SIMULATION OF GROUNDWATER FLOW REGIME: A CASE OF YALA RIVER CATCHMENT, KENYA
DOI:
https://doi.org/10.33736/jcest.10765.2026Keywords:
Aquifer, groundwater, hydrogeology, recharge, visual-MODFLOWAbstract
The hydrogeological regime that includes the vadose and phreatic zones significantly supports the hydrological cycle and influences surface and groundwater bodies for a sustainable ecosystem. Since these zones are unseen, they are prone to anthropogenic threats, which include groundwater overabstraction, reduced infiltration or aquifer recharge, and adversity from climate change. There is also inadequate knowledge of groundwater capacity and flow regime in catchments. This study developed hydrogeological knowledge to understand the groundwater flow regime and provide a decision tool for catchment management. The model was developed using Visual MODFLOW and ran through a set of scenarios to widely understand hydrogeological aspects in the Yala River catchment. While running the model through day 147 to 190, the trends indicated a maximum head of 0.00624 m and a minimum of -0.00676 m. The head changes recorded a maximum of 0.00524 m and a minimum of -0.0068 m with the residual of less than 2, indicating that the verifications were within acceptable levels. It was observed that the catchment storage improved from 0.050238 m3/day in the reference scenario to 7.16 m3/day, and when the catchment was assumed to be well managed, the model’s groundwater inflow-outflow difference increased to 429 m3/day, an increase of 422.4 m3/day in the zonal unit, which gave a 98.33% increase. There was evidence of groundwater backflow at the midblock, indicating the development of a cone of depression that requires further research. It is worth noting that the boundary conditions used in the calibrated model were representative combinations of selected parameter values and boundary conditions. This model can be replicated for simulation of the hydrogeological flow regime in other catchments with similar or relative geographical characteristics.
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