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Exposure and Health

, Volume 10, Issue 1, pp 1–13 | Cite as

Distribution and Enrichment Factors of High-Arsenic Groundwater in Inland Arid Area of P. R. China: A Case Study of the Shihezi Area, Xinjiang

  • Yanyan Zeng
  • Yinzhu Zhou
  • Jinlong ZhouEmail author
  • Ruiliang Jia
  • Jichun Wu
Original Paper

Abstract

To study the distribution, sources and enrichment factors of groundwater As in the Shihezi area in Xinjiang, China, 19 indexes in 23 groundwater samples were tested and analyzed with a control area of 1611 km2. Results showed that As concentrations ranged between non-detected and 49.1 μg/L with an average of 11.0 μg/L. Among all the samples, 34.8% of which had As concentrations greater than 10 μg/L, according to “Standards for Drinking Water Quality (GB5749-2006)”. Groundwater As showed a significant spatial distribution. High-As groundwaters (>10 μg/L) were mainly distributed in the confined groundwater in the northern part of the study area. Arsenic concentrations in the deep confined groundwater were higher than that in the shallow confined groundwater due to mixed exploitation of groundwater in confined groundwater region and overexploitation of deep groundwater in the Shihezi area. The hydrogeochemical type of groundwater changed from HCO3·SO4–Ca·Na in the southern piedmont zone to HCO3·SO4–Na in the northern fine soil plain. High-As groundwater generally occurred under weakly alkaline and reducing conditions with dominant hydrogeochemical type of groundwater of HCO3·SO4–Na. Groundwater As mainly derived from As-containing minerals in the coal seam of the southern mountain and the extensive use of As-containing pesticides in agricultural areas. Enrichment of groundwater As was mainly influenced by climate, geological settings and hydrogeochemical characteristic. In the transition zone of oasis and desert in the north of study area, intensive evaporation of groundwater promoted the enrichment of As in shallow groundwater. In the confined groundwater area in the northern part of the study area, relatively weak groundwater runoff and reducing environment may contribute to groundwater As enrichment in confined aquifers. In addition, high pH values and high F concentrations in the groundwater may contribute to the enrichment of groundwater As, while TDS, total Fe and Mn concentrations of groundwater had little effect on As enrichment in the study area. Two confined groundwater flow paths were selected in the study area. Inverse geochemical modeling was performed using PHREEQC. The results showed that As-containing realgar dissolved in groundwater, indicating that realgar was the major mineral source of groundwater As. The dissolved amount of realgar along deep confined groundwater flow path was higher than that along shallow confined groundwater flow path, indicating that the concentrations of As dissolved in deep confined groundwater were higher than that in shallow confined groundwater. Meanwhile, dissolution of fluorite in groundwater caused the increase in groundwater F, which further confirmed that groundwater As and F had a positive correlation.

Keywords

High-arsenic groundwater Distribution Enrichment factors Inverse geochemical modeling The Shihezi area, Xinjiang 

Notes

Acknowledgements

The study has been financially supported by NSFC-Xinjiang project “Transport of typical organic pollutants in the groundwater flow system of arid region and its risk assessment” (U1503282); China Geological Survey Bureau project “Groundwater pollution survey of main cities in north western China” (1212011220982); peak discipline project of hydraulic engineering of Xinjiang Uyghur Autonomous Region (xjslgcgfxk20161103).

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Copyright information

© Springer Science+Business Media Dordrecht 2016

Authors and Affiliations

  • Yanyan Zeng
    • 1
    • 2
  • Yinzhu Zhou
    • 3
    • 4
  • Jinlong Zhou
    • 1
    • 2
    Email author
  • Ruiliang Jia
    • 1
    • 2
  • Jichun Wu
    • 5
  1. 1.College of Water Conservancy and Civil EngineeringXinjiang Agricultural UniversityÜrümqiPeople’s Republic of China
  2. 2.Xinjiang Hydrology and Water Resources Engineering Research CenterÜrümqiPeople’s Republic of China
  3. 3.School of Water Resources and EnvironmentChina University of GeosciencesBeijingPeople’s Republic of China
  4. 4.U.S. Geological Survey, MS 963Denver Federal CenterDenverUSA
  5. 5.School of Earth Sciences and EngineeringNanjing UniversityNanjingPeople’s Republic of China

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