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dc.contributor.authorNaik, S.
dc.contributor.authorSenGupta, R.
dc.date.accessioned1994-10-26T09:56:45Z
dc.date.accessioned2017-09-29T13:47:07Z
dc.date.available1994-10-26T09:56:45Z
dc.date.available2017-09-29T13:47:07Z
dc.date.issued1975
dc.identifier.citationIndian Journal of Marine Sciences, vol.4; 1975; 141-144
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/5565
dc.description.abstractThe concept pE, expressed as a dimensionless quantity to study the redox potential of a system at equilibrium, is applied to study the chemistry of the system NO-<sub>3</sub>-NO-<sub>2</sub>NH+<sub>4</sub> in the northern Arabian Sea. Values observed are found to be close to the equilibrium values calculated from theoretical relations and are nearer to the more recent concept of the normal value for sea water.It is inferred that the system approaches equilibrium conditions in the deeper waters of the oceans along with the O<sub>2</sub>H<sub>2</sub>O<sub>2</sub> couple.
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectChemistry and Biogeochemistry
dc.subject.otherwater masses
dc.subject.othervertical distribution
dc.subject.otherocean basins
dc.subject.otherdissolved oxygen
dc.subject.othernutrients (mineral)
dc.subject.otherchemical Oceanography
dc.subject.otherISW, Arabian Sea
dc.titleChemical oceanography of the Arabian Sea: Part II - Equilibrium of inorganic nitrogen system
dc.typeJournal Article


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