Zhang Chun-Hua, Huang Ting-Lin, Fang Kai-Kai, Zhou Shi-Lei, Xia Chao
School of Environmental and Municipal Engineering, Xi'an University of Architecture and Technology, Xi'an 710055, China.
Huan Jing Ke Xue. 2016 Nov 8;37(11):4187-4193. doi: 10.13227/j.hjkx.201605153.
In order to explore the trend and driving factors of nitrogen in the early stage of the thermal stratification in Zhoucun reservoir, the water quality indicators in main reservoir area of Zhoucun reservoir were monitored regularly form February to April (2016). Meanwhile, the fresh water and surface sediments in the sampling point were collected to study the effect of water and sediment denitrification by simulation in laboratory. The results showed that: the concentration of TN decreased from (2.28±0.09) mg·L to (1.08±0.09) mg·L, the concentration of nitrate nitrogen decreased from (1.66±0.09) mg·L to (0.25±0.06) mg·L, whereas the concentration of ammonia nitrogen and nitrite showed little change in the early thermal stratification of Zhoucun reservoir. At the same time, chlorophyll was not significantly increased, so the algae had little effect on nitrogen; the decreasing nitrogen was mainly due to the aerobic denitrification. Gradually increased temperature,the changes of DO and pH and the composition of organic matter (low molecular weight) were beneficial to the growth of aerobic denitrifying bacteria. Furthermore, the number of bacteria increased from 1.06×10 cfu·L to 8.33×10 cfu·L, which enhanced the denitrification of the reservoir; Meanwhile, in the simulation experiments, the TN removal rates of water and water-sediment systems reached 0.7 mg and 3.3 mg, respectively. Water and sediment denitrification ratio was generally 1:4, and the aerobic denitrification of surface sediment was an important factor in the removal of nitrogen in reservoir.
为探究周村水库热分层前期氮素的变化趋势及驱动因素,于2016年2月至4月对周村水库主库区水质指标进行定期监测。同时,采集采样点的淡水和表层沉积物,在实验室通过模拟研究水和沉积物的反硝化作用。结果表明:周村水库热分层前期,总氮浓度从(2.28±0.09)mg·L降至(1.08±0.09)mg·L,硝态氮浓度从(1.66±0.09)mg·L降至(0.25±0.06)mg·L,而氨氮和亚硝酸盐浓度变化不大。同时,叶绿素未显著增加,藻类对氮素影响较小;氮素减少主要归因于好氧反硝化作用。温度逐渐升高、溶解氧和pH值的变化以及低分子量有机物的组成有利于好氧反硝化细菌的生长。此外,细菌数量从1.06×10 cfu·L增加到8.33×10 cfu·L,增强了水库的反硝化作用;同时,模拟实验中,水和水-沉积物系统的总氮去除率分别达到0.7mg和3.3mg。水和沉积物的反硝化比例一般为1:4,表层沉积物的好氧反硝化是水库氮素去除的重要因素。