Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/39458
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dc.contributor.authorSrivastava, P. C.-
dc.date.accessioned2016-12-30T10:48:47Z-
dc.date.available2016-12-30T10:48:47Z-
dc.date.issued1976-06-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/39458-
dc.description121-124en_US
dc.description.abstractFluorescent tracer studies carried out during February 1972 indicate that offshore sediments move predominantly towards north-east with some movement westward and shoreward; the beach sand moves west-southwesterly. Northeasterly direction of movement of sediments seems to be due to prevailing coastal currents and tides; westward and shoreward movements may be due to waves and tides. West-south-westerly movement of beach sand also seems to be due to waves approaching from south-east. Depletion rate for the beach experiment is 4.9% per min for the first 20 min.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.05(1) [June 1976]en_US
dc.titleStudy of movement of sediments by fluorescent tracers at paradip port, east coast of Indiaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.05(1) [June 1976]

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