Coefficient of Permeability at Temperature of Permeameter Experiment Calculator

✖The Discharge referred as volumetric flow rate of water that is transported through a given cross-sectional area. It includes any suspended solids, dissolved chemicals, or biologic material.ⓘ Discharge [Q]			+10% -10%
✖The Cross-Sectional Area is referred as product of width multiplied by average water depth.ⓘ Cross-Sectional Area [A]			+10% -10%
✖The Constant Head Difference is referred as difference between the hydraulic head or pressure difference separated by a small distance dl.ⓘ Constant Head Difference [ΔH]			+10% -10%
✖The Length referred as measurement or extent of something from end to end.ⓘ Length [L]			+10% -10%

✖The Coefficient of Permeability at 20° C refers to the measure of a porous medium’s ability to allow fluid flow through its voids.ⓘ Coefficient of Permeability at Temperature of Permeameter Experiment [K]

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Coefficient of Permeability at Temperature of Permeameter Experiment Solution

STEP 0: Pre-Calculation Summary

Formula Used

Coefficient of Permeability at 20° C = (Discharge/Cross-Sectional Area)*(1/(Constant Head Difference/Length))
K = (Q/A)*(1/(ΔH/L))
This formula uses 5 Variables

Variables Used

Coefficient of Permeability at 20° C - (Measured in Meter per Second) - The Coefficient of Permeability at 20° C refers to the measure of a porous medium’s ability to allow fluid flow through its voids.
Discharge - (Measured in Cubic Meter per Second) - The Discharge referred as volumetric flow rate of water that is transported through a given cross-sectional area. It includes any suspended solids, dissolved chemicals, or biologic material.
Cross-Sectional Area - (Measured in Square Meter) - The Cross-Sectional Area is referred as product of width multiplied by average water depth.
Constant Head Difference - The Constant Head Difference is referred as difference between the hydraulic head or pressure difference separated by a small distance dl.
Length - (Measured in Meter) - The Length referred as measurement or extent of something from end to end.

STEP 1: Convert Input(s) to Base Unit

Discharge: 3 Cubic Meter per Second --> 3 Cubic Meter per Second No Conversion Required
Cross-Sectional Area: 100 Square Meter --> 100 Square Meter No Conversion Required
Constant Head Difference: 2 --> No Conversion Required
Length: 3.9 Meter --> 3.9 Meter No Conversion Required

STEP 2: Evaluate Formula

Substituting Input Values in Formula

K = (Q/A)*(1/(ΔH/L)) --> (3/100)*(1/(2/3.9))

Evaluating ... ...

K = 0.0585

STEP 3: Convert Result to Output's Unit

0.0585 Meter per Second -->5.85 Centimeter per Second (Check conversion here)

FINAL ANSWER

5.85 Centimeter per Second <-- Coefficient of Permeability at 20° C

(Calculation completed in 00.004 seconds)

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< Coefficient of Permeability Calculators

Hagen Poiseuille Flow or Mean Particle Size of Porous Medium Laminar Flow through Conduit

LaTeX Go Mean Particle Size of the Porous Medium = sqrt((Coefficient of Permeability (Hagen-Poiseuille)*Dynamic Viscosity of the Fluid)/(Shape Factor*(Unit Weight of Fluid/1000)))

Dynamic Viscosity of Fluid of Laminar Flow through Conduit or Hagen Poiseuille Flow

LaTeX Go Dynamic Viscosity of the Fluid = (Shape Factor*Mean Particle Size of the Porous Medium^2)*((Unit Weight of Fluid/1000)/Coefficient of Permeability (Hagen-Poiseuille))

Coefficient of Permeability from Analogy of Laminar Flow (Hagen Poiseuille flow)

LaTeX Go Coefficient of Permeability (Hagen-Poiseuille) = Shape Factor*(Mean Particle Size of the Porous Medium^2)*(Unit Weight of Fluid/1000)/Dynamic Viscosity of the Fluid

Unit weight of fluid

LaTeX Go Unit Weight of Fluid = Density of Fluid*Acceleration due to Gravity

Coefficient of Permeability at Temperature of Permeameter Experiment Formula

LaTeX Go

Coefficient of Permeability at 20° C = (Discharge/Cross-Sectional Area)*(1/(Constant Head Difference/Length))
K = (Q/A)*(1/(ΔH/L))

What is Aquifer Transmissivity?

Transmissivity describes the ability of the aquifer to transmit groundwater throughout its entire saturated thickness. Transmissivity is measured as the rate at which groundwater can flow through an aquifer section of unit width under a unit hydraulic gradient.

How to Calculate Coefficient of Permeability at Temperature of Permeameter Experiment?

Coefficient of Permeability at Temperature of Permeameter Experiment calculator uses Coefficient of Permeability at 20° C = (Discharge/Cross-Sectional Area)*(1/(Constant Head Difference/Length)) to calculate the Coefficient of Permeability at 20° C, The Coefficient of Permeability at Temperature of Permeameter Experiment formula is defined as the rate of flow under laminar flow conditions through a unit cross sectional are of porous medium under unit hydraulic gradient. Coefficient of Permeability at 20° C is denoted by K symbol.

How to calculate Coefficient of Permeability at Temperature of Permeameter Experiment using this online calculator? To use this online calculator for Coefficient of Permeability at Temperature of Permeameter Experiment, enter Discharge (Q), Cross-Sectional Area (A), Constant Head Difference (ΔH) & Length (L) and hit the calculate button. Here is how the Coefficient of Permeability at Temperature of Permeameter Experiment calculation can be explained with given input values -> 585 = (3/100)*(1/(2/3.9)).

FAQ

What is Coefficient of Permeability at Temperature of Permeameter Experiment?

The Coefficient of Permeability at Temperature of Permeameter Experiment formula is defined as the rate of flow under laminar flow conditions through a unit cross sectional are of porous medium under unit hydraulic gradient and is represented as K = (Q/A)*(1/(ΔH/L)) or Coefficient of Permeability at 20° C = (Discharge/Cross-Sectional Area)*(1/(Constant Head Difference/Length)). The Discharge referred as volumetric flow rate of water that is transported through a given cross-sectional area. It includes any suspended solids, dissolved chemicals, or biologic material, The Cross-Sectional Area is referred as product of width multiplied by average water depth, The Constant Head Difference is referred as difference between the hydraulic head or pressure difference separated by a small distance dl & The Length referred as measurement or extent of something from end to end.

How to calculate Coefficient of Permeability at Temperature of Permeameter Experiment?

The Coefficient of Permeability at Temperature of Permeameter Experiment formula is defined as the rate of flow under laminar flow conditions through a unit cross sectional are of porous medium under unit hydraulic gradient is calculated using Coefficient of Permeability at 20° C = (Discharge/Cross-Sectional Area)*(1/(Constant Head Difference/Length)). To calculate Coefficient of Permeability at Temperature of Permeameter Experiment, you need Discharge (Q), Cross-Sectional Area (A), Constant Head Difference (ΔH) & Length (L). With our tool, you need to enter the respective value for Discharge, Cross-Sectional Area, Constant Head Difference & Length 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 Coefficient of Permeability at 20° C?

In this formula, Coefficient of Permeability at 20° C uses Discharge, Cross-Sectional Area, Constant Head Difference & Length. We can use 1 other way(s) to calculate the same, which is/are as follows -

Coefficient of Permeability at 20° C = Intrinsic Permeability*((Unit Weight of Fluid/1000)/Dynamic Viscosity of the Fluid)

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