Python implementation of Tully's Fewest Switches Surface Hopping (FSSH) for model problems including a propagator and an implementation of Tully's model problems described in Tully, J.C. J. Chem. Phys. (1990) 93 1061. The current implementation probably works for more than two electronic states, is completely untested for more than one dimensional potentials.
mudslide
package that contains- implementation of all surface hopping methods
TrajectorySH
- FSSHTrajectoryCum
- FSSH with a cumulative point of viewEhrenfest
- Ehrenfest dynamics
- collection of 1D models
TullySimpleAvoidedCrossing
TullyDualAvoidedCrossing
TullyExtendedCouplingReflection
SuperExchange
SubotnikModelX
SubotnikModelS
ShinMetiu
- now some 2D models
Subotnik2D
- implementation of all surface hopping methods
mudslide
script that runs simple model trajectoriesmudslide-surface
script that prints 1D surface and couplings
- numpy
- scipy (for Shin-Metiu model)
FSSH has switched to a proper python package structure, which means to work properly it now needs to be "installed". The most straightforward way to do this is
cd /path/to/mudslide
pip install --user -e .
which install into your user installation dir. You can find out your user installation directory with the command
python -m site --user-base
To set up your PATH
and PYTHONPATH
to be able to use both the command line scripts
and the python package, use
export PATH=$(python -m site --user-base)/bin:$PATH
export PYTHONPATH=$(python -m site --user-base):$PYTHONPATH
Sets of simulations are run using the BatchedTraj
class. A BatchedTraj
object must be instantiated by passing a model object
(handles electronic PESs and couplings), and a traj_gen
generator that generates new initial conditions. Some simple canned examples are provided for traj_gen
. All
other options are passed as keyword arguments to the constructor. The compute()
function of the
BatchedTraj
object returns a TraceManager
object that contains all the results, but functionally behaves
like a python dictionary. Custom TraceManager
s can also be
provided. For example:
import mudslide
simple_model = mudslide.models.TullySimpleAvoidedCrossing()
# Generates trajectories always with starting position -5, starting momentum 10.0, on ground state
traj_gen = mudslide.TrajGenConst(-5.0, 10.0, "ground")
simulator = mudslide.BatchedTraj(simple_model, traj_gen, mudslide.TrajectorySH, samples = 4)
results = simulator.compute()
outcomes = results.outcomes
print("Probability of reflection on the ground state: %12.4f" % outcomes[0,0])
print("Probability of transmission on the ground state: %12.4f" % outcomes[0,1])
print("Probability of reflection on the excited state: %12.4f" % outcomes[1,0])
print("Probability of transmission on the excited state: %12.4f" % outcomes[1,1])
will run 20 scattering simulations in parallel with a particle starting at -5.0 a.u. and traveling with an initial momentum of 10.0 a.u.
initial_state
- specify how the initial electronic state is chosen- "ground" (default) - start on the ground state
mass
- particle mass (default: 2000 a.u.)initial_time
- starting value oftime
variable (default: 0.0 a.u.)dt
- timestep (default: abs(0.05 / velocity)))total_time
- total simulation length (default: 2 * abs(position/velocity))samples
- number of trajectories to run (default: 2000)seed
- random seed for trajectories (defaults however numpy does)propagator
- method used to propagate electronic wavefunction- "exponential" (default) - apply exponentiated Hamiltonian via diagonalization
- "ode" - scipy's ODE integrator
nprocs
- number of processes over which to parallelize trajectories (default: 1)outcome_type
- how to count statistics at the end of a trajectory- "state" (default) - use the state attribute of the simulation only
- "populations" - use the diagonals of the density matrix
trace_every
- save snapshot data every nth step (i.e., whennsteps%trace_every==0
)
The model provided to the FSSH class needs to have three functions implemented:
V(self, x)
--- returns (nstates,nstates)-shaped numpy array containing the Hamiltonian matrix at nuclear positionx
dV(self, x)
--- returns (nstates,nstates,ndim)-shaped numpy array containing the gradient of the Hamiltonian matrix at nuclear positionx
nstates(self)
--- returns the number of electronic states in the modelndim(self)
--- returns the number nuclear degrees of freedom in the model
In all cases, the input x
ought to be a numpy array with ndim
elements.
For simple diabatic models, there is a helper class, DiabaticModel_
that will
simplify construction of classes for new models. If you derive your class from
DiabaticModel_
, you only need to implement V()
and dV()
in the diabatic basis,
and define class variables ndim_
and nstates_
that hold the number of
nuclear degrees of freedom and the number of electronic states, respectively. See
the file mudslide/models.py
for examples.
The file models.py implements the three models in Tully's original paper. They are:
- TullySimpleAvoidedCrossing
- TullyDualAvoidedCrossing
- TullyExtendedCouplingReflection
Additional models included are:
SuperExchange
- Oleg Prezhdo's three-state super exchange model from Wang, Trivedi, Prezhdo JCTC (2014) doi:10.1021/ct5003835SubotnikModelX
- 'Model X' from Subotnik JPCA (2011) doi: 10.1021/jp206557hSubotnikModelS
- 'Model S' from Subotnik JPCA (2011) doi: 10.1021/jp206557hSubotnik2D
- 2D model from Subotnik JPCA (2011) doi: 10.1021/jp206557hShin-Metiu
For batch runs, one must tell BatchedTraj
how to decide on new initial conditions
and how to decide when a trajectory has finished. The basic requirements for each of those
is simple.
The structure of these classes is somewhat strange because of the limitations of
multiprocessing in python. To make use of multiprocessing, every object
must be able to be pickle
d, meaning that multiprocessing inherits all the
same limitations. As a result, when using multiprocessing, the trajectory generator class must
be fully defined in the default namespace.
This should be a generator function that accepts a number of samples and returns a dictionary with starting conditions filled in, e.g., the yield statement should be something like
yield { "position" : x0, "momentum" : p0, "initial_state" : "ground" }
See TrajGenConst
for an example.
Scans of the surfaces can be printed using the surface
command that is included
for the installation. For usage, make sure your PATH
includes the installation
directory for scripts (e.g., by running
export PATH=$(python -m site --user-base)/bin:$PATH
) and run
surface -h
- This package is written to take advantage of doxygen!