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应用生态学报 ›› 2026, Vol. 37 ›› Issue (8): 2627-2636.doi: 10.13287/j.1001-9332.202608.015

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黄土高原退耕还林对深层土壤细菌群落多样性及组成的影响

史冬玉1,5, 邓家健2, 邱天逸3, 张圆浩4, 徐知远1, 胡振宏2,5*   

  1. 1西北农林科技大学资源环境学院, 陕西杨凌 712100;
    2西北农林科技大学水土保持科学与工程学院, 水土保持与荒漠化整治全国重点实验室, 陕西杨凌 712100;
    3武汉理工大学资源与环境工程学院, 关键非金属矿产资源绿色利用教育部重点实验室, 武汉 430000;
    4中国科学院东北地理与农业生态研究所, 长春 130102;
    5西北农林科技大学深圳研究院, 广东深圳 518057
  • 收稿日期:2025-12-12 修回日期:2026-07-07 出版日期:2026-08-18 发布日期:2027-02-18
  • 通讯作者: *E-mail: zhhu2020@nwafu.edu.cn
  • 作者简介:史冬玉, 女, 2000年生, 硕士研究生。主要从事森林土壤学研究。E-mail: sdy39832231@163.com
  • 基金资助:
    国家重点研发计划项目(2024YFF1308600)和深圳市科技计划项目(JCYJ20230807111402004)

Effects of “Grain for Green” on bacterial community diversity and composition in deep soil layer on the Loess Plateau, Northwest China

SHI Dongyu1,5, DENG Jiajian2, QIU Tianyi3, ZHANG Yuanhao4, XU Zhiyuan1, HU Zhenhong2,5*   

  1. 1College of Natural Resources and Environment, Northwest A&F University, Yangling 712100, Shaanxi, China;
    2State Key Laboratory of Soil and Water Conservation and Desertification Control, College of Soil and Water Conservation Science and Engineering, Northwest A&F University, Yangling 712100, Shaanxi, China;
    3Ministry of Education Key Laboratory of Green Utilization of Critical Non-metallic Mineral Resources, School of Resources and Environmental Engineering, Wuhan University of Technology, Wuhan 430000, China;
    4Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, China;
    5Northwest A&F University Shenzhen Research Institute, Shenzhen 518057, Guangdong, China
  • Received:2025-12-12 Revised:2026-07-07 Online:2026-08-18 Published:2027-02-18

摘要: 退耕还林是黄土高原水土保持与生态修复的关键治理措施,深刻影响区域土壤生态过程。但现有研究多聚焦表层土壤,退耕还林如何调控深层土壤细菌群落及其响应机制仍不明确。本研究以黄土高原典型干旱区退耕后刺槐人工林(25年)和撂荒年限相当的农田为对象,以表层(0~20 cm)土壤为参照,分析深层(160~200 cm)土壤细菌多样性、群落组成及其与土壤理化因子的耦合关系。结果表明:表层土壤中,刺槐林全碳较农田显著提高7.4%,有效磷显著降低80.5%;深层土壤中,刺槐林全碳较农田显著提高17.6%,全磷和含水量分别显著降低15.6%和63.5%。层间对比,刺槐林深层土壤全氮和含水量较表层显著降低,pH显著提高;农田深层土壤全碳和全氮含量较表层显著降低,pH显著提高。表层土壤细菌α多样性指数(Chao1指数和系统发育多样性指数)显著高于深层,刺槐林土壤α多样性指数均低于农田。土地利用类型与土层的交互作用显著影响细菌群落组成,二者共同解释了48.3%的群落变异。刺槐人工林深层土壤绿弯菌门、放线菌门等寡营养细菌类群丰度分别较农田提升19.7%和65.0%,而变形菌门等富营养细菌类群丰度降低26.9%。细菌群落对环境因子的响应存在明显垂直分异,表层土壤群落受氮、磷养分和水分调控,深层土壤群落主要受土壤碳储量和水分含量驱动。刺槐林较农田土壤细菌具有更高的网络复杂度和稳定性,且表层与深层差异显著。综上,退耕还林改变了土壤理化性质,显著重塑了旱区土壤细菌群落组成与垂直分布,促使深层土壤微生物向寡营养化转变,进而影响深层土壤养分循环、碳固持与水分平衡。

关键词: 退耕还林, 黄土高原, 细菌群落结构, 深层土壤, 旱区

Abstract: The “Grain for Green” program, a key measure for soil and water conservation and ecological restoration on the Loess Plateau, profoundly affects soil ecological processes. However, existing research mostly focuses on topsoil. How returning farmland to forest regulates bacterial communities in deep soil and the response mechanisms remain unclear. Taking Robinia pseudoacacia plantation (25 a) after returning farmland to forest and cropland with similar fallow periods in a typical arid area of the Loess Plateau as research subjects, with the topsoil layer (0-20 cm) as the reference, we analyzed bacterial diversity, community composition, and their relationship with soil physicochemical factors in deep soil layer (160-200 cm). The results showed that, in the topsoil, the total carbon content of R. pseudoacacia plantation was significantly 7.4% higher than that of cropland, while the available phosphorus content was 80.5% lower. In the deep soil, the total carbon content of R. pseudoacacia plantation was significantly 17.6% higher than that of cropland, and total phosphorus content and soil water content were significantly reduced by 15.6% and 63.5%, respectively. For the inter-layer comparison, total nitrogen content and water content in the deep soil of R. pseudoacacia plantation were significantly lower than those in the topsoil, while soil pH value increased significantly. For cropland, total carbon and total nitrogen contents in the deep soil were significantly lower than those in the topsoil, and pH value also increased significantly. Bacterial α diversity indexes (Chao1 index and phylogenetic diversity index) were significantly higher in topsoil than in deep soil. Moreover, the indices of α diversity in the both soil layers of the R. pseudoacacia plantation were significantly lower than those of cropland. The interaction between land use type and soil layer significantly affected bacterial community composition, together explaining 48.3% of the community variation. The abundance of oligotrophic bacterial groups such as Chloroflexi and Actinomycetes in the deep soil of R. pseudoacacia plantations increased by 19.7% and 65.0% respectively compared to cropland, while the abundance of copiotrophic bacterial groups such as Proteobacteria decreased by 26.9%. The response of bacterial community to environmental factors exhibited significant vertical differentiation. The topsoil community was regulated by nitrogen, phosphorus, and water availability, while the deep soil community was mainly driven by soil carbon storage and water content. Compared with croplands, R. pseudoacacia plantations had higher bacterial network complexity and stability, with significant differences between topsoil and deep soil. In summary, returning farmland to forest altered soil physical and chemical properties, and reshaped the composition and vertical distribution of soil bacterial communities, promoting a shift towards oligotrophic bacteria in deep soils, thereby affecting nutrient cycling, carbon sequestration, and water balance in deep soils.

Key words: Grain for Green, the Loess Plateau, bacterial community structure, deep soil, dryland