4.4 Article

Trace Element Hydrochemistry Indicating Water Contamination in and Around the Yangbajing Geothermal Field, Tibet, China

Journal

Publisher

SPRINGER
DOI: 10.1007/s00128-009-9812-7

Keywords

Geothermal water; Trace element; Water contamination; Yangbajing

Funding

  1. National Natural Science of Foundation of China [40830748, 40702041, 40425001]
  2. Open Fund of State Key Laboratory of Environmental Geochemistry
  3. Research Fund for the Doctoral Program of Higher Education of China [20070491008]
  4. Natural Science Foundation of Hubei Province of China [2007ABA312]
  5. Open Fund of State Key Laboratory of Geological Processes and Mineral Resources [GPMR200714]
  6. Open Fund of MOE Key Laboratory of Biogeology and Environmental Geology [BGEGF200813]

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Thirty-eight water samples were collected at Yangbajing to investigate the water contamination resulting from natural geothermal water discharge and anthropogenic geothermal wastewater drainage. The results indicate that snow or snow melting waters, Yangbajing River waters and cold groundwaters are free from geothermal water-related contamination, whereas Zangbo river waters are contaminated by geothermal wastewaters. Moreover, there may exist geothermal springs under the riverbed of a tributary stream of Zangbo River as shown by its Cd, Li, Mo and Pb concentrations. The efforts made in this study show trace element hydrochemistry can well indicate water quality degradation related to geothermal water exploitation.

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