Effects of irrigation-mediated continuously moist and dry-rewetting pattern on soil physicochemical properties, structure and bacterial community

IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Applied Soil Ecology Pub Date : 2024-11-28 DOI:10.1016/j.apsoil.2024.105767
Fuhui Yang , Pute Wu , Lin Zhang , Yuqing Hang , Yiqian Wei
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Abstract

The drying-rewetting cycles (DRW) shaped by climate change are known to affect the physicochemical cycles of natural soils. In irrigated soils, changes in irrigation methods make DRW cycles more repetitive and frequent. However, how irrigation regimes affect the physicochemical properties of irrigated soils and their selection of microbial communities have yet to be discovered. Two irrigation methods for two DRW patterns were selected: (1) continuous irrigation for constantly moist (including three soil wetness, low for CL, medium for CM, and high for CH) and (2) intermittent irrigation for DRW (including three intermittent irrigation frequencies, low for DL, medium for DM and high for DH), to determine the selection of soil physicochemical properties and microbial communities and their effect on yield by mediating soil DRW patterns with different irrigation methods. The results revealed that the DRW pattern mediated by irrigation regimes significantly affected soil physicochemical properties. Constantly moist treatments maintained a more stable soil hydrothermal status, with less soil salinity and slight alkalinity than DRW treatments. The water-stable aggregate was greater in CM, but it was progressively enhanced with increased intermittent frequency. In addition, SOM and TN in CM were 15 %, 25 %, and 35 % higher than in DL, DM, and DH, respectively. High-throughput sequencing results showed that CM had the largest Chao1 index (2610.10), Shannons index (10.23), and Simpsons index (0.9982). The results of the Mental tests indicated that soil moisture patterns exhibited a high degree of explanation by environmental factors. The RDA analysis demonstrated that the PC1 axis (28.7 %) significantly separated the soil bacterial communities of different treatments. These results extend the theoretical understanding of how continuously moist soil and continuous irrigation affect soil physicochemical properties and microbial community diversity. This study provides theoretical guidance for strengthening the application and popularization of continuous irrigation in irrigated soil in the future.

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以灌溉为媒介的持续湿润和干燥润湿模式对土壤理化性质、结构和细菌群落的影响
众所周知,气候变化所形成的干燥-润湿循环(DRW)会影响天然土壤的物理化学循环。在灌溉土壤中,灌溉方法的变化使干燥-湿润循环更加重复和频繁。然而,灌溉制度如何影响灌溉土壤的理化性质及其微生物群落的选择还有待研究。选择了两种DRW模式的两种灌溉方法:(1)持续湿润的连续灌溉(包括三种土壤湿润度,低为CL、中为CM、高为CH)和(2)DRW的间歇灌溉(包括三种间歇灌溉频率,低为DL、中为DM、高为DH),通过不同灌溉方法对土壤DRW模式的介导,确定土壤理化性质和微生物群落的选择及其对产量的影响。结果表明,灌溉制度介导的 DRW 模式对土壤理化性质有显著影响。与 DRW 处理相比,恒湿处理能保持更稳定的土壤水热状态,土壤盐度更低,碱度更轻。CM 中的水稳骨料更大,但随着间歇频率的增加,水稳骨料逐渐增加。此外,CM 的 SOM 和 TN 分别比 DL、DM 和 DH 高 15%、25% 和 35%。高通量测序结果显示,CM 的 Chao1 指数(2610.10)、Shannons 指数(10.23)和 Simpsons 指数(0.9982)最高。心理测试结果表明,土壤水分模式在很大程度上可以用环境因素来解释。RDA 分析表明,PC1 轴(28.7%)显著区分了不同处理的土壤细菌群落。这些结果拓展了对持续湿润土壤和持续灌溉如何影响土壤理化性质和微生物群落多样性的理论认识。该研究为今后加强连续灌溉在灌溉土壤中的应用和推广提供了理论指导。
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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.
期刊最新文献
Editorial Board Influence of land-use type on earthworm diversity and distribution in Yunnan: Insights from soil properties Breeding-induced changes in the rhizosphere microbial communities in Lima bean (Phaseolus lunatus) Corrigendum to “Characteristics of microbial community during the different growth stages of yam (Dioscorea opposita Thunb. cv. Tiegun)” [Appl. Soil Ecol. 201 (2024) 105519] Erratum to “Lack of inhibitory effects of 1-Octyne and PTIO on ammonia oxidizers, nitrite oxidizers, and nitrate formation in acidic paddy soils” [Appl. Soil Ecol. 203 (2024) 105673]
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