1970
DOI: 10.3126/bdg.v12i0.2249
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Hydrogeologic assessment and groundwater reserve evaluation in northwestern parts of Dun valley aquifers of Chitwan, inner Terai

Abstract: The Chitwan Valley is one of the largest Dun Valleys in the Himalayan foothills of Nepal. Dun gravels perhaps deposited in the late Pleistocene to very early Holocene about 22,000-7000 yr. B.P. Chitwan Dun Valley is underlain by Dun fan gravels or Dun gravels which form unconfined to semiconfined or leaky confined aquifers. The study area, situated in the NW part of the valley occupies an area of 70.8 km2.The hydrogeological situation in the study area is inferred from drilling data of Ground Water Resources… Show more

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“…Since the evapotranspiration data for the Surkhet valley is not available, it is estimated with reference to that of the Chitwan valley as both the valleys are under similar geomorphic and geologic setup. Neupane and Shrestha (2009) calculated the evapotranspiration for Chitwan Valley which is 27.69% of the rainfall. Thus for the Surkhet valley, it can be assumed about 25% losses takes place due to evapotranspiration, which is 40.53 Mm³/year (25% of 162.14).…”
Section: Water Balance Methodsmentioning
confidence: 99%
“…Since the evapotranspiration data for the Surkhet valley is not available, it is estimated with reference to that of the Chitwan valley as both the valleys are under similar geomorphic and geologic setup. Neupane and Shrestha (2009) calculated the evapotranspiration for Chitwan Valley which is 27.69% of the rainfall. Thus for the Surkhet valley, it can be assumed about 25% losses takes place due to evapotranspiration, which is 40.53 Mm³/year (25% of 162.14).…”
Section: Water Balance Methodsmentioning
confidence: 99%