Active Learning · Groundwater · IGW-NET
The foundational physics, one idea at a time — flow, pumping, contamination, remediation, and surface-water exchange. Groundwater is the hardest water science to teach because the system is invisible; these lessons make it visible. Pose a question, run the model, and watch the aquifer answer.
0 clipsThe four engines of contaminant fate — advection, dispersion, sorption, and decay — isolated one at a time.
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0 clipsCones of depression, well interference, and how transmissivity and storage shape an aquifer’s response to pumping.
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0 clipsHow plumes form, spread, and reach wells — sources, pathways, and the journey from spill to receptor.
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0 clipsPump-and-treat, capture zones, and reactive barriers — and why heterogeneity makes cleanup slow.
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0 clipsStreams, lakes, and aquifers as one system — gaining and losing reaches and the exchange between them.
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0 clipsHow conductivity, storage, and stream penetration control the exchange between a stream and its aquifer.
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0 clipsCapture zones and time-of-travel — delineating the land area that drains to a drinking-water well.
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0 clipsTopography-driven flow — local, intermediate, and regional cells, recharge and discharge zones, stagnation points.
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0 clipsFlow bends at conductivity contrasts — the tangent law, and why water runs along high-K layers and across confining beds.
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0 clipsFlow nets, uplift, exit gradients, and piping — and how sheet piles control seepage beneath a dam.
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0 clipsBanking water underground — injection, storage, and recovery, and what controls recovery efficiency.
Open lesson →Every lesson here runs on the live engine. Open IGW-NET and build the model yourself — free, in the browser, nothing to install.