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首页> 外文期刊>Biogeochemistry >The influence of climate on average nitrogen export from large watersheds in the Northeastern United States.
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The influence of climate on average nitrogen export from large watersheds in the Northeastern United States.

机译:气候对美国东北大流域平均氮出口的影响。

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摘要

The flux of nitrogen in large rivers in North America and Europe is well explained as a function of the net anthropogenic inputs of nitrogen to the landscape, with on average 20 to 25% of these inputs exported in rivers and 75 to 80% of the nitrogen retained or denitrified in the landscape. Here, we use data for average riverine nitrogen fluxes and anthropogenic inputs of nitrogen over a 6-year period (1988-1993) for 16 major watersheds in the northeastern United States to examine if there is also a climatic influence on nitrogen fluxes in rivers. Previous studies have shown that for any given river, nitrogen fluxes are greater in years with higher discharge, but this can be interpreted as storage of nitrogen in the landscape during dry years and flushing of this stored nitrogen during wet years. Our analyses demonstrate that there is also a longer-term steady-state influence of climate on riverine nitrogen fluxes. Those watersheds that have higher precipitation and higher discharge export a greater fraction of the net anthropogenic inputs of nitrogen. This fractional export ranges from 10 to 15% of the nitrogen inputs in drier watersheds in the northeastern United States to over 35% in the wetter watersheds. We believe this is driven by lower rates of denitrification in the wetter watersheds, perhaps because shorter water residence times do not allow for as much denitrification in riparian wetlands and low-order streams. Using mean projections for the consequences of future climate change on precipitation and discharge, we estimate that nitrogen fluxes in the Susquehanna River to Chesapeake Bay may increase by 3 to 17% by 2030 and by 16 to 65% by 2095 due to greater fractional delivery of net anthropogenic nitrogen inputs as precipitation and discharge increase. Although these projections are highly uncertain, they suggest a need to better consider the influence of climate on riverine nitrogen fluxes as part of management efforts to control coastal nitrogen pollution..
机译:很好地解释了北美和欧洲大河中的氮通量与人为景观净输入的氮的函数关系,这些输入中平均有20%至25%出口到河流中,而氮的75%至80%在景观中保留或反硝化。在这里,我们使用美国东北部16个主要流域的6年时间段(1988-1993年)中平均河流氮通量和人为氮输入的数据,来检查气候是否对河流中的氮通量也有影响。以前的研究表明,对于任何给定的河流,氮流量在年份中随着排放量的增加而更大,但这可以解释为干旱年份景观中的氮存储,而潮湿年份中氮的冲洗。我们的分析表明,气候对河流氮通量也有长期的稳态影响。那些具有较高降水量和较高排放量的流域出口的人为净氮净输入量所占比例较大。在美国东北较干燥的流域,该部分出口量占氮输入量的10%到15%,在较湿润的流域中占35%以上。我们认为,这是由于湿润的流域反硝化率降低所致,这也许是因为较短的水停留时间无法在河岸湿地和低阶河流中进行同样多的反硝化作用。使用对未来气候变化对降水和排放的影响的平均预测,我们估计到2030年萨斯奎哈那河至切萨皮克湾的氮通量可能会增加3%至17%,到2095年可能增加16%至65%,这是因为随着降水和排放量的增加,人为氮的净输入量增加。尽管这些预测是高度不确定的,但它们表明有必要更好地考虑气候对河流氮通量的影响,作为控制沿海氮污染的管理工作的一部分。

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