Wen Cheng-Cheng, Huang Ting-Lin, Li Nan, Zhang Hai-Han, Lin Zi-Shen, Li Yan-Qing, Yang Shang-Ye, Dong Ya-Jun
Key Laboratory of Northwest Water Resource, Environment and Ecology, Ministry of Education, School of Environmental and Municipal Engineering, Xi'an University of Architecture and Technology, Xi'an 710055, China.
Shaanxi Key Laboratory of Environmental Engineering, School of Environmental and Municipal Engineering, Xi'an University of Architecture and Technology, Xi'an 710055, China.
Huan Jing Ke Xue. 2020 Mar 8;41(3):1227-1235. doi: 10.13227/j.hjkx.201909176.
To explore the effects of water quality improvement by artificial destratification and artificially-induced mixing, as well as realize the conditions of artificial mixing and natural mixing, the Lijiahe Reservoir was selected to monitor the indexes of water quality and hydrometeorology from June 2017 to April 2019 and to analyze the characteristics of variations in water temperature, dissolved oxygen, and pollutants during the natural and induced-mixing processes. The results demonstrated that:① The natural process had the features of a long period of thermal stratification and only a short period of mixing of about 2.5 months. Through the operation of water-lifting aerators (WLAs) during the induced-mixing process, the water body was completely mixed and entered the cooling period at the end of September, achieving the conditions of induced-natural mixing. The surface water temperature and average air temperature were 20.17℃ and 16.5℃, respectively, and the water body continued to be naturally mixed after the WLA system was shut down, which led to a natural mixing cycle of 5.5 months. ② During the natural-mixing process, the concentration of pollutants was relatively high in the whole period, and the concentration of surface pollutants in the mixing stage presented a trend of increasing first and then decreasing. The oxycline appeared with thermal stratification, and the anaerobic cycle in the bottom of water column reached 6 months. ③ Compared with the natural-mixing process, the hypolimnetic anaerobic condition was eliminated and the control effects of pollutants dominated during the induced-mixing process. Simultaneously, the concentrations of NH-N, TP, Fe, and Mn in the bottom of the water column were cut by 76.2%, 75.5%, 82.2%, and 82.1%, respectively, during the same period from October to March of the following year, and met the "Environmental Quality Standards for Surface Water". This study shows that the artificially-induced mixing process contributes to water quality improvement and mixing-period prolongation.
为探究人工消分层和人工诱导混合对水质改善的效果,以及实现人工混合和自然混合的条件,选取李家河水库,于2017年6月至2019年4月监测水质和水文气象指标,分析自然混合和诱导混合过程中水温、溶解氧及污染物的变化特征。结果表明:①自然过程具有热分层期长、混合期短(约2.5个月)的特点。通过诱导混合过程中运行提水曝气器,水体完全混合并于9月底进入降温期,实现了诱导-自然混合的条件。地表水温和平均气温分别为20.17℃和16.5℃,提水曝气系统关闭后水体继续自然混合,自然混合周期达5.5个月。②在自然混合过程中,污染物浓度在整个时期相对较高,混合阶段表层污染物浓度呈先升高后降低的趋势。温跃层随热分层出现,水柱底部厌氧周期达6个月。③与自然混合过程相比,诱导混合过程消除了下层水体的厌氧状况,污染物控制效果显著。同时,次年10月至3月同期,水柱底部NH-N、TP、Fe和Mn的浓度分别降低了76.2%、75.5%、82.2%和82.1%,达到《地表水环境质量标准》。本研究表明,人工诱导混合过程有助于水质改善和延长混合期。