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生物炭基肥料改良剂改善了喀斯特山区的土壤微生物群落结构。

Biochar-based fertilizer amendments improve the soil microbial community structure in a karst mountainous area.

机构信息

College of Biology and the Environment, Nanjing Forestry University, Nanjing, China; Co-Innovation Center for Sustainable Forestry in Southern China, Nanjing Forestry University, Nanjing, China.

College of Biology and the Environment, Nanjing Forestry University, Nanjing, China; Co-Innovation Center for Sustainable Forestry in Southern China, Nanjing Forestry University, Nanjing, China; Institute of Botany, Jiangsu Province and Chinese Academy of Sciences, Nanjing, China.

出版信息

Sci Total Environ. 2021 Nov 10;794:148757. doi: 10.1016/j.scitotenv.2021.148757. Epub 2021 Jun 29.

Abstract

Biochar-based fertilizer amendment can improve soil properties partly due to stimulated microbial activities and growths. The karst ecosystem is prone to degradation and accounts for a large proportion of southwest China. Understanding of the response of the microbial community structure to biochar-based fertilizer application is of great significance in karst soil restoration. A field experiment located in southwest China was conducted in typical karst soil, and a high-throughput sequencing approach was used to investigate the effect of biochar-based fertilizer application on microbial community structure in karst soil. Field trials were set up for 24 months using the following treatments: control (CK), compost plus NPK fertilizer (MF), biochar (B), less biochar (half the quantity of biochar in B) plus compost and NPK fertilizer (B1MF), biochar plus compost and NPK fertilizer (BMF), and more biochar (double the quantity of biochar in B) plus compost and NPK fertilizer (B4MF). The results elucidated that BMF and B4MF treatments had higher contents of soil carbon and soil nutrients N, P, and K than the other treatments. Soil microbial abundance and diversity were significantly increased by biochar-based fertilizer amendments (BMF and B4MF), compared to CK (P < 0.05). BMF and B4MF treatments significantly increased the relative abundance of dominant microorganisms, compared to CK (P < 0.05). The difference in the composition of indicator microbes between each treated group indicated that soil amendments altered the microbial community structure. There was a strong correlation between soil properties (soil C-, N-, and P-fractions) and microbial community structure. Furthermore, network analysis revealed that the addition of biochar-based fertilizer increased the scale and complexity of the microbial co-occurrence network. To summarize, the application of biochar-based fertilizer enabled more keystone species in the soil microbial network to participate in soil carbon resource management and soil nutrient cycling, indicating that biochar-based fertilizer is beneficial for the restoration of karst-degraded soils.

摘要

基于生物炭的肥料改良可以通过刺激微生物的活性和生长来改善土壤性质。喀斯特生态系统容易退化,占中国西南地区的很大比例。了解生物炭基肥料施用对微生物群落结构的响应,对于喀斯特土壤恢复具有重要意义。在中国西南地区的典型喀斯特土壤中进行了田间试验,采用高通量测序方法研究了生物炭基肥料施用对喀斯特土壤微生物群落结构的影响。田间试验设置了 24 个月的时间,采用以下处理:对照(CK)、堆肥加 NPK 肥料(MF)、生物炭(B)、少生物炭(B 生物炭量的一半加堆肥和 NPK 肥料(B1MF)、生物炭加堆肥和 NPK 肥料(BMF)、多生物炭(B 生物炭量的两倍加堆肥和 NPK 肥料(B4MF)。结果表明,BMF 和 B4MF 处理的土壤碳和土壤养分 N、P、K 含量均高于其他处理。与 CK 相比,生物炭基肥料改良(BMF 和 B4MF)显著增加了土壤微生物的丰度和多样性(P<0.05)。与 CK 相比,BMF 和 B4MF 处理显著增加了优势微生物的相对丰度(P<0.05)。各处理组指示微生物的组成差异表明,土壤改良改变了微生物群落结构。土壤性质(土壤 C、N 和 P 组分)与微生物群落结构之间存在很强的相关性。此外,网络分析表明,生物炭基肥料的添加增加了微生物共生网络的规模和复杂性。总之,生物炭基肥料的应用使更多的土壤微生物网络中的关键种参与土壤碳资源管理和土壤养分循环,表明生物炭基肥料有利于喀斯特退化土壤的恢复。

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