Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/1720
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dc.contributor.authorRao, S. V. N.-
dc.contributor.authorRao, N. V.-
dc.date.accessioned2019-05-01T10:45:14Z-
dc.date.available2019-05-01T10:45:14Z-
dc.date.issued1995-
dc.identifier.urihttp://117.252.14.250:8080/xmlui/handle/123456789/1720-
dc.description.abstractThe young Himalayas have a serious problem of soil erosion and consequent sedimentation in river reaches downstream. Since a large number of hydel projects are envisaged in the Chenab valley by the Govt of India, correct assessment and estimation of sediment yield at any given point in space and time is of vital importance in the design of reservoirs. Also it would not be practical to set up a large number of sediment gauging sites. Spatial sediment yield models can be useful in such circumstances. In the present report data of 9 sediment stations within in Chenab basin varying from 17 to 27 years was utilised to develop a statistically significant spatial model to estimate sediment yield using geomorphological, climatic and landuse, landcover parameters. The sediment yield was estimated for total and fine sediment for monsoon, winter, premonsoon and annual seasons. The study also reveals the high rates of sedimentation in Chenab basin and its effect on existing Salal dam near Jammu.en_US
dc.language.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.relation.ispartofseries;CS(AR)-197-
dc.subjectSediment yield from Chenaben_US
dc.subjectSoil erosion -in Chenaben_US
dc.titleCS(AR)-197 : A study of sediment yield from Chenab river system in western Himalayasen_US
dc.typeTechnical Reporten_US
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