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dc.contributor.authorMartin, G.D.
dc.contributor.authorMuraleedharan, K.R.
dc.contributor.authorVijay, J.G.
dc.contributor.authorRejomon, G.
dc.contributor.authorMadhu, N.V.
dc.contributor.authorShivaprasad, A.
dc.contributor.authorHaridevi, C.K.
dc.contributor.authorNair, M.
dc.contributor.authorBalachandran, K.K.
dc.contributor.authorRevichandran, C.
dc.contributor.authorJayalakshmy, K.V.
dc.contributor.authorChandramohanakumar, N.
dc.date.accessioned2017-09-27T13:04:53Z
dc.date.available2017-09-27T13:04:53Z
dc.date.issued2010
dc.identifier.citationBiogeosciences Discussions, vol.7; 2010; 1751-1782.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/5148
dc.description.abstractHydrographic characteristics of the southwest coast of India and its adjoining Cochin backwaters (CBW) were studied during the summer monsoon. Anomalous formation of anoxia and denitrification were observed in the bottom layers of CBW. The prevalent upwelling in the Arabian Sea (AS) brought cool, high saline, oxygen deficient and nutrient-rich waters towards the coastal zone and bottom layers of CBW during the high tide. High freshwater discharge in the surface layers brought high amount of nutrients and makes the CBW system highly productive. Intrusion of AS waters seems to be stronger towards the upstream end (approx. 15 km), than had been previously reported, as a consequence of the lowering of river discharges and deepening of channels in the estuary. Time series measurements in the lower reaches of CBW indicated a low mixing zone with increased stratification, 3 h after the high tide (highest high tide) and high variation in vertical mixing during the spring and neap phases. The upwelled waters (O sub(2) less than or equal to 40 mu M) intruded into the estuary was found to lose more oxygen during the neap phase (suboxic O sub(2) less than or equal to 4 mu M) than spring phase (hypoxic O sub(2) less than or equal to 10 mu M). Increased stratification coupled with low ventilation and presence of high organic matter have resulted in an anoxic condition (O sub(2)=0), 2-6 km away from barmouth of the estuary and leads to the formation of hydrogen sulphide. The reduction of nitrate and formation of nitrite within the oxygen deficient waters indicated strong denitrification intensity in the estuary. The expansion of oxygen deficient zone, denitrification and formation of hydrogen sulphide may lead to a destruction of biodiversity and an increase of green house gas emissions from this region.
dc.language.isoen
dc.publisherCopernicus Publications
dc.rightsCopyright [2010]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjectanoxia
dc.subjectdenitrification
dc.subjectestuarine chemistry
dc.titleFormation of anoxia and denitrification in the bottom waters of a tropical estuary, southwest coast of India.
dc.typeJournal Article


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