微生物
土壤生态学
生物地球化学循环
土壤肥力
土壤生物学
土壤生物多样性
环境科学
营养循环
土壤有机质
微生物种群生物学
土壤碳
农学
生态系统
环境化学
生态学
生物
化学
细菌
土壤水分
土壤科学
遗传学
标识
DOI:10.1007/978-981-99-4113-1_12
摘要
Soil microbial community include bacteria, fungi, actinomycetes, algae, and protozoa. The quantity is very large, there are hundreds of millions to tens of billions of microorganisms in 1 gram soil. Most soil microorganisms are beneficial to the growth and development of crops, and they have a significant impact on the formation and development of soil, material circulation, and fertility evolution. There are millions of species of bacteria and fungi on Earth, and they participate in almost all life processes. In addition, the total carbon content of bacteria is about 60–100% of the carbon content of plant. Soil is not simply a simple combination of soil particles and nutrient elements. As an active component of soil, soil microorganisms contribute to soil particles through the exchange of carbon dioxide and oxygen through metabolic activities in their life processes, as well as through the secretion of organic acids. A large aggregate structure is formed, and finally, a real soil is formed. Soil formation and development are closely related to the flora composition, biomass, and life activities of soil microorganisms. Microorganisms also play an important role in the biogeochemical cycle, including carbon, nitrogen, phosphorus, etc. The feedback or response of soil microbial communities to bamboo expansion will substantially impact the nutrient cycling process in the expanded ecosystem.
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