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dc.contributor.authorKrishna, M.S.
dc.contributor.authorViswanadham, R.
dc.contributor.authorPrasad, M.H.K.
dc.contributor.authorKumari, V.R.
dc.contributor.authorSarma, V.V.S.S.
dc.date.accessioned2019/04/29
dc.date.accessioned2019-04-30T12:48:26Z
dc.date.available2019/01/30
dc.date.available2019-04-30T12:48:26Z
dc.date.issued2019
dc.identifier.citationBiogeosciences, vol.16(2); 2019; 505-519
dc.identifier.issn1726-4189
dc.identifier.urihttps://doi.org/10.5194/bg-16-505-2019
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/8132
dc.description.abstractRivers are an important source of dissolved inorganic carbon (DIC) to the adjacent coastal waters. In order to examine the spatial variability in the distribution and major sources of DIC in the Indian monsoonal rivers and to quantify their export flux to the northern Indian Ocean, 27 major and medium-sized rivers were sampled during the discharge period. Significant spatial variability in concentrations of DIC (3.4-73.6-mg-L-1) was observed, and it is attributed to spatial variations in the precipitation pattern, the size of rivers, pollution and lithology of the catchments. The stable isotopic composition of DIC (-13CDIC) also showed strong spatial variability (-13.0 to -1.4‰) in the Indian monsoonal rivers with relatively depleted -13CDIC values in rivers of the northwest of India (-11.1±2.3-‰) and enriched values in the southeast of India (-3.5±2.3-‰). Results of the linear least-squares regression models of Keeling and Miller-Tans plots indicated that the chemical weathering of carbonate and silicate minerals by soil CO2 is the major source of DIC in the Indian monsoonal rivers. Spatial variability in the deviation of -13CDIC from the approximated -13C of the source may probably be due to dominant autotrophic production in rivers of the southeastern region, whereas heterotrophic decomposition of organic matter largely influences the other Indian monsoonal rivers. It is estimated that the Indian monsoonal rivers annually export -10.3-Tg of DIC to the northern Indian Ocean, of which the major fraction (75-%) enters into the Bay of Bengal, and the remaining fraction reaches to the Arabian Sea. This is consistent with the freshwater flux, which is 3 times higher for the Bay of Bengal (-378-km3-yr-1) than for the Arabian Sea (122-km3-yr-1). Despite discharge from the Indian monsoonal rivers accounting for only 1.3-% of the global freshwater discharge, they disproportionately export 2.5-% of the total DIC exported by the world's major rivers. Despite rivers from the region in the southwest (SW) of India exporting DIC that is an order of magnitude lower (0.3-Tg-yr-1) than the rivers from other regions of India, the highest yield of DIC was found in the rivers of the SW region of India. It is attributed to intense precipitation (-3000-mm), favorable natural vegetation of tropical moist deciduous and tropical wet evergreen and semi-evergreen forests, tropical wet climate, high soil organic carbon, and the dominance of red loamy soils in catchments of the rivers from SW region.
dc.languageen
dc.publisherEuropean Geosciences Union
dc.relation.isreferencedbySCI
dc.rightsCreative commons
dc.titleExport fluxes of dissolved inorganic carbon to the northern Indian Ocean from the Indian monsoonal rivers
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Visakhapatnam, Andhra Pradesh, India


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