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This file contains a presentation on " interlinking of rivers in India ". Describing the efforts made in past, present scenario, possibilities, problems their solution and alternatives.
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This file contains a presentation on " interlinking of rivers in India ". Describing the efforts made in past, present scenario, possibilities, problems their solution and alternatives.
Interlinking of rivers in India
Interlinking of rivers in India
Aditya Kumar
here I describe how Indian rivers are linked...and for that what type of advantage and disadvantage....happen due to this....
Inter linking of river in india...
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Puspendu Samanta
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Proposed solution of water crisis in India, ILR and its component,stated benefits and consequences , alternatives to river linking.
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Ground water recharge is the process whereby the amount of water present in or flowing through the interstices of the sub-soil increases by natural or artificial means. Rainfall is the principal source for replenishment of recharge of ground water. Other sources include recharge from rivers, streams, irrigation water etc. An unconfined aquifer is recharged directly by local rainfall, rivers, and lakes, and the rate of recharge will be influenced by the permeability of overlying rocks and soils. A confined aquifer, on the other hand, is characterized by an overlying bed that is impermeable, and local rainfall does not influence the aquifer. It is normally recharged from lakes, rivers, and rainfall that may occur at distances ranging from a few kilometers to thousands of kilometers.
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Ground water recharge is the process whereby the amount of water present in or flowing through the interstices of the sub-soil increases by natural or artificial means. Rainfall is the principal source for replenishment of recharge of ground water. Other sources include recharge from rivers, streams, irrigation water etc. An unconfined aquifer is recharged directly by local rainfall, rivers, and lakes, and the rate of recharge will be influenced by the permeability of overlying rocks and soils. A confined aquifer, on the other hand, is characterized by an overlying bed that is impermeable, and local rainfall does not influence the aquifer. It is normally recharged from lakes, rivers, and rainfall that may occur at distances ranging from a few kilometers to thousands of kilometers.
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Interlinking of rivers
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