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Minor responses of soil microbial biomass, community structure and enzyme activities to nitrogen and phosphorus addition in three grassland ecosystems

机译:三种草地生态系统中的土壤微生物测量,群落结构和氮素添加的少量反应

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摘要

Background and aims Human activities have significantly increased nitrogen (N) and phosphorous (P) inputs to terrestrial ecosystems. However, the impact of N and P enrichment on soil microbial community structure and functioning in temperate and alpine grassland ecosystems remains unclear. Methods In this study, we investigated the responses of soil microbial communities to nutrient (N and P) additions in two temperate and one alpine grassland ecosystems in China. We measured soil chemical properties, microbial community composition (indicated by the phospholipid fatty acids, PLFA) and potential enzyme activities related to carbon (C), N, and P cycling in the peak growing season after 4 years of nutrient addition. Results We found that N addition reduced soil pH and increased soil total N content at two meadow sites, P addition increased soil total P content at all three sites, but both N and P additions had minimal effects on soil organic C content. Bacteria and total microbial abundances did not change after N and P additions, while fungi and arbuscular mycorrhizal fungi (AMF) abundances were suppressed by N addition. Moreover, the activity of soil extracellular enzymes involved in C, N and P cycling and their stoichiometric ratios were not responsive to N and P additions, except for inhibition of acid phosphatase by P addition at the temperate meadow site. Conclusions Despite significant changes in soil chemistry (e.g., pH and available nutrients), soil microbial biomass (except fungi and AMF abundances), community structure, and enzyme activities (except phosphatase) were generally resistant to 4 years of N and P addition in the three temperate and alpine grassland ecosystems in China.
机译:背景和AIMS人类活性具有显着增加的氮气(N)和磷(P)对陆地生态系统的投入。然而,N和P富集对土壤微生物群落结构的影响和温带和高山草原生态系统的运作仍然尚不清楚。方法在本研究中,我们调查了在中国的两个温带和一个高山草原生态系统中对土壤微生物社区对营养(N和P)添加的反应。我们测量了土壤化学性质,微生物群落组合物(由磷脂脂肪酸,PLFA表示,与碳(c),n和p循环4年后的碳(c),n和p循环的潜在酶活性。结果我们发现,在两个草地部位,N添加降低的土壤pH值并增加土壤总含量N含量,在所有三个位置增加土壤总P含量,但是N和P添加对土壤有机C含量的影响很小。在N和P添加后,细菌和总微生物丰度没有改变,而N添加则抑制真菌和丛枝菌根真菌(AMF)丰富。此外,除了在温带酸磷酸酶的抑制在温带在温度草地部位,除了酸性磷酸酶之外,涉及C,N和P循环的土壤细胞外酶的活性并不应对N和P.结论尽管土壤化学(例如pH和可用营养物质)的显着变化,但土壤微生物生物量(除菌和AMF丰度除外),群落结构和酶活性(除磷酶除外)通常耐受4年和P添加三个温带和高山草原生态系统在中国。

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