Discharge when Coefficient of Permeability at Permeameter Experiment is Considered Solution

STEP 0: Pre-Calculation Summary
Formula Used
Discharge = Coefficient of Permeability at the temperature*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) - Discharge is the 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 the temperature - (Measured in Meter per Second) - The coefficient of Permeability at the temperature describes how easily a liquid will move through the porous medium.
Cross-Sectional Area - (Measured in Square Meter) - Cross-Sectional Area is the product of width multiplied by average water depth.
Constant Head Difference - Constant Head Difference is the difference between the Points separated by a small distance dl.
Length - (Measured in Meter) - Length is the measurement or extent of something from end to end.
STEP 1: Convert Input(s) to Base Unit
Coefficient of Permeability at the temperature: 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 00.020 seconds)

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21 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
Coefficient of permeability at any temperature t for standard value of coefficient of permeability
Go Coefficient of Permeability at any Temperature t = (Standard Coefficient of Permeability at 20°C*Kinematic Viscosity at 20° C)/Kinematic Viscosity at t° C
Kinematic Viscosity at 20 degree Celsius for standard value of coefficient of permeability
Go Kinematic Viscosity at 20° C = (Coefficient of Permeability at any Temperature t*Kinematic Viscosity at t° C)/Standard Coefficient of Permeability at 20°C
Kinematic Viscosity for standard value of coefficient of permeability
Go Kinematic Viscosity at t° C = (Standard Coefficient of Permeability at 20°C*Kinematic Viscosity at 20° C)/Coefficient of Permeability at any Temperature t
Standard value of coefficient of permeability
Go Standard Coefficient of Permeability at 20°C = Coefficient of Permeability at any Temperature t*(Kinematic Viscosity at t° C/Kinematic Viscosity at 20° C)
Coefficient of permeability at temperature of permeameter experiment
Go Coefficient of Permeability at the temperature = (Discharge/Cross-Sectional Area)*(1/(Constant Head Difference/Length))
Cross sectional area when coefficient of permeability at permeameter experiment is considered
Go Cross-Sectional Area = Discharge/(Coefficient of Permeability at the temperature*(Constant Head Difference/Length))
Discharge when Coefficient of Permeability at Permeameter Experiment is Considered
Go Discharge = Coefficient of Permeability at the temperature*Cross-Sectional Area*(Constant Head Difference/Length)
Length when Coefficient of Permeability at Permeameter Experiment is Considered
Go Length = (Constant Head Difference*Cross-Sectional Area*Coefficient of Permeability at the temperature)/Discharge
Coefficient of Permeability when Specific or Intrinsic Permeability is Considered
Go Coefficient of Permeability at the temperature = Intrinsic Permeability*((Unit Weight of Fluid/1000)/Dynamic Viscosity of the Fluid)
Specific or Intrinsic Permeability when Coefficient of Permeability is Considered
Go Intrinsic Permeability = (Coefficient of Permeability at the temperature*Dynamic Viscosity of the Fluid)/(Unit Weight of Fluid/1000)
Specific or Intrinsic Permeability when Dynamic Viscosity is Considered
Go Intrinsic Permeability = (Coefficient of Permeability at the temperature*Dynamic Viscosity of the Fluid)/(Unit Weight of Fluid/1000)
Dynamic Viscosity when Specific or Intrinsic Permeability is Considered
Go Dynamic Viscosity of the Fluid = Intrinsic Permeability*((Unit Weight of Fluid/1000)/Coefficient of Permeability at the temperature)
Kinematic Viscosity when Specific or Intrinsic Permeability is Considered
Go Kinematic Viscosity = (Intrinsic Permeability*Acceleration due to Gravity)/Coefficient of Permeability
Equation for Specific or Intrinsic Permeability
Go Intrinsic Permeability = Shape Factor*Mean Particle Size of the Porous Medium^2
Kinematic Viscosity and Dynamic Viscosity Relation
Go Kinematic Viscosity = Dynamic Viscosity of the Fluid/Density of Fluid
Unit weight of fluid
Go Unit Weight of Fluid = Density of Fluid*Acceleration due to Gravity
Coefficient of Permeability when Transmissibility is Considered
Go Coefficient of Permeability = Transmissibility/Aquifer Thickness
Equivalent permeability when transmissivity of aquifer is considered
Go Equivalent Permeability = Transmissivity/Aquifer Thickness

Discharge when Coefficient of Permeability at Permeameter Experiment is Considered Formula

Discharge = Coefficient of Permeability at the temperature*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 the temperature*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 the temperature (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 the temperature*Cross-Sectional Area*(Constant Head Difference/Length). The coefficient of Permeability at the temperature describes how easily a liquid will move through the porous medium, Cross-Sectional Area is the product of width multiplied by average water depth, Constant Head Difference is the difference between the Points separated by a small distance dl & Length is the 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 the temperature*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 the temperature (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 the temperature, 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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