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dc.contributor.authorSridevi, B.
dc.contributor.authorVaury, V.
dc.contributor.authorKumar, B.S.K.
dc.contributor.authorSarma, V.V.S.S.
dc.contributor.authorCardinal, D.
dc.contributor.authorSebilo, M.
dc.date.accessioned2023-07-17
dc.date.accessioned2023-07-17T16:02:27Z
dc.date.available2023-06-14
dc.date.available2023-07-17T16:02:27Z
dc.date.issued2023
dc.identifier.citationEstuarine, Coastal and Shelf Science, vol.290; 2023; Article no: 108404
dc.identifier.issn0272-7714
dc.identifier.urihttps://doi.org/10.1016/J.ECSS.2023.108404
dc.identifier.urihttp://drs.nio.res.in/drs/handle/2264/9089
dc.description3.229
dc.description.abstractIndian estuaries are hypothesized to export a significant amount of nitrogen nutrients to the coastal waters due to the high use of fertilizers. To examine the possible sources of nitrogen nutrients and their modifications within the estuary, a study was conducted by collecting samples at monthly intervals for a period of a year. The river Godavari is the largest monsoonal estuary in India and is fed by monsoon rainfall. Hence the entire estuary is filled with fresh water from July to September (the wet period) whereas saline water is dominant during the dry period. An order of magnitude increase in nitrate concentrations was observed during the wet due to a peak in discharge compared to the dry period. The isotopic composition of nitrogen in nitrate (δ15NNO3) was lower during the wet than the dry period and displayed a significant linear relationship with Chlorophyll-a (Chl-a), particulate organic nitrogen (PON) and carbon (POC) indicating that biological process modified their composition. The lower δ15NNO3 and higher δ18ONO3 values were noticed during the wet than during the dry period. The δ15NNO3 versus δ18ONO3 plot suggests a possible source of nitrate through the nitrification of soil/sewage-borne nitrogen. The higher δ18ONO3/δ15NNO3 ratios (>1) were observed during August and September than in other months indicating the occurrence of denitrification during the former months. In contrast, an insignificant change in δ15NNO3 and δ18ONO3 within the estuary suggested that denitrification occurred upstream and not within the estuarine zone. River discharge brought residual nitrate to the estuary leading to less input of nitrate to the coastal Bay of Bengal than hitherto hypothesized
dc.languageen
dc.publisherElsevier
dc.relation.isreferencedbySCI
dc.rightsOnly the author version of the copright reserved papers uploaded. Contact drs@nio.org for any complaints regarding copyright violations
dc.titleAssessing seasonal nitrogen transformations in the Godavari estuary, India
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Visakhapatnam, Andhra Pradesh, India


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