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首页> 外文期刊>Global change biology >Winter climate change effects on soil C and N cycles in urban grasslands.
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Winter climate change effects on soil C and N cycles in urban grasslands.

机译:冬季气候变化对城市草原土壤碳氮循环的影响。

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Despite growing recognition of the role that cities have in global biogeochemical cycles, urban systems are among the least understood of all ecosystems. Urban grasslands are expanding rapidly along with urbanization, which is expected to increase at unprecedented rates in upcoming decades. The large and increasing area of urban grasslands and their impact on water and air quality justify the need for a better understanding of their biogeochemical cycles. There is also great uncertainty about the effect that climate change, especially changes in winter snow cover, will have on nutrient cycles in urban grasslands. We aimed to evaluate how reduced snow accumulation directly affects winter soil frost dynamics, and indirectly greenhouse gas fluxes and the processing of carbon (C) and nitrogen (N) during the subsequent growing season in northern urban grasslands. Both artificial and natural snow reduction increased winter soil frost, affecting winter microbial C and N processing, accelerating C and N cycles and increasing soil : atmosphere greenhouse gas exchange during the subsequent growing season. With lower snow accumulations that are predicted with climate change, we found decreases in N retention in these ecosystems, and increases in N2O and CO2 flux to the atmosphere, significantly increasing the global warming potential of urban grasslands. Our results suggest that the environmental impacts of these rapidly expanding ecosystems are likely to increase as climate change brings milder winters and more extensive soil frost.
机译:尽管人们日益认识到城市在全球生物地球化学循环中的作用,但城市系统是所有生态系统中最少了解的系统之一。随着城市化的发展,城市草原正在迅速扩张,预计在未来几十年中,草原将以前所未有的速度增长。城市草原面积越来越大,及其对水和空气质量的影响,证明有必要更好地了解其生物地球化学循环。气候变化,特别是冬季积雪的变化,对城市草地养分循环的影响也存在很大的不确定性。我们旨在评估减少的积雪如何直接影响冬季土壤霜动态,并间接影响随后的北部城市草原生长季期间的温室气体通量以及碳(C)和氮(N)的处理。人工降雪和自然降雪都增加了冬季土壤的霜冻,影响了冬季微生物的碳和氮加工,加速了碳和氮循环,并在随后的生长季节增加了土壤:大气温室气体交换。根据气候变化预测的较低积雪量,我们发现这些生态系统中的N保留量降低,并且N 2 O和CO 2 通向大气的通量显着增加增加城市草原的全球变暖潜力。我们的结果表明,随着气候变化带来更温和的冬季和更广泛的土壤霜冻,这些迅速扩展的生态系统对环境的影响可能会增加。

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