Boron-Chlorinity Relationship in Western Bay of Bengal

dc.contributor.author	Narvekar, P.V.
dc.contributor.author	Zingde, M.D.
dc.contributor.author	SenGupta, R.
dc.date.accessioned	1995-05-07T09:57:14Z
dc.date.accessioned	2017-09-29T13:48:42Z
dc.date.available	1995-05-07T09:57:14Z
dc.date.available	2017-09-29T13:48:42Z
dc.date.issued	1981
dc.identifier.citation	Indian Journal of Marine Sciences, vol.10; 1981; 183-185
dc.identifier.issn	0379-5136
dc.identifier.uri	http://drs.nio.org/drs/handle/2264/6686
dc.description.abstract	Significant 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.language	en
dc.publisher	CSIR-NISCAIR
dc.relation.ispartof	Indian J Mar Sci
dc.relation.isreferencedby	SCI
dc.subject	Chemistry and Biogeochemistry
dc.subject.other	spatial variations
dc.subject.other	water column
dc.subject.other	organic matter
dc.subject.other	chlorinity
dc.subject.other	Boron
dc.subject.other	ISW, Bengal Bay
dc.title	Boron-Chlorinity Relationship in Western Bay of Bengal
dc.type	Journal Article
dc.affiliation.author	CSIR-National Institute of Oceanography, Bombay, Maharastra, India