土壤碳
根际
渗出液
生态系统
土壤有机质
营养物
环境科学
大块土
碳纤维
总有机碳
土壤水分
农学
化学
土壤科学
环境化学
生物
植物
生态学
材料科学
复合材料
复合数
细菌
遗传学
作者
Lei Xue,Yuting Shen,Jianing Zhao,Jiajia Huang,Hui Wang,Yang Yu,Chunwang Xiao
出处
期刊:Plants
[Multidisciplinary Digital Publishing Institute]
日期:2023-01-31
卷期号:12 (3): 630-630
被引量:69
标识
DOI:10.3390/plants12030630
摘要
Root exudates, as an important form of material input from plants to the soil, regulate the carbon input and efflux of plant rhizosphere soil and play an important role in maintaining the carbon and nutrient balance of the whole ecosystem. Root exudates are notoriously difficult to collect due to their underlying characteristics (e.g., low concentration and fast turnover rate) and the associated methodological challenges of accurately measuring root exudates in native soils. As a result, up until now, it has been difficult to accurately quantify the soil organic carbon input from root exudates to the soil in most studies. In recent years, the contribution and ecological effects of root exudates to soil organic carbon input and efflux have been paid more and more attention. However, the ecological mechanism of soil organic carbon input and efflux mediated by root exudates are rarely analyzed comprehensively. In this review, the main processes and influencing factors of soil organic carbon input and efflux mediated by root exudates are demonstrated. Soil minerals and soil microbes play key roles in the processes. The carbon allocation from plants to soil is influenced by the relationship between root exudates and root functional traits. Compared with the quantity of root exudates, the response of root exudate quality to environmental changes affects soil carbon function more. In the future, the contribution of root exudates in different plants to soil carbon turnover and their relationship with soil nutrient availability will be accurately quantified, which will be helpful to understand the mechanism of soil organic carbon sequestration.
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