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First assessment of water and carbon cycles in two tropical coastal rivers of south‐west India: an isotopic approach
Author(s) -
Tripti M.,
Lambs L.,
Otto T.,
Gurumurthy G. P.,
Teisserenc R.,
Moussa I.,
Balakrishna K.,
Probst J. L.
Publication year - 2013
Publication title -
rapid communications in mass spectrometry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.528
H-Index - 136
eISSN - 1097-0231
pISSN - 0951-4198
DOI - 10.1002/rcm.6616
Subject(s) - carbon cycle , dissolved organic carbon , total organic carbon , weathering , biogeochemical cycle , evapotranspiration , hydrology (agriculture) , organic matter , carbon fibers , monsoon , water cycle , isotopes of carbon , environmental science , environmental chemistry , chemistry , geology , oceanography , geochemistry , ecosystem , ecology , materials science , geotechnical engineering , organic chemistry , composite number , composite material , biology
RATIONALE The contribution of tropical coastal rivers to the global carbon budget remains unmeasured, despite their high water dynamics, i.e. higher run‐off with their basin characteristic of warm temperature. Two rivers draining the western part of the Western Ghats, the Swarna (length 80 km) and Nethravati (147 km) Rivers, were studied for water and carbon cycles. METHODS The stable isotope ratios of oxygen (δ 18 O values), hydrogen (δ 2 H values) and carbon (δ 13 C values) were used to understand the water circulation, the weathering processes and the carbon biogeochemical cycle. The river water samples were collected during the dry post‐monsoonal season (November 2011). RESULTS The δ 18 O and δ 2 H values of river water suggested that the monsoonal vapour source and its high recycling have a dominant role because of the orographical and tropical conditions. The absence of calcareous rocks has led to dissolved inorganic carbon (DIC) mainly originating from atmospheric/soil CO 2 , via rock‐weathering processes, and the low soil organic matter combined with high run‐off intensity has led to low riverine dissolved organic carbon (DOC) contents. The δ 13 C values increase from upstream to downstream and decrease with increasing pCO 2 . There is a positive relationship between the δ 13 C DIC values and the DOC concentrations in these two rivers that is contrary to that in most of the studied rivers of the world. CONCLUSIONS The higher evapotranspiration supported by tropical conditions suggests that there are higher vapour recycling process in the Swarna and Nethravati basins as studied from the water δ 18 O and δ 2 H values. The basin characteristics of higher rainfall/run‐off accompanied by warm temperature suggest that the δ 13 C value of riverine DIC is mainly controlled by the weathering of source rocks (silicates) with variation along the river course by CO 2 degassing from the river water to the atmosphere and is less dominated by the oxidation of DOC. Copyright © 2013 John Wiley & Sons, Ltd.