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Surface domain represented as 2-D overland flow.
HGS dynamically integrates key components of the hydrologic cycle such as evaporation from bare soil and water bodies, vegetation-dependent transpiration with root uptake, snowmelt and soil freeze/thaw. Features such as macro pores, fractures, and tile drains can either be incorporated discretely or using a dual-porosity, dual permeability formulation.
The Aquanty team specializes in the development and application of fully-integrated surface and subsurface flow and transport models using HGS. Our models have been applied in many water management settings including the assessment of climate change impacts on basin scale water management, detailed mine closure design assessments, nuclear waste repository design, sea water intrusion, contaminant transport, and agricultural applications.
Matrix diffusion effects and solute advection in the matrix.
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