The imod
Python package is an open source project to make working with
MODFLOW groundwater models in Python easier. It builds on top of popular
packages such as xarray, pandas, geopandas, dask, and rasterio
to provide a versatile toolset for working with large groundwater modeling
datasets. Some of its core functionalities are:
- Preparing and modifying data from a variety of GIS, scientific, and MODFLOW file formats;
- Regridding, clipping, masking, and splitting MODFLOW 6 models;
- Fast writing of data to MODFLOW-based models;
- Selecting and evaluating, e.g. for time series comparison or water budgets;
- Visualizing cross sections, time series, or 3D animations.
We currently support the following MODFLOW-based kernels:
- USGS MODFLOW 6, structured (DIS) and discretization by vertices (DISV) grids only. Not all advanced stress packages are supported (only LAK and UZF)
- iMOD-WQ, which integrates SEAWAT (density-dependent groundwater flow) and MT3DMS (multi-species reactive transport calculations)
Development currently focuses on supporting more MODFLOW 6 functionalities. iMOD-WQ has been sunset and will no longer be developed.
Seamlessly integrate your GIS rasters or meshes with MODFLOW 6, by using xarray and xugrid arrays, for structured and unstructured grids, respectively, to create grid-based model packages.
import imod
# Open Geotiff with elevation data as xarray DataArray
elevation = imod.rasterio.open("elevation.tif")
# Create idomain grid
layer_template = xr.DataArray([1, 1, 1], dims=('layer',), coords={'layer': [1, 2, 3]})
idomain = layer_template * xr.ones_like(elevation).astype(int)
# Compute bottom elevations of model layers
layer_thickness = xr.DataArray([10.0, 20.0, 10.0], dims=('layer',), coords={'layer': [1, 2, 3]})
bottom = elevation - layer_thickness.cumsum(dim='layer')
# Create MODFLOW 6 DIS package
dis_pkg = imod.mf6.StructuredDiscretization(
idomain=idomain, top=elevation, bottom=bottom.transpose("layer", "y", "x")
)
Assign wells based on x, y coordinates and filter screen depths, instead of layer, row and column:
# Specify well locations
x = [150_200.0, 160_800.0]
y = [450_300.0, 460_200.0]
# Specify well screen depths
screen_top = [0.0, 0.0]
screen_bottom = [-4.0, -10.0]
# Specify flow rate, which changes over time.
weltimes = pd.date_range("2000-01-01", "2000-01-03", freq="2D")
well_rates_period1 = [0.5, 1.0]
well_rates_period2 = [2.5, 3.0]
rate = xr.DataArray([well_rates_period1, well_rates_period2], coords={"time": weltimes}, dims=("time","index"))
# Now construct the Well package
wel_pkg = imod.mf6.Well(x=x, y=y, rate=rate, screen_top=screen_top, screen_bottom=screen_bottom)
iMOD Python will take care of the rest and assign the wells to the correct model layers upon writing the model. It will furthermore distribute well rates based on transmissivities. To verify how wells will be assigned to MODFLOW 6 cells before writing the entire simulation, you can use the following command:
# Wells have been distributed across two model layers based on screen depths.
wel_mf6_pkg = wel_pkg.to_mf6(idomain, top, bottom, k=1.0)
print(wel_mf6_pkg["cellid"])
# Well rates have been distributed based on screen overlap
print(wel_mf6_pkg["rate"])
A common problem in groundwater modeling is to assign 2D river or drain grids to 3D model layers. iMOD Python has utilities to do this, supporting all kinds of different methods. Furthermore, it can help you distribute the conductance across layers.
MODFLOW 6 requires that all stress periods are defined in the time discretization package. However, usually boundary conditions are defined at inconsistent times. iMOD Python can help you to create a time discretization package that is consistent, based on all the unique times assigned to the boundary conditions.
# First add the packages to the simulation. NOTE: To get a functional model,
# more packages are needed than these two.
simulation = imod.mf6.Modflow6Simulation("example")
simulation["gwf"] = imod.mf6.GroundwaterFlowModel()
simulation["gwf"]["dis"] = dis_pkg
simulation["gwf"]["wel"] = wel_pkg
# Create a time discretization based on the times assigned to the packages.
# Specify the end time of the simulation as one of the additional_times
simulation.create_time_discretization(additional_times=["2000-01-07"])
# Note that timesteps in well package are also inserted in the time
# discretization
print(simulation["time_discretization"].dataset)
Regrid MODFLOW 6 models to different grids, even from structured to unstructured grids. iMOD Python takes care of properly scaling the input parameters. You can also configure scaling methods yourself for each input parameter, for example when you want to upscale drainage elevations with the minimum instead of the average.
sim_regridded = simulation.regrid_like(new_unstructured_grid)
# Notice that discretization has converted to VerticesDiscretization (DISV)
print(sim_regridded["gwf"]["dis"])
To reduce the size of your model, you can clip it to a bounding box. This is useful for example when you want to create a smaller model for testing purposes.
sim_clipped = simulation.clip_box(x_min=125_000, x_max=175_000, y_min=425_000, y_max=475_000)
You can even provide states for the model, which will be set on the model boundaries of the clipped model.
# Create a grid of zeros, which will be used to
# set as heads at the boundaries of clipped parts.
head_for_boundary = xr.zeros_like(idomain, dtype=float)
states_for_boundary = {"gwf": head_for_boundary}
sim_clipped = simulation.clip_box(
x_min=125_000, x_max=175_000, y_min=425_000, y_max=475_000, states_for_boundary=states_for_boundary
)
# Notice that a Constant Head (CHD) package has been created for the clipped
# model.
print(sim_clipped["gwf"])
iMOD Python efficiently writes MODFLOW 6 models to disk, especially large models.
Tests we have conducted for the Dutch National Groundwater Model (LHM) show that
iMOD Python can write a model with 21.84 million cells 5 to 60 times faster (for
respectively 1 and 365 stress periods) than the alternative Flopy package.
Furthermore imod
can even write models that are larger than the available
memory, using dask arrays.
NOTE: We don't hate Flopy, nor seek its demise. iMOD developers also contribute and aid in the development of Flopy.
Models made with iMOD5 can be imported into iMOD Python, provided that they are defined in a projectfile.
# Open projectfile data
imod5_data, period_data = imod.formats.prj.open_projectfile_data("path/to/projectfile.prj")
# Specify times for the simulation, this will be used to resample iMOD5 wells
# to and to set the time discretization
times = [np.datetime64("2000-01-01"), np.datetime64("2000-01-02"), np.datetime64("2000-01-03")]
# Create a simulation object
simulation = imod.mf6.Modflow6Simulation.from_imod5_data(imod5_data, period_data, times)
See this page for a full list of supported iMO5 functionalities.
If you are not interested in deriving models from spatial data, but just want to allocate boundary conditions based on layer, row, column numbers, or create a model of a 2D cross-section: You are better off using Flopy.
Currently, we don't support the following MODFLOW 6 features:
- timeseries files
- DISU package
- Groundwater Energy Model (GWE)
- Streamflow routing (SFR) package (in development)
- Ghost Node Correction (GNC) package
- Multi-aquifer well (MAW) package
- Water mover (MVR) package
- Particle tracking (PRT)
Most of these features can be implemented with some effort, but we have not prioritized them yet. The exceptions are the DISU package and the timeseries files, which would require significant work to our backend. As a result, we will likely not support these two features in the foreseeable future. If you need any of the other features, feel free to open an issue on our GitHub page.
Documentation: https://deltares.github.io/imod-python
Source code: https://github.com/Deltares/imod-python