中国农业气象 ›› 2024, Vol. 45 ›› Issue (01): 1-11.doi: 10.3969/j.issn.1000-6362.2024.01.001

• 农业生态环境栏目 •    下一篇

全球气候变化下土壤呼吸对温度和水分变化的响应特征综述

冉漫雪,丁军军,孙东宝,顾峰雪   

  1. 中国农业科学院农业环境与可持续发展研究所/农业农村部旱地节水农业重点实验室,北京 100081
  • 收稿日期:2023-03-17 出版日期:2024-01-20 发布日期:2024-01-15
  • 作者简介:冉漫雪,E-mail:2329697098@qq.com
  • 基金资助:
    国家重点研发计划课题“晋东黄土丘陵区适水改土与种养结合协同技术集成及示范”(2021YFD1900705)

A Review of the Response Characteristics of Soil Respiration to Temperature and Moisture Changes under Global Climate Change

RAN Man-xue, DING Jun-jun, SUN Dong-bao, GU Feng-xue   

  1. Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences/Key Laboratory of Dryland Water-saving Agriculture, Ministry of Agriculture and Rural Affairs, Beijing 100081, China
  • Received:2023-03-17 Online:2024-01-20 Published:2024-01-15

摘要: 气候变暖、降水格局变化等是气候变化的主要表现形式,也是影响土壤呼吸主要的非生物因素,探明气象条件(温度、水分)对土壤呼吸影响及作用机制是理解陆地生态系统碳循环的重要内容之一。本文对近年来国内外学者关于温度和水分对土壤呼吸的影响及机制的研究进展进行综述。结果表明,(1)气候变暖与土壤呼吸存在正反馈调节,但温度适应性削弱了二者的反馈关系。增温时长和土壤碳储量不同导致温度对土壤呼吸的影响具有时空差异。土壤呼吸对温度适应性机制主要包括土壤微生物适应性、底物消耗和土壤矿物质活化等。(2)降水对土壤呼吸的作用取决于土壤初始水分含量。当土壤含水量低于萎蔫系数时,降水不仅增加土壤含水量还可促进土壤呼吸,在土壤含水量接近田间持水量时土壤呼吸达到最大值,当土壤含水量达到饱和值时土壤呼吸又会受到抑制。水分对土壤呼吸影响机制主要为替代效应与阻滞效应、底物供给、微生物胁迫以及根系响应等。(3)土壤呼吸与土壤温度、水分的耦合关系取决于土壤水热因子配比,当土壤温度成为胁迫因子时,降水引发的土壤水分含量升高对土壤呼吸的激发效应被低温的负面影响所抑制;当土壤水分成为胁迫因子时,气候变暖引发的土壤温度升高对土壤呼吸的促进作用被干旱的负面影响所抵消,进行土壤呼吸研究时需充分考虑土壤温度和水分的交互作用。为更全面深入地明晰陆地生态系统土壤碳排放扰动因素,未来气候变化下土壤呼吸与环境关系等相关领域研究应为重点方向,一是加强多因素交互作用对土壤呼吸影响的研究,并定量化研究土壤呼吸组分;二是持续关注土壤呼吸对土壤初始温度和温度波动的响应特征,探索生物多样性或群落结构组成对土壤呼吸的影响。

关键词: 土壤呼吸, 温度, 降水, 响应特征

Abstract: Warming of the climate and changes in precipitation patterns are major manifestations of climate change and abiotic factors affecting soil respiration. Authors presents a systematic analysis of recent research advances on the effects and mechanisms of temperature and moisture on soil respiration. The results show that:(1)there is positive feedback between soil respiration and climate warming, but the temperature adaptation weakens this positive feedback. The effect of temperature on soil respiration varies spatially and temporally due to the different duration of warming and soil carbon storage. The main mechanisms of soil respiration adaptation to temperature include soil microbial adaptation, substrate depletion and soil mineral activation.(2)The effect of precipitation on soil respiration depends on the initial soil water content. When soil water content is lower than the wilting factor, precipitation not only increases soil water content but also promotes soil respiration, reaching a maximum when soil water content is close to the field holding capacity, while soil respiration is inhibited when soil water content reaches saturation value. The main mechanisms by which water affects soil respiration are substitution and blocking effects, substrate supply, microbial stress and root response. (3)The coupling of soil respiration with soil temperature and moisture depends on the ratio of soil water and heat factors. When soil temperature becomes a stress factor, the stimulating effect of increasing soil water content induced by precipitation on soil respiration is suppressed by the negative effect of low temperature. When soil moisture becomes a stress factor, the promoting effect of increased soil temperature due to climate warming on soil respiration is counteracted by the negative impact of drought. The interaction between soil temperature and moisture should be fully considered when studying soil respiration. In order to understand the disturbance factors of soil carbon emissions in terrestrial ecosystems, this paper proposes that future research on the relationship between soil respiration and the environment under climate change. Firstly, strengthen the research on the effects of multi-factor interaction on soil respiration and quantify the soil respiration components. Secondly, continue to pay attention to the characteristics of soil respiration in response to initial soil temperature and temperature fluctuations, and to explore the effects of biodiversity or community structure composition on soil respiration.

Key words: Soil respiration, Temperature, Rainfall, Response characteristics