Soil nitrogen availability mediates the positive effects of intercropping on soil organic carbon at global scales

被引:2
作者
Sun, Tingting [1 ,2 ]
Zhou, Jie [3 ]
Fu, Yue [1 ,2 ]
Wu, Lixue [1 ,2 ]
Zhang, Tian [1 ,2 ]
机构
[1] Guangxi Univ, Coll Agron, Nanning, Guangxi, Peoples R China
[2] Guangxi Univ, Key Lab Agroenvironm & Agroprod Safety, Nanning 530005, Peoples R China
[3] Nanjing Agr Univ, Coll Agr, Nanjing 210095, Peoples R China
基金
中国国家自然科学基金;
关键词
Intercropping effects; Carbon fraction; Soil nitrogen availability; Management practice; Microbial biomass carbon; PHOSPHORUS; DYNAMICS; INPUT; ROOT;
D O I
10.1016/j.still.2024.106063
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Intercropping is an effective cultivation practice to develop sustainable agroecosystems and increase soil organic carbon (SOC) and nitrogen (N) with rich crop diversity. With increased duration, the changes in soil N availability might affect microbial and plant growth and consequently regulate the intercropping effects on SOC sequestration. However, the response of intercropping effects on SOC components to soil N availability has been poorly explored. In this study, we constructed a global database with 939 paired data (intercropping vs. monoculture) from 60 publications. We found that intercropping increased SOC (by 7.94%), microbial biomass carbon (MBC, by 23.73%), particulate organic carbon (POC, by 23.27%), and dissolved organic carbon (DOC, by 16.46%) compared to monoculture. The intercropping effects (percentage change, %) on SOC content strongly depends on soil N availability (soil C: N) and the interactions with duration and crop types. In N -limited soils (soil C: N > 15), intercropping increased SOC and POC contents by 14% and 31%, respectively, which were 2-3 times higher than those in N -rich soils (soil C: N < 15). It implies higher intercropping effects in more N -limited soils. In addition, intercropping increased MBC:SOC by 63% in N -limited but not in N -rich soils, indicating greater contributions of microbial -derived C to SOC storage in N -limited but not in N -rich soils. This might be attributed to that the stimulated microbial decomposition of soil organic matter counterbalanced the microbial -derived C accumulation in N -rich soils. Taken together, these results indicate that soil N availability regulates the intercropping effects on SOC content and the contributions of microbial -derived C to SOC storage. Overall, these findings highlight the importance of soil N availability on SOC content with intercropping, implying that intercropping is a suitable agricultural approach especially in N -limited soils and nutrient management should be carefully considered in long-term intercropping experiments.
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页数:9
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