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Overexploitation of groundwater resources upstream of the Khirbet Al-Samra wastewater treatment plant (KSWTP) has lowered the water table 43 m since the beginning of groundwater development in 1968.
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Shortages of surface water supplies have increased the need of groundwater development in many canal commands.
Since the stage of groundwater development has reached to a level of about 78% in Shirpur taluka; hence, future groundwater development is not feasible.
The overall stage of groundwater development is 53.55%; therefore, there is a scope for further development of groundwater particularly in Dhule, Sakri, and Shindkheda taluka.
Rate of groundwater development and management is not at par with rate of utilization.
Yet, the capital cost of groundwater development is also relatively low.
Transmissivity can help us understand the groundwater potential, secondary porosity, and hydrogeological conditions of an area for groundwater development.
This isolation was maintained until the beginning of fruit development.
The distribution of groundwater storage and potential areas for groundwater development are then mapped using GIS.
GWD is groundwater development; A is availability of groundwater resources; R is groundwater release potential of soil matrix; C is cost for groundwater extraction.
A groundwater development program requires a large volume of data from various sources.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com