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Volume 39 Issue 10
Jan.  2022
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Article Contents
LIU Si-xuan, LI Yi-ping, ZHU Ya, TANG Chun-yan, WEI Yao, LI Rong-hui, CHEN Gang. MIGRATION OF IRON, MANGANESE AND SULFIDE IN BLACK RESERVOIR WATER IN SOUTH CHINA: A CASE STUDY OF TIANBAO RESERVOIR, NANNING[J]. ENVIRONMENTAL ENGINEERING , 2021, 39(10): 78-84. doi: 10.13205/j.hjgc.202110011
Citation: LIU Si-xuan, LI Yi-ping, ZHU Ya, TANG Chun-yan, WEI Yao, LI Rong-hui, CHEN Gang. MIGRATION OF IRON, MANGANESE AND SULFIDE IN BLACK RESERVOIR WATER IN SOUTH CHINA: A CASE STUDY OF TIANBAO RESERVOIR, NANNING[J]. ENVIRONMENTAL ENGINEERING , 2021, 39(10): 78-84. doi: 10.13205/j.hjgc.202110011

MIGRATION OF IRON, MANGANESE AND SULFIDE IN BLACK RESERVOIR WATER IN SOUTH CHINA: A CASE STUDY OF TIANBAO RESERVOIR, NANNING

doi: 10.13205/j.hjgc.202110011
  • Received Date: 2020-12-24
    Available Online: 2022-01-26
  • Iron and manganese are redox sensitive elements. Anaerobic and aerobic process can cause the release and morphological transformation of iron, manganese and sulfide sediments, resulting in the deterioration of water quality. At present, few studies combined black water of reservoir with migration of iron, manganese and sulfide. In order to explore the frequent blackening phenomenon of reservoirs in the southern water source area, we selected the Tianbao reservoir in Nanning as the research object, and collected samples from different depths of the reservoir from March 2018 to December 2018, to analyze the seasonal variation characteristics of water quality of the reservoir and the influence on the migration and transformation of iron, manganese and sulfide. The results showed that the thermal stratification structure was mainly affected by the temperature change. The formation of thermocline in stratification period led to the vertical physical and chemical properties difference, which formed the low temperature anaerobic environment at the bottom. And the unique red soil structure made iron and manganese have stronger endogenous release capacity. Under the influence of rainfall erosion and long-term anaerobic situation, the iron and manganese layer released in large quantities (0.76 mg/L and 1.47 mg/L), the sulfide release was inhibited by high concentration iron (0.005 mg/L). During the blackening period, the stratification failure caused vertical convective mixing. Reoxygenation transformed the forms of iron, manganese and sulfide, and simultaneously migration upward produced FES, MNS and other blackening substances, which triggered the surface blackening phenomenon. The key to solve the problem of blackening was to carry out researches on triggering mechanism and substance screening of black water.
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