![]() The flow domain is discretized by a grid containing cells. MODFLOW is a modular finite-difference model solving the groundwater flow equation in three dimensions and it is used to simulate the flow of groundwater through aquifers. ![]() MODFLOW-2005 is based on the Darcy equation (Darcy, 1856): THEORETICAL BACKGROUND Flow model (MODFLOW) The INOWAS platform furthermore provides optimization algorithms to find the best location for an ASR well using a calibrated groundwater flow and solute transport model. Solute transport (MT3DMS)) as well as variable-density flow (see T03c. In addition, solute transport using MT3DMS can be added to the groundwater flow model (see T03b. The tool is based on MODFLOW-2005 (Harbaugh, 2005) and FloPy (Bakker et al., 2016) and enables the user to create, write and read input and output files as well as calculate models. ![]() The INOWAS tool helps to setup a new MODFLOW model for a study area in order to better understand the local groundwater flow system or as a basis for further scenario analysis (see T07. The most widely applied numerical model for MAR assessment is MODFLOW which is a numerical groundwater flow model developed by the USGS (Harbaugh, 2005 Ringleb et al., 2016). This tool can be used for setting up a new numerical groundwater flow and solute transport model.
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