Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/6402
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dc.contributor.authorBasak, P.-
dc.contributor.authorNazimuddin, M.-
dc.date.accessioned2021-10-13T19:49:14Z-
dc.date.available2021-10-13T19:49:14Z-
dc.date.issued1987-06-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/6402-
dc.description.abstractSeasonal increase in salinity in the wells near the sea shore is primarily due to salt water encroachment from the Arabian Sea which is hydraulically connected with the coastal aquifers running parallel to the ocean. The results from the field investigation carried out in this aspect with reference to coastal tracts in Malabar region are presented in this paper. Three years of observation on the coastal wells along Malabar region between Trichur and Kasaragod are analysed and correlated with depth to water level and distance of the well from the sea shore through a simple conceptual model. The model forwarded would be direct help to the well users to find out maximum quantity of water he can withdraw without adversely affecting the quality of water. It will also be of direct help in forecasting the likely level of salinity intrusion into the coastal aquifers and device possible remedial measures for the same.en_US
dc.language.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.subjectGroundwater Managementen_US
dc.subjectSea Water Intrusionen_US
dc.subjectSouth Western Peninsulaen_US
dc.subjectTrichuren_US
dc.subjectKasaragoden_US
dc.title7-Sea Water Intrusion in Coastal Unconfined Aquifers of South Western Peninsula.en_US
dc.typeTechnical Reporten_US
Appears in Collections:3-Jal Vigyan Sameeksha Vol.-2(1)-June-1987

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