Cylindrical Surface through which Velocity of Flow Occurs Solution

STEP 0: Pre-Calculation Summary
Formula Used
Surface through which the Velocity of Flow Occurs = 2*pi*Radial Distance*Width of Aquifer
S = 2*pi*r*Ha
This formula uses 1 Constants, 3 Variables
Constants Used
pi - Archimedes' constant Value Taken As 3.14159265358979323846264338327950288
Variables Used
Surface through which the Velocity of Flow Occurs - (Measured in Square Meter) - Surface through which the Velocity of Flow Occurs s defined as the surface area of well through which the flow occurs.
Radial Distance - (Measured in Meter) - Radial Distance is the distance from the pumped well to the observation well located.
Width of Aquifer - (Measured in Meter) - Width of Aquifer measured from impermeable layer to the initial level of water table.
STEP 1: Convert Input(s) to Base Unit
Radial Distance: 3 Meter --> 3 Meter No Conversion Required
Width of Aquifer: 45 Meter --> 45 Meter No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
S = 2*pi*r*Ha --> 2*pi*3*45
Evaluating ... ...
S = 848.230016469244
STEP 3: Convert Result to Output's Unit
848.230016469244 Square Meter --> No Conversion Required
FINAL ANSWER
848.230016469244 848.23 Square Meter <-- Surface through which the Velocity of Flow Occurs
(Calculation completed in 00.004 seconds)

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10+ Steady Flow into a Well Calculators

Thiem's equilibrium equation for steady flow in confined aquifer
Go Steady Flow in a Confined Aquifer = 2*pi*Coefficient of Permeability*Width of Aquifer*(Piezometric Head at Radial Distance r2-Piezometric Head at Radial Distance r1)/ln(Radial Distance at Observation Well 2/Radial Distance at Observation Well 1)
Equilibrium Equation for Flow in Confined Aquifer at Observation Well
Go Discharge entering cylindrical surface into Well = (2*pi*Transmissivity*(Piezometric Head at Radial Distance r2-Piezometric Head at Radial Distance r1))/ln(Radial Distance at Observation Well 2/Radial Distance at Observation Well 1)
Transmissivity when Discharge and Drawdowns are considered
Go Transmissivity = Steady Flow in a Confined Aquifer*ln(Radial Distance at Observation Well 2/Radial Distance at Observation Well 1)/(2*pi*(Drawdown at the Start of Recuperation-Drawdown at a Time))
Discharge Observed at Edge of Zone of Influence
Go Discharge entering cylindrical surface into Well = 2*pi*Transmissivity*Possible Drawdown in Confined Aquifer/ln(Radial Distance at Observation Well 2/Radial Distance at Observation Well 1)
Discharge entering cylindrical surface to well discharge
Go Discharge entering cylindrical surface into Well = (2*pi*Radial Distance*Width of Aquifer)*(Coefficient of Permeability*(Change in the piezometric head/Change in Radial Distance))
Transmissivity when discharge at edge of zone of influence
Go Transmissivity = (Steady Flow in a Confined Aquifer*ln(Radial Distance at Observation Well 2/Radial Distance at Observation Well 1))/(2*pi*Possible Drawdown in Confined Aquifer)
Velocity of flow by Darcy's Law at Radical Distance
Go Velocity of Flow at Radial Distance = Coefficient of Permeability*(Change in the piezometric head/Change in Radial Distance)
Change in Piezometric Head
Go Change in the piezometric head = Velocity of Flow at Radial Distance*Change in Radial Distance/Coefficient of Permeability
Change in Radial Distance
Go Change in Radial Distance = Coefficient of Permeability*Change in the piezometric head/Velocity of Flow at Radial Distance
Cylindrical Surface through which Velocity of Flow Occurs
Go Surface through which the Velocity of Flow Occurs = 2*pi*Radial Distance*Width of Aquifer

Cylindrical Surface through which Velocity of Flow Occurs Formula

Surface through which the Velocity of Flow Occurs = 2*pi*Radial Distance*Width of Aquifer
S = 2*pi*r*Ha

What is Coefficient of Permeability?

The Coefficient of Permeability of a soil describes how easily a liquid will move through a soil. It is also commonly referred to as the hydraulic conductivity of a soil. This factor can be affected by the viscosity, or thickness(fluidity) of a liquid and its density.

How to Calculate Cylindrical Surface through which Velocity of Flow Occurs?

Cylindrical Surface through which Velocity of Flow Occurs calculator uses Surface through which the Velocity of Flow Occurs = 2*pi*Radial Distance*Width of Aquifer to calculate the Surface through which the Velocity of Flow Occurs, The Cylindrical Surface through which Velocity of Flow Occurs is defined as surface of well through which flow occurs. Surface through which the Velocity of Flow Occurs is denoted by S symbol.

How to calculate Cylindrical Surface through which Velocity of Flow Occurs using this online calculator? To use this online calculator for Cylindrical Surface through which Velocity of Flow Occurs, enter Radial Distance (r) & Width of Aquifer (Ha) and hit the calculate button. Here is how the Cylindrical Surface through which Velocity of Flow Occurs calculation can be explained with given input values -> 848.23 = 2*pi*3*45.

FAQ

What is Cylindrical Surface through which Velocity of Flow Occurs?
The Cylindrical Surface through which Velocity of Flow Occurs is defined as surface of well through which flow occurs and is represented as S = 2*pi*r*Ha or Surface through which the Velocity of Flow Occurs = 2*pi*Radial Distance*Width of Aquifer. Radial Distance is the distance from the pumped well to the observation well located & Width of Aquifer measured from impermeable layer to the initial level of water table.
How to calculate Cylindrical Surface through which Velocity of Flow Occurs?
The Cylindrical Surface through which Velocity of Flow Occurs is defined as surface of well through which flow occurs is calculated using Surface through which the Velocity of Flow Occurs = 2*pi*Radial Distance*Width of Aquifer. To calculate Cylindrical Surface through which Velocity of Flow Occurs, you need Radial Distance (r) & Width of Aquifer (Ha). With our tool, you need to enter the respective value for Radial Distance & Width of Aquifer 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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