Suppr超能文献

[汉江上游金水河流域大气氮湿沉降]

[Wet deposition of atmospheric nitrogen of the Jinshui watershed in the upper Hanjiang River].

作者信息

Wang Jin-Jie, Zhang Ke-Rong, Wu Chuan, Zhang Quan-Fa

出版信息

Huan Jing Ke Xue. 2014 Jan;35(1):66-72.

Abstract

The Jinshui River, a tributary of the Hanjiang River, is an important region of water conservation for the Middle Route of South to North Water Transfer Project. However, water quality has been deteriorated in recent years, in particular nitrogen increasing pollution. In this study, the wet deposition of atmospheric nitrogen in the Jinshui watershed was investigated between Feb. 2012-Feb. 2013, and the corresponding contribution to the river N loading was calculated using N retention model. The results indicated that the volume-weighted concentration of dissolved total nitrogen (DTN) was 0.24-2.89 mg x L(-1), consisting of ammonium (NH(4+)-N) (42.8%), nitrate (NO3- N) (13.3%) and dissolved organic nitrogen (DON) (43.9%), which decreased with rainfall volume as a result of dilution. The wet deposition of atmospheric N was mainly from anthropogenic pollution and the flux was between 4.97-7.00 kg x (hm2 x a)(-1), dominated by seasonal rainfall, of which about 81% occurred in spring and summer and the flux in a decreasing order of upstream, downstream, and middlestream. The wet deposition contributed approximately 34,000-46,000 kg N to the river, accounting for only 5.05%-6.78% of the contribution by fertilizers, which was too small to be the main source of the river N loading.

摘要

金水河是汉江的一条支流,是南水北调中线工程的重要水源涵养区。然而,近年来水质有所恶化,尤其是氮污染加剧。本研究于2012年2月至2013年2月对金水河流域大气氮的湿沉降进行了调查,并利用氮滞留模型计算了其对河流氮负荷的相应贡献。结果表明,溶解态总氮(DTN)的体积加权浓度为0.24 - 2.89 mg·L(-1),由铵态氮(NH(4+)-N)(42.8%)、硝态氮(NO3-N)(13.3%)和溶解有机氮(DON)(43.9%)组成,因稀释作用随降雨量减少。大气氮的湿沉降主要来自人为污染,通量在4.97 - 7.00 kg·(hm2·a)(-1)之间,受季节性降雨主导,其中约81%发生在春季和夏季,通量大小顺序为上游、下游、中游递减。湿沉降对河流的氮贡献约为34000 - 46000 kg,仅占肥料贡献量的5.05% - 6.78%,太小不足以成为河流氮负荷的主要来源。

文献AI研究员

20分钟写一篇综述,助力文献阅读效率提升50倍。

立即体验

用中文搜PubMed

大模型驱动的PubMed中文搜索引擎

马上搜索

文档翻译

学术文献翻译模型,支持多种主流文档格式。

立即体验