Darcy's Law Calculator
An aquifer with K = 10 m/day and a 2 m head drop over 100 m passes 10 m³/day through a 50 m² cross-section.
10 m³/day
- Hydraulic gradient i = Δh/L
- 0.02
- Darcy velocity q = Ki
- 0.2 m/day
- Seepage (average linear) velocity q/nₑ
- 0.8 m/day
- Travel time over L
- 125 days
Step-by-step solution
- i = Δh ÷ L = 2 ÷ 100 = 0.02
- Q = K i A = 0.0001157407407 m/s × 0.02 × 50 m² = 10 m³/day
- Seepage velocity = q ÷ nₑ = 0.8 m/day
Darcy's Law Formula
Q = K i A, i = Δh/L
Darcy velocity q = Ki; seepage (linear) velocity = q/nₑ
Worked Example
An aquifer with K = 10 m/day, 2 m head drop over 100 m and 50 m² cross-section:
- i = Δh ÷ L = 2 ÷ 100 = 0.02
- Q = K i A = 0.0001157407407 m/s × 0.02 × 50 m² = 10 m³/day
- Seepage velocity = q ÷ nₑ = 0.8 m/day
Darcy velocity q = Ki: 0.2 m/day · Seepage (average linear) velocity q/nₑ: 0.8 m/day · Travel time over L: 125 days
GATE tip
Transmissivity T = Kb for a confined aquifer of thickness b. Questions often give T, so Q = T i W for a strip of width W.
More Hydraulics and Groundwater Calculators
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Well Yield Calculator
Confined: Q = 2πKb(h₂ − h₁)/ln(r₂/r₁)
unconfined: Q = πK(h₂² − h₁²)/ln(r₂/r₁)
Example: A confined aquifer, K = 20 m/day, 30 m thick, with heads 40 m at the 0.15 m well and 45 m at 300 m: Well discharge Q = 2479.91 m³/day.
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Manning's Equation Calculator
V = (1/n) R^(2/3) S^(1/2), Q = VA
R = A/P hydraulic radius; SI units (multiply by 1.49 in US units)
Example: A 2 m wide concrete rectangular channel flowing 0.5 m deep at a slope of 0.001: Discharge Q = 1.01351 m³/s.
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Critical Depth Calculator
y_c = (q²/g)^(1/3), E_c = 1.5 y_c
specific energy E = y + q²/(2gy²); V_c = √(g y_c)
Example: A rectangular channel carrying 2 m²/s per metre width: Critical depth y_c = 0.741617 m.
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Hydraulic Jump Calculator
y₂/y₁ = ½(√(1 + 8F₁²) − 1)
F₁ = V₁/√(gy₁); head loss h_L = (y₂ − y₁)³/(4y₁y₂)
Example: Flow 0.3 m deep at 6 m/s entering a 3 m wide stilling basin: Sequent depth y₂ = 1.34167 m.
Frequently asked questions
Why is seepage velocity faster than Darcy velocity?
Water moves only through the pores, so the actual speed is the Darcy flux divided by the effective porosity: four times faster at 25 %.
When does Darcy’s law fail?
At high Reynolds numbers in coarse gravel or karst, where flow becomes non-linear, and in very fine clays with threshold gradients.
Sources
- The International System of Units (SI), 9th edition (SI Brochure), Bureau International des Poids et Mesures .
Last reviewed: . Factors are stored exactly and computed with 50-digit decimal arithmetic. See how we verify conversion factors.
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APA
Scientific Converters. (2026, October 15). Darcy's Law Calculator. Retrieved October 25, 2026, from https://scientificconverters.com/calculators/darcys-law-calculator/
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Scientific Converters, "Darcy's Law Calculator," scientificconverters.com. Accessed: Oct. 25, 2026. [Online]. Available: https://scientificconverters.com/calculators/darcys-law-calculator/