Recharge From Rainfall In Alluvial Indo Gangetic And Inland Areas Formula:
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The Recharge from Rainfall in Alluvial Indo formula calculates the amount of water that infiltrates through the soil and percolates down to replenish groundwater aquifers in alluvial plains of the Indo-Gangetic and inland areas. This is crucial for managing groundwater resources in these regions.
The calculator uses the formula:
Where:
Explanation: The formula calculates groundwater recharge by multiplying the catchment area with normal monsoon rainfall and applying a conversion factor of 22 to account for infiltration rates and other hydrological parameters specific to alluvial Indo-Gangetic and inland areas.
Details: Accurate recharge calculation is essential for sustainable groundwater management, water resource planning, and preventing over-extraction of groundwater in alluvial plains of the Indo-Gangetic and inland regions.
Tips: Enter the area of computation for recharge in square meters and normal rainfall in monsoon season in meters. All values must be positive numbers.
Q1: What is the significance of the constant 22 in the formula?
A: The constant 22 represents a conversion factor that accounts for infiltration rates, soil characteristics, and other hydrological parameters specific to alluvial Indo-Gangetic and inland areas.
Q2: How is normal rainfall in monsoon season determined?
A: Normal rainfall refers to the statistical average of rainfall measured over a specified period, typically 30 years, during the monsoon months in a given region.
Q3: What areas are considered "alluvial Indo-Gangetic and inland areas"?
A: These refer to the fertile alluvial plains formed by the Indus, Ganges, and Brahmaputra river systems, as well as similar inland alluvial formations.
Q4: Why is groundwater recharge important in these regions?
A: These regions are heavily dependent on groundwater for agriculture and domestic use, making sustainable recharge management crucial for water security.
Q5: Are there limitations to this calculation method?
A: The formula provides an estimate and may need adjustment based on local soil conditions, land use patterns, and specific hydrological characteristics.