WebDec 1, 2024 · Deuterium excess shows that non-direct evaporation (capillary evaporation, transpiration) and mineral/evaporite dissolution contribute to >60% salinity in groundwater with TDS>1000mg/L. Non-direct evaporation, like capillary evaporation and transpiration, is proposed as important processes contributing to groundwater salinity based on Cl/Br ... WebDec 1, 2012 · Deuterium excess (d) and TDS versus remaining fraction of reservoir (f) during water evaporation with an initial water d of 10‰ and TDS of 0.15 g/L at 25 °C and …
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WebAridity and seasonality of precipitation are characteristics of the highland region in Bolivia. Groundwater becomes an important and safe source of water when surficial bodies are intermittent and affected by natural and anthropogenic contamination. Decades of exploitation of the Challapampa aquifer, combined with lack of information required to … WebAug 1, 2024 · Historical data on nutrients (nitrogen and phosphorus) from about 12,000 ground-water and more than 22,000 stream samples have been compiled and related to … on the border plumbing lloydminster
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WebStable water isotopes (18O and deuterium) were used for the first time in this region to determine the isotopic characteristics of the different waters. There is a clear seasonal difference in the isotopic ratios and d-excess values between the summer and winter monsoon periods, with a predominance of lighter isotopes in the latter period. WebSep 22, 2006 · Abstract We measured deuterium excess (d = δD − 8δ18O) in throughfall, groundwater, soil water, spring water, and stream water for 3 years in a small headwater catchment ... This may imply the existence of bypass flow in the soil. Groundwater in the hillslope zone had short residence times, similar to those of the soil water. For ... Webobserved for the δ13C of groundwater and the calculated 14C boron-based dilution, except where the waters emerge in thick peat soil resulting in low δ13C values. 1. INTRODUCTION In Iceland, the deuterium content has been used extensively to trace the origin of groundwater, including geothermal water (Árnason, 1976, 1977). Since 1986 ... i only want to be with youtube