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Response of soil CO2 efflux to precipitation manipulation in a semiarid grassland

机译:半干旱草原土壤CO2流出对降水处理的响应

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摘要

Soil CO2 efflux (SCE) is an important component of ecosystem CO2 exchange and is largely temperature and moisture dependent, providing feedback between C cycling and the climate system. We used a precipitation manipulation experiment to examine the effects of precipitation treatment on SCE and its dependences on soil temperature and moisture in a semiarid grassland. Precipitation manipulation included ambient precipitation, decreased precipitation (-43%), or increased precipitation (+17%). The SCE was measured from July 2013 to December 2014, and CO2 emission during the experimental period was assessed. The response curves of SCE to soil temperature and moisture were analyzed to determine whether the dependence of SCE on soil temperature or moisture varied with precipitation manipulation. The SCE significantly varied seasonally but was not affected by precipitation treatments regardless of season. Increasing precipitation resulted in an upward shift of SCE-temperature response curves and rightward shift of SCE-moisture response curves, while decreasing precipitation resulted in opposite shifts of such response curves. These shifts in the SCE response curves suggested that increasing precipitation strengthened the dependence of SCE on temperature or moisture, and decreasing precipitation weakened such dependences. Such shifts affected the predictions in soil CO2 emissions for different precipitation treatments. When considering such shifts, decreasing or increasing precipitation resulted in 43 or 75% less change, respectively, in CO2 emission compared with changes in emissions predicted without considering such shifts. Furthermore, the effects of shifts in SCE response curves on CO2 emission prediction were greater during the growing than the non-growing season. (C) 2016 The Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences. Published by Elsevier B.V.
机译:土壤CO 2外排(SCE)是生态系统CO 2交换的重要组成部分,在很大程度上取决于温度和湿度,从而提供碳循环和气候系统之间的反馈。我们使用了一个降水处理实验,以检验降水处理对半干旱草地上SCE的影响及其对土壤温度和湿度的依赖性。降水操作包括环境降水,降水减少(-43%)或降水增加(+ 17%)。从2013年7月至2014年12月测量了SCE,并评估了实验期间的CO2排放量。分析了SCE对土壤温度和水分的响应曲线,以确定SCE对土壤温度或水分的依赖性是否随降水的变化而变化。 SCE季节变化显着,但不受季节影响的降水处理。降水增加导致SCE温度响应曲线向上移动,而SCE湿度响应曲线向右移动,而降水减少导致此类响应曲线相反。 SCE响应曲线中的这些变化表明,降水增加会增强SCE对温度或湿度的依赖性,而降水减少会减弱这种依赖性。这种变化影响了不同降水处理对土壤CO2排放的预测。当考虑这种变化时,与不考虑这种变化的情况下预测的排放变化相比,降水量的减少或增加分别导致二氧化碳排放量减少了43%或75%。此外,在生长期间,SCE响应曲线的变化对CO2排放预测的影响要大于非生长季节。 (C)2016中国科学院生态环境研究中心。由Elsevier B.V.发布

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