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Meta-analyses of the effects of major global change drivers on soil respiration across China

机译:对全球主要变化驱动因素对中国土壤呼吸的影响的荟萃分析

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摘要

Soil respiration (Rs) is affected largely by major global change drivers, global meta-analysis studies have synthesized the available information to determine how Rs responds to these drivers. However, little is known about the effects of these drivers on Rs across China. Here, we conducted a meta-analysis to synthesize 80 studies published in the literature with 301 paired comparisons to quantify the responses of Rs to simulated warming, nitrogen addition, precipitation increase and acid rain across Chinese terrestrial ecosystem. Results showed that global change drivers significantly changed Rs across Chinese ecosystems. Warming, nitrogen addition, and precipitation increase significantly increased Rs by 9.08%, 5.21%, 31.68%, respectively, while simulated acid rain decreased Rs by 7.06%. The responses of Rs to warming, nitrogen addition, and precipitation increase are similar in both direction and magnitude to those reported in global syntheses, except for higher response ratio under precipitation increase in China. In addition, the responses of Rs were different among ecosystem types, and among experimental treatments. Warming significantly increased Rs in croplands but did not change in forests and grasslands. The effect magnitude of N addition on Rs in grasslands and croplands was much higher than those in other ecosystems. In general, precipitation increase stimulated Rs in different ecosystems, and its effect magnitudes increased with changed precipitation levels. However, acid rain inhibited Rs in different biomes and intensities of acid rain. Our findings contribute to better understanding of how Rs will change under global change, and provide important parameters for carbon cycle model at the regional scale. (C) 2016 Elsevier Ltd. All rights reserved.
机译:土壤呼吸(Rs)在很大程度上受主要的全球变化驱动因素影响,全球荟萃分析研究综合了可用信息,以确定Rs如何响应这些驱动因素。但是,对于这些驱动因素对中国全国Rs的影响知之甚少。在这里,我们进行了荟萃分析,综合了文献中发表的80项研究和301个配对比较,以量化Rs对整个中国陆地生态系统模拟的变暖,氮添加,降水增加和酸雨的响应。结果表明,全球变化驱动力极大地改变了中国生态系统中的自然资源。增温,氮添加和降水增加分别使Rs分别增加9.08%,5.21%和31.68%,而模拟酸雨使Rs减少7.06%。 Rs对变暖,氮添加和降水增加的响应在方向和大小上都与全球综合报告中的相似,只是中国降水增加下的响应率更高。此外,Rs的响应在生态系统类型之间和实验处理之间也不同。变暖大大增加了耕地的Rs,但在森林和草地上没有改变。氮和氮在草地和农田中对Rs的影响程度远高于其他生态系统。一般而言,降水增加刺激了不同生态系统中的Rs,其影响幅度随降水水平的变化而增加。然而,酸雨抑制了不同生物群落和酸雨强度中的Rs。我们的发现有助于更好地理解Rs在全球变化下将如何变化,并为区域规模的碳循环模型提供重要参数。 (C)2016 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Atmospheric environment》 |2017年第2期|181-186|共6页
  • 作者单位

    Chinese Acad Sci, Qianyanzhou Ecol Res Stn, Key Lab Ecosyst Network Observat & Modeling, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China|Renmin Univ China, Sch Environm & Nat Resources, Beijing 100872, Peoples R China;

    Chinese Acad Sci, Qianyanzhou Ecol Res Stn, Key Lab Ecosyst Network Observat & Modeling, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China;

    Renmin Univ China, Sch Environm & Nat Resources, Beijing 100872, Peoples R China;

    Renmin Univ China, Sch Environm & Nat Resources, Beijing 100872, Peoples R China;

    Renmin Univ China, Sch Environm & Nat Resources, Beijing 100872, Peoples R China;

    Chinese Acad Sci, Qianyanzhou Ecol Res Stn, Key Lab Ecosyst Network Observat & Modeling, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China|Renmin Univ China, Sch Environm & Nat Resources, Beijing 100872, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Soil respiration; Warming; Nitrogen addition; Precipitation increase; Simulated acid rain; Meta-analysis;

    机译:土壤呼吸温热氮添加降水增加模拟酸雨元分析;

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