Legume cover crops enhance soil organic carbon via microbial necromass in orchard alleyways

被引:8
|
作者
Hu, Qijuan [1 ]
Jiang, Tao [1 ,2 ]
Thomas, Ben W. [3 ]
Chen, Ji [4 ,5 ]
Xie, Jun [1 ]
Hu, Yingxiao [1 ]
Kong, Faming [1 ]
Yang, Yuanyu [1 ]
Chen, Xinping [1 ,2 ]
Zhang, Yuting [1 ,2 ]
Shi, Xiaojun [1 ,2 ]
机构
[1] Southwest Univ, Coll Resources & Environm, Chongqing 400716, Peoples R China
[2] Southwest Univ, Interdisciplinary Res Ctr Agr Green Dev Yangtze Ri, Chongqing 400715, Peoples R China
[3] Agr & Agrifood Canada, Agassiz Res & Dev Ctr, Agassiz, BC V0M 1A0, Canada
[4] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
[5] Aarhus Univ, Dept Agroecol, DK-8830 Tjele, Denmark
来源
SOIL & TILLAGE RESEARCH | 2023年 / 234卷
关键词
Green manure; Microbial carbon; Amino sugars; Microbial residue; Mineral-associated organic matter; GREEN MANURE; AMINO-SUGARS; COMMUNITY; STABILIZATION; RESIDUES; ACCUMULATION; CULTIVATION; MANAGEMENT; RELEVANCE; DYNAMICS;
D O I
10.1016/j.still.2023.105858
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Cover crops may enhance soil organic carbon (SOC) sequestration, but the links among SOC fractions, microbial necromass carbon (C), and SOC sequestration potential in legume and non-legume cover-cropped orchards are unclear. We leveraged data from seven orchards with varying climatic and edaphic properties in China to assess the effects of legume and non-legume cover crops on SOC and microbial necromass C in bulk soil, particulate organic matter (POM), and mineral-associated organic matter (MAOM). Legume cover crops led to a significantly greater increase in SOC than non-legumes (23 % vs. 2 %), compared with no cover crops. The MAOM-C with legumes and non-legumes were similar but were both significantly greater than the control plots without cover crops. Legume cover crops positively influenced bacterial and fungal necromass C in all SOC fractions, while nonlegume cover crops only affected fungal necromass C in bulk soil and MAOM. The effect of cover crops on the microbial necromass C to SOC ratio was negligible. Fungal necromass contributed most of the microbial necromass C to SOC accumulation, particularly in MAOM. Linear regression showed SOC, POM-C, and MAOM-C accumulated with increasing microbial necromass C. Microbial necromass C was the key factor explaining the variation in POM-C and MAOM-C compared to other climatic and edaphic factors. Partial least squares path modeling showed a causal relationship among cover crops, climate, soil substrates, soil properties, microbial necromass, and SOC and SOC fractions. Our study suggests that changes in microbial necromass C and composition may explain most of the increase in SOC in cover-cropped orchards and that MAOM-C is the principal sink of microbial necromass. This information is valuable for improving our understanding of the potential impact of microbial necromass C on enhancing SOC sequestration potential in orchard soils under cover crop management.
引用
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页数:13
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