One can use absolutely localized molecular orbitals (ALMOs, see Chapter 12)
to construct charge-localized diabatic states directly from DFT calculations. The ALMOs
on each fragment are expanded by the AO basis functions belonging to the same fragment
alone, whose corresponding MO coefficient matrix is
fragment block-diagonal.
599
J. Chem. Phys.
(2006),
124,
pp. 204105.
Link
In energy decomposition analysis methods,
598
J. Phys. Chem. A
(2007),
111,
pp. 8753.
Link
,
515
Phys. Chem. Chem. Phys.
(2016),
18,
pp. 23067.
Link
ALMOs are utilized to separate the effects of polarization and charge transfer in
intermolecular binding, because they have the useful property that they do not allow for
charge transfer between fragments under the Mulliken definition of charge population.
Making use of this property, one can construct charge-localized diabats for hole
and electron transfer. For example, considering the initial and final states of a hole
transfer process, and , the two diabats
can be represented in the following form:
(10.135a) | ||||
(10.135b) |
For systems where the donor and acceptor moieties are well-separated, one can
construct the ALMO-based diabats by simply concatenating orbitals obtained from
isolated fragment calculations: and for one diabat, and and
for the other. The energy of each ALMO diabat can then be variationally optimized
with respect to orbital rotations on fragment, using the SCFMI technique (see
Section 12.4).
1151
Theor. Chem. Acc.
(1980),
57,
pp. 169.
Link
,
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Int. J. Quantum Chem.
(1996),
60,
pp. 157.
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,
599
J. Chem. Phys.
(2006),
124,
pp. 204105.
Link
These
ALMO-based diabatic states are variationally optimized such that the associated
nuclear forces can be easily computed.
778
Phys. Chem. Chem. Phys.
(2017),
19,
pp. 5944.
Link
The mutual polarization of
donor and acceptor moieties in the presence of each other is also taken into account.
To calculate the electronic coupling between two ALMO diabats, one should first construct the diabatic Hamiltonian in the ALMO state basis
(10.136) |
and then transform that into the Löwdin-orthogonalized basis
(10.137) |
whose off-diagonal element, , corresponds to the diabatic coupling to be evaluated. In the 2-state case, we have
(10.138) |
which requires the overlap between two ALMO diabats and the diagonal and off-diagonal elements of . The interstate overlap is given by
(10.139) |
where and are MO coefficients for the occupied orbitals in diabats and , respectively, and is the AO overlap matrix.
The elements of the diabatic Hamiltonian matrix can be evaluated using the multi-state
DFT (MSDFT) approach.
187
J. Chem. Theory Comput.
(2009),
5,
pp. 2702.
Link
,
1014
J. Phys. Chem. Lett.
(2016),
7,
pp. 2286.
Link
,
782
J. Chem. Phys.
(2019),
151,
pp. 164114.
Link
For the diagonal
elements, it is straightforward to employ the KS energies of the two diabats:
(10.140) |
where and are the one-electron density matrices
associated with two ALMO states and , respectively.
The approximation for the off-diagonal element is theoretically more challenging. In the original
MSDFT scheme,
187
J. Chem. Theory Comput.
(2009),
5,
pp. 2702.
Link
,
1014
J. Phys. Chem. Lett.
(2016),
7,
pp. 2286.
Link
(10.141) |
where is the one-particle transition density matrix between two ALMO states
(10.142) |
The first three terms on the right-hand side of Eq. (10.141) correspond to the contributions
from nuclear repulsion, one-electron Hamiltonian (kinetic energy and nuclei-electron attraction),
and full two-electron integrals (Coulomb and full HF exchange),
which can be derived as in non-orthogonal CI.
1187
J. Chem. Phys.
(2009),
131,
pp. 124113.
Link
The last term accounts for the contribution from exchange-correlation (XC) functional
as a correction to the HF coupling, which is given by the average of the difference between the
KS and HF energies calculated from the same one-electron density matrix for each diabat:
(10.143a) | ||||
(10.143b) |
This approach was denoted as ALMO(MSDFT) in Ref.
782
J. Chem. Phys.
(2019),
151,
pp. 164114.
Link
and it was found to
overestimate the electronic couplings for the tested hole and electron transfer systems.
A modified approach, denoted as ALMO(MSDFT2), was proposed in Ref.
782
J. Chem. Phys.
(2019),
151,
pp. 164114.
Link
,
which evaluates the XC contribution using the XC energy of the symmetrized transition density matrix
(10.144) |
where
(10.145) |
Note that in Eq. (10.144), includes only Coulomb integrals and a fraction of exact exchange if hybrid functionals are employed.
According to the benchmark results in Ref.
782
J. Chem. Phys.
(2019),
151,
pp. 164114.
Link
, ALMO(MSDFT2) shows better accuracy
than the original MSDFT method for hole and electron transfer, and thus it is implemented as the default
approach to compute electronic couplings between ALMO diabats in Q-Chem. We note that the results
given by Eq. (10.144) may become inaccurate when the overlap between two states
becomes near-singular, as
(10.146) |
is inverted when constructing the transition density [Eq. (10.142)].
To circumvent this numerical issue, one can replace the inverse in
Eq. (10.142) with the Penrose pseudo-inverse, which was suggested for a similar objective in
Ref.
912
J. Chem. Phys.
(2013),
138,
pp. 054101.
Link
.
Besides ALMO-based diabatization method, other fragment-based diabatization methods are
available in Q-Chem. The projection operator diabatization (POD) method
618
J. Phys. Chem. C
(2007),
111,
pp. 11970.
Link
starts from a standard KS-DFT calculation of the system and post-processes the converged
Fock matrix. It first transforms the Fock matrix into the Löwdin-orthogonalized AO basis and
then partitions that into the donor and acceptor blocks, assuming that these orthogonalized AO
basis functions still retain their original fragment tags:
(10.147) |
One then diagonalizes and separately
(10.148) |
where the eigenvectors and define the single-particle “diabatic states”:
(10.149) |
and transforms the off-diagonal block of the Fock matrix into this diabatic basis
(10.150) |
yielding
(10.151) |
The couplings between these single-particle diabatic orbitals can then be directly read off from the elements of .
The Q-Chem implementation of the POD method follows the description in
Refs.
618
J. Phys. Chem. C
(2007),
111,
pp. 11970.
Link
and
1318
Phys. Chem. Chem. Phys.
(2018),
20,
pp. 2571.
Link
, where a closed-shell
reference system is used to generate the Fock matrix to be processed, i.e.,
in Eq. (10.147). By default, only the D(HOMO) - A(HOMO) coupling is calculated
for the hole transfer cases, and the D(LUMO) - A(LUMO) coupling for the electron transfer
cases. To calculate the couplings between multiple pairs of donor and acceptor orbitals,
the user can set $rem variable POD_MULTI_PAIRS to TRUE and
control the number of orbitals pairs through POD_WINDOW. See the
instruction in Sec. 10.15.3.4.
Because of the use of globally Löwdin-orthogonalized orbitals in Eq. (10.147), the
diabatic orbitals created by POD cannot be strictly localized on fragments. This renders the
POD results unstable with the change of employed AO basis sets: when larger basis sets
are used, the mixing between AO basis functions on different fragments becomes stronger,
and the resulting decreases. To alleviate this problem, a revised POD method,
which was named as “POD2”, was proposed by Ghan et al..
376
J. Chem. Theory Comput.
(2020),
16,
pp. 7431.
Link
It avoids the global Löwdin-orthogonalization of the AO basis; instead, it separately
diagonalizes the the donor and acceptor blocks of the Fock matrix
(in the original AO basis):
(10.152) |
The obtained diabatic MO coefficient matrix is fragment-block-diagonal in the AO basis:
(10.153) |
Transforming the AO Fock matrix into this diabatic MO basis, the D-D and A-A blocks of the resulting matrix are diagonal matrices:
(10.154) |
Using the matrix elements in the off-diagonal block () directly would yield overestimated couplings since the diabatic MOs and are not orthogonal to each other. Therefore, a final orthogonalization step is required to obtain the diabatic coupling between a pair of orbitals that are located on the donor and acceptor, respectively. Denoting this pair of orbital as and , one can construct the Hamiltonian and overlap matrices:
(10.155) |
Two orthogonalization schemes have been investigated by Ghan et al..
376
J. Chem. Theory Comput.
(2020),
16,
pp. 7431.
Link
The first approach performs a Löwdin orthgonalization on and , which
is denoted as POD2L. The resulting coupling between the orthogonalized diabatic orbitals
are
(10.156) |
The second approach employs the Gram-Schmidt orthogonalization, which keeps one of the two orbitals ( or ) intact while ensures that the other is strictly orthogonal to it. This approach is denoted as POD2GS, and it might be better choice for asymmetric cases (e.g. surface and adsorbates) where one can choose to retain the orbital on the less sizable fragment. These two POD2 variants afford significantly improved accuracy over the original POD method, especially in terms of the robustness with regard to the use of extensive basis sets.
Fragment orbital DFT (FODFT)
875
Phys. Chem. Chem. Phys.
(2012),
14,
pp. 13846.
Link
,
1081
J. Chem. Phys.
(2003),
119,
pp. 9809.
Link
,
1067
J. Chem. Phys.
(2016),
144,
pp. 054103.
Link
is an approach to compute the diabatic couplings for hole and electron transfer between
fragments. There have been several different flavors of FODFT approaches developed
in literature, and here we introduce the most recent variant by Schober et al.
1067
J. Chem. Phys.
(2016),
144,
pp. 054103.
Link
Considering a hole transfer process or an electron transfer
process , where the donor () and acceptor () fragments
have and electrons, respectively, the procedure is as follows:
Perform KS-DFT calculations for isolated donor and acceptor fragments;
collect the converged fragment orbitals:
and
Löwdin-orthogonalize the occupied orbitals on two fragments. The reactant diabat ( or ) can be represented as
(10.157) |
where “” denotes Löwdin-orthogonalized orbitals, and . Note that the lowest unoccupied orbital where the electron is transferring to, in the case of HT or in the case of ET, also needs to be made orthogonal to the space spanned by all occupied orbitals.
Construct the product diabat ( or ), simply by moving the hole from to (HT), or the excess electron from to (ET)
(10.158) |
Compute the electronic coupling between and , which is approximated by the coupling of the orthogonalized fragment orbitals through the Kohn-Sham Fock operator (built from the reactant diabat)
(10.159) |
The approach described above is denoted as FODFT()@ (HT) /
FODFT()@ (ET)
1067
J. Chem. Phys.
(2016),
144,
pp. 054103.
Link
as the charged fragment
is explicitly taken into account when preparing the fragment orbitals and the KS Fock
matrix is built from occupied orbitals. Besides this, there are two other variants
of FODFT:
According to the benchmark results,
1067
J. Chem. Phys.
(2016),
144,
pp. 054103.
Link
,
782
J. Chem. Phys.
(2019),
151,
pp. 164114.
Link
FODFT()@ (HT) /
FODFT()@ (ET) is the best-performing method, possibly because
of its explicit account for charged fragments and consistent electron count in
the preparation of fragment orbitals and in the construction of Fock matrix.
One issue associated with the FODFT methods is that for asymmetric systems, the
results would depend on how one chooses the initial and final states for an electron or
hole transfer process (e.g. vs. ), especially for the two variants that
build the Fock matrix with occupied orbitals.
782
J. Chem. Phys.
(2019),
151,
pp. 164114.
Link
The Q-Chem
implementation of FODFT()@ /
FODFT()@ automatically computes in both ways
and then reports the average, as it only requires an extra Fock matrix build. This, however,
is not automatically done for FODFT()@ /
FODFT()@.
POD, FODFT, and ALMO(MSDFT) calculations in Q-Chem require specification of fragments in the $molecule section (see Sec. 12.2). For ALMO(MSDFT) calculations, one also needs to specify the charge and multiplicity of each fragment in each diabatic state in the $almo_coupling section, where two hyphens indicate the separation of different diabats:
$almo_coupling charge_frag_1 mult_frag_1 !diabat 1 charge_frag_2 mult_frag_2 -- charge_frag_1 mult_frag_1 !diabat 2 charge_frag_2 mult_frag_2 $end
The current implementation of FODFT is limited to hole transfer between the HOMOs of two fragments or electron transfer between the LUMOs, and the current simplementation of ALMO(MSDFT) is limited to ground state electron or hole transfer involving two states.
FRAG_DIABAT_METHOD
FRAG_DIABAT_METHOD
Specify fragment based diabatization method
TYPE:
STRING
DEFAULT:
NONE
OPTIONS:
ALMO_MSDFT
Perform ALMO(MSDFT) diabatization
POD
Perform projection operator diabatization (the original method)
POD2_L
Perform POD2 with Löwdin orthogonalization
POD2_GS
Perform POD2 with Grad-Schmidt orthogonalization
ESID
The energy-split-in-dimer method,
1210
J. Am. Chem. Soc.
(2006),
128,
pp. 9882.
Link
which is equivalent to
the FMO approach
introduced in Section 10.15.2.5
FODFT
Calculate electronic coupling using fragment orbital DFT
RECOMMENDATION:
NONE
FRAG_DIABAT_DOHT
FRAG_DIABAT_DOHT
Specify whether hole or electron transfer is considered
TYPE:
BOOLEAN
DEFAULT:
TRUE
OPTIONS:
TRUE
Do hole transfer
FALSE
Do electron transfer
RECOMMENDATION:
Need to be specified for POD and FODFT calculations
FRAG_DIABAT_PRINT
FRAG_DIABAT_PRINT
Specify the print level for fragment based diabatization calculations
TYPE:
INTEGER
DEFAULT:
0
OPTIONS:
0
No additional prints
Print additional details
RECOMMENDATION:
Use the default unless debug information is needed
MSDFT_METHOD
MSDFT_METHOD
Specify the scheme for ALMO(MSDFT)
TYPE:
INTEGER
DEFAULT:
2
OPTIONS:
1
The original MSDFT scheme [Eq. (10.141)]
2
The ALMO(MSDFT2) approach [Eq. (10.144)]
RECOMMENDATION:
Use the default method. Note that the method will be automatically
reset to 1 if a meta-GGA functional is requested.
MSDFT_PINV_THRESH
MSDFT_PINV_THRESH
Set the threshold for pseudo-inverse of the interstate overlap
TYPE:
INTEGER
DEFAULT:
4
OPTIONS:
Set the threshold to 10
RECOMMENDATION:
Use the default value
POD_MULTI_PAIRS
POD_MULTI_PAIRS
Calculate the couplings between multiple pairs of donor and acceptor
orbitals in POD
TYPE:
BOOLEAN
DEFAULT:
FALSE
OPTIONS:
TRUE
Calculate the couplings between multiple pairs of orbitals
FALSE
Only calculate the D(HOMO)–A(HOMO) coupling (for HT) or
D(LUMO)–A(LUMO) coupling (for ET)
RECOMMENDATION:
None
POD_WINDOW
POD_WINDOW
Specify the number of donor and acceptor orbitals when couplings between
multiple pairs are requested
TYPE:
INTEGER
DEFAULT:
5
OPTIONS:
Including frontier occupied orbitals (from to HOMO)
and frontier virtual orbitals (from LUMO to ) for both
donor and acceptor
RECOMMENDATION:
None
FODFT_METHOD
FODFT_METHOD
Specify the flavor of FODFT method
TYPE:
INTEGER
DEFAULT:
1
OPTIONS:
1
FODFT()@ (HT) / FODFT()@ (ET)
2
FODFT()@
3
FODFT()@ (HT) / FODFT()@ (ET)
RECOMMENDATION:
The default approach shows the best overall performance
FODFT_DONOR
FODFT_DONOR
Specify the donor fragment in FODFT calculation
TYPE:
INTEGER
DEFAULT:
1
OPTIONS:
1
First fragment as donor
2
Second fragment as donor
RECOMMENDATION:
With FODFT_METHOD = 1, the charged fragment needs to be the
donor fragment
$molecule 1 2 -- 1 2 C 0.000000 0.000000 0.000000 C 1.332000 0.000000 0.000000 H -0.574301 0.000000 -0.928785 H -0.574301 0.000000 0.928785 H 1.906301 0.000000 0.928785 H 1.906301 0.000000 -0.928785 -- 0 1 C -0.000000 4.000000 0.000000 C 1.332000 4.000000 -0.000000 H -0.574301 4.000000 0.928785 H -0.574301 4.000000 -0.928785 H 1.906301 4.000000 -0.928785 H 1.906301 4.000000 0.928785 $end $rem METHOD PBE0 BASIS 6-31+G(D) UNRESTRICTED TRUE THRESH 14 SCF_CONVERGENCE 8 SYMMETRY FALSE SYM_IGNORE TRUE SCFMI_MODE 1 FRGM_METHOD STOLL FRAG_DIABAT_METHOD ALMO_MSDFT $end $almo_coupling 1 2 0 1 -- 0 1 1 2 $end
$molecule 0 1 -- 0 1 C 0.000000 0.000000 0.000000 C 1.332000 0.000000 0.000000 H -0.574301 0.000000 -0.928785 H -0.574301 0.000000 0.928785 H 1.906301 0.000000 0.928785 H 1.906301 0.000000 -0.928785 -- 0 1 C -0.000000 4.000000 0.000000 C 1.332000 4.000000 -0.000000 H -0.574301 4.000000 0.928785 H -0.574301 4.000000 -0.928785 H 1.906301 4.000000 -0.928785 H 1.906301 4.000000 0.928785 $end $rem METHOD lrc-wpbeh BASIS 6-31+g(d) FRAG_DIABAT_METHOD pod SCF_CONVERGENCE 8 THRESH 14 SYMMETRY false SYM_IGNORE true $end
$molecule 1 2 -- 1 2 C 0.000000 0.000000 0.000000 C 1.332000 0.000000 0.000000 H -0.574301 0.000000 -0.928785 H -0.574301 0.000000 0.928785 H 1.906301 0.000000 0.928785 H 1.906301 0.000000 -0.928785 -- 0 1 C -0.000000 4.000000 0.000000 C 1.332000 4.000000 -0.000000 H -0.574301 4.000000 0.928785 H -0.574301 4.000000 -0.928785 H 1.906301 4.000000 -0.928785 H 1.906301 4.000000 0.928785 $end $rem METHOD wb97x-d BASIS 6-31+g(d) UNRESTRICTED true SCF_CONVERGENCE 8 THRESH 14 SYMMETRY false SYM_IGNORE true FRAG_DIABAT_METHOD fodft FODFT_METHOD 1 $end