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首页> 外文期刊>Ecological engineering: The Journal of Ecotechnology >Understanding gaseous nitrogen removal through direct measurement of dissolved N2 and N2O in a subtropical river-reservoir system
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Understanding gaseous nitrogen removal through direct measurement of dissolved N2 and N2O in a subtropical river-reservoir system

机译:通过直接测量亚热带河流水库系统中溶解的N2和N2O来了解气态氮的去除

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摘要

Dam construction within a river basin modifies hydrology and affects nitrogen (N) removal during transport to coast. In this study, direct measurements of dissolved N2 and N2O were carried out in a subtropical river reservoir (Xipi) in southeast China to understand the effectiveness of reservoirs in removal of fixed N by N gas fluxes. Results showed that larger excess N2 and N2O emissions were found in the riverine zone where effluents from the upper dam mix with the shallow river. Excess N2, mainly derived from denitrification, occurred in the sediment below deep water, while N2O was largely produced from nitrification in the water column, particularly in dry season. Seasonal variation of excess N2 was associated with temperature and DO level, while N2O production was controlled by DIN concentration. The gaseous N dynamics and distribution in the studied reservoir reflected an interactive effect of hydrology, geomor-phology and biogeochemistry. In the reservoir lacustrine zone, gaseous N removal accounted for 85% ol total retention and less than 1% of DIN loads. The negligible retention of N by the reservoir highlights the importance of appropriate watershed management practices to reduce N losses from terrestrial systems
机译:流域内的大坝建设改变了水文学,并影响了向海岸运输过程中氮(N)的去除。在这项研究中,在中国东南部的一个亚热带河流水库(Xipi)中对溶解的N2和N2O进行了直接测量,以了解水库对通过N气通量去除固定N的有效性。结果表明,在上游大坝的流出物与浅河相混合的河流地区发现了更多的过量N2和N2O排放。过量的N2主要来自反硝化作用,发生在深水下方的沉积物中,而N2O很大程度上是由水柱中的硝化作用产生的,特别是在旱季。 N2过量的季节变化与温度和DO水平有关,而N2O的产生则受DIN浓度控制。研究储层中气态氮的动态和分布反映了水文学,地貌学和生物地球化学的相互作用。在储层湖相带中,气态氮的去除占总滞留量的85%,不到DIN负荷的1%。水库对氮的保留量微不足道,这突出表明了采取适当的流域管理做法以减少陆地系统氮损失的重要性。

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