✖Reynolds Number is the ratio of inertial forces to viscous forces within a fluid which is subjected to relative internal movement due to different fluid velocities.ⓘ Reynolds Number [Re]			+10% -10%
✖Kinematic Viscosity in Stokes is a measure of a fluid's internal resistance to flow under the influence of gravity. It is defined as the ratio of the dynamic viscosity to the fluid's density.ⓘ Kinematic Viscosity in Stokes [ν_stokes]			+10% -10%
✖Representative Particle Size is the size of sediment particles that best represent the overall distribution of particle sizes in a sediment sample or bed material.ⓘ Representative Particle Size [d_a]			+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 given Reynolds Number of Value Unity [V]

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Apparent Velocity of Seepage given Reynolds Number of Value Unity

Formula

`"V" = ("Re"*"ν"_{"stokes"})/"d"_{"a"}`

Example

`"24.00662m/s"=("5000"*"7.25St")/"0.151m"`

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Apparent Velocity of Seepage given Reynolds Number of Value Unity Solution

STEP 0: Pre-Calculation Summary

Formula Used

Apparent Velocity of Seepage = (Reynolds Number*Kinematic Viscosity in Stokes)/Representative Particle Size
V = (Re*ν_stokes)/d_a
This formula uses 4 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.
Reynolds Number - Reynolds Number is the ratio of inertial forces to viscous forces within a fluid which is subjected to relative internal movement due to different fluid velocities.
Kinematic Viscosity in Stokes - (Measured in Square Meter per Second) - Kinematic Viscosity in Stokes is a measure of a fluid's internal resistance to flow under the influence of gravity. It is defined as the ratio of the dynamic viscosity to the fluid's density.
Representative Particle Size - (Measured in Meter) - Representative Particle Size is the size of sediment particles that best represent the overall distribution of particle sizes in a sediment sample or bed material.

STEP 1: Convert Input(s) to Base Unit

Reynolds Number: 5000 --> No Conversion Required
Kinematic Viscosity in Stokes: 7.25 Stokes --> 0.000725 Square Meter per Second (Check conversion here)
Representative Particle Size: 0.151 Meter --> 0.151 Meter No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

V = (Re*ν_stokes)/d_a --> (5000*0.000725)/0.151

Evaluating ... ...

V = 24.0066225165563

STEP 3: Convert Result to Output's Unit

24.0066225165563 Meter per Second --> No Conversion Required

FINAL ANSWER

24.0066225165563 ≈ 24.00662 Meter per Second <-- Apparent Velocity of Seepage

(Calculation completed in 00.020 seconds)

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< 11 Darcy's Law Calculators

Apparent Velocity of Seepage given Reynolds Number of Value Unity

Go Apparent Velocity of Seepage = (Reynolds Number*Kinematic Viscosity in Stokes)/Representative Particle Size

Kinematic Viscosity of Water given Reynolds Number of Value Unity

Go Kinematic Viscosity in Stokes = (Apparent Velocity of Seepage*Representative Particle Size)/Reynolds Number

Reynolds Number of Value Unity

Go Reynolds Number = (Apparent Velocity of Seepage*Representative Particle Size)/Kinematic Viscosity in Stokes

Representative Particle Size given Reynolds Number of Value Unity

Go Representative Particle Size = (Reynolds Number*Kinematic Viscosity)/Apparent Velocity of Seepage

Darcy's Law

Go Flow Rate = Hydraulic Conductivity*Cross Sectional Area*Hydraulic Gradient

Coefficient of Permeability when Apparent Velocity of Seepage is considered

Go Coefficient of Permeability = Apparent Velocity of Seepage/Hydraulic Gradient

Hydraulic Gradient when Apparent Velocity of Seepage is considered

Go Hydraulic Gradient = Apparent Velocity of Seepage/Coefficient of Permeability

Apparent Velocity of Seepage

Go Apparent Velocity of Seepage = Coefficient of Permeability*Hydraulic Gradient

Apparent Velocity of Seepage when Discharge and Cross-Sectional Area are considered

Go Apparent Velocity of Seepage = Discharge/Cross Section Area of Porous Medium

Apparent Velocity and Bulk Pore Velocity Relationship

Go Apparent Velocity of Seepage = Bulk Pore Velocity*Porosity of Soil

Bulk Pore Velocity

Go Bulk Pore Velocity = Apparent Velocity of Seepage/Porosity of Soil

Apparent Velocity of Seepage given Reynolds Number of Value Unity Formula

Apparent Velocity of Seepage = (Reynolds Number*Kinematic Viscosity in Stokes)/Representative Particle Size
V = (Re*ν_stokes)/d_a

What is Darcy's Law in Hydrology?

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, a branch of earth sciences.

How to Calculate Apparent Velocity of Seepage given Reynolds Number of Value Unity?

Apparent Velocity of Seepage given Reynolds Number of Value Unity calculator uses Apparent Velocity of Seepage = (Reynolds Number*Kinematic Viscosity in Stokes)/Representative Particle Size to calculate the Apparent Velocity of Seepage, The Apparent Velocity of Seepage given Reynolds Number of Value Unity formula is defined as the volumetric flow rate of fluid per unit area through a porous medium. It is a conceptual velocity that assumes the fluid is moving uniformly through the entire cross-sectional area of the porous medium. Apparent Velocity of Seepage is denoted by V symbol.

How to calculate Apparent Velocity of Seepage given Reynolds Number of Value Unity using this online calculator? To use this online calculator for Apparent Velocity of Seepage given Reynolds Number of Value Unity, enter Reynolds Number (Re), Kinematic Viscosity in Stokes (ν_stokes) & Representative Particle Size (d_a) and hit the calculate button. Here is how the Apparent Velocity of Seepage given Reynolds Number of Value Unity calculation can be explained with given input values -> 24.00662 = (5000*0.000725)/0.151.

FAQ

What is Apparent Velocity of Seepage given Reynolds Number of Value Unity?

The Apparent Velocity of Seepage given Reynolds Number of Value Unity formula is defined as the volumetric flow rate of fluid per unit area through a porous medium. It is a conceptual velocity that assumes the fluid is moving uniformly through the entire cross-sectional area of the porous medium and is represented as V = (Re*ν_stokes)/d_a or Apparent Velocity of Seepage = (Reynolds Number*Kinematic Viscosity in Stokes)/Representative Particle Size. Reynolds Number is the ratio of inertial forces to viscous forces within a fluid which is subjected to relative internal movement due to different fluid velocities, Kinematic Viscosity in Stokes is a measure of a fluid's internal resistance to flow under the influence of gravity. It is defined as the ratio of the dynamic viscosity to the fluid's density & Representative Particle Size is the size of sediment particles that best represent the overall distribution of particle sizes in a sediment sample or bed material.

How to calculate Apparent Velocity of Seepage given Reynolds Number of Value Unity?

The Apparent Velocity of Seepage given Reynolds Number of Value Unity formula is defined as the volumetric flow rate of fluid per unit area through a porous medium. It is a conceptual velocity that assumes the fluid is moving uniformly through the entire cross-sectional area of the porous medium is calculated using Apparent Velocity of Seepage = (Reynolds Number*Kinematic Viscosity in Stokes)/Representative Particle Size. To calculate Apparent Velocity of Seepage given Reynolds Number of Value Unity, you need Reynolds Number (Re), Kinematic Viscosity in Stokes (ν_stokes) & Representative Particle Size (d_a). With our tool, you need to enter the respective value for Reynolds Number, Kinematic Viscosity in Stokes & Representative Particle Size 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 Reynolds Number, Kinematic Viscosity in Stokes & Representative Particle Size. We can use 3 other way(s) to calculate the same, which is/are as follows -

Apparent Velocity of Seepage = Coefficient of Permeability*Hydraulic Gradient
Apparent Velocity of Seepage = Discharge/Cross Section Area of Porous Medium
Apparent Velocity of Seepage = Bulk Pore Velocity*Porosity of Soil

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