Conservation tillage enhances both organic and inorganic carbon in dryland: Insights from a 20-year field experiment and meta-analysis
文献类型: 外文期刊
作者: Ding, Weiting 1 ; Sun, Liangjie 1 ; Qi, Zhidong 1 ; Li, Shengping 3 ; Filipovic, Vilim 4 ; Wu, Xueping 3 ; He, Hailong 1 ;
作者机构: 1.Northwest A&F Univ, Coll Nat Resources & Environm, Yangling 712100, Shaanxi, Peoples R China
2.Minist Agr & Rural Affairs, Key Lab Plant Nutr & Agrienvironm Northwest China, Yangling 712100, Shaanxi, Peoples R China
3.Chinese Acad Agr Sci, State Key Lab Efficient Utilizat Arable Land China, Inst Agr Resources & Reg Planning, Beijing 100081, Peoples R China
4.Univ Queensland, Sch Agr & Food Sustainabil, St Lucia, Qld 4072, Australia
5.Univ Zagreb, Fac Agr, Dept Soil Ameliorat, Div Agroecol, Svetosimunska Cesta 25, Zagreb 10000, Croatia
6.Univ Manitoba, Dept Soil Sci, Winnipeg, MB R3T 2N2, Canada
关键词: Conservation agriculture; Soil organic carbon; Soil inorganic carbon; Dryland agriculture; Microbially induced carbonate precipitation; Carbon sequestration
期刊名称:AGRICULTURE ECOSYSTEMS & ENVIRONMENT ( 影响因子:6.4; 五年影响因子:6.8 )
ISSN: 0167-8809
年卷期: 2025 年 393 卷
页码:
收录情况: SCI
摘要: Conservation tillage is widely recognized as a promising practice for sequestering soil organic carbon (SOC). However, its impact on soil inorganic carbon (SIC) remains less understood and has seldom been quantified. This study aimed to examine the effects of conservation tillage on soil carbon pools, focusing on SIC, by combining a 20-year field experiment in an arid-calcareous cropland of China with a meta-analysis of 76 pairwise data from 7 studies. The field experiment confirms that conservation tillage significantly increases carbon stock, with reduced tillage (RT) increasing SOC (25.09 %, 0-40 cm) and no-tillage (NT) increasing SIC (10.67 %, 0-20 cm). SOC and SIC exhibit a complementary relationship, whereby an increase in SOC effectively compensates for reduced SIC within RT. Notably, the proliferation of calcifying bacteria (e.g., Bacillus) and reduced urease activity suggest that microbial-induced carbonate precipitation, a process known to be facilitated by these bacteria, may contribute significantly to SIC formation under NT. Agronomic practices, as well as soil abiotic and biotic factors, collectively influence SIC. The relative importance of these factors varies with soil depth: biotic variables effects weaken with depth, while abiotic variables increase. Furthermore, our meta-analysis reveals that the response of SIC to conservation tillage varies with climatic, edaphic, and agronomic factors. Arid regions benefit the most from NT in enhancing SIC stock (3.27 %). These findings provide valuable insights into how conservation tillage influences soil carbon, particularly SIC, and enhance our understanding of carbon dynamics in arid systems.
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