MCP For Claude Marketplace
Groundwater Inflow Predictor

Groundwater Inflow Predictor MCP Connector for Claude

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Predicts groundwater inflow, drawdown, and seepage patterns for excavations.

4 tools Official Updated Oct 1, 2026 Official Vinkius Partner
More Details Connect to Claude

This MCP server provides analytical tools to model groundwater behavior around excavations. It allows users to calculate steady-state inflow using get_steady_state_inflow, model time-dependent progression with get_transient_inflow_progression, map water level reductions via calculate_drawdown_profile, and evaluate flow directionality through analyze_seepage_patterns.

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4 tools expose this connector's capabilities to your AI agent.

analyze_seepage_patterns

Determines the direction and intensity of water movement

calculate_drawdown_profile

Maps the reduction in water level at various distances from the excavation

get_steady_state_inflow

Calculates the steady-state groundwater inflow rate into an excavation

get_transient_inflow_progression

Predicts the time-dependent progression of groundwater inflow

See how to talk to your AI agent using Groundwater Inflow Predictor.

What is the steady-state inflow for an aquifer with 1e-4 permeability, 10m thickness, 0.05 gradient, and 50m perimeter?

The steady-state inflow rate is 2.5 m³/s with a total drawdown of 4.2m and a seepage velocity of 0.15 m/s.

Predict the inflow progression starting at 10 m³/s, heading to 50 m³/s, with storativity of 0.2 at times 1, 5, and 10 minutes.

At 1 minute, the inflow is 15.2 m³/s; at 5 minutes, it is 32.8 m³/s; and at 10 minutes, it reaches 41.5 m³/s.

Analyze the seepage patterns for an excavation 20m wide, 15m deep, with a 0.03 hydraulic gradient.

The water flow is convergent with an intensity index of 0.85 and a convergence factor of 1.2.

You can use the `get_steady_state_inflow` tool by providing the aquifer permeability, thickness, hydraulic gradient, and excavation perimeter.

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