Gurumurthy G. P., Balakrishna K., Tripti M., Riotte Jean, Audry S., Braun Jean-Jacques, Shankar H. N. U. (2015). Use of Sr isotopes as a tool to decipher the soil weathering processes in a tropical river catchment, southwestern India. Applied Geochemistry, 63, p. 498-506. ISSN 0883-2927.
Titre du document
Use of Sr isotopes as a tool to decipher the soil weathering processes in a tropical river catchment, southwestern India
Gurumurthy G. P., Balakrishna K., Tripti M., Riotte Jean, Audry S., Braun Jean-Jacques, Shankar H. N. U.
Source
Applied Geochemistry, 2015,
63, p. 498-506 ISSN 0883-2927
River water composition (major ion and Sr-87/Sr-86 ratio) was monitored on a monthly basis over a period of three years from a mountainous river (Nethravati River) of southwestern India. The total dissolved solid (TDS) concentration is relatively low (46 mg L-1) with silica being the dominant contributor. The basin is characterised by lower dissolved Sr concentration (avg. 150 nmol L-1), with radiogenic Sr-87/Sr-86 isotopic ratios (avg. 0.72041 at outlet). The composition of Sr and Sr-87/Sr-86 and their correlation with silicate derived cations in the river basin reveal that their dominant source is from the radiogenic silicate rock minerals. Their composition in the stream is controlled by a combination of physical and chemical weathering occurring in the basin. The molar ratio of SiO2/Ca and Sr-87/Sr-86 isotopic ratio show strong seasonal variation in the river water, i.e., low SiO2/Ca ratio with radiogenic isotopes during non-monsoon and higher SiO2/Ca with less radiogenic isotopes during monsoon season. Whereas, the seasonal variation of Rb/Sr ratio in the stream water is not significant suggesting that change in the mineral phase being involved in the weathering reaction could be unlikely for the observed molar SiO2/Ca and Sr-87/Sr-86 isotope variation in river water. Therefore, the shift in the stream water chemical composition could be attributed to contribution of ground water which is in contact with the bedrock (weathering front) during non-monsoon and weathering of secondary soil minerals in the regolith layer during monsoon. The secondary soil mineral weathering leads to limited silicate cation and enhanced silica fluxes in the Nethravati river basin.
