Well Yield Calculator
A well in a 30 m thick confined aquifer with K = 20 m/day and 5 m of drawdown to the radius of influence yields 2479.91 m³/day.
2479.9102503776 m³/day
Full answer, then cut to fewer decimals (not rounded):
- 2479.9102503776 m³/day
- 2479.910250377 m³/day
- 2479.91025037 m³/day
- 2479.9102503 m³/day
- 2479.910250 m³/day
- 2479.91025 m³/day
- 2479.9102 m³/day
- 2479.910 m³/day
- 2479.91 m³/day
- 2479.9 m³/day
- In litres per second
- 28.70266493 L/s
- Transmissivity T = Kb
- 600 m²/day
- Drawdown between the points
- 5 m
Step-by-step solution
- Q = 2πKb(h₂ − h₁) ÷ ln(r₂/r₁) = 2π × 20 × 30 × 5 ÷ 7.60090246
- Q = 2479.91025 m³/day
Well Yield Formula
Confined: Q = 2πKb(h₂ − h₁)/ln(r₂/r₁)
unconfined: Q = πK(h₂² − h₁²)/ln(r₂/r₁)
Worked 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:
- Q = 2πKb(h₂ − h₁) ÷ ln(r₂/r₁) = 2π × 20 × 30 × 5 ÷ 7.60090246
- Q = 2479.91025 m³/day
Transmissivity T = Kb: 600 m²/day · Drawdown between the points: 5 m
GATE tip
With drawdowns s₁, s₂ at two observation wells in a confined aquifer, Q = 2πT(s₁ − s₂)/ln(r₂/r₁). Use this to back out T from a pumping test.
More Hydraulics and Groundwater Calculators
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Darcy's Law Calculator
Q = K i A, i = Δh/L
Darcy velocity q = Ki; seepage (linear) velocity = q/nₑ
Example: An aquifer with K = 10 m/day, 2 m head drop over 100 m and 50 m² cross-section: Discharge Q = 10 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.
-
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
What is the radius of influence?
The distance beyond which pumping no longer lowers the water table measurably. It appears inside a logarithm, so rough estimates still give reasonable yields.
Why do unconfined aquifers use h²?
The saturated thickness itself falls near the well, so the flow area shrinks; integrating gives the h² difference.
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). Well Yield Calculator. Retrieved October 25, 2026, from https://scientificconverters.com/calculators/well-yield-calculator/
IEEE
Scientific Converters, "Well Yield Calculator," scientificconverters.com. Accessed: Oct. 25, 2026. [Online]. Available: https://scientificconverters.com/calculators/well-yield-calculator/