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长期施肥模式对黄壤旱地细菌群落结构和土壤养分的影响。

Effects of long-term fertilization patterns on bacterial community structure and soil nutrients in dryland of yellow soil.

机构信息

Institute of Soil and Fertilizer, Guizhou Academy of Agricultural Sciences, Guiyang 550006, China.

Scientific Observing and Experimental Station of Arable Land Conservation and Agriculture Environment (Guizhou), Ministry of Agriculture and Rural Affairs, Guiyang 550006, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2023 Jul;34(7):1949-1956. doi: 10.13287/j.1001-9332.202307.011.

Abstract

Understanding the responses of soil bacterial community to long-term fertilization in dryland of yellow soil could provide theoretical basis for establishing scientific fertilization system and cultivating healthy soil. Based on a 25-year long-term fertilization experiment on yellow soil, we collected soil samples from 0-20 cm layer under different fertilization treatments: no fertilization (CK), balanced application of N, P and K fertilizers (NPK), single application of organic fertilizer (M), combined application of constant organic and inorganic fertilizer (MNPK), and 1/2 organic fertilizer instead of 1/2 chemical fertilizer (MNP). Illumina MiSeq high-throughput sequencing technology was used to examine the effects of different fertilization patterns on soil bacterial community structure and soil nutrient content. The main driving factors of soil bacterial community were explored. The results showed that soil pH and organic matter content under treatments with organic fertilizer increased by 11.4%-13.5% and 28.8%-52.0%, respectively, compared to that under NPK treatment. Long-term fertilization did not affect soil bacterial α diversity, but significantly affected soil bacterial β diversity. Compared with CK and NPK treatment, treatments of M, MNP, and MNPK significantly changed soil bacterial community structure, and increased the relative abundance of Fusobacteria and Anaerobes. Four fertilization treatments increased the relative abundance of Bacteroidetes, and decreased the relative abundance of Actinomyces and Campylobacter, compared to CK. Soil pH was the most important factor affecting soil bacterial community structure. Fertilization-stimulated rare microbial taxa (Pumilomyces and Anaerobes) were more sensitive to changes in different environmental factors and were the main drivers of the formation of community versatility. In conclusion, organic fertilizer improved soil properties and fertility and changed soil bacterial community structure, which are conducive to cultivating healthy soil.

摘要

了解旱地黄壤土壤细菌群落对长期施肥的响应,可以为建立科学施肥体系和培育健康土壤提供理论依据。本研究在长期施肥的基础上,采集了不同施肥处理(不施肥 CK、氮磷钾平衡施肥 NPK、单施有机肥 M、恒量有机肥和无机肥配施 MNPK、1/2 有机肥替代 1/2 化肥 MNP)下 0-20cm 土层的土壤样本。利用 Illumina MiSeq 高通量测序技术研究了不同施肥模式对土壤细菌群落结构和土壤养分的影响,探讨了土壤细菌群落的主要驱动因素。结果表明,与 NPK 处理相比,有机肥处理的土壤 pH 和有机质含量分别提高了 11.4%-13.5%和 28.8%-52.0%。长期施肥没有影响土壤细菌α多样性,但显著影响土壤细菌β多样性。与 CK 和 NPK 处理相比,M、MNP 和 MNPK 处理显著改变了土壤细菌群落结构,增加了厚壁菌门和厌氧菌的相对丰度。与 CK 相比,4 种施肥处理增加了拟杆菌门的相对丰度,降低了放线菌门和弯曲菌门的相对丰度。土壤 pH 是影响土壤细菌群落结构的最重要因素。施肥刺激的稀有微生物类群(毛壳菌属和厌氧菌)对不同环境因子的变化更敏感,是群落多样性形成的主要驱动因素。综上所述,有机肥改良了土壤性质和肥力,改变了土壤细菌群落结构,有利于培育健康土壤。

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