For Researchers · Groundwater Drawdown
Groundwater Drawdown for an ice age
Built for researchers prototyping or validating an idea. Prototype fast, reproduce exactly, and share a citable, interactive version of your model. Simulate an ice age live below — adjust the inputs and watch it respond, right in your browser.
Groundwater Well DrawdownLive
Thiem steady-state cone of depression
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Pumping a well lowers the water table into a cone of depression. Under the Thiem steady-state solution the drawdown is s(r) = Q/(2πT)·ln(R/r): more pumping deepens the cone, higher transmissivity flattens it. Fundamental to well design, water supply, and contaminant capture.
Data Inspector
Drawdown at well4.7 m
Drawdown at 50 m1.47 m
Radius of influence500 m
Governing equation
Reading this result: Drawdown is Q/(2πT)·ln(R/r): here it is about 4.7 m at the well and falls off logarithmically, so most of the depression sits in the first tens of metres.
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Frequently asked questions
- Is this good for researchers?
- Yes — this version of "Groundwater Drawdown for an ice age" is framed for researchers prototyping or validating an idea. Prototype fast, reproduce exactly, and share a citable, interactive version of your model.
- Do I need to install anything?
- No. It runs in any modern browser, free, with no account required.