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Climate Effects on Recharge and Evolution of Natural Water Resources in middle-latitude Watersheds Under Arid Climate

  • Bingqi ZhuEmail author
  • Jingjie Yu
  • Patrick Rioual
  • Yan Gao
  • Yichi Zhang
  • Heigang Xiong
Chapter
Part of the Springer Earth System Sciences book series (SPRINGEREARTH)

Abstract

This paper analyzes the physico-chemical characteristics of natural waters in middle-latitude drainage systems of central Asia, including the climatic, lithological and geomorphological conditions in which water flows and resides. This analysis allowed the identification of the geological evolution and recharge mechanism of the water resources in an arid environment. The studied waters at various sites are different in mineralization but similar to the majority of large rivers on earth, which are typically alkaline. However, no Cl-dominated water type occurs in the study area, indicating that these natural waters are still at an early stage of evolution. The regolith and geomorphological parameters controlling ground-surface temperature may play a large role in rock weathering regime and so in the geological evolution of water. Three main morphological and hydrological units are reflected in water physico-chemistry: the montane areas (recharge area) with silicate and carbonate weathering, the piedmonts and sedimentary platform (runoff area) with carbonate weathering, and the desert plains (discharge area) with evaporite dissolution. Climate influences the salinization of natural waters substantially. Direct recharge from seasonal snow and meltwater and infiltration of rainfall into the ground are thought to be significant recharge processes for natural waters in the study area, while recharge from potential deep groundwater may be much less important. The chemistry of lakes is generally consistent with those of large lakes in the world, but the enrichment of the ions in the lakes has been caused mainly by evaporation, rather than through the quality of the recharged water.

Keywords

Natural water Geological evolution Recharge mechanism Arid environment Climatic effect Central Asia 

Notes

Acknowledgements

This work was financially supported by the National Natural Science Foundation of China (Grant No.: 41371060, 41271049) and the Kezhen Young Talent Project of the Institute of Geographic Sciences and Natural Resources Research, CAS (Grant No.: 2013RC101).

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Copyright information

© Springer International Publishing Switzerland 2015

Authors and Affiliations

  • Bingqi Zhu
    • 1
    Email author
  • Jingjie Yu
    • 1
  • Patrick Rioual
    • 2
  • Yan Gao
    • 3
  • Yichi Zhang
    • 1
  • Heigang Xiong
    • 4
  1. 1.Key Laboratory of Water Cycle and Related Land Surface ProcessesInstitute of Geographic Sciences and Natural Resources Research, Chinese Academy of SciencesBeijingChina
  2. 2.Key Laboratory of Cenozoic Geology and EnvironmentInstitute of Geology and Geophysics, Chinese Academy of SciencesBeijingChina
  3. 3.Centro de Investigaciones en Geografia AmbientaUniversidad Nacional Autonoma de Mexico, Campus MoreliaMoreliaMexico
  4. 4.Key Laboratory of Oasis EcologyMinistry of EducationUrumqiChina

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