Earth & First Responders Pack · Multi-Solver
River Meander
Erosion & migration. This multi-solver chains 1 solvers into a single guided workflow — run each step in order and carry the result forward.
Workflow steps
Groundwater Well DrawdownLive
Thiem steady-state cone of depression
Controls
Presets
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.
Runs locally in your browser — free forever. Scale to the cloud when reality gets heavy.
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Frequently asked questions
- What is the River Meander multi-solver?
- River Meander is a guided workflow that chains 1 individual PolySim solvers into one end-to-end analysis, piping each result into the next step.
- Is it free to use?
- Yes. Every step runs entirely in your browser using real numerics — no install, no account, no cloud cost. Custom or private solver packs are available as a paid service.