1. Effects of Recharge and Discharge on &delta²H and &delta18O Composition and Chloride Concentration of High Arsenic/Fluoride Groundwater from the Datong Basin, Northern China.
- Author
-
Xianjun Xie, Yanxin Wang, Chunli Su, and Duan, Mengyu
- Subjects
- *
GROUNDWATER recharge , *CHLORIDE content of water , *DELTAS , *ARSENIC in water , *GEOLOGICAL basins , *WATER chemistry - Abstract
To better understand the effects of recharge and discharge on the hydrogeochemistry of high levels of arsenic (As) and fluoride (F) in groundwater, environmental isotopic composition (&delta²H and &delta18O) and chloride (CI) concentrations were analyzed in 29 groundwater samples collected from the Datong Basin. High arsenic groundwater samples (As > 50 μg/L) were found to be enriched in lighter isotopic composition that ranged from --92 to --78 ∞ for deuterium (&delta²H) and from -12.5 to -9.9 ∞ for oxygen-18 (&delta18O). High F-containing groundwater (F > 1 mg/L) was relatively enriched in heavier isotopic composition and varied from --90 to -57 ∞ and from -12.2 to -6.7 ∞ for &delta²H and &delta18O, respectively. High chloride concentrations and &delta18O values were primarily measured in groundwater samples from the northern and southwestern portions of the study area, indicating the effect of evaporation on groundwater. The observation of relatively homogenized and low &delta18O values and chloride concentrations in groundwater samples from central part of the Datong Basin might be a result of fast recharge by irrigation returns, which suggests that irrigation using arsenic-contaminated groundwater affected the occurrence of high arsenic-containing groundwater in the basin. [ABSTRACT FROM AUTHOR]
- Published
- 2013
- Full Text
- View/download PDF