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Volume 38 Issue 10
Nov.  2020
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YUAN Xiao-min, LIU Qiang, MA Xiao-jing, SUN Ying-shan, YAN Si-rui, LI Miao. HYDROCHEMICAL CHARACTERISTICS AND POSSIBLE CONTROLS OF THE SURFACE WATER IN LAKE BAIYANGDIAN BASIN[J]. ENVIRONMENTAL ENGINEERING , 2020, 38(10): 1-6. doi: 10.13205/j.hjgc.202010001
Citation: YUAN Xiao-min, LIU Qiang, MA Xiao-jing, SUN Ying-shan, YAN Si-rui, LI Miao. HYDROCHEMICAL CHARACTERISTICS AND POSSIBLE CONTROLS OF THE SURFACE WATER IN LAKE BAIYANGDIAN BASIN[J]. ENVIRONMENTAL ENGINEERING , 2020, 38(10): 1-6. doi: 10.13205/j.hjgc.202010001

HYDROCHEMICAL CHARACTERISTICS AND POSSIBLE CONTROLS OF THE SURFACE WATER IN LAKE BAIYANGDIAN BASIN

doi: 10.13205/j.hjgc.202010001
  • Received Date: 2020-05-21
  • To explore the characteristics and sources of surface water hydrochemistry in semi-arid areas, we analyzed the main ion composition characteristics and sources of surface water in Lake Baiyangdian basin, using hrochemical technics such as Piper Triangular diagrams and Gibbs water-rock model. The results showed that the pH of the surface water in the Lake Baiyangdian basin varied from 7.56 to 8.23, which was weakly alkaline. And the total dissolved solids, was 100 mg/L to 650 mg/L in different regions of the basin, ranking as Lake Baiyangdian > downstream > dpstream. The cations in the surface water of Lake Baiyangdian basin were mainly Na+ and Ca2+, which accounted for 76.60% of the total cations. And the anions were mainly HCO3-, which accounted for about 61.52% of total anions. The water chemistry types of surface water were HCO3-Ca in upstream, and HCO3·SO4·Cl-Na·Ca in downstream and Lake Baiyangdian. The hydrogeochemical process of Lake Baiyangdian basin was controlled by both human activities and natural functions. For natural sources, the ions of the surface water of the Lake Baiyangdian basin originated from rock weathering, carbonate weathering and silicate weathering mainly, which also affected by evaporation-crystallization.
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