# Matt Watkins for the CP2K-UK summer school 2016
It is a very common problem that we need to describe an imhomogeneous system, and we may be more interested in some parts than others. However, the rest of the system is still important.
We could consider
Also, we might need to collect a lot of data when dealing with amorphous or disordered systems. Within CP2K there is quite reasonable task farming capability allowing complex jobs to be automated internally. Practically this can mean only a single job being submitted into a queue, rather than thousands…
If we have our QM system experiencing an applied field we can use several methods in CP2K - this can be confusing.
External fields can be applied in two general ways, reminding us of the GPW method.
CP2K_INPUT / FORCE_EVAL / DFT / EXTERNAL_POTENTIAL (CP2K_INPUT / FORCE_EVAL / DFT / EFIELD (for real time propagation))
CP2K_INPUT / FORCE_EVAL / DFT / PERIODIC_EFIELD CP2K_INPUT / FORCE_EVAL / DFT / EFIELD
This works exactly in the same way that nuclear charge or electrostatics in general is dealt with in GPW.
&EXTERNAL_POTENTIAL FUNCTION (A/B)*Z VALUES [eV] 0.2 [angstrom] 1.0 PARAMETERS A B &END EXTERNAL_POTENTIAL
by default it places an analytical function onto the grid.
Here a constant potential gradient 0.2 eV / Angstrom (electric field) in the $z$ direction.
It is alternatively possible to read the potential on a grid (the cube file read must be a valid cube file with points the fit the finest grid).
Note that this is not periodic! Can only be used with molecules and slabs.
The periodic_efield
(and efield
) keywords apply electric fields that are calculated analytically in the Gaussian basis.
$$ \big{<} \phi_a \big{|} \hat{O} \big{|} \phi_b \big{>} $$
Periodic electric field uses the Berry phase formalism of the Modern Theory of Polarizablility and can be used for periodic systems.
Well known method is QMMM, one main strand arose from the bio community - aiming to accurately model active sites in proteins
typically the active site was surrounded by a finite number of classical point charges
and the surface terms (boundary of the MM) was just hydrogen terminated, or extra point charges were added to make electrostatics well behaved, or a continuum field model was added.
An attractive feature of CP2K's QMMM implementation is that it can be fully periodic, or anything from a cluster to a 3D system.
Generally CP2K works with an additive QMMM Hamiltonian:
$$ E_{tot}(\mathbf{R}_\alpha , \mathbf{R}_a) = E_{QM}(\mathbf{R}_\alpha) + E_{MM}( \mathbf{R}_a) + E_{QMMM}(\mathbf{R}_\alpha , \mathbf{R}_a) $$
Total energy is just the QM energy + the MM energy + the interaction between them.
Where the system is partitioned into QM atoms, at positions $(\mathbf{R}_\alpha)$ and MM atoms at position $(\mathbf{R}_a)$.
It is also possible to use 'subtractive schemes' (ONIOMM in Gaussian code for instance):
$$ E_{tot}(\mathbf{R}_\alpha , \mathbf{R}_a) = E_{QM}(\mathbf{R}_\alpha) - E_{MM}( \mathbf{R}_\alpha) + E_{MM}(\mathbf{R}_\alpha , \mathbf{R}_a) $$
or for a QM in QM embedding:
$$ E_{tot}(\mathbf{R}_\alpha , \mathbf{R}_a) = E_{QM^1}(\mathbf{R}_\alpha) - E_{QM^2}( \mathbf{R}_\alpha) + E_{QM^2}(\mathbf{R}_\alpha , \mathbf{R}_a) $$
$$ E_{tot}(\mathbf{R}_\alpha , \mathbf{R}_a) = E_{QM}(\mathbf{R}_\alpha) + E_{MM}( \mathbf{R}_a) + E_{QMMM}(\mathbf{R}_\alpha , \mathbf{R}_a) $$
where the coupling term is mainly electrostatic
$$ E_{QMMM}(\mathbf{R}_\alpha , \mathbf{R}_a) = \sum_{a \in MM} q_a \int_r \frac{n_{tot} (\mathbf{r})}{\mid \mathbf{r} - \mathbf{R}_a \mid} \text{d}\mathbf{r} $$
where $n_{tot}$ is the total electronic and nuclear charge density of the QM system and $q_a$ is the charge of the MM atom at location $\mathbf{R}_a$
As always in CP2K, we try and use Gaussians …
$$ n(|\mathbf{r}-\mathbf{R}_a|) = \left( \frac{1}{\sqrt \pi r_{c,a}}\right) exp \left( \frac{|\mathbf{r}-\mathbf{R}_a|^2}{r_{c,a}^2}\right) \Rightarrow v_a(\mathbf{r},\mathbf{R}_a) = \frac{erf(\frac{|\mathbf{r}-\mathbf{R}_a|}{r_{c,a}})}{|\mathbf{r}-\mathbf{R}_a|} $$ where the error function is $erf(x) = \frac{2}{\sqrt \pi} \int_0^x e^{-t^2}\text{d}t$
$$ v_a(\mathbf{r},\mathbf{R}_a) = \frac{erf(\frac{|\mathbf{r}-\mathbf{R}_a|}{r_{c,a}})}{|\mathbf{r}-\mathbf{R}_a|} = \sum_{N_g} A_g exp \big(\frac{|\mathbf{r}-\mathbf{R}_a|^2}{r_{c,a}^2} \big) + R_{low} (|\mathbf{r}-\mathbf{R}_a|) $$ the final term $R_{low} (|\mathbf{r}-\mathbf{R}_a|)$ is the residual part of the function not represented by the Gaussians, and should be rather smooth.
The number of terms in the sum $N_g$ is set by the input variable USE_GEEP_LIB
METHOD QMMMM @include QS.inc @include MM.inc &QMMM #this defines the QS cell in the QMMM calc &CELL ABC 12.6 15.0 12.6 PERIODIC XZ &END CELL ECOUPL GAUSS # use GEEP method NOCOMPATIBILITY USE_GEEP_LIB 6 # use GEEP method
The short range part is put onto grids in much the same manner as in the GPW method.
this is the confusing bit to work with. Must be activated with the
CP2K_INPUT / FORCE_EVAL / QMMM / PERIODIC
section. The default is non periodic embedding.
has two components
CP2K_INPUT / FORCE_EVAL / QMMM / PERIODIC / MULTIPOLE this is on be default if the periodic keyword is activated
Alternatively for Semi Empirical Hamiltonians or DFTB it is possible to use “coulomb” embedding.
Here the field from the classical ions acts on the Gaussian basis functions, much like the efield talked about earlier
METHOD QMMMM @include QS.inc @include MM.inc &QMMM #this defines the QS cell in the QMMM calc &CELL ABC 12.6 15.0 12.6 PERIODIC XZ &END CELL ECOUPL COULOMB # use classical point charge method
$$ V_{ab,QMMM}^{coulomb} = -\sum_{I \in MM atoms} \big{<} \phi_a \big{|} \frac{Z_I}{\mid \mathbf{R_I}-\mathbf{r} \mid} \big{|} \phi_b \big{>} $$
see this exercise
Example setup for KCl that we used here.
We need to define the whole system as normal
&SUBSYS #this defines the cell of the whole system #must be orthorhombic, I think &CELL ABC 12.6 100.0 12.6 &END CELL &TOPOLOGY COORD_FILE_NAME kcl.xyz COORD_FILE_FORMAT XYZ &GENERATE &ISOLATED_ATOMS #ignores bonds dihedrals etc in classical part LIST 1..48 &END &END &END &KIND K ELEMENT K BASIS_SET DZVP-MOLOPT-SR-GTH POTENTIAL GTH-PBE-q9 &END KIND &KIND Cl BASIS_SET DZVP-MOLOPT-GTH POTENTIAL GTH-PBE-q7 &END &END SUBSYS
We need a normal section for the QM part
&DFT BASIS_SET_FILE_NAME BASIS_MOLOPT POTENTIAL_FILE_NAME GTH_POTENTIALS &MGRID COMMENSURATE # this keyword is required for QMMM with GEEP CUTOFF 150 &END MGRID &QS EPS_DEFAULT 1.0E-12 &END QS &SCF EPS_SCF 1.0E-06 MAX_SCF 26 SCF_GUESS RESTART &OT MINIMIZER CG PRECONDITIONER FULL_SINGLE_INVERSE &END OT &OUTER_SCF EPS_SCF 1.0E-05 &END OUTER_SCF &END SCF &XC &XC_FUNCTIONAL PBE &END XC_FUNCTIONAL &END XC &PRINT &MO_CUBES NLUMO 10 WRITE_CUBE F &END MO_CUBES &END PRINT &END DFT <\code> A MM section <code> &MM &FORCEFIELD &CHARGE ATOM K CHARGE 1.0 &END CHARGE &CHARGE ATOM Cl CHARGE -1.0 &END CHARGE &NONBONDED &WILLIAMS atoms K Cl A [eV] 4117.9 B [angstrom^-1] 3.2808 C [eV*angstrom^6] 0.0 RCUT [angstrom] 3.0 &END WILLIAMS &WILLIAMS atoms Cl Cl A [eV] 1227.2 B [angstrom^-1] 3.1114 C [eV*angstrom^6] 124.0 RCUT [angstrom] 3.0 &END WILLIAMS &WILLIAMS atoms K K A [eV] 3796.9 B [angstrom^-1] 3.84172 C [eV*angstrom^6] 124.0 RCUT [angstrom] 3.0 &END WILLIAMS &END NONBONDED &END FORCEFIELD &POISSON &EWALD EWALD_TYPE spme ALPHA .44 GMAX 40 &END EWALD &END POISSON &END MM
The QMMM section is
&QMMM #this defines the QS cell in the QMMM calc &CELL ABC 12.6 15.0 12.6 PERIODIC XZ &END CELL ECOUPL GAUSS # use GEEP method NOCOMPATIBILITY USE_GEEP_LIB 6 # use GEEP method &PERIODIC # apply periodic potential #in this case QM box = MM box in XZ so turn #off coupling/recoupling of the QM multipole &MULTIPOLE OFF &END &END PERIODIC #these are just the ionic radii of K Cl #but should be treated as parameters in general #fit to some physical property &MM_KIND K RADIUS 1.52 &END MM_KIND &MM_KIND Cl RADIUS 1.67 &END MM_KIND #define the model &QM_KIND K MM_INDEX 25..32 41..48 &END QM_KIND &QM_KIND Cl MM_INDEX 17..24 33..40 &END QM_KIND &END QMMM
Note the CELL in the QMMM section is not the same size as in the main `&SUBSYS` section. We only need a cell large enough to contain the electron density of the QM region.
it is possible to create rather interesting effects by combining results from several calculations in some way: For instance there is an example in `$CP2K/cp2k/tests/QS/regtest-meta/H2O-IP-meta.inp` that performs metadynamics using the ionisation energy of a molecule as a collective variable.
A mixed calculation in CP2K will have multiple `FORCE_EVAL` sections
&MULTIPLE_FORCE_EVALS FORCE_EVAL_ORDER 2 3 &END &FORCE_EVAL METHOD MIXED &MIXED MIXING_TYPE GENMIX &GENERIC MIXING_FUNCTION X+Y VARIABLES X Y &END GENERIC &END &END FORCE_EVAL &FORCE_EVAL METHOD FIST &END FORCE_EVAL &FORCE_EVAL METHOD QS &END FORCE_EVAL
The default is to have a mapping 1-1 between atom index (i.e. all force_eval share the same geometrical structure).
This can be changed by providing a mapping between atoms in the different force_evals.
See this exercise
We can implement very simple subractive QMMM using a mixed force_env that would look schematically like this
&MULTIPLE_FORCE_EVALS FORCE_EVAL_ORDER 2 3 &END &FORCE_EVAL METHOD MIXED &MIXED MIXING_TYPE GENMIX &GENERIC MIXING_FUNCTION X+Y-Z VARIABLES X Y Z &END GENERIC &END &END FORCE_EVAL &FORCE_EVAL METHOD FIST &END FORCE_EVAL &FORCE_EVAL METHOD QS &END FORCE_EVAL &FORCE_EVAL METHOD FIST &END FORCE_EVAL
A final note is that CP2K has quite reasonable task farming capability
There are some examples in the test directories $CP2K/cp2k/tests/