Drawdown in aquifer caused by pumping at any point in aquifer Formula

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Possible Drawdown in Confined Aquifer is the drawdown that would have occurred if the aquifer had been confined (that is, if no dewatering had occurred). Check FAQs
s'=qtτSr2
s' - Possible Drawdown in Confined Aquifer?q - Pumping Rate?t - Time Period?τ - Transmissivity?S - Storage Coefficient?r - Distance from Pumping Well?

Drawdown in aquifer caused by pumping at any point in aquifer Example

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Here is how the Drawdown in aquifer caused by pumping at any point in aquifer equation looks like with Values.

Here is how the Drawdown in aquifer caused by pumping at any point in aquifer equation looks like with Units.

Here is how the Drawdown in aquifer caused by pumping at any point in aquifer equation looks like.

0.1961Edit=7Edit30Edit1.4Edit85Edit3Edit2
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Drawdown in aquifer caused by pumping at any point in aquifer Solution

Follow our step by step solution on how to calculate Drawdown in aquifer caused by pumping at any point in aquifer?

FIRST Step Consider the formula
s'=qtτSr2
Next Step Substitute values of Variables
s'=7m³/s30s1.4m²/s853m2
Next Step Prepare to Evaluate
s'=7301.48532
Next Step Evaluate
s'=0.196078431372549m
LAST Step Rounding Answer
s'=0.1961m

Drawdown in aquifer caused by pumping at any point in aquifer Formula Elements

Variables
Possible Drawdown in Confined Aquifer
Possible Drawdown in Confined Aquifer is the drawdown that would have occurred if the aquifer had been confined (that is, if no dewatering had occurred).
Symbol: s'
Measurement: LengthUnit: m
Note: Value can be positive or negative.
Pumping Rate
The Pumping Rate is referred as volume of water (or other fluid) that is pumped per unit of time. It’s typically measured in units like liters per second (L/s) or cubic meters per hour (m³/h).
Symbol: q
Measurement: Volumetric Flow RateUnit: m³/s
Note: Value can be positive or negative.
Time Period
Time Period (pumping has been in Progress) or Time can be defined as the ongoing and continuous sequence of events that occur in succession, from the past through the present to the future.
Symbol: t
Measurement: TimeUnit: s
Note: Value can be positive or negative.
Transmissivity
The Transmissivity refers to the measure of how much water can be transmitted horizontally through an aquifer is the product of the hydraulic conductivity of the aquifer and its saturated thickness.
Symbol: τ
Measurement: Kinematic ViscosityUnit: m²/s
Note: Value should be greater than 0.
Storage Coefficient
Storage Coefficient is the volume of water released from storage per unit decline in hydraulic head in the aquifer, per unit area of the aquifer.
Symbol: S
Measurement: NAUnit: Unitless
Note: Value can be positive or negative.
Distance from Pumping Well
Distance from Pumping Well to the point where drawdown occurs.
Symbol: r
Measurement: LengthUnit: m
Note: Value can be positive or negative.

Other formulas in Single Well Tests category

​Go Total Drawdown in Pumping Well
st=s+CQn
​Go Total Drawdown in Pumping Well expressed given Factors related to Hydraulic Characteristics
st=Bq+(Cq2)
​Go Drawdown in aquifer for total drawdown
s=st-CQn
​Go Well Loss for Total Drawdown
CQn=st-s

How to Evaluate Drawdown in aquifer caused by pumping at any point in aquifer?

Drawdown in aquifer caused by pumping at any point in aquifer evaluator uses Possible Drawdown in Confined Aquifer = Pumping Rate*Time Period/(Transmissivity*Storage Coefficient*Distance from Pumping Well^2) to evaluate the Possible Drawdown in Confined Aquifer, The Drawdown in aquifer caused by pumping at any point in aquifer is a change in groundwater level due to an applied stress. Possible Drawdown in Confined Aquifer is denoted by s' symbol.

How to evaluate Drawdown in aquifer caused by pumping at any point in aquifer using this online evaluator? To use this online evaluator for Drawdown in aquifer caused by pumping at any point in aquifer, enter Pumping Rate (q), Time Period (t), Transmissivity (τ), Storage Coefficient (S) & Distance from Pumping Well (r) and hit the calculate button.

FAQs on Drawdown in aquifer caused by pumping at any point in aquifer

What is the formula to find Drawdown in aquifer caused by pumping at any point in aquifer?
The formula of Drawdown in aquifer caused by pumping at any point in aquifer is expressed as Possible Drawdown in Confined Aquifer = Pumping Rate*Time Period/(Transmissivity*Storage Coefficient*Distance from Pumping Well^2). Here is an example- 0.196078 = 7*30/(1.4*85*3^2).
How to calculate Drawdown in aquifer caused by pumping at any point in aquifer?
With Pumping Rate (q), Time Period (t), Transmissivity (τ), Storage Coefficient (S) & Distance from Pumping Well (r) we can find Drawdown in aquifer caused by pumping at any point in aquifer using the formula - Possible Drawdown in Confined Aquifer = Pumping Rate*Time Period/(Transmissivity*Storage Coefficient*Distance from Pumping Well^2).
Can the Drawdown in aquifer caused by pumping at any point in aquifer be negative?
Yes, the Drawdown in aquifer caused by pumping at any point in aquifer, measured in Length can be negative.
Which unit is used to measure Drawdown in aquifer caused by pumping at any point in aquifer?
Drawdown in aquifer caused by pumping at any point in aquifer is usually measured using the Meter[m] for Length. Millimeter[m], Kilometer[m], Decimeter[m] are the few other units in which Drawdown in aquifer caused by pumping at any point in aquifer can be measured.
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