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Positive effect of carbohydrate-metabolizing bacteria determines increasing soil organic carbon during long-term fertilization and straw returning in the black soil region of China

土壤碳 稻草 人类受精 农学 总有机碳 微生物 背景(考古学) 土壤有机质 碳纤维 化学 环境科学 环境化学 生物 细菌 土壤水分 土壤科学 数学 古生物学 遗传学 算法 复合数
作者
Yingxin Li,Yu Sun,Eiko E. Kuramae,Shaoqing ZHANG,Enze WANG,Zongmu Yao,Fahad Nasir,Lei Tian,Qiang Gao,Chunjie Tian
出处
期刊:Pedosphere [Elsevier BV]
卷期号:34 (5): 853-864 被引量:15
标识
DOI:10.1016/j.pedsph.2023.07.001
摘要

In the context of global efforts to reduce carbon emissions, several studies have examined the effects of agricultural practices like straw returning and fertilization on the sequestration of carbon by microorganisms. However, our understanding of the specific microbial groups and their roles in long-term carbon increase remains limited. Therefore, we conducted a 36-year farmland experiment (1984–2020) to investigate the impact of bacterial carbon metabolism on the augmentation of soil organic carbon. Our findings demonstrated a noteworthy increase in the diversity of microorganisms in farmland as a result of long-term straw returning and the application of mixed chemical fertilizers. However, when we examined the functions of farmland microorganisms involved in carbon metabolism, we observed that the effects of fertilization on carbon metabolism were relatively consistent. This consistency was attributed to a deterministic competitive exclusion process, which minimized differences between treatment groups. On the other hand, the influence of straw addition on carbon metabolism appeared to follow a more random pattern. These changes in microbial activity were closely linked to the down-representation of core metabolic pathways related to carbon metabolism. Notably, long-term fertilization had a negative impact on soil organic carbon levels, while long-term straw fertilization resulted in a positive increase in soil organic carbon. These findings have important implications for enhancing soil organic carbon content and grain yield in regions with typical black soil characteristics.
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