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Supervised by Ministry of Industry and Information Technology of The People's Republic of China Sponsored by Harbin Institute of Technology Editor-in-chief Yu Zhou ISSNISSN 1005-9113 CNCN 23-1378/T

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Related citation:Ling-Yan Feng,Li-Xin Li,Yi-Xing Yuan.Study on the Reservoir Water Quality Change Rule in Northern China[J].Journal of Harbin Institute Of Technology(New Series),2013,20(4):26-30.DOI:10.11916/j.issn.1005-9113.2013.04.005.
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Study on the Reservoir Water Quality Change Rule in Northern China
Author NameAffiliation
Ling-Yan Feng School of Municipal and Environmental Engineering, Harbin Institute of Technology, Harbin 150090, China 
Li-Xin Li School of Municipal and Environmental Engineering, Harbin Institute of Technology, Harbin 150090, China
School of Environment and Chemical Engineering, Heilongjiang University of Science and Technology, Harbin 150022, China 
Yi-Xing Yuan School of Municipal and Environmental Engineering, Harbin Institute of Technology, Harbin 150090, China 
Abstract:
Water quality index of reservoir source water were tracked during three years in a north frigid area, the effect on supplied water quality was also studied. Based on the analysis of the monitoring data during the same season, the reservoir source water had typical and seasonal variation characteristics that was divided into four periods including the icebound period, spring period (or peach blossom period), stable period in summer and autumn and winter period. The icebound period was charactered by the typical low temperature and turbidity, pH and oxygen consumption decreased gradually showed that the gradually anaerobic trend existed in the reservoir. In May as the reservoir completely thawed, upstream water inflow and the total pollutant in the reservoir gradually increased, but the bottom of reservoir bottom was stable in the anaerobic state temporarily. The state completely disappeared, various index increased significantly in the middle of July. The water had high chroma characteristics, chroma and turbidity increased significantly in the summer and autumn (7-11 months), but stability of water quality was poor because of rainfall. The reservoir gradually froze after the middle of November and the flow of water decreased. The peak of chroma appeared a month later than the water temperature. Due to the water turbidity was low, and the floc was small and light, the conventional water purification process design based on removal of turbidity achieved removal of chroma through a lot dosing of coagulant.
Key words:  reservoir source water in frigid area  quality of water supply  chroma  low temperature and low turbidity
DOI:10.11916/j.issn.1005-9113.2013.04.005
Clc Number:X524
Fund:

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