基于Meta分析的土壤呼吸对降水改变的非对称响应
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海南大学科研启动基金项目(RZ2200001133);国家自然科学青年基金(4220070870);海南省自然科学青年基金(422QN264)


Asymmetric response of soil respiration to precipitation change based on meta-analysis
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Evolution Characteristics and Regulation Mechanism of Soil Water Conservation Function in Hainan Tropical Rainforest Restoration Process

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    摘要:

    气候变暖已经引起全球降水格局改变。土壤呼吸作为陆地生态系统向大气释放CO2最大的碳库,对降水变化的响应将进一步影响碳循环,从而对全球气候变化产生反馈。尽管以往已有大量关于土壤呼吸与降水变化关系的相关研究,但存在较大争议。因此,亟待进一步深入探究土壤呼吸对降水改变的响应。基于此,研究Meta分析方法,整合了来自Web of Science 英文数据库和中国知网文献数据库(CNKI)的284篇已发表的论文和367组数据,进而分析全球中低纬度地区土壤呼吸对降水改变的响应。研究结果表明,土壤呼吸对降水改变的响应呈现出非对称特征,降水量增加能够提高16.7%的土壤呼吸,而降水量减少则会抑制17.88%的土壤呼吸。研究还发现,不同生态系统和气候区域的土壤呼吸对降水改变的响应存在较大差别。其中,降水量增加能够提高草地生态系统22%的土壤呼吸,比森林生态系统土壤呼吸高出12%;而降水量减少则会削弱草地生态系统28%的土壤呼吸,这要比森林生态系统土壤呼吸还高16%。与湿润地区相比,降水量的增加对干旱地区土壤呼吸的促进作用更加明显。而降水量的减少对干旱地区和湿润地区土壤呼吸的影响均无显著差异。此外,本研究也证实了土壤呼吸对不同降水强度和年限的响应也存在差异。在不同降水强度上,无论增加降水还是减少降水,重度增减雨的土壤呼吸均改变最大,即:重度增减雨(>75%)>中度增减雨(25% -75%) >轻度增减雨(<25%);在不同降水年限上,长期增雨对土壤呼吸的促进作用尤为突出,但长期减雨对土壤呼吸影响无显著差异。研究结果可为未来气候情景下陆地生态系统土壤呼吸变化的准确预测以及模型模拟和改进提供重要的科学依据和理论基础。

    Abstract:

    Warming has already caused changes in global precipitation patterns. Soil respiration, as the largest carbon reservoir of CO2 released by terrestrial ecosystems to the atmosphere, will further affect the carbon cycle in response to precipitation changes, thus producing feedback to global climate change. Although there were a lot of studies on the relationship between soil respiration and precipitation change in the past, there are a lot of controversies. Therefore, it is urgent to further explore the response of soil respiration to precipitation change. Here, the meta-analysis method was used to integrate 284 published papers and 367 sets of data from the English database of Web of Science and the China National Knowledge Network Literature Database (CNKI) to analyze the response of soil respiration to precipitation change in middle and low latitudes around the world. The results showed that the response of soil respiration to precipitation change presented asymmetric characteristics,the increase of precipitation increased the soil respiration by 16.7%, while the decrease of precipitation inhibited the soil respiration by 17.88%. The study also found that the responses of soil respiration to precipitation change in different ecosystems and climate zones were quite different. Among them, the increase of precipitation could improve the soil respiration of grassland ecosystem by 22%, which was 12% higher than that of forest ecosystem. While the decrease of precipitation will weaken the soil respiration of grassland ecosystem by 28%, which was 16% higher than that of forest ecosystem. Compared with humid areas, the increased of precipitation had a greater effect on soil respiration in arid areas. But the decrease of precipitation had no significant difference on soil respiration in arid and humid areas. In addition, this study also indicated that there were differences in the response of soil respiration to different precipitation intensities and years. In different precipitation intensities,regardless of increased precipitation or decreased precipitation, the soil respiration of heavy increased precipitation and decreased precipitation changed the most. that is, heavy increased precipitation and decreased precipitation (>75%), moderate increased precipitation and decreased precipitation (25%-75%), and slight rainfall decreased and increased (<25%); In different precipitation years, the long-term increased precipitation had the most prominent effect on soil respiration, while long-term decreased precipitation had no significant difference on soil respiration. The results can provide importantly scientific basis and theoretical basis for accurate prediction of soil respiration change of terrestrial ecosystem and improvement of model simulation under future climate scenarios.

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赵智慧,陈俏艳,程思源,戴黎聪.基于Meta分析的土壤呼吸对降水改变的非对称响应.生态学报,2024,44(7):2886~2897

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