Crop residues reshape microbial community composition and function across acidic soils via interactions between carbon chemistry, soil pH and nutrient availability

IF 6.6 1区 农林科学 Q1 SOIL SCIENCE
Wenbin Zhu , Chenwei Liu , Clayton R. Butterly , Shuang Ouyang , Lianghu Su , Longjiang Zhang , Lei Wang
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Abstract

There is a significant gap in understanding how crop residues with varying carbon-to-nitrogen (C/N) ratios mitigate soil acidification in acidic soils, particularly considering the complex interplay between soil C chemistry, pH, nutrient dynamics, and their subsequent effects on microbial community composition and enzymatic activities. Here, a 65-day incubation experiment was conducted using four crop residues with varying C/N ratio (rapeseed cake 7.6; peanut straw 27.0; rice straw 48.6 and wheat straw 93.6), aiming to fill these knowledge gaps in the two typical acidic long-term tea garden soils. Results showed that the incorporation of crop residues significantly enhanced edaphic characteristics and mitigated soil acidification. In strongly acidic soil (pH 4.12), rapeseed cake increased SOC recalcitrance, while promoting SOC decomposition in slightly acidic soil (pH 4.75). Furthermore, residue incorporation markedly altered microbial community composition, notably reducing fungal-to-bacterial and G+-to-G ratios in slightly acidic soil. Soil C chemistry, the primary factor, interacting with pH and nutrients influenced microbial composition and enzymatic activities. Specifically, in strongly acidic soils, microbial composition was determined by the interaction of pH and C chemistry, whereas in slightly acidic soils, it was driven by the interaction between C chemistry and phosphorus content. Correspondingly, enzyme activities were influenced by the interaction of C chemistry with phosphorus in the former soils and nitrogen in the latter soils. Overall, our findings confirm the importance of rapeseed cake in enhancing soil multifunctionality, especially in strongly acidic soil, and highlight the critical role of C chemistry, soil pH, and nutrient interactions in shaping microbial composition and function in acidic soils.
作物残茬通过碳化学、土壤pH和养分有效性之间的相互作用重塑酸性土壤微生物群落组成和功能
在了解不同碳氮比(C/N)的作物残茬如何缓解酸性土壤酸化方面存在重大差距,特别是考虑到土壤C化学、pH、养分动态及其对微生物群落组成和酶活性的后续影响之间的复杂相互作用。本研究利用四种不同碳氮比的作物秸秆(油菜籽饼7.6、花生秸秆27.0、水稻秸秆48.6、小麦秸秆93.6)进行65天的培养实验,填补两种典型酸性长期茶园土壤的知识空白。结果表明,作物秸秆的掺入显著改善了土壤特征,缓解了土壤酸化。在强酸性土壤(pH 4.12)中,油菜籽饼增加了有机碳的抗性,而在微酸性土壤(pH 4.75)中,油菜籽饼促进了有机碳的分解。此外,残渣掺入显著改变了微酸性土壤的微生物群落组成,显著降低了微酸性土壤中真菌与细菌的比值和G+与G−的比值。土壤C化学是主要因子,与pH和养分相互作用影响微生物组成和酶活性。其中,在强酸性土壤中,微生物组成由pH和C化学的相互作用决定,而在微酸性土壤中,微生物组成由C化学和磷含量的相互作用决定。相应的,酶活性受到前一种土壤中C化学与磷和后一种土壤中氮的相互作用的影响。总的来说,我们的研究结果证实了油菜籽饼在增强土壤多功能性方面的重要性,特别是在强酸性土壤中,并强调了C化学、土壤pH和养分相互作用在塑造酸性土壤微生物组成和功能方面的关键作用。
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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