Regulation of soil microbial nitrogen limitation by soybean rhizosphere diazotrophs under long-term no-till mulching

IF 5 2区 农林科学 Q1 SOIL SCIENCE Applied Soil Ecology Pub Date : 2025-02-01 Epub Date: 2025-01-08 DOI:10.1016/j.apsoil.2025.105873
Jiajie Song , Shahzad Haider , Jianheng Song , Dingding Zhang , Sen Chang , Jinze Bai , Jiaqi Hao , Gaihe Yang , Guangxin Ren , Xinhui Han , Xiaojiao Wang , Chengjie Ren , Yongzhong Feng , Xing Wang
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Abstract

Diazotrophs play a vital role in biological nitrogen fixation in agroecosystems. Stoichiometric characterization of soil extracellular enzymes is a key indicator of the effectiveness of microbial nutrient acquisition. However, the mechanisms for exploring the effects of long-term mulching practices on rhizosphere diazotrophic communities and their response to enzyme stoichiometry from the soybean phenology remain unclear. In this study, based on long-term experiments, we adopted four mulching patterns no mulching (CK), straw mulching (SM), plastic mulching (PM) and ridged and plastic mulching (RM). The dynamic changes of rhizosphere soil nutrient characteristics, enzyme stoichiometry characteristics, and diazotrophic dominant communities of soybean were investigated. The study results showed that nutrient content, enzyme activity, and diazotrophic community structure of the rhizosphere soil changed significantly as the soybean growth phenology progressed. Compared to CK, SM treatment enhanced the soil organic carbon (SOC) content (four-leaf (V4) +18.78 %, full-pod (R4) +18.23 %, full maturity (R8) +28.66 %). At R8, the SM treatment significantly increased the soil total nitrogen (STN) content by 16.67 % compared to CK. Our applying vector-threshold (V-T) modeling analysis showed that rhizosphere soil was not carbon (C)-limited. Soil microbial nutrient limitation shifts from nitrogen (N) to phosphorus (P) limitation and finally to N-limitation. In addition, we found that diazotrophs were dominated by Alphaproteobacteria and Betaproteobacteria, at the diazotrophic class level. The dominant diazotrophic genera were Azohydromonas, Bradyrhizobium, and Skermanella. Furthermore, microbial nutrient limitation regressed linearly with the dominant genus. The results indicated a negative correlation between the relative abundance of Azohydromonas, Bradyrhizobium, and Skermanella and microbial N limitation; we observed that mulching measures significantly increased soil mineral N content and promoted an increase in the abundance of dominant diazotrophic genera, thereby effectively mitigating the N limitation faced by microorganisms. Finally, partial least squares path model was used to verify that mulching measures can improve the dominant diazotrophic genera by adjusting the soil physical and chemical properties and regulating VTN/P limitation. Additionally, diazotrophs modify VTN/P limitation by regulating the activity of extracellular enzyme secretion. This study presents a valuable contribution to the domain of enzymatic stoichiometry within agricultural ecosystems, enriching the understanding of relevant processes and offering scientific and technological support for agricultural production.

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长期免耕覆盖下大豆根际重氮营养体对土壤微生物限氮的调控
重氮营养体在农业生态系统生物固氮中起着至关重要的作用。土壤胞外酶的化学计量学特征是衡量微生物养分获取有效性的重要指标。然而,长期覆盖对根际重氮营养群落的影响及其对大豆物候酶化学计量学的响应机制尚不清楚。本研究在长期试验的基础上,采用无覆盖(CK)、秸秆覆盖(SM)、地膜覆盖(PM)和垄作地膜覆盖(RM) 4种覆盖模式。研究了大豆根际土壤养分特征、酶化学计量特征和重氮营养优势群落的动态变化。研究结果表明,随着大豆生长物候的进展,根际土壤养分含量、酶活性和重氮营养群落结构发生了显著变化。与对照相比,SM处理提高了土壤有机碳(SOC)含量(四叶(V4) + 18.78%,全荚(R4) + 18.23%,全熟(R8) + 28.66%)。在R8时,SM处理显著提高了土壤全氮(STN)含量,比对照提高了16.67%。应用向量阈值(V-T)模型分析表明,根际土壤不受碳(C)限制。土壤微生物养分限制由氮(N)限制转变为磷(P)限制,最后转变为氮(N)限制。此外,我们发现重氮营养菌群在重氮营养类水平上以Alphaproteobacteria和Betaproteobacteria为主。重氮营养菌属主要为氮水单胞菌、缓生根瘤菌和斯克曼菌。此外,微生物营养限制与优势属呈线性回归。结果表明,固氮单胞菌、慢生根瘤菌和斯氏菌的相对丰度与微生物氮限制呈负相关;我们发现,覆盖措施显著提高了土壤矿质氮含量,促进了重氮营养优势菌丰度的增加,从而有效缓解了微生物面临的氮限制。最后,利用偏最小二乘路径模型验证了覆盖措施可以通过调节土壤理化性质和VTN/P限制来改善重氮营养优势属。此外,重氮营养体通过调节细胞外酶分泌活性来改变VTN/P限制。本研究为农业生态系统酶化学计量学领域的研究做出了重要贡献,丰富了对相关过程的理解,为农业生产提供了科学技术支持。
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来源期刊
Applied Soil Ecology
Applied Soil Ecology 农林科学-土壤科学
CiteScore
9.70
自引率
4.20%
发文量
363
审稿时长
5.3 months
期刊介绍: Applied Soil Ecology addresses the role of soil organisms and their interactions in relation to: sustainability and productivity, nutrient cycling and other soil processes, the maintenance of soil functions, the impact of human activities on soil ecosystems and bio(techno)logical control of soil-inhabiting pests, diseases and weeds.
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