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Volume 38 Issue 9
Nov.  2020
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ZHU Tao, WANG Run-ze, WANG Zong-zhou, ZHANG Dan, YANG Sheng-ke, ZHOU Min, WANG Ya-qiong. BEHAVIORAL CHARACTERISTICS OF NITROGEN IN THE ZAOHE AND WEIHE RIVER INTERSECTION[J]. ENVIRONMENTAL ENGINEERING , 2020, 38(9): 6-13,22. doi: 10.13205/j.hjgc.202009002
Citation: ZHU Tao, WANG Run-ze, WANG Zong-zhou, ZHANG Dan, YANG Sheng-ke, ZHOU Min, WANG Ya-qiong. BEHAVIORAL CHARACTERISTICS OF NITROGEN IN THE ZAOHE AND WEIHE RIVER INTERSECTION[J]. ENVIRONMENTAL ENGINEERING , 2020, 38(9): 6-13,22. doi: 10.13205/j.hjgc.202009002

BEHAVIORAL CHARACTERISTICS OF NITROGEN IN THE ZAOHE AND WEIHE RIVER INTERSECTION

doi: 10.13205/j.hjgc.202009002
  • Received Date: 2019-07-28
  • Focusing on the spatial distribution characteristics and pollution of nitrogen in the interaction zone of rivers under specific geological and geomorphological control, it is helpful to fully understand the characteristics of river water environment and the causes of pollution. In this paper, the intersection of Zaohe River and Weihe River was taken as the research area, and sampling points were set along the river direction, vertical and horizontal, respectively. The variation characteristics of the distribution of nitrogen in surface water, groundwater and sediments in the interaction zone and their biogeochemistry properties were studied. The results showed that:1) along the river, the concentration of NO3--N in the Zaohe River was lower than that in the Weihe River. The concentration of NO3--N increases after the intersection of the two rivers, while the concentration in the groundwater gradually decreased. Both NO2--N and NH4+-N in surface water and groundwater had a tendency to gradually decrease in river flow direction. In the transverse section, the NO3--N distribution was obviously affected by the groundwater recharge mode of the river. 2) By the space, NO3--N increased with depth, showing a distribution law of increasing first and then decreasing. The NH4+-N began to decrease with depth and then increased. 3) The pH of water was significantly positively correlated with NO3--N, and DO was significantly negatively correlated with NH4+-N. TOC in the sediment showed a significant negative correlation with NO2--N. There was a very significant positive correlation between NO2--N and NH4+-N between the nitrogen.
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