Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/3271
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dc.contributor.authorGhosh, Arindam-
dc.date.accessioned2014-09-30T11:50:01Z-
dc.date.available2014-09-30T11:50:01Z-
dc.date.issued2012-
dc.identifierM.Techen_US
dc.identifier.urihttp://hdl.handle.net/123456789/3271-
dc.guideIsrail, M.-
dc.guideSinchal, D. C.-
dc.description.abstractIn the present study an attempt has been made to investigate the physicochemical features of springs and to detect the nature of subsurface fractures using VLF method in southern and south-western Dabka watershed, located towards north-west of Nainital. Physicochemical studies including chemical analyses of the spring water samples have been done. VLF method was used to delineate the nature of sub-surface fractures near springs. If the fractures can be detected the nature of subsurface water flow can be established. Anomaly along a profile in southern part of Dabka microwatershed have been found that indicates subsurface fracture or a water conductive body.en_US
dc.language.isoenen_US
dc.subjectHYDROGEOLOGICALen_US
dc.subjectNAINITALen_US
dc.subjectWATERSHEDen_US
dc.subjectEARTH SCIENCE ENGINEERINGen_US
dc.titleHYDROGEOLOGICAL AND VLF STUDIES OF SPRINGS IN SOUTHERN AND SOUTH-WESTERN PART OF DABKA MICRO-WATERSHED, DISTRICT NAINITALen_US
dc.typeDoctoral Thesisen_US
dc.accession.numberG21427en_US
Appears in Collections:MASTERS' DISSERTATIONS (Earth Sci.)

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