Groundwater chemistry is largely controlled by carbonate minerals. While the hydrogeochemical data are broadly

consistent with microbially mediated reductive dissolution of Fe(III) oxyhydroxides being an important mechanism releasing As into the aquifer, further work is required to unambiguously resolve the mechanism(s) and definitively explain the apparent decoupling with Fe2+. Other geochemical processes, e.g., silicate weathering and carbonate dissolution, are primarily responsible for distribution of solutes in Cobimetinib groundwater. This project was funded by Australian Research Council Future Fellowship (Grant no. FT110100130) and Southern Cross University. The authors would like to thank Mr. Makhan Maharjan (ENPHO) for providing blanket testing data

of groundwater arsenic. We also appreciate the support of Environment and Public Health Organization (ENPHO), Nepal Red Cross Society (NRCS), Central Department of Geology (CDG) of Tribhuvan University, Department of Mines and Geology (DMG), Groundwater Resources Development Board (GRDB), HEMS Nepal and ASHA/Nepal for their kind cooperation. We acknowledge the invaluable contribution of Mr. Gyan Prakash Yadav, Ms. Lauren Hook and Er. Om Shrestha during the field study at Nawalparasi. We thank Barbara Harrison for assisting with sample quarantine and Environmental Analysis Laboratory for chemical analyses. We would like to thank anonymous reviewers for their suggestions. J. Diwakar was financially

supported by the Australian Everolimus molecular weight Postgraduate Award/International Postgraduate Research Scholarship (APA/IPRS) provided by Australian Government. Salary support for Scott Johnston was provided by the Australian Research Council Future Fellowship (Grant no. FT110100130). “
“Climate change is predicted to lead to an intensification of the global hydrological cycle (Huntington, 2006). Reverse transcriptase Freshwater resources in dry subtropical regions may be impacted adversely, but favorably affected at higher latitudes (Cisneros et al., 2014). Quantifying current and future freshwater availability is a critical aspect of adapting to changing and variable climate because access to sufficient freshwater is linked to food security, human health, ecosystem health, land use change, economic development, and regional conflicts (Schuol et al., 2008). The Brahmaputra River basin located in south Asia is one of the world’s major river basins for human and ecological needs and supports the livelihoods of over 66 million people through subsistence agriculture. Despite the growing attention to quantify freshwater resources and to assess the vulnerability of freshwater to global change (Alcamo and Henrichs, 2002, Faramarzi et al., 2009, Lehner et al., 2006, Oki and Kanae, 2006, Piao et al., 2010, Schuol et al., 2008, Srinivasan et al., 1998a, Srinivasan et al., 1998b and Vörösmarty et al.