Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/2022
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dc.contributor.authorKumar, Sudhir-
dc.contributor.authorSingh, Hukum-
dc.contributor.authorSingh, Mohar-
dc.date.accessioned2019-05-09T07:43:55Z-
dc.date.available2019-05-09T07:43:55Z-
dc.date.issued1996-
dc.identifier.urihttp://117.252.14.250:8080/xmlui/handle/123456789/2022-
dc.description.abstractInfiltration is an important component of the hydrologic cycle and is defined as the process of entry of water through the soil surface. Earlier, the term infiltration was used to denote the difference between rainfall and runoff in small areas. Hydrological importance of the infiltration process is to be seen from the fact that it marks the transition from fast moving surface water to slow moving soil moisture and groundwater.en_US
dc.language.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.relation.ispartofseries;CS(AR)-6/96-97-
dc.subjectInfiltration studies in Sher-Umar river Doaben_US
dc.subjectNarmada basinen_US
dc.titleCS(AR)-6/96-97 : Infiltration studies in Sher-Umar river Doab in Narmada basinen_US
dc.typeTechnical Reporten_US
Appears in Collections:Case studies

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