The following is meant to give a very quick overview of how OpenPNM works.
The first step in an OpenPNM project is to create a network.
>>> import openpnm as op >>> pn = op.network.Cubic(shape=[10, 10, 10], spacing=0.0001)
The resulting network can be quickly visualized using
plot_connections in the Topotools module to get the following:
network module has a number of network types to chose from, and they can be found on the Network page.
The Network only contains spatial information (pore coordinates) and topological information (throat connections), so it is necessary to add geometrical information by creating a Geometry object:
>>> Ps = pn.pores('all') >>> Ts = pn.throats('all') >>> geo = op.geometry.StickAndBall(network=pn, pores=Ps, throats=Ts)
In this case the StickAndBall class was used, which has preset pore-scale models that calculate properties such as pore diameters and throat lengths, based on the assumption that the pores are spherical and the throats are cylinders.
- The Network (
pn) was passed to the Geometry class as an argument, so that
geoknows which network it’s associated with.
- the Geometry was assigned to specified pores (
Ps) and throats (
Ts), in this case it was ‘all’ of them but it’s possible to use several different Geometry objects for different subsets of the domain. This explained in more detail here XXX.
Phases must created to calculate the thermophysical properties of the fluids (and solids) used in the simulations:
>>> hg = op.phases.Mercury(network=pn) >>> h2o = op.phases.Water(network=pn)
Phase objects are associated with a Network, but they are not assigned to specific pores and throats. This is because phases can exist anywhere and everywhere in the domain, and can move around.
>>> phys_hg = op.physics.GenericPhysics(network=pn, phase=hg, geometry=geo) >>> phys_h2o = op.physics.GenericPhysics(network=pn, phase=h2o, geometry=geo)
GenericPhysics class was used, which has NO pore-scale models attached. We will add this manually in the next step.
- The Network must be given as an argument so that the Physics knows which network it’s associated with
- One Physics object is required for each Phase, since physics models require thermophysical properties. For example, the Hagan-Poisseuille equation requires the viscosity of the phase.
- Each Physics object is also associated with a Geometry. The reason for this is to assign different pore-scale physics models to different regions. In this case both are associated with
geosince there is only one Geometry in the whole domain.
We must assign models to each of our Physics. The
hg phase will be used to simulate a Porosimetry experiment, so it needs a capillary pressure model, and
h2o will be used in a permeability simulation so we must define a hydraulic conductance. The following shows how to fetch models from the
models library, attach them to the target object, and specify the model parameters:
>>> model = op.models.physics.capillary_pressure.washburn >>> phys_hg.add_model(propname='throat.entry_pressure', ... model=model, ... contact_angle='pore.contact_angle', ... surface_tension='pore.surface_tension') >>> model = op.models.physics.hydraulic_conductance.hagen_poiseuille >>> phys_h2o.add_model(propname='throat.hydraulic_conductance', ... model=model, ... pore_viscosity='pore.viscosity', ... pore_area='pore.area', ... throat_area='throat.area', ... conduit_lengths='throat.conduit_lengths')
We are now ready to conduct some simulations. The most important step in validating a pore network model is to ensure that it reproduces experimentally measured porosimetry curves and absolute permeability.
>>> mip = op.algorithms.Porosimetry(network=pn) >>> mip.setup(phase=hg) >>> mip.set_inlets(pn.pores(['left', 'right', 'top', 'bottom', 'front', ... 'back'])) >>> mip.run(points=25)
Which can be visualized using the
plot_intrusion_curve method of the Porosimetry class:
Similarly for the permeability calculation:
>>> perm = op.algorithms.StokesFlow(network=pn) >>> perm.setup(phase=h2o) >>> perm.set_value_BC(pores=pn.pores('left'), values=1) >>> perm.set_value_BC(pores=pn.pores('right'), values=0) >>> # perm.run()
The above code solves for the pressure in each pore and stores the result as
perm['pore.pressure']. To find the permeability of the network, there is a
calc_eff_permeability method on the StokeFlow class:
>>> perm.domain_area = (10*0.0001)**2 >>> perm.domain_length = (10*0.0001) >>> # K = perm.calc_eff_permeability()
calc_eff_permeabilitymethod finds K by inverting Darcy’s law, and looking up all the necessary information (pressure drop, viscosity) from the objects which the algorithm is associated.
- If the domain area and length are not given, an attempt is made to estimate them but it’s more accurate to provide it.
Now that the simulation is finished, it can be saved to a
.pnm file for future use. OpenPNM has two levels of management: the Workspace and the Project. Each Project contains a single network and its associated object (all the code in this guide are a single Project). The Workspace contains all the active Projects. You can save the entire Workspace including all active Projects, or you can save a single Project.
Each object has a
project attribute which returns a handle to the Project to which it belongs.
>>> proj = pn.project # Retrieve the project handle
The Project object offers several useful tools, including the ability to
export_data to various formats, including VTK for viewing in Paraview. Using Paraview provides much better visualization than the
plot_coordinates used above: