Darcy's Law Solution

STEP 0: Pre-Calculation Summary
Formula Used
Flow Rate = Hydraulic Conductivity*Cross Sectional Area*Hydraulic Gradient
qflow = K*Acs*dhds
This formula uses 4 Variables
Variables Used
Flow Rate - (Measured in Cubic Meter per Second) - Flow Rate is the volume of water passing through a specific cross-section of a river, stream, or any conduit per unit of time.
Hydraulic Conductivity - (Measured in Meter per Second) - Hydraulic Conductivity is a property of porous materials (such as soil or rock) that describes the ease with which water can move through pore spaces or fractures.
Cross Sectional Area - (Measured in Square Meter) - Cross Sectional Area is the area of a specific section of a stream, river, or other water body perpendicular to the direction of flow.
Hydraulic Gradient - Hydraulic Gradient is the slope of the hydraulic head (or piezometric head) along the direction of flow in a given medium.
STEP 1: Convert Input(s) to Base Unit
Hydraulic Conductivity: 0.77 Meter per Second --> 0.77 Meter per Second No Conversion Required
Cross Sectional Area: 13 Square Meter --> 13 Square Meter No Conversion Required
Hydraulic Gradient: 2.4 --> No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
qflow = K*Acs*dhds --> 0.77*13*2.4
Evaluating ... ...
qflow = 24.024
STEP 3: Convert Result to Output's Unit
24.024 Cubic Meter per Second --> No Conversion Required
FINAL ANSWER
24.024 Cubic Meter per Second <-- Flow Rate
(Calculation completed in 00.004 seconds)

Credits

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Created by Mithila Muthamma PA
Coorg Institute of Technology (CIT), Coorg
Mithila Muthamma PA has created this Calculator and 2000+ more calculators!
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Verified by Himanshi Sharma
Bhilai Institute of Technology (BIT), Raipur
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Darcy's Law Calculators

Darcy's Law
​ LaTeX ​ Go Flow Rate = Hydraulic Conductivity*Cross Sectional Area*Hydraulic Gradient
Coefficient of Permeability when Apparent Velocity of Seepage is considered
​ LaTeX ​ Go Coefficient of Permeability = Apparent Velocity of Seepage/Hydraulic Gradient
Apparent Velocity of Seepage
​ LaTeX ​ Go Apparent Velocity of Seepage = Coefficient of Permeability*Hydraulic Gradient
Apparent Velocity of Seepage when Discharge and Cross-Sectional Area are considered
​ LaTeX ​ Go Apparent Velocity of Seepage = Discharge/Cross Section Area of Porous Medium

Darcy's Law Formula

​LaTeX ​Go
Flow Rate = Hydraulic Conductivity*Cross Sectional Area*Hydraulic Gradient
qflow = K*Acs*dhds

What does Darcy's Law determine?

Darcy's law is the equation that defines the ability of a fluid to flow through porous media such as rock.

How to Calculate Darcy's Law?

Darcy's Law calculator uses Flow Rate = Hydraulic Conductivity*Cross Sectional Area*Hydraulic Gradient to calculate the Flow Rate, The Darcy's Law formula is defined as the discharge rate of a fluid through a porous medium is directly proportional to the hydraulic gradient and the cross-sectional area of the flow, and inversely proportional to the medium's resistance to flow. Flow Rate is denoted by qflow symbol.

How to calculate Darcy's Law using this online calculator? To use this online calculator for Darcy's Law, enter Hydraulic Conductivity (K), Cross Sectional Area (Acs) & Hydraulic Gradient (dhds) and hit the calculate button. Here is how the Darcy's Law calculation can be explained with given input values -> 24.024 = 0.77*13*2.4.

FAQ

What is Darcy's Law?
The Darcy's Law formula is defined as the discharge rate of a fluid through a porous medium is directly proportional to the hydraulic gradient and the cross-sectional area of the flow, and inversely proportional to the medium's resistance to flow and is represented as qflow = K*Acs*dhds or Flow Rate = Hydraulic Conductivity*Cross Sectional Area*Hydraulic Gradient. Hydraulic Conductivity is a property of porous materials (such as soil or rock) that describes the ease with which water can move through pore spaces or fractures, Cross Sectional Area is the area of a specific section of a stream, river, or other water body perpendicular to the direction of flow & Hydraulic Gradient is the slope of the hydraulic head (or piezometric head) along the direction of flow in a given medium.
How to calculate Darcy's Law?
The Darcy's Law formula is defined as the discharge rate of a fluid through a porous medium is directly proportional to the hydraulic gradient and the cross-sectional area of the flow, and inversely proportional to the medium's resistance to flow is calculated using Flow Rate = Hydraulic Conductivity*Cross Sectional Area*Hydraulic Gradient. To calculate Darcy's Law, you need Hydraulic Conductivity (K), Cross Sectional Area (Acs) & Hydraulic Gradient (dhds). With our tool, you need to enter the respective value for Hydraulic Conductivity, Cross Sectional Area & Hydraulic Gradient and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
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