Seepage Discharge Formula:
Definition: Seepage discharge is the volume of water flowing through the dam's soil in unit time, which is crucial for dam stability analysis.
Purpose: This calculator helps civil engineers estimate water seepage through earth dams to ensure proper design and safety measures.
The calculator uses Darcy's law formula:
Where:
Explanation: The formula calculates how much water passes through the dam's soil based on permeability, hydraulic gradient, area, and time.
Details: Accurate seepage estimation prevents dam failure, controls water loss, and ensures structural integrity by identifying potential piping risks.
Tips: Enter the coefficient of permeability (default 0.1 m/s), hydraulic gradient (default 2.02 ±5%), cross-sectional area (default 13 m²), and time (default 6 s).
Q1: What is a typical permeability coefficient for earth dams?
A: It varies from 10-9 m/s (clay) to 10-3 m/s (gravel). Common earth dam materials range 10-6 to 10-4 m/s.
Q2: Why is hydraulic gradient important?
A: It represents the driving force for seepage. High gradients may indicate potential erosion (piping) risks.
Q3: How do I measure cross-sectional area?
A: It's the area perpendicular to flow direction, typically the dam's base width × height of seepage zone.
Q4: What affects permeability coefficient?
A: Soil type, compaction, saturation, and particle size distribution significantly influence permeability.
Q5: How accurate are these calculations?
A: Results are estimates (±5%). Field tests provide more accurate permeability values for critical projects.