 1.5564
0.50 296.11 1.5421 296.16 1.5522 296.14 1.5547
1.00 296.02 1.5348 296.24 1.5574 296.12 1.5531
2.00 295.89 1.5256 296.27 1.5607
4.00 295.62 1.5097 296.27 1.5496
a

MR-LDSRG­(2) computation on the ground state fails to converge.

4.2. Size Intensivity

In this section, we carefully examine the core intensivity and quantify the size-intensity error of EOM-DSRG. As discussed in Section , although the EOM-DSRG formalism is not size-intensive, rigorous core intensivity can be achieved by solving a set of modified MR-DSRG equations. To begin, we discuss the impact of the core-intensive modification of the MR-DSRG on the ground-state energy. For this purpose, we consider the CO molecule along the dissociation path. To properly describe the atomic asymptotic limit, we include all 2p orbitals of C and O in the active space while including all 2s orbitals in the core space. This setup is designed to artificially increase the magnitude of one-body core-virtual components em .

In Table , we compare results from the original MR-DSRG framework with those from the modified MR-DSRG equations where we set em=0 . As shown in Table , the core-intensive formulation of MR-DSRG has a negligible effect on the MR-DSRG ground-state energy. The largest deviation, observed in the MR-LDSRG(2) calculation at the 4.0 Å geometry, is approximately 7.0 × 10–5 E h. The impact on the core-ionization energy is also small, with the largest deviation being about 0.037 eV, occurring at the 1.0 Å geometry in the MR-LDSRG(2) calculation.

3. Ground-State MR-DSRG Energy (E DSRG, in E h) and Core-Ionization Energy (CVS-IP, in eV) for CO at Each Geometry Computed Using EOM-DSRG Methods [PT2 = DSRG-MRPT2, PT3 = DSRG-MRPT3, and LDSRG(2) = MR-LDSRG(2)] .

geometry (Å)
PT2
PT3
LDSRG(2)
  original core-intensive original core-intensive original core-intensive
E DSRG (E h)
1.0 –113.136378 –113.136378 –113.157834 –113.157836 –113.169934 –113.170001
2.0 –112.893327 –112.893329 –112.901037 –112.901056 –112.907672 –112.907739
3.0 –112.840977 –112.840977 –112.828473 –112.828499 –112.832786 –112.832832
4.0 –112.801600 –112.801600 –112.810382 –112.810382 –112.816276 –112.816346
5.0 –112.807485 –112.807485 –112.814293 –112.814293 –112.817197 –112.817201
CVS-IP (eV)
1.0 295.937 295.963 295.629 295.618 295.675 295.637
2.0 298.864 298.878 298.597 298.585 298.522 298.492
3.0 298.571 298.598 297.951 297.945 298.061 298.028
4.0 297.560 297.588 297.368 297.362 297.340 297.305
5.0 297.390 297.390 297.238 297.238 297.235 297.235
a

Results for the original theory (“original”) and a modified ground-state MR-DSRG aproach that solves for the condition em=0 and ensures core intensivity of the ionization energies (“core-intensive”). All results use a value of s=0.5Eh2 .

We then test core intensivity numerically. We compute the vertical core and valence ionization energies of HF at the equilibrium (r e) and stretched (2r e) geometries using EOM-DSRG-PT3, in the presence of an increasing number of noninteracting helium atoms. We use the cc-pCVTZ-DK basis and a scalar 1e-sf-X2C relativistic treatment, the same computational strategy that will be used for benchmarking our methods in Section . The active space contains 6 electrons and 5 active orbitals (H 1s, F 2s/2p orbitals). In all our numerical tests, the core-intensivity error is within the convergence threshold used to converge the EOM-DSRG excitation energies (<10–9 eV), confirming that the EOM-DSRG formalism is core intensive.

We also examine the full-intensity error by computing the vertical core-ionization energies of the HF + HF composite system. The active space for the composite system contains 12 electrons and 10 orbitals, which is double the size of the single HF subsystem. The full-intensivity error of EOM-DSRG-PT3 is 15.7 meV at the equilibrium geometry and 6.3 meV at the stretched geometry, both at least 1 order of magnitude smaller than the intrinsic error of the method, as will be shown in Section .

To conclude this section, we discuss the core intensities of the fc-CVS scheme. In the fc-CVS scheme, cluster amplitudes involving CVS orbitals are set to zero in the ground-state calculation, so eq is not fulfilled for residuals involving these orbitals. In typical calculations, the core orbitals of the environment should be excluded from both the ground- and excited-state computations by including them in the frozen set. In this case, the environment only contributes core and virtual orbitals, so eq is still strictly satisfied for core-virtual residuals and core-intensivity is preserved. We illustrate this with the HF + Ne composite system. When we include the F 1s orbital in the CVS set and the Ne 1s orbital in the frozen set, the resulting core-intensivity error for the F K-edge ionization is less than 10–9 eV, confirming that EOM-DSRG remains core-intensive. However, if core orbitals from the environment were included in I, eq would not be satisfied and core intensivity would be violated. In this case, for the HF + Ne system, the core-intensivity error is 7.41 × 10–3 meV, which is still much smaller than the full-intensivity error.

4.3. Vertical Ionization Energies

In this section, we benchmark the accuracy of the EOM-DSRG methods using a set of 16 medium-sized molecules previously studied by Liu et al. We use the same geometries, with diatomic molecules taken from experiment and polyatomic molecules optimized at the SFX2C-1e-CCSD­(T)/cc-pCVQZ level of theory. We benchmark the EOM-DSRG methods against various levels of state-specific and state-averaged GAS-DSRG theory, as well as SR-ADC, MR-ADC, and CVS-EOM-CCSDT. All EOM-DSRG computations employ the cc-pCVTZ-DK basis set and a scalar 1e-sf-X2C relativistic treatment, consistent with the GAS-DSRG study. Reference data for SR-ADC and MR-ADC are taken from the work by de Moura and Sokolov, while CVS-EOM-CCSDT results are from Liu et al. In those studies, the cc-pCVTZ basis set was used for nonrelativistic computations, and the recontracted cc-pCVTZ-X2C basis set was employed when scalar relativistic effects were included. The detailed choice of active spaces and the raw data used in this section are listed in the Supporting Information. We assess the accuracy of each method by calculating errors with respect to the experimental values. We note that the experimental ionization energies used for comparison are taken from studies that lack the resolution to resolve vibrational levels and therefore approximately correspond to vertical ionization energies.

In Figure , we present the error distributions and statistics for a range of methods, including SR-ADC, MR-ADC, EOM-DSRG, GAS-DSRG, and CVS-EOM-CCSDT. All EOM-DSRG methods show good agreement with experiment, with MAEs below 0.8 eV and STDs below 0.9 eV. Among them, EOM-DSRG-PT3 and EOM-LDSRG(2) exhibit nearly identical accuracy, with MAEs of 0.52 and 0.51 eV and STDs of 0.49 and 0.52 eV, respectively. Compared to MR-ADC methods, which are based on a similar multideterminantal many-body expansion, EOM-DSRG approaches significantly outperform the strict second-order MR-ADC(2) (MAE = 2.31 eV, STD = 0.70 eV) and offer accuracy comparable to the extended MR-ADC(2)-X (MAE = 0.41 eV, STD = 0.52 eV). The maximum absolute error (MAX) of each EOM-DSRG method is also comparable to that of MR-ADC(2)-X (all below 2 eV) and significantly smaller than that of MR-ADC(2), which reaches 3.54 eV. As expected, EOM-DSRG-PT2 yields larger errors (MAE = 0.74 eV, STD = 0.90 eV) compared to its higher-level counterparts.

2.

2

Violin plots of the errors in vertical core-ionization energies for a test set of 16 molecules, computed using various electronic structure methods and referenced against experimental values.

When compared to SR-ADC methods, EOM-DSRG theories are generally more accurate. Notably, the performance of single-reference methods improves substantially upon inclusion of 3h2p-type excitations, as evidenced by the CVS-EOM-CCSDT method, which achieves a MAE of just 0.14 eV. However, this comes at the cost of increased computational scaling of O(NINC2NV4) . These findings suggest that for molecules at equilibrium geometries, the improvements in core-ionization energies are mostly brought by the higher-level description of the dynamical correlation. Finally, GAS-DSRG methods are more accurate than SR-ADC, MR-ADC, and EOM-DSRG theories, and their accuracy is similar to that of CVS-EOM-CCSDT. This improved performance is primarily attributed to the explicit orbital optimization of the core-ionized state.

Overall, our benchmark results demonstrate that EOM-DSRG methods accurately predict K-edge core-ionization energies across the test set with the performance trend approximately following EOM-LDSRG(2) ≈ EOM-DSRG-PT3 > EOM-DSRG-PT2. In particular, the DSRG-MRPT3 level of theory offers a good balance between accuracy and computational efficiency, making it a reliable choice for modeling core-ionized states.

4.4. Potential Energy Curves and Vibrationally Resolved X-ray Photoelectron Spectra

After benchmarking the EOM-DSRG methods on vertical core-ionization energies, we focus on applications that require a multireference treatment to accurately model ground- and core-ionized states far from the equilibrium geometry. To this end, we extend our core ionization computations to full potential energy curves of diatomics and simulate the corresponding vibrationally resolved XPS, comparing theoretical results with experimental data. We focus on the bond dissociation curves of N2 and CO, comparing our results against MR-ADC(2)-X and state-specific GAS-DSRG. For N2, we use reference data computed at the MR-LDSRG(2) truncation level, while for CO, we employ the DSRG-MRPT3 level due to the lack of convergence of the GAS-LDSRG(2) procedure. Both GAS-DSRG-PT3 and GAS-LDSRG(2) incorporate dynamical correlation effects beyond second-order perturbation theory in a state-specific manner. Previous benchmarks have shown that GAS-DSRG-PT3 and GAS-LDSRG(2) provide highly accurate core-ionization energies across various sizes of molecules, with MAEs of about 0.3 eV compared to experiment, while also yielding reliable potential energy surfaces. GAS-DSRG has also been adopted as a benchmark reference in a previous MR-ADC study. MR-ADC(2)-X computations are performed using the Prism software package, while GAS-DSRG computations are carried out with the Forte software package. All computations employed the cc-pCVTZ-DK basis set and the 1e-sf-X2C relativistic treatment.

Figure shows potential energy curves (PECs) for the ground- and core-ionized states of N2 (N K-edge) and CO (C and O K-edge) computed using different methods. All EOM-DSRG methods follow the reference GAS-LDSRG(2) curve for N2 at short bond distances [r(N–N) ≤ 1.3 Å], with deviations consistently within 0.50 eV, indicating accurate descriptions near equilibrium. In contrast, MR-ADC(2)-X deviates the most in this region, underestimating the vertical ionization energy by 1.18 eV relative to that of the GAS-LDSRG(2) result. As the bond is stretched, all methods continue to yield the qualitatively correct PECs. EOM-DSRG curves remain nearly indistinguishable, whereas the MR-ADC(2)-X curve runs almost parallel but lies consistently lower in energy. In the strongly correlated dissociation limit, the EOM-DSRG methods and MR-ADC(2)-X overestimate the ionization energy. This is because GAS-LDSRG(2) includes double excitations in the (N–1) electron Hilbert space, effectively capturing 3h2p-type correlation effects that are important for accurately describing core-ionized states.

3.

3

Potential energy curves for the ground and K-edge core-ionized states of N2 (left) and CO (right) computed using various levels of EOM-DSRG, GAS-DSRG, and MR-ADC(2)-X. All energies shown in the plots are vertical ionization energies in units of eV. For N2, the2Σu core-ionized state is shown; for CO, both C 1s and O 1s core-ionized states are included. All curves are shifted such that the energy minima of the GAS-DSRG curves in all panels are set to zero. Additionally, all methods except GAS-DSRG are further shifted so that their ground-state energy minima align with the minimum of GAS-DSRG.

For the CO system, the EOM-DSRG methods show good agreement with the GAS-DSRG-PT3 reference for the C 1s core-ionized state near the equilibrium geometry [r(C–O) ≤ 1.5 Å]. However, EOM-DSRG-PT2 significantly underestimates the ionization energy of the O 1s by 1.44 eV. EOM-DSRG-PT3 and EOM-LDSRG(2) yield nearly identical results across all states and consistently overestimate the ionization energy in the stretched-bond regime. MR-ADC(2)-X exhibits pronounced discontinuities in both the C and the O K-edge core-ionized PECs. This issue is a known limitation of internally contracted methods that involve amplitude truncation, though it is less pronounced in EOM-DSRG methods for the CO system.

To further explore the accuracy of the EOM-DSRG PECs, we compute vibrational constants for all computed core-ionized PECs in Table , obtained by fitting the PECs to Morse potentials. For the N2 system, all methods reproduce the experimentally observed bond-length contraction upon core ionization with reasonable accuracy. GAS-LDSRG(2) achieves the best agreement, with differences in bond lengths (Δr e ) deviating by less than 0.001 Å from the experiment. EOM-DSRG-PT2 shows the largest deviations, with Δr e differing from experiment by −0.0110 Å and −0.0127 Å for the 2Σ u and 2Σ g states, respectively. GAS-LDSRG(2) performs well also for vibrational frequencies, deviating by less than 5 cm–1 from the experiment. EOM-DSRG-PT2 and MR-ADC(2)-X exhibit larger errors (approximately 160 cm–1), while EOM-DSRG-PT3 and EOM-LDSRG(2) reduce the error to below 100 cm–1.

4. Vibrational Constants for K-Edge Core-Ionized States of N2 and CO Computed Using Various EOM-DSRG Methods [PT2 = DSRG-MRPT2, PT3 = DSRG-MRPT3, and LDSRG(2) = MR-LDSRG(2)], as Well as GAS-DSRG [MR-LDSRG(2) for N2 and DSRG-MRPT3 for CO+] and MR-ADC(2)-X .

parameters GAS-DSRG PT2 PT3 LDSRG(2) MR-ADC(2)-X exp
N2, N K-edge (2Σ u )
Δr e (Å) –0.0229 –0.0350 –0.0294 –0.0298 –0.0286 –0.0240
ω e (cm–1) 2410 2581 2510 2508 2571 2407
ω e χ e (cm–1) 20 17 19 18 21
N2, N K-edge (2Σ g )
Δr e (Å) –0.0191 –0.0313 –0.0256 –0.0261 –0.0254 –0.0186
ω e (cm–1) 2411 2582 2509 2507 2568 2414
ω e χ e (cm–1) 21 18 20 19 22
CO, C K-edge
Δr e (Å) –0.0464 –0.0728 –0.0541 –0.0546 –0.0600 –0.0514
ω e (cm–1) 2427 2611 2540 2554 2658 2479
ω e χ e (cm–1) 23 22 20 20 25 23
CO, O K-edge
Δr e (Å) 0.0307 –0.0332 0.0342 0.0337 0.0589 0.0370
ω e (cm–1) 1868 2210 1874 1885 1548 1864
ω e χ e (cm–1) 9 16 8 8 43 7
a

Difference in equilibrium bond-length between the core-ionized and ground state (Δr e ), vibrational frequency (ω e ), and anharmonic constant (ω e χ e ). Reference experimental values taken from refs and .

For the CO system, all methods correctly predict bond-length contraction upon C 1s core ionization. EOM-DSRG-PT2 again shows the largest deviation, overestimating the contraction by 0.0214 Å. For the O 1s core-ionized state, EOM-DSRG-PT2 fails to capture the correct trend: while the experiment shows a bond-length increase of 0.0370 Å, it instead predicts a contraction of 0.0332 Å. The other methods correctly predict bond elongation, but MR-ADC(2)-X significantly overestimates the magnitude, predicting an increase of 0.0589 Å, which is more than 1.5 times the experimental value.

Lastly, we use the computed PECs to evaluate the vibrational levels of the core-ionized states and Franck–Condon factors. The vibrational eigenvalues and eigenstates are obtained using the discrete variable representation (DVR) method, , with the potential energy values at each grid point evaluated through cubic spline interpolation. Figure presents both experimental and theoretical spectra for both N2 and CO. To enable direct comparison, energy shifts are applied to align the simulated spectra with the first experimental peak. These shifts reflect the errors in the zero-point-corrected adiabatic transition energies. For the N2 system, all methods successfully reproduce the vibrational structure observed in the experiment. Among these methods, EOM-DSRG-PT2 requires the smallest energy shift (−0.12 eV), likely due to fortuitous error cancellation. GAS-LDSRG(2) requires a shift of −0.23 eV, while EOM-DSRG-PT3 and EOM-LDSRG(2) require slightly larger shifts of −0.51 and −0.40 eV, respectively. For CO, the GAS-DSRG-PT3, EOM-DSRG-PT3, and EOM-LDSRG(2) methods accurately capture the vibrational structure for both the C and the O core-ionized states. In contrast, EOM-DSRG-PT2 fails to predict the correct relative intensities for the C 1s spectrum and MR-ADC(2)-X fails for both C 1s and O 1s spectra. Among all tested methods, EOM-DSRG-PT3 exhibits the best agreement with experiment for both C 1s and O 1s ionized states and performs comparably to EOM-LDSRG(2).

4.

4

Vibrationally resolved X-ray photoelectron spectra (XPS) of (a) N2 N 1s, (b) CO C 1s, and (c) CO O 1s, simulated using various levels of EOM-DSRG theory, GAS-DSRG, and MR-ADC(2)-X. The experimental spectrum of N2 is adapted with permission from ref . Copyright 2009 Springer Nature. The experimental spectra of CO are adapted with permission from ref . Copyright 2006 Elsevier. For best comparison, all theoretical spectra are aligned to experiment by applying energy shifts, which are indicated in each panel. The Cohen–Fano interference effect is not included in the N2 simulations.

4.5. X-ray Photoelectron Spectrum of Ozone

Our last application of the EOM-DSRG methods focuses on the more challenging problem of the ozone molecule (O3). In its ground state, the wave function of ozone is dominated by a closed-shell configuration featuring a doubly occupied 1a 2 orbital and a smaller contribution from the doubly excited determinant (1a2)2(2b1)2 . The experimental XPS of ozone features two peaks that correspond to K-edge core ionization of the terminal O atoms (OT, resulting from the 2a 1 and 1b 2 orbitals, found at 541.5 eV) and the central atom (OC, 1a 1 orbital, found at 546.2 eV). Unlike valence ionization energies, EOM methods can struggle to accurately predict the core-excitation energies of O3 and their splitting (ΔCT ≈ 4.70 eV). ,,

To simulate the XPS of ozone, we adopt the same active space used in a previous MR-ADC study, including 12 electrons in 9 active orbitals (four active electrons and three 2p orbitals from each oxygen atom). The CASSCF semicanonical orbitals for the CVS, core, and active spaces are listed in Figure . All EOM-DSRG computations use the recontracted cc-pCVTZ-X2C basis and account for relativistic effects using the one-electron spin-free X2C (1e-sf-X2C) method. For the EOM-DSRG-PT3 approach, we also examine a truncated variant including only 1h excitations in the EOM excitation operator (eq ), which we denote as EOM-DSRG-PT3-S. SR-ADC, EOM-CCSD, and MR-ADC results are taken from the work of de Moura and Sokolov, while nonrelativistic single-reference EOM/LR-CC results were provided by Coriani.

5.

5

Semicanonical orbitals for the CVS, core, and active spaces of the ozone molecule computed using CASSCF with the (12e, 9o) active space.

In Table , we show a comparison of a variety of theoretical and experimental results for XPS of ozone. For the terminal peaks, we report the average core-ionization energy for the (1a1)1 and (1b2)1 states since they typically differ by less than 0.01 eV. In reporting these data, we also note if the core electrons were frozen in the ground state computation (when applicable) and if relativistic effects were included in the Hamiltonian. Relative to nonrelativistic, all-electron computations, the 1e-sf-X2C treatment increases core-ionization energies by 0.37–0.39 eV and freezing ground-state core orbitals reduces them by 1.25–1.27 eV. However, since these shifts are uniform for the core-ionized states, neither changes ΔCT by more than 0.02 eV.

5. Theoretical and Experimental O K-Edge Core-Ionization Energies (in eV) and Spectroscopic Factors for the Terminal (OT) and Central (OC) Oxygen Atoms .

method frozen core 1e-sf-X2C OT (2a1 /1b2 ) OC (1a1 ) ΔCT
SR-ADC(2) No Yes 541.02 (1.461) 546.83 (1.490) 5.81
SR-ADC(2)-X No Yes 540.87 (1.471) 546.46 (1.492) 5.59
SR-ADC(3) No Yes 548.55 (1.635) 551.75 (1.664) 3.20
EOM-CCSD No No 544.15 549.23 5.07
EOM-CCSD Yes No 542.90 547.96 5.06
CCSDR(3) No No 542.36 547.43 5.07
CC3 No No 540.78 546.16 5.38
MR-ADC(2) No Yes 543.85 (1.531) 548.48 (1.552) 4.63
MR-ADC(2)-X No Yes 541.00 (1.291) 545.43 (1.380) 4.43
EOM-DSRG-PT2 Yes Yes 545.49 (1.476) 549.17 (1.488) 3.68
EOM-DSRG-PT3 Yes Yes 544.66 (1.431) 548.81 (1.473) 4.15
EOM-DSRG-PT3 No Yes 545.93 (1.432) 550.08 (1.475) 4.15
EOM-DSRG-PT3-S Yes Yes 563.33 (2.000) 567.75 (2.000) 4.42
EOM-LDSRG(2) Yes Yes 544.64 (1.435) 548.65 (1.472) 4.01
SA-DSRG-MRPT2 No Yes 540.84 545.53 4.69
SA-DSRG-MRPT3 No Yes 541.35 545.64 4.29
MS-RASPT2 No No 541.52 547.25 5.73
Experiment 541.5 546.2 4.70
a

The energy splitting (in eV) between the OT and OC peaks is reported as ΔCT. EOM-DSRG methods are labeled as PT2, PT3, PT3-S, and LDSRG(2), corresponding to EOM-DSRG-PT2, EOM-DSRG-PT3, EOM-DSRG-PT3-S, and EOM-LDSRG(2), respectively. All EOM-DSRG results employ a value of s=0.5Eh2 , while SA-DSRG results use s=1.0Eh2 .

b

Yes = core electrons are frozen in the ground-state computation, No = all-electron ground-state computation.

c

Yes = one-electron 1e-sf-X2C treatment and cc-pCVTZ-X2C basis, No = nonrelativistic Hamiltonian and cc-pCVTZ basis.

d

From ref .

e

From ref .

f

From ref , with cc-pVQZ basis set.

g

From ref , with cc-pVTZ basis set.

h

From ref .

We first analyze the results for the single-reference methods. As shown in Table , the ADC(2) and ADC(2)-X core-ionization energies are within 0.7 eV from experiment; going to the next order, SR-ADC(3) worsens the core-ionization energies, overestimating them by 5–7 eV, suggesting cancellation of errors at second order or poor convergence behavior of the ADC series at higher order. The EOM-CC results based on the all-electron CVS scheme overestimate the ionization energies at the CCSD level by up to 3 eV. The addition of triples via the CCSDR(3) and CC3 methods reduces the error down to less than 0.8 eV (CC3), consistent with a previous benchmark. Nevertheless, across the EOM-CC hierarchy, the value of ΔCT is consistently predicted to be in a narrow range (5.1–5.4 eV).

Among the multireference ADC methods, MR-ADC(2)-X best reproduces the ionization energies, with errors of only 0.50–0.77 eV and ΔCT = 4.43 eV. For the EOM-DSRG methods, the most accurate LDSRG(2) treatment yields a value of ΔCT = 4.01 eV, with absolute excitation energies overestimated by 3.1 and 2.5 eV for the OT and OC transitions, respectively. A comparison of the regular EOM-DSRG-PT3 with the 1h-only variant (-S) shows that the missing orbital relaxation and coupling to 2h1p configurations lead to severely overestimating the core-ionization energies by more than 20 eV. In contrast to the EOM methods, approaches such as state-averaged DSRG-MRPT2/3 and multistate RASPT2 optimize variational parameters specifically for the target states. As a consequence, these methods yield more consistent results and accurately reproduce the experimental core-ionization energy and ΔCT. Overall, this example shows that for both single and multireference variants of the EOM methods, it is essential to include higher-order dynamical correlation effects (3h2p) to accurately reproduce the core-ionization energies.

While an implementation is not yet available, we evaluate the challenges of incorporating 3h2p excitations into EOM-DSRG. We first consider the case in which the ground-state MR-DSRG calculation is still performed with up to double excitations. In the regime N V > N C N A , the dominant computational cost scales as O(NINC2NV4) , which matches the scaling of CVS-IP-EOM-CCSDT. The active space contribution scales as O(NINA12) , arising from the contraction between the AAAA block of the with the operator âIAAAA . A direct evaluation of this contraction would require up to 6-body reduced density cumulant. Instead, we may follow eq (27) of ref and rewrite it into a commutator form. The commutator formalism, originally proposed by Dyall, will only require up to 5-body reduced density cumulant and has been widely adopted in internally contracted methods, including IP-EOM-DSRG. One may also consider neglecting the âIAAAA excitations, and the resulting truncated variant would only require up to the 4-body reduced density cumulant, consistent with our current EOM-DSRG implementation. In order to balance the descriptions of ground and excited states, treating three-body clusters in the MR-DSRG computation would be necessary.

5. Conclusions

In this work, we formulate and implement a core–valence separated multireference equation-of-motion-driven similarity renormalization group method (CVS-IP-EOM-DSRG) and apply it to compute core-ionization energies and simulate X-ray photoelectron spectra (XPS). To ensure rigorous core intensivity of the ionization energies, we propose a modification of the ground-state DSRG formalism that solves projective equations for core-virtual singles amplitudes.

The CVS-EOM-DSRG framework is tested using ground states obtained at three truncation levels: the perturbative DSRG-MRPT2 and DSRG-MRPT3 methods and the nonperturbative MR-LDSRG(2) approach. For each truncation level, we systematically investigated the dependence on the flow parameter and the choice of the CVS scheme. We find that the ionization energies show only a weak dependence on the flow parameter within the recommended range. Two CVS schemes are compared, differing in their treatment of the occupied orbitals in the MR-DSRG ground-state wave function. We observe that the frozen-core CVS scheme systematically lowers the computed ionization energies, leading to very good agreement with benchmark CVS-EOMIP-CCSDTQ results. Numerical tests show that enforcing a subset of the projective conditions restores the core intensivity of the ionization energies while introducing only negligible differences in the ground-state energy. We then benchmark the CVS-IP-EOM-DSRG method based on the three ground state truncation schemes by computing K-edge vertical ionization energies for a set of small molecules. Our results show that the DSRG-PT3 truncation scheme balances well the computational cost and accuracy: it slightly underperforms compared to state-specific methods like GAS-DSRG and CVS-EOM-CCSDT (due to the lack of orbital relaxation and higher-order excitations). Still, it is on par with or outperforms the accuracy of the CVS-MR-ADC(2) and CVS-MR-ADC(2)-X schemes. Moreover, the PT3 truncation level matches the accuracy of CVS-IP-EOM-LDSRG(2) while offering improved computational efficiency by avoiding iterative ground-state optimization and its associated convergence challenges.

To assess the applicability of these methods to molecules with open-shell character, we compute potential energy curves for the N K-edge ionized states of N2 and the C and O K-edge ionized states of CO, comparing them with CVS-MR-ADC(2)-X results using GAS-DSRG curves as references. While all methods yield qualitatively correct potentials, CVS-IP-EOM-DSRG-PT3 and -LDSRG(2) accurately predict vibrational constants and show small nonparallelism errors. Using these curves, we simulate the vibrationally resolved XPS of N2 and CO, finding that the DSRG-PT3 and LDSRG(2) truncation schemes show excellent agreement with experiment. At the same time, CVS-IP-EOM-DSRG-PT2 and CVS-MR-ADC(2)-X fail to capture the correct vibrational intensities in some cases. We also applied the CVS-EOM-DSRG method to compute the XPS of ozone, which is more challenging for EOM methods that lack 3h2p excitations. Both CVS-EOM-DSRG-PT3 and CVS-EOM-LDSRG(2) correctly reproduce the energy splitting between ionization energies to within 0.7 eV, although a sizable shift (≈3.1 eV) is needed to match the lowest experimental ionization energy.

Overall, the relative accuracy of the new methods introduced follows the trend: CVS-EOM-LDSRG(2) ≈ CVS-EOM-DSRG-PT3 > CVS-EOM-DSRG-PT2. In particular, CVS-EOM-DSRG-PT3 offers a good balance between accuracy and computational efficiency, making it a reliable choice for modeling core-ionized states. Extending the method to incorporate particle-preserving excitation operators will enable applications in X-ray absorption (XAS) and UV/vis spectroscopy, and efforts in this direction are currently ongoing in our group. Finally, although numerical tests in this study indicate that enforcing projective conditions for core-virtual singles has little effect on the MR-DSRG ground-state energy, a systematic investigation is needed to better establish the impact of this choice on the accuracy and numerical stability of ground-state computations. The current multireference EOM formalism could also be extended to the closely related renormalized internally contracted multireference coupled-cluster theory (ric-MRCC), further reducing the computational cost.

Supplementary Material

ct5c01616_si_001.pdf (96.7KB, pdf)
ct5c01616_si_002.zip (11.1KB, zip)

Acknowledgments

We thank Sonia Coriani for providing the EOM-CCSD, CCSDR(3), and CC3 results for ozone reported in the article. We thank Kevin Marin and Meng Huang for insightful discussions. This research was supported by the U.S. National Science Foundation under award number CHE-2312105. S.L. was supported to develop the NiuPy package by the National Science Foundation and the Molecular Sciences Software Institute under Grant No. CHE-2136142.

All data are available upon reasonable request. The software used to produce the data presented in this work is available in an accompanying public code repository.

The Supporting Information is available free of charge at https://pubs.acs.org/doi/10.1021/acs.jctc.5c01616.

  • Choice of active spaces and reference energies for the CASSCF computations, where applicable, and vertical ionization energies and spectroscopic factors of ozone (PDF)

  • Zip file containing comma-separated value (CSV) files of the raw data for all figures in the main text (ZIP)

The authors declare no competing financial interest.

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Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Supplementary Materials

ct5c01616_si_001.pdf (96.7KB, pdf)
ct5c01616_si_002.zip (11.1KB, zip)

Data Availability Statement

All data are available upon reasonable request. The software used to produce the data presented in this work is available in an accompanying public code repository.


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