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 velocity with which groundwater moves through the bulk of the porous medium.
Coefficient of Permeability - (Measured in Meter per Second) - The coefficient of permeability is the velocity in m or cm/s of water through soils. Fine-grained soils have values (of 10-8m/sec) or sand and gravel could be (10-4m/sec).
Hydraulic Gradient - Hydraulic Gradient due to gravity is the ratio of difference in height of water to that of the horizontal distance between the wells or a specific measurement of liquid pressure above vertical datum.
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)

Credits

Created by Mithila Muthamma PA
Coorg Institute of Technology (CIT), Coorg
Mithila Muthamma PA has created this Calculator and 2000+ more calculators!
Verified by Ishita Goyal
Meerut Institute of Engineering and Technology (MIET), Meerut
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11 Darcy's Law Calculators

Representative Particle Size given Reynolds Number of Value Unity
Go Representative Particle Size = (Reynolds Number*Kinematic Viscosity)/Apparent Velocity of Seepage
Kinematic Viscosity of Water given Reynolds Number of Value Unity
Go Kinematic Viscosity = (Apparent Velocity of Seepage*Representative Particle Size)/Reynolds Number
Apparent Velocity of Seepage given Reynolds Number of Value Unity
Go Apparent Velocity of Seepage = (Reynolds Number*Kinematic Viscosity)/Representative Particle Size
Reynolds Number of Value Unity
Go Reynolds Number = (Apparent Velocity of Seepage*Representative Particle Size)/Kinematic Viscosity
Darcy's Law
Go Rate of Flow = -Hydraulic Conductivity*Cross-Sectional Area*Hydraulic Gradient
Apparent velocity of seepage when discharge and cross-sectional area are considered
Go Apparent Velocity of Seepage = Discharge/Cross section area of the porous medium
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 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 Formula

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 is defined as the velocity with which groundwater moves through the bulk of the porous medium. 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 is defined as the velocity with which groundwater moves through the bulk of the porous medium and is represented as V = K*dhds or Apparent Velocity of Seepage = Coefficient of Permeability*Hydraulic Gradient. The coefficient of permeability is the velocity in m or cm/s of water through soils. Fine-grained soils have values (of 10-8m/sec) or sand and gravel could be (10-4m/sec) & Hydraulic Gradient due to gravity is the ratio of difference in height of water to that of the horizontal distance between the wells or a specific measurement of liquid pressure above vertical datum.
How to calculate Apparent Velocity of Seepage?
The Apparent Velocity of Seepage is defined as the velocity with which groundwater moves through the bulk of the porous medium 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 the porous medium
  • Apparent Velocity of Seepage = (Reynolds Number*Kinematic Viscosity)/Representative Particle Size
  • Apparent Velocity of Seepage = Bulk Pore Velocity*Porosity of soil
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