Discharge when Coefficient of Permeability at Permeameter Experiment is Considered Calculator

✖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 20° C [K]			+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 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 when Coefficient of Permeability at Permeameter Experiment is Considered [Q]

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Formula

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Discharge when Coefficient of Permeability at Permeameter Experiment is Considered

Formula

Q = K \cdot A \cdot (\frac{ΔH}{L})

Example

3.076923 m³/s = 6 cm/s \cdot 100 m² \cdot (\frac{2}{3.9 m})

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Discharge when Coefficient of Permeability at Permeameter Experiment is Considered Solution

STEP 0: Pre-Calculation Summary

Formula Used

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

Variables Used

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.
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.
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

Coefficient of Permeability at 20° C: 6 Centimeter per Second --> 0.06 Meter per Second (Check conversion here)
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

Q = K*A*(ΔH/L) --> 0.06*100*(2/3.9)

Evaluating ... ...

Q = 3.07692307692308

STEP 3: Convert Result to Output's Unit

3.07692307692308 Cubic Meter per Second --> No Conversion Required

FINAL ANSWER

3.07692307692308 ≈ 3.076923 Cubic Meter per Second <-- Discharge

(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

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

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)

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

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

Discharge when Coefficient of Permeability at Permeameter Experiment is Considered Formula

Discharge = Coefficient of Permeability at 20° C*Cross-Sectional Area*(Constant Head Difference/Length)
Q = K*A*(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 Discharge when Coefficient of Permeability at Permeameter Experiment is Considered?

Discharge when Coefficient of Permeability at Permeameter Experiment is Considered calculator uses Discharge = Coefficient of Permeability at 20° C*Cross-Sectional Area*(Constant Head Difference/Length) to calculate the Discharge, The Discharge when Coefficient of Permeability at Permeameter Experiment is Considered is defined as the volumetric flow rate of water that is transported through a given cross-sectional area. Discharge is denoted by Q symbol.

How to calculate Discharge when Coefficient of Permeability at Permeameter Experiment is Considered using this online calculator? To use this online calculator for Discharge when Coefficient of Permeability at Permeameter Experiment is Considered, enter Coefficient of Permeability at 20° C (K), Cross-Sectional Area (A), Constant Head Difference (ΔH) & Length (L) and hit the calculate button. Here is how the Discharge when Coefficient of Permeability at Permeameter Experiment is Considered calculation can be explained with given input values -> 3.076923 = 0.06*100*(2/3.9).

FAQ

What is Discharge when Coefficient of Permeability at Permeameter Experiment is Considered?

The Discharge when Coefficient of Permeability at Permeameter Experiment is Considered is defined as the volumetric flow rate of water that is transported through a given cross-sectional area and is represented as Q = K*A*(ΔH/L) or Discharge = Coefficient of Permeability at 20° C*Cross-Sectional Area*(Constant Head Difference/Length). The Coefficient of Permeability at 20° C refers to the measure of a porous medium’s ability to allow fluid flow through its voids, 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 Discharge when Coefficient of Permeability at Permeameter Experiment is Considered?

The Discharge when Coefficient of Permeability at Permeameter Experiment is Considered is defined as the volumetric flow rate of water that is transported through a given cross-sectional area is calculated using Discharge = Coefficient of Permeability at 20° C*Cross-Sectional Area*(Constant Head Difference/Length). To calculate Discharge when Coefficient of Permeability at Permeameter Experiment is Considered, you need Coefficient of Permeability at 20° C (K), Cross-Sectional Area (A), Constant Head Difference (ΔH) & Length (L). With our tool, you need to enter the respective value for Coefficient of Permeability at 20° C, 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.

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