Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt Solution

STEP 0: Pre-Calculation Summary
Formula Used
Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
R = (1*h*A)-DG
This formula uses 4 Variables
Variables Used
Possible Recharge - (Measured in Cubic Meter per Second) - Possible Recharge is defined as the gross recharge minus the natural recharge of the area.
Water Level Fluctuation - (Measured in Meter) - Water Level Fluctuation during monsoon season is an irregular rising and falling in number or amount of water.
Watershed Area - (Measured in Square Meter) - Watershed Area is an isolated area with a well demarcated boundary line, draining the rainwater to a single outlet.
Gross Water Draft - (Measured in Cubic Meter per Second) - Gross Water Draft due to Rainfall and other sources.
STEP 1: Convert Input(s) to Base Unit
Water Level Fluctuation: 5 Meter --> 5 Meter No Conversion Required
Watershed Area: 20 Square Meter --> 20 Square Meter No Conversion Required
Gross Water Draft: 10 Cubic Meter per Second --> 10 Cubic Meter per Second No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
R = (1*h*A)-DG --> (1*5*20)-10
Evaluating ... ...
R = 90
STEP 3: Convert Result to Output's Unit
90 Cubic Meter per Second --> No Conversion Required
FINAL ANSWER
90 Cubic Meter per Second <-- Possible Recharge
(Calculation completed in 00.004 seconds)

Credits

Created by Mithila Muthamma PA
Coorg Institute of Technology (CIT), Coorg
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13 Minimum Value of Specific Yield for Various Hydrogeologic Conditions based on Norms Calculators

Possible Recharge in Hard Rock Area with Massive, poorly fractured Rock
Go Possible Recharge = (0.2*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible Recharge in Sandy Alluvial Area given Minimum value of Specific Yield for Area
Go Possible Recharge = (12*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible Recharge in Hard Rock Area with Low Clay Content given Minimum value of Specific Yield
Go Possible Recharge = (2*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible Recharge in Hard Rock Area with Kartstified Limestone given Minimum Specific Yield
Go Possible Recharge = (5*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible Recharge in Clayey Alluvial Area given Minimum value of Specific Yield for Area
Go Possible Recharge = (4*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible Recharge in Silty Alluvial Area given Minimum value of Specific Yield for Area
Go Possible Recharge = (8*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible recharge in hard rock area with limestone given minimum specific yield of area
Go Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible Recharge in Hard Rock Area with Phyllites, Shales given Minimum Specific Yield
Go Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible recharge in hard rock area with laterite for minimum specific yield of area
Go Possible Recharge = (2*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt
Go Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible recharge in hard rock area with quartzite given minimum specific yield
Go Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible recharge in hard rock area with sandstone for minimum specific yield
Go Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
Possible Recharge in Hard Rock Area with significant Clay Content
Go Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft

Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt Formula

Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
R = (1*h*A)-DG

What is Recharge in Hydrology?

Groundwater Recharge or deep drainage or deep percolation is a hydrologic process, where water moves downward from surface water to groundwater. Recharge is the primary method through which water enters an aquifer.

How to Calculate Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt?

Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt calculator uses Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft to calculate the Possible Recharge, The Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt is defined for the specific region of consideration based on the value of recommended norms for specific yield in percentage. Possible Recharge is denoted by R symbol.

How to calculate Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt using this online calculator? To use this online calculator for Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt, enter Water Level Fluctuation (h), Watershed Area (A) & Gross Water Draft (DG) and hit the calculate button. Here is how the Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt calculation can be explained with given input values -> 90 = (1*5*20)-10.

FAQ

What is Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt?
The Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt is defined for the specific region of consideration based on the value of recommended norms for specific yield in percentage and is represented as R = (1*h*A)-DG or Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft. Water Level Fluctuation during monsoon season is an irregular rising and falling in number or amount of water, Watershed Area is an isolated area with a well demarcated boundary line, draining the rainwater to a single outlet & Gross Water Draft due to Rainfall and other sources.
How to calculate Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt?
The Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt is defined for the specific region of consideration based on the value of recommended norms for specific yield in percentage is calculated using Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft. To calculate Possible Recharge in Hard Rock Area with Weathered or Vesicular, Jointed Basalt, you need Water Level Fluctuation (h), Watershed Area (A) & Gross Water Draft (DG). With our tool, you need to enter the respective value for Water Level Fluctuation, Watershed Area & Gross Water Draft and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
How many ways are there to calculate Possible Recharge?
In this formula, Possible Recharge uses Water Level Fluctuation, Watershed Area & Gross Water Draft. We can use 12 other way(s) to calculate the same, which is/are as follows -
  • Possible Recharge = (12*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (8*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (4*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (2*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (2*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (5*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (1*Water Level Fluctuation*Watershed Area)-Gross Water Draft
  • Possible Recharge = (0.2*Water Level Fluctuation*Watershed Area)-Gross Water Draft
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