Long-term mulched drip irrigation facilitates soil organic carbon stabilization and the dominance of microbial stochastic assembly processes

IF 5.9 1区 农林科学 Q1 AGRONOMY Agricultural Water Management Pub Date : 2024-08-15 DOI:10.1016/j.agwat.2024.109008
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Abstract

Mulched drip irrigation (MDI) is generally accepted as a method to decrease soil salinization and improve crop yields in arid and semi-arid regions. However, there remain gaps in how MDI drives soil organic carbon (SOC) dynamic microbial assembly processes with time, and the mediating role of microorganisms remains unclear. In this study, we investigated the aforementioned issues across soil profiles in cotton fields with different years of MDI. The results showed that MDI did not cause the differences in SOC, particular organic carbon (POC), and mineral-associated organic carbon (MOC) in soil layers. The POC and MOC contents had a parabola relationship with time, and showed an opposite trend in soil. After 15 years of MDI, the ratio of MOC/SOC increased to a peak value of 50 % and 52 % in topsoil and subsoil, respectively; the ratio of POC/SOC decreased to valley values of 50 % and 48 %, respectively (P < 0.05). Long-term MDI reduced the differences in oxidase between soil layers but accelerated SOC loss by increasing polyphenol oxidase activity (P < 0.05). Compared with that of other years, with 10 years of MDI, bacterial Shannon diversity decreased to a valley value, and fungal Shannon diversity reached to a top value in subsoil (P < 0.05). In general, stochastic processes were mainly controlled by dispersal limitation, and undominated processes dominated microbial assembly; however, there was a close relationship between bacterial communities and organic carbon fractions. The high percentage of positive linkages among microorganisms indicated that long-term MDI was beneficial for carbon fixation. Additionally, a decrease of fungal oligotroph/copiotroph ratio, the relative abundance of Ascomycota and Basidiomycota was beneficial for the accumulation of SOC and POC in topsoil (P < 0.05). In conclusion, long-term MDI is useful for the fixation of organic carbon via improving soil POC content and strengthening linkages within community assemblies.

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长期地膜滴灌有利于土壤有机碳的稳定和微生物随机组装过程的主导地位
在干旱和半干旱地区,地膜覆盖滴灌(MDI)被普遍认为是减少土壤盐碱化和提高作物产量的一种方法。然而,MDI 如何随着时间的推移推动土壤有机碳(SOC)动态微生物组装过程仍是一个空白,微生物的中介作用也仍不清楚。在本研究中,我们对不同年份 MDI 的棉田土壤剖面的上述问题进行了调查。结果表明,MDI 并未造成土壤层中 SOC、特定有机碳(POC)和矿质相关有机碳(MOC)的差异。POC 和 MOC 含量与时间呈抛物线关系,在土壤中呈相反趋势。经过 15 年的 MDI,表层土壤和底层土壤中的 MOC/SOC 比率分别增加到 50 % 和 52 % 的峰值;POC/SOC 比率分别下降到 50 % 和 48 % 的谷值(P < 0.05)。长期 MDI 减少了土壤层间氧化酶的差异,但通过增加多酚氧化酶的活性加速了 SOC 的流失(P < 0.05)。与其他年份相比,MDI 持续 10 年后,细菌香农多样性下降到谷值,真菌香农多样性在底土达到最高值(P < 0.05)。总体而言,随机过程主要受扩散限制的控制,非主导过程主导微生物的组合;但细菌群落与有机碳组分之间存在密切关系。微生物之间高比例的正向联系表明,长期的 MDI 有利于碳固定。此外,真菌寡养/共养比例的降低、子囊菌群和担子菌群相对丰度的降低有利于表土中 SOC 和 POC 的积累(P <0.05)。总之,长期 MDI 有助于通过提高土壤 POC 含量和加强群落组合内的联系来固定有机碳。
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来源期刊
Agricultural Water Management
Agricultural Water Management 农林科学-农艺学
CiteScore
12.10
自引率
14.90%
发文量
648
审稿时长
4.9 months
期刊介绍: Agricultural Water Management publishes papers of international significance relating to the science, economics, and policy of agricultural water management. In all cases, manuscripts must address implications and provide insight regarding agricultural water management.
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