Sources of major ions and processes affecting the geochemical and isotopic signatures of subsurface waters along a tropical river, Southwestern India

• Published in: Environmental earth sciences Vol. 73; no. 1; pp. 333 - 346
• Main Authors: Gurumurthy, G. P, Balakrishna, K, Tripti, M, Riotte, Jean, Audry, Stéphane, Braun, Jean-Jacques, Lambs, Luc, Udaya Shankar, H. N
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer-Verlag 01.01.2015; Springer Berlin Heidelberg; Springer Nature B.V
• Subjects: Biogeosciences; Earth and Environmental Science; Earth Sciences; Environmental Science and Engineering; Geochemistry; Geology; groundwater; hydrochemistry; Hydrology/Water Resources; Ions; Isotopes; Local precipitation; minerals; monitoring; monsoon season; Monsoons; Original Article; Rainforests; River flow; Rivers; Rocks; Seasonal variations; Stable isotopes; Surface water; Surface-groundwater relations; Terrestrial Pollution; Tropical environments; tropics; Water levels; Weathering; India; Major ions; Southwestern India; Nethravati–Gurupur catchment; Groundwater chemistry; Stable isotopes
• ISSN: 1866-6280; 1866-6299
• DOI: 10.1007/s12665-014-3428-x

Systematic monitoring of subsurface hydrogeochemistry has been carried out for a period of one year in a humid tropical region along the Nethravati–Gurupur River. The major ion and stable isotope (δ¹⁸O and δ²H) compositions are used to understand the hydrogeochemistry of groundwater and its interaction with surface water. In the study, it is observed that intense weathering of source rocks is the major source of chemical elements to the surface and subsurface waters. In addition, agricultural activities and atmospheric contributions also control the major ion chemistry of water in the study area. There is a clear seasonality in the groundwater chemistry, which is related to the recharge and discharge of the hydrological system. On a temporal scale, there is a decrease in major cation concentrations during the monsoon which is a result of dilution of sources from the weathering of rock minerals, and an increase in anion concentrations which is contributed by the atmosphere, accompanied by an increase in water level during the monsoon. The stable isotope composition indicates that groundwater in the basin is of meteoric origin and recharged directly from the local precipitation during the monsoonal season. Soon after the monsoon, groundwater and surface water mix in the subsurface region. The groundwater feeds the surface water during the lean river flow season.