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Invention of Artificial Rice Field Soil: A Tool to Study the Effect of Soil Components on the Activity and Community of Microorganisms Involved in Anaerobic Organic Matter Decomposition

机译:人工稻田土壤发明:一种研究土壤成分对厌氧有机质分解中涉及的微生物活动和群落的工具

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摘要

Soils are characterized by diverse biotic and abiotic constituents, and this complexity hinders studies on the effects of individual soil components on microorganisms in soil. Although artificial soils have been used to overcome this issue, anoxic soils have not yet been examined. We herein aimed to create artificial soil that reproduces anaerobic methane production by soil from a rice field. Organic materials and mineral particles separated from rice field soil were mixed to prepare an artificial soil matrix; the matrix was added with a small volume of a soil suspension as a microbial inoculum. When the microbial inoculum was added immediately after matrix preparation, anaerobic decomposition was markedly less than that by original soil. When the inoculum was added 9–15 days after soil matrix preparation, anaerobic CO2 and methane production was markedly activated, similar to that by original soil after 40 days of incubation, which suggested that the maturation of the soil matrix was crucial for the reproduction of anaerobic microbial activities. The diversity of the microbial community that developed in artificial soil was markedly less than that in original soil, whereas their predicted functional profiles were similar. Humic substances altered the composition and network patterns of the microbial community. These results suggested that the functional redundancy of soil microorganisms was sustained by different microbial sub-communities. The present study demonstrated that artificial soil is a useful tool for investigating the effects of soil components on microorganisms in anoxic soil.
机译:土壤的特点是各种生物和非生物成分,而这种复杂性妨碍了各种土壤成分对土壤中微生物的影响的研究。虽然人造土壤已被用于克服这个问题,但尚未检查缺氧土壤。我们在此旨在创造人造土壤,从稻田中形成厌氧甲烷产量。将从水稻土壤中分离的有机材料和矿物颗粒混合以制备人工土壤基质;添加基质的土壤悬浮液作为微生物接种物。当在基质制剂后立即加入微生物接种物时,厌氧分解明显小于原始土壤。当土壤基质制备后9-15天加入时,厌氧CO 2和甲烷产量明显激活,类似于孵育40天后的原始土壤,这表明土壤基质的成熟对于繁殖至关重要厌氧微生物活动。人工土壤中发展的微生物群落的多样性明显低于原始土壤中的多样性,而其预测的功能性曲线也是相似的。腐殖质改变了微生物群落的组成和网络模式。这些结果表明土壤微生物的功能冗余由不同的微生物亚群体维持。本研究表明,人造土是一种有用的工具,用于研究土壤成分对缺氧土壤中微生物的影响。

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