Please use this identifier to cite or link to this item: http://nopr.niscair.res.in/handle/123456789/38814
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dc.contributor.authorShirodkar, P V-
dc.contributor.authorSankaranarayanan, V N-
dc.date.accessioned2016-12-16T10:50:13Z-
dc.date.available2016-12-16T10:50:13Z-
dc.date.issued1984-12-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38814-
dc.description178-180en_US
dc.description.abstractIn the upper 200 m in the Wadge Bank region B varies from 3.09 to 4.95 mg.kg-1. B/Cl ratio ranges from 0.159 to 0.256. Depthwise distribution of B shows its inverse relationship with dissolved oxygen, direct relationship with inorganic phosphate and no clear relationship with particulate matter. The data suggest that a part of the variation in B/Cl ratio is associated with oxidative degradation of organic matter in the subsurface layers.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.13(4) [December 1984]en_US
dc.titleBoron in seawater of Wadge Bank region in the Indian Oceanen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.13(4) [December 1984]

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