Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/39675
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dc.contributor.authorNaqvi, S.W.A.-
dc.contributor.authorReddy, C.V.G-
dc.date.accessioned2017-01-04T10:45:48Z-
dc.date.available2017-01-04T10:45:48Z-
dc.date.issued1975-12-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/39675-
dc.description213-215en_US
dc.description.abstractDegree of saturation of calcium carbonate as a function of depth has been studied at 3 locations in the Indian Ocean from alkalinity and pH measurements. Surface waters are 4-5 fold supersaturated with respect to calcite. Degree of saturation is maximum within the first 50 m. As the depth increases, the degree of saturation decreases and at about 1000 m the waters become either undersaturated or near-saturated.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.04(2) [December 1975]en_US
dc.titleVertical Distribution of the Degree of Calcium Carbonate Saturation in the Indian Oceanen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.04(2) [December 1975]

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