首页|增温和降水改变对土壤CO2释放影响研究进展

增温和降水改变对土壤CO2释放影响研究进展

扫码查看
全球变暖正在扩大严重干旱和强降雨事件发生的频率、范围、持续时间和严重程度.高温、干旱、强降水等极端气候事件显著改变了土壤有机碳矿化和无机碳释放的速率和强度.土壤CO2输出释放作为陆地生态系统碳循环的重要组成部分,对气候变化高度敏感,探究土壤CO2释放与气候变化的关系与响应机制,可为深入理解全球变暖背景下土壤碳循环和源汇机制提供理论支撑.系统分析了前人在全球变暖引起增温和降水改变对土壤呼吸(soil respiration,Rs)、碳酸盐矿物溶蚀影响的研究成果与结论,从Rs和碳酸盐矿物溶蚀两个方面解析增温和降水改变对土壤CO2 释放的影响.未来应加强气候变化与土壤性质、营养物质含量和有效性、微生物生物量和活性等其他多种因子耦合作用对Rs影响的研究,构建极端气候条件下多变量因子耦合的Rs速率模型.深入探究碳酸盐岩基岩土壤区Rs、碳酸盐矿物溶蚀对极端强降水事件的响应阈值,并精准量化极端强降水下两者间碳迁移转化通量.
A Review of Influence of Warming and Precipitation Changes on Soil CO2 Release
Global warming is expanding the frequency,scope,duration,and severity of severe drought and heavy rainfall events.Extreme climate events such as high temperatures,droughts,and heavy rainfall have significantly changed the rate and intensity of soil organic carbon mineralization and inorganic carbon release.The release of soil CO2,as an important component of the carbon cycle in terrestrial ecosystems,is highly sensitive to climate change.Exploring the relationship and response mechanism between soil CO2 release and climate change can provide theoretical support for in-depth understanding of soil carbon cycling and source sink mechanisms in the context of global warming.In this paper systematically it analyzes the previous studies on the effects of warming and precipitation changes on soil respiration(Rs)and soil carbonate mineral dissolution,and analyzed the impact of warming and precipitation changes on soil CO2 release from the aspects of Rs and soil carbonate mineral dissolution.In the future,efforts should be done to strengthen research on the coupling effects of climate change and other factors such as soil properties,nutrient content and availability,and microbial biomass and activity on Rs.Constructing an Rs rate model with multivariate factor coupling under extreme climate conditions.Deeply explore the response thresholds of Rs and carbonate mineral dissolution in carbonate bedrock soil areas to extreme heavy precipitation events.Accurately quantify the carbon migration and transformation flux between Rs and carbonate mineral dissolution under extreme heavy rainfall conditions.

warmingprecipitation changesoil CO2soil respirationcarbonate mineral dissolutionenvironmental geology

赵光帅、普政功、黄奇波、朱义年、吴华英

展开 >

中国地质科学院岩溶地质研究所,自然资源部/广西壮族自治区岩溶动力学重点实验室,广西桂林 541004

桂林理工大学环境科学与工程学院,广西桂林 541004

联合国教科文组织国际岩溶研究中心,岩溶动力系统与全球变化国际联合研究中心,广西桂林 541004

增温 降水改变 土壤CO2 土壤呼吸 碳酸盐矿物溶蚀 环境地质

2024

地球科学
中国地质大学

地球科学

CSTPCD北大核心
影响因子:1.447
ISSN:1000-2383
年,卷(期):2024.49(12)