Apparent Velocity of Seepage Calculator

✖Coefficient of Permeability is a measure of the ability of a porous material to allow fluids to pass through it. It is a key parameter which deals with the movement, distribution of water resources.ⓘ Coefficient of Permeability [K'']			+10% -10%
✖Hydraulic Gradient is the slope of the hydraulic head (or piezometric head) along the direction of flow in a given medium.ⓘ Hydraulic Gradient [dhds]			+10% -10%

✖Apparent Velocity of Seepage is the velocity at which groundwater moves through the porous medium, as observed over a larger scale.ⓘ Apparent Velocity of Seepage [V]

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Apparent Velocity of Seepage Solution

STEP 0: Pre-Calculation Summary

Formula Used

Apparent Velocity of Seepage = Coefficient of Permeability*Hydraulic Gradient
V = K''*dhds
This formula uses 3 Variables

Variables Used

Apparent Velocity of Seepage - (Measured in Meter per Second) - Apparent Velocity of Seepage is the velocity at which groundwater moves through the porous medium, as observed over a larger scale.
Coefficient of Permeability - (Measured in Meter per Second) - Coefficient of Permeability is a measure of the ability of a porous material to allow fluids to pass through it. It is a key parameter which deals with the movement, distribution of water resources.
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

Coefficient of Permeability: 10 Meter per Second --> 10 Meter per Second No Conversion Required
Hydraulic Gradient: 2.4 --> No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

V = K''*dhds --> 10*2.4

Evaluating ... ...

V = 24

STEP 3: Convert Result to Output's Unit

24 Meter per Second --> No Conversion Required

FINAL ANSWER

24 Meter per Second <-- Apparent Velocity of Seepage

(Calculation completed in 00.004 seconds)

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Created by Mithila Muthamma PA

Coorg Institute of Technology (CIT), Coorg

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Meerut Institute of Engineering and Technology (MIET), Meerut

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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

Apparent Velocity of Seepage Formula

LaTeX Go

Apparent Velocity of Seepage = Coefficient of Permeability*Hydraulic Gradient
V = K''*dhds

What is Darcy's Law?

Darcy's law is an equation that describes the flow of a fluid through a porous medium. The law was formulated by Henry Darcy based on results of experiments on the flow of water through beds of sand, forming the basis of hydrogeology.

How to Calculate Apparent Velocity of Seepage?

Apparent Velocity of Seepage calculator uses Apparent Velocity of Seepage = Coefficient of Permeability*Hydraulic Gradient to calculate the Apparent Velocity of Seepage, The Apparent Velocity of Seepage formula is defined as the flow rate of water through a porous medium. It is defined by Darcy's Law and is calculated as the volumetric flow rate per unit area of the medium. The design of hydraulic structures like dams, levees, and groundwater recharge facilities requires knowledge of seepage velocities to ensure stability and prevent failure due to uncontrolled seepage or piping. Apparent Velocity of Seepage is denoted by V symbol.

How to calculate Apparent Velocity of Seepage using this online calculator? To use this online calculator for Apparent Velocity of Seepage, enter Coefficient of Permeability (K'') & Hydraulic Gradient (dhds) and hit the calculate button. Here is how the Apparent Velocity of Seepage calculation can be explained with given input values -> 24 = 10*2.4.

FAQ

What is Apparent Velocity of Seepage?

The Apparent Velocity of Seepage formula is defined as the flow rate of water through a porous medium. It is defined by Darcy's Law and is calculated as the volumetric flow rate per unit area of the medium. The design of hydraulic structures like dams, levees, and groundwater recharge facilities requires knowledge of seepage velocities to ensure stability and prevent failure due to uncontrolled seepage or piping and is represented as V = K''*dhds or Apparent Velocity of Seepage = Coefficient of Permeability*Hydraulic Gradient. Coefficient of Permeability is a measure of the ability of a porous material to allow fluids to pass through it. It is a key parameter which deals with the movement, distribution of water resources & Hydraulic Gradient is the slope of the hydraulic head (or piezometric head) along the direction of flow in a given medium.

How to calculate Apparent Velocity of Seepage?

The Apparent Velocity of Seepage formula is defined as the flow rate of water through a porous medium. It is defined by Darcy's Law and is calculated as the volumetric flow rate per unit area of the medium. The design of hydraulic structures like dams, levees, and groundwater recharge facilities requires knowledge of seepage velocities to ensure stability and prevent failure due to uncontrolled seepage or piping is calculated using Apparent Velocity of Seepage = Coefficient of Permeability*Hydraulic Gradient. To calculate Apparent Velocity of Seepage, you need Coefficient of Permeability (K'') & Hydraulic Gradient (dhds). With our tool, you need to enter the respective value for Coefficient of Permeability & Hydraulic Gradient and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.

How many ways are there to calculate Apparent Velocity of Seepage?

In this formula, Apparent Velocity of Seepage uses Coefficient of Permeability & Hydraulic Gradient. We can use 3 other way(s) to calculate the same, which is/are as follows -

Apparent Velocity of Seepage = Discharge/Cross Section Area of Porous Medium
Apparent Velocity of Seepage = (Reynolds Number*Kinematic Viscosity in Stokes)/Representative Particle Size
Apparent Velocity of Seepage = Bulk Pore Velocity*Porosity of Soil

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