Time at which Drawdowns are measured for Storage Coefficient Solution

STEP 0: Pre-Calculation Summary
Formula Used
Total Drawdown = Storage Coefficient*Distance from Pumping Well to Point Intersection^2/(2.25*Transmissivity)
st = S*ro^2/(2.25*T)
This formula uses 4 Variables
Variables Used
Total Drawdown - (Measured in Meter) - The Total Drawdown is referred as reduction in hydraulic head observed at a well in an aquifer, typically due to pumping a well as part of an aquifer test or well test.
Storage Coefficient - The Storage Coefficient is referred as volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer.
Distance from Pumping Well to Point Intersection - (Measured in Meter) - The Distance from Pumping Well to Point Intersection is referred as the straight line which intersects the zero-drawdown line.
Transmissivity - (Measured in Square Meter per Second) - Transmissivity is the rate at which groundwater flows horizontally through an aquifer or the degree to which a medium allows something, in particular electromagnetic radiation, to pass through it.
STEP 1: Convert Input(s) to Base Unit
Storage Coefficient: 0.0545 --> No Conversion Required
Distance from Pumping Well to Point Intersection: 4 Meter --> 4 Meter No Conversion Required
Transmissivity: 11 Square Meter per Second --> 11 Square Meter per Second No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
st = S*ro^2/(2.25*T) --> 0.0545*4^2/(2.25*11)
Evaluating ... ...
st = 0.0352323232323232
STEP 3: Convert Result to Output's Unit
0.0352323232323232 Meter --> No Conversion Required
FINAL ANSWER
0.0352323232323232 0.035232 Meter <-- Total Drawdown
(Calculation completed in 00.004 seconds)

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Distance Drawdown Analysis Calculators

Storage Coefficient from Distance-Drawdown Graphs
​ LaTeX ​ Go Storage Coefficient = 2.25*Transmissivity*Total Drawdown/Distance from Pumping Well to Point Intersection^2
Drawdown across One Log Cycle from Distance Drawdown Graphs given Transmissivity
​ LaTeX ​ Go Drawdown Across Log Cycle = 2.3*Pumping Rate/(Transmissivity*2*pi)
Transmissivity from Distance Drawdown Graphs
​ LaTeX ​ Go Transmissivity = 2.3*Pumping Rate/(2*pi*Drawdown Across Log Cycle)
Pumping Rate from Distance Drawdown Graphs
​ LaTeX ​ Go Pumping Rate = Transmissivity*2*pi*Drawdown Across Log Cycle/2.3

Time at which Drawdowns are measured for Storage Coefficient Formula

​LaTeX ​Go
Total Drawdown = Storage Coefficient*Distance from Pumping Well to Point Intersection^2/(2.25*Transmissivity)
st = S*ro^2/(2.25*T)

What is Water Well Drawdown?

Drawdown is a change in groundwater level due to an applied stress, caused by events such as: Pumping from a well, pumping from a neighboring well, intensive water taking from local area, seasonal declines as recharge rates lower.

How to Calculate Time at which Drawdowns are measured for Storage Coefficient?

Time at which Drawdowns are measured for Storage Coefficient calculator uses Total Drawdown = Storage Coefficient*Distance from Pumping Well to Point Intersection^2/(2.25*Transmissivity) to calculate the Total Drawdown, The Time at which Drawdowns are measured for Storage Coefficient formula is defined as the time at which the reduction in hydraulic head observed at a well in an aquifer, typically due to pumping a well as part of an aquifer test or well test. Total Drawdown is denoted by st symbol.

How to calculate Time at which Drawdowns are measured for Storage Coefficient using this online calculator? To use this online calculator for Time at which Drawdowns are measured for Storage Coefficient, enter Storage Coefficient (S), Distance from Pumping Well to Point Intersection (ro) & Transmissivity (T) and hit the calculate button. Here is how the Time at which Drawdowns are measured for Storage Coefficient calculation can be explained with given input values -> 0.035232 = 0.0545*4^2/(2.25*11).

FAQ

What is Time at which Drawdowns are measured for Storage Coefficient?
The Time at which Drawdowns are measured for Storage Coefficient formula is defined as the time at which the reduction in hydraulic head observed at a well in an aquifer, typically due to pumping a well as part of an aquifer test or well test and is represented as st = S*ro^2/(2.25*T) or Total Drawdown = Storage Coefficient*Distance from Pumping Well to Point Intersection^2/(2.25*Transmissivity). The Storage Coefficient is referred as volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer, The Distance from Pumping Well to Point Intersection is referred as the straight line which intersects the zero-drawdown line & Transmissivity is the rate at which groundwater flows horizontally through an aquifer or the degree to which a medium allows something, in particular electromagnetic radiation, to pass through it.
How to calculate Time at which Drawdowns are measured for Storage Coefficient?
The Time at which Drawdowns are measured for Storage Coefficient formula is defined as the time at which the reduction in hydraulic head observed at a well in an aquifer, typically due to pumping a well as part of an aquifer test or well test is calculated using Total Drawdown = Storage Coefficient*Distance from Pumping Well to Point Intersection^2/(2.25*Transmissivity). To calculate Time at which Drawdowns are measured for Storage Coefficient, you need Storage Coefficient (S), Distance from Pumping Well to Point Intersection (ro) & Transmissivity (T). With our tool, you need to enter the respective value for Storage Coefficient, Distance from Pumping Well to Point Intersection & Transmissivity 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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