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首页> 外文期刊>The Science of the Total Environment >An approach to identify the spatiotemporal patterns of nitrogen flows in food production and consumption systems within watersheds
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An approach to identify the spatiotemporal patterns of nitrogen flows in food production and consumption systems within watersheds

机译:确定流域内粮食生产和消费系统中氮流的时空分布的方法

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Human has greatly disturbed nitrogen (N) cycles through the food production and consumption (FPC) activities, which caused serious environmental consequences. A few studies address the pathways of N cycles to clarify the interrelationships between human activities and the altered N cycles, especially in terms of the spatial aspects of N flows, which are also influenced by natural factors. Here, we developed an integrated model to quantify the spatiotemporal patterns of N flows within the FPC and applied it to the Chaohu Watershed from 1949 to 2012. We found that total N inputs into the FPC increased by 6-fold during 1949–2012, while N inputs from chemical fertilizer had the largest increase, with an annual growth rate of 8.6%. N generation in manure doubled, but the recycling rate decreased by 50% in the study period. The total N losses increased from 17 to 130Gg-N/yr between 1949 and 2012. Annually, ~7% of total N losses was discharged into surface water annually, which peaked at 9.5Gg-N/yr during 1998–2003, two times as that in the early 1980s when algae blooms first occurred in Chaohu lake. Spatially, around one-fifth of the catchment area was responsible for all of N losses to surface water. These intensive areas located in the eastern and southern-central regions, which were identified as the critical areas for priority N mitigation. This study provided a method to depict spatiotemporal patterns of regional N flows for identifying the critical sources and areas of N pollution for precision watershed management.
机译:人类通过食品生产和消费(FPC)活动极大地干扰了氮(N)循环,从而造成了严重的环境后果。一些研究探讨了N循环的途径,以阐明人类活动与改变的N循环之间的相互关系,尤其是在N流动的空间方面,这也受自然因素的影响。在这里,我们开发了一个集成模型来量化FPC中N流量的时空模式,并将其应用于1949年至2012年的巢湖流域。我们发现1949-2012年期间,FPC中的总N输入量增加了6倍,而化肥氮投入增幅最大,年均增长8.6%。肥料中的氮生成量增加了一倍,但在研究期间,其回收率降低了50%。 1949年至2012年间,氮的总损失量从17 Gg-N / yr增加到了130Gg-N / yr。每年,每年约有7%的N损失被排放到地表水中,在1998-2003年期间,峰值为9.5Gg-N / yr,两次。就像1980年代初期藻类开花首次在巢湖中发生那样。在空间上,约有五分之一的集水区造成了地表水氮的全部损失。这些密集地区位于东部和南部中部地区,被确定为优先缓解N的关键地区。这项研究提供了一种描述区域氮流的时空分布的方法,以识别氮源污染的关键来源和区域,从而进行精确的流域管理。

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