Miao Ying, Zhang Cheng, Xiao Qiong, Zhao Hai-Juan, Li Cheng-Xi
Key Laboratory of Karst Dynamics, Ministry of Land and Resources & Guangxi, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China.
Chongqing Key Laboratory of Karst Environment, School of Geographical Science, Southwest University, Chongqing 400715, China.
Huan Jing Ke Xue. 2018 Apr 8;39(4):1589-1597. doi: 10.13227/j.hjkx.201708140.
Dynamic variations and sources of nitrate during dry season in the Lijiang River were analyzed using the nitrate concentrations and N and O isotope techniques, from the samples obtained from 13 sections in the Lijiang River from September 28, 2016 to December 28, 2016. Results show that the nitrate concentrations range from 0.46 to 18.48 mg·L, with an average of 6.18 mg·L, and that the nitrate levels are low during the dry season. Nitrate concentrations in the Lijiang River increase slowly from September to December, mainly being influenced by rainfall, runoff, and human activity. Nitrate concentrations in the Lijiang River from upstream to downstream show a trend of "increase-decrease-increase." Nitrate in the Lijiang River during the dry season mainly originates from organic nitrogen in soil, human and animal feces, sewage (largely living sewage), human and animal waste, and tourism. In order to better protect the water quality of the Lijiang River, the urban sewage pipe network must be expanded, in addition to building small sewage treatment facilities and strengthening tourism management and environmental awareness.
利用2016年9月28日至2016年12月28日期间从漓江13个断面采集的样品中的硝酸盐浓度以及氮、氧同位素技术,分析了漓江枯水期硝酸盐的动态变化及来源。结果表明,硝酸盐浓度范围为0.46至18.48mg·L,平均为6.18mg·L,枯水期硝酸盐水平较低。漓江硝酸盐浓度从9月至12月缓慢上升,主要受降雨、径流和人类活动影响。漓江硝酸盐浓度从上游到下游呈“升高-降低-升高”趋势。漓江枯水期硝酸盐主要来源于土壤中的有机氮、人畜粪便、污水(主要是生活污水)、人畜废弃物及旅游业。为更好地保护漓江水质,除建设小型污水处理设施、加强旅游管理和环境意识外,还必须扩大城市污水管网。