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dc.contributor.authorNarvekar, P.V.
dc.contributor.authorZingde, M.D.
dc.contributor.authorSenGupta, R.
dc.date.accessioned1995-05-07T09:57:14Z
dc.date.accessioned2017-09-29T13:48:42Z
dc.date.available1995-05-07T09:57:14Z
dc.date.available2017-09-29T13:48:42Z
dc.date.issued1981
dc.identifier.citationIndian Journal of Marine Sciences, vol.10; 1981; 183-185
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6686
dc.description.abstractSignificant scatter in B/Cl beyond the limit of experimental error indicates that the ratio is not truly constant. B/Cl maximum, centred around 100 m, appears to be influenced by colloidal and particulate matter while the maximum at 400 m appears to be due to the influence of Persian Gulf and Red Sea water and also due to the release of boron by oxidative degradation of organic matter. At 3000 m depth the ratio is typical of Antarctic bottom water.
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectChemistry and Biogeochemistry
dc.subject.otherspatial variations
dc.subject.otherwater column
dc.subject.otherorganic matter
dc.subject.otherchlorinity
dc.subject.otherBoron
dc.subject.otherISW, Bengal Bay
dc.titleBoron-Chlorinity Relationship in Western Bay of Bengal
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Bombay, Maharastra, India


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