Agriculture driven nitrogen wet deposition in a karst catchment in southwest China

喀斯特 中国 氮气 沉积(地质) 环境科学 农业 水文学(农业) 流域 水资源管理 地理 构造盆地 地质学 地貌学 考古 岩土工程 化学 有机化学 地图学
作者
Jie Zeng,Si-Liang Li,Zhong-Jun Wang,Cai-Qing Qin,Qixin Wu,Sheng Xu
出处
期刊:Agriculture, Ecosystems & Environment [Elsevier BV]
卷期号:294: 106883-106883 被引量:27
标识
DOI:10.1016/j.agee.2020.106883
摘要

Abstract Nitrogen (N) deposition plays a key role in ecosystem function as one of the major N sources for natural vegetation, particularly in karst agricultural areas with thin soil cover, which drive the karst N fate via rainwater. To understand the seasonal and spatial variation in nitrogen deposition and to identify the major sources of nitrate in wet deposition in a karst agricultural area (Houzhai Catchment) in southwestern China, two sites with different land use were selected to assess wet and dry deposition for one year. Houzhai village (HZV) is an area highly influenced by agriculture, whereas Muzhu reservoir (MZR) is a more pristine environment with less anthropogenic influence. Nitrogenous species and dual nitrate isotopes were analyzed. The results showed that agriculture-derived NH4+ was the major contributor of annual total wet N deposition (>55 %). The contribution of NH4+ to wet N deposition was 1.63 times higher than that of NO3− and dissolved organic nitrogen (DON). The annual nitrogen deposition in this study was approximately twice as much as the average wet N deposition over China, while lower dry N deposition relative to other Chinese monitoring sites was observed. The δ15N-NO3− showed a seasonal trend of negative summer values and positive winter values, which were primarily controlled by the variations in NOx emission sources. Seasonal variation in δ18O-NO3− was mainly controlled by NOx oxidation pathways and showed a similar trend to δ15N-NO3−. The contributions from four endmembers (coal combustion, vehicle exhaust, biomass burning, and soil emission) were calculated using a stable isotope mixing model. Contributions show a clear seasonal variation (except vehicle exhaust), with the four sources accounting for 20.0 %, 25.6 %, 22.9 % and 31.5 % respectively (annual mean probability estimate, AMPE) at HZV, and 19.0 %, 27.8 %, 23.2 % and 30.0 % (AMPE) at MZR. Isotopic evidence determined agricultural soil emission is a major contributor to rainwater during the summer growing season, which can significantly impact the agricultural ecosystems.
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