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The Possible Recharge refers to the gross recharge minus the natural recharge of the area. Check FAQs
R=(2⋅h⋅A)-DG
R - Possible Recharge?h - Water Level Fluctuation?A - Watershed Area?DG - Gross Water Draft?

Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt Example

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With units
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Here is how the Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt equation looks like with Values.

Here is how the Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt equation looks like with Units.

Here is how the Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt equation looks like.

190Edit=(2⋅5Edit⋅20Edit)-10Edit
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HomeIcon Home » Category Engineering » Category Civil » Category Engineering Hydrology » fx Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt

Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt Solution

Follow our step by step solution on how to calculate Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt?

FIRST Step Consider the formula
R=(2⋅h⋅A)-DG
Next Step Substitute values of Variables
∴ R=(2⋅5m⋅20m²)-10m³/s
Next Step Prepare to Evaluate
∴ R=(2⋅5⋅20)-10
LAST Step Evaluate
∴R=190m³/s

Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt Formula Elements

Variables
Possible Recharge
The Possible Recharge refers to the gross recharge minus the natural recharge of the area.
Symbol: R
Measurement: Volumetric Flow RateUnit: m³/s
Note: Value should be greater than 0.
Formulas to find Possible RechargeOpen Variable
Water Level Fluctuation
The Water Level Fluctuation refers to the irregular rising and falling in number or amount of water during monsoon season.
Symbol: h
Measurement: LengthUnit: m
Note: Value can be positive or negative.
Formulas to find Water Level FluctuationOpen Variable
Watershed Area
The Watershed Area refers to the isolated area with a well demarcated boundary line, draining the rainwater to a single outlet.
Symbol: A
Measurement: AreaUnit: m²
Note: Value should be greater than 0.
Formulas to find Watershed AreaOpen Variable
Gross Water Draft
The Gross Water Draft refers to the total volume of water extracted or utilized from a catchment area.
Symbol: DG
Measurement: Volumetric Flow RateUnit: m³/s
Note: Value should be greater than 0.
Formulas to find Gross Water DraftOpen Variable

Other Formulas to find Possible Recharge

​Go Possible Recharge in Sandy Alluvium Areas based on Known norms of Recommended Specific Yield
R=(16⋅h⋅A)-DG
​Go Possible Recharge in Silty Alluvium Areas based on Known norms of Recommended Specific Yield
R=(10⋅h⋅A)-DG
​Go Possible Recharge in Clayey Alluvium Areas based on Known Norms of Specific Yield
R=(6⋅h⋅A)-DG
​Go Possible Recharge in Weathered Hard Rock Areas with Low Clay content based on Recommended Norms
R=(3⋅h⋅A)-DG

How to Evaluate Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt?

Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt evaluator uses Possible Recharge = (2*Water Level Fluctuation*Watershed Area)-Gross Water Draft to evaluate the Possible Recharge, The Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt is defined for the specific region of consideration. Possible Recharge is denoted by R symbol.

How to evaluate Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt using this online evaluator? To use this online evaluator for Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt, enter Water Level Fluctuation (h), Watershed Area (A) & Gross Water Draft (DG) and hit the calculate button.

FAQs on Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt

What is the formula to find Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt?
The formula of Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt is expressed as Possible Recharge = (2*Water Level Fluctuation*Watershed Area)-Gross Water Draft. Here is an example- 190 = (2*5*20)-10.
How to calculate Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt?
With Water Level Fluctuation (h), Watershed Area (A) & Gross Water Draft (DG) we can find Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt using the formula - Possible Recharge = (2*Water Level Fluctuation*Watershed Area)-Gross Water Draft.
What are the other ways to Calculate Possible Recharge?
Here are the different ways to Calculate Possible Recharge-
  • Possible Recharge=(16*Water Level Fluctuation*Watershed Area)-Gross Water DraftOpenImg
  • Possible Recharge=(10*Water Level Fluctuation*Watershed Area)-Gross Water DraftOpenImg
  • Possible Recharge=(6*Water Level Fluctuation*Watershed Area)-Gross Water DraftOpenImg
Can the Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt be negative?
No, the Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt, measured in Volumetric Flow Rate cannot be negative.
Which unit is used to measure Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt?
Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt is usually measured using the Cubic Meter per Second[m³/s] for Volumetric Flow Rate. Cubic Meter per Day[m³/s], Cubic Meter per Hour[m³/s], Cubic Meter per Minute[m³/s] are the few other units in which Possible Recharge in Hard Rock Areas with Weathered or vesicular, Jointed Basalt can be measured.
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