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三峡库区氮湿沉降特征、通量及其对水生态环境的贡献

Nitrogen wet deposition in the Three Gorges Reservoir area: Characteristics, fluxes, and contributions to the aquatic environment.

机构信息

Chongqing Key Laboratory of Water Environment Evolution and Pollution Control in Three Gorges Reservoir Area, Chongqing Three Gorges University, Wanzhou 404000, China; CAS Key Laboratory of Reservoir Environment, Chongqing Institute of Green and Intelligent Technology, Chinese Academy of Sciences, Chongqing 400714, China.

College of Environmental and Ecology, Chongqing University, Chongqing 400044, China.

出版信息

Sci Total Environ. 2020 Oct 10;738:140309. doi: 10.1016/j.scitotenv.2020.140309. Epub 2020 Jun 18.

Abstract

Measurements of nitrate nitrogen (NO-N), ammonia nitrogen (NH-N), and dissolved organic nitrogen (DON) in precipitation were conducted at six different sites in the hinterland of the Three Gorges Reservoir (TGR) area from January 2016 to December 2017. The characteristics and the sources of nitrogen (N) species were identified. N flux of wet deposition in the hinterland of the TGR area were 13.56 ± 2.95 kg N ha yr, of which the proportions of NO-N, NH-N and DON were 60.9%, 25.1% and 14.0%, respectively. N flux in urban area was significantly higher than those in suburban, agricultural, and wetland areas. Industrial activities, biomass burning, and secondary transformation were the main contributors of N in urban area. In agricultural area, biomass burning, crustal, and manure were main sources of N. In suburban area, mixed emissions from industry, agriculture, and crustal sources were primary contributors of N. For wetlands, the major contributions were from industrial sector and biomass burning. Additional, analysis of regional distribution of dissolved N deposition in the TGR area was conducted by combining current study data and previously published data between 2000 and 2017. N flux of wet deposition in the entire TGR area ranged from 12.17 to 51.93 kg N ha yr, with an average of 26.81 kg N ha yr. Regional N distribution was greatest in the tail region, followed by the head region, and then the hinterland in the TGR area. The amount of N entering the TGR directly through atmospheric wet deposition was 2906 t yr, accounting for 2.1% of the total N inputs. N load from wet deposition had exceeded the critical loads from that of the water, forest, and even some farmland ecosystems in the TGR area. Decreasing NH emissions from agricultural activities is the key to alleviate the regional N deposition.

摘要

对 2016 年 1 月至 2017 年 12 月三峡库区腹地 6 个不同地点的降水硝酸盐氮(NO-N)、氨氮(NH-N)和溶解有机氮(DON)进行了测量。确定了氮物种的特征和来源。三峡库区腹地湿沉降氮通量为 13.56±2.95kgNha yr,其中 NO-N、NH-N 和 DON 的比例分别为 60.9%、25.1%和 14.0%。城区氮通量明显高于郊区、农业区和湿地。工业活动、生物质燃烧和二次转化是城区氮的主要贡献者。在农业区,生物质燃烧、地壳和粪肥是氮的主要来源。在郊区,工业、农业和地壳源的混合排放是氮的主要贡献者。对于湿地,主要贡献来自工业部门和生物质燃烧。此外,通过结合当前研究数据和 2000 年至 2017 年以前发表的数据,对三峡库区区域溶解氮沉积分布进行了分析。整个三峡库区湿沉降氮通量范围为 12.17-51.93kgNha yr,平均值为 26.81kgNha yr。三峡库区区域氮分布以尾部最大,其次是头部,然后是腹地。大气湿沉降直接进入三峡水库的氮量为 2906t yr,占总氮输入量的 2.1%。来自湿沉降的氮负荷已经超过了水、森林甚至一些农田生态系统的临界负荷。减少农业活动中的氨排放是缓解区域氮沉积的关键。

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