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[土地利用类型变化对土壤硝化作用及氨氧化细菌群落组成的影响]

[Impact of land-use type changes on soil nitrification and ammonia-oxidizing bacterial community composition].

作者信息

Yang Li-Lin, Mao Ren-Zhao, Liu Jun-Jie, Liu Xiao-Jing

机构信息

Key Laboratory of Agricultural Water Resources, Center for Agricultural Research Resources, Institute of Genetics and Developmental Biology, Chinese Academy of Sciences, Shijiazhuang 050021, China.

出版信息

Huan Jing Ke Xue. 2011 Nov;32(11):3455-60.

Abstract

A comparative study was conducted to determine nitrification potentials and ammonia-oxidizing bacterial (AOB) community composition in 0-20 cm soil depth in adjacent native forest,natural grassland, and cropland soils on the Tibetan Plateau, by incubation experiment and by denaturing gradient gel electrophoresis (DGGE) of 16S rDNA, respectively. Cropland has the highest nitrification potential and nitrate concentration among the three land-use types (LUT), approximately 9 folds and more than 11 folds than that of the forests and grasslands, respectively. NO3(-) -N accounted for 70%-90% of inorganic N in cropland soil, while NH4(+) -N was the main form of inorganic N in forest and grassland soils. Nitrification potentials and nitrate concentrations showed no significant difference between native forest and grassland soils. The native forest showed the lowest nitrification potentials and the lowest AOB diversity and community composition among the three LUT. Conversions from natural grasslands to croplands remarkably decreased the AOB diversity and composition, but croplands remain high similarity in AOB community composition compared with grasslands. The minimal and the lowest diversity of AOB in native forests directly resulted to the lowest nitrification potentials compared to natural grasslands and croplands. From the fact of the highest nitrification potentials and nitrate concentrations in croplands indicated that there were the most substantial AOB with higher activity and priority. The results provide evidence that changes of land-use type can affect both soil nitrogen internal cycling process, the diversity, community and activity of AOB, which further affect soil environment quality and the long-term sustainability of ecosystems.

摘要

通过培养实验和16S rDNA的变性梯度凝胶电泳(DGGE),对青藏高原相邻原生林、天然草地和农田土壤0-20厘米土层深度的硝化潜力和氨氧化细菌(AOB)群落组成进行了比较研究。在三种土地利用类型(LUT)中,农田的硝化潜力和硝酸盐浓度最高,分别约为森林和草地的9倍和11倍以上。农田土壤中NO3(-)-N占无机氮的70%-90%,而NH4(+)-N是森林和草地土壤中无机氮的主要形式。原生林和草地土壤的硝化潜力和硝酸盐浓度无显著差异。在三种土地利用类型中,原生林的硝化潜力最低,AOB多样性和群落组成也最低。从天然草地转变为农田显著降低了AOB的多样性和组成,但与草地相比,农田的AOB群落组成仍具有较高的相似性。与天然草地和农田相比,原生林中AOB的最低多样性直接导致了最低的硝化潜力。农田中最高的硝化潜力和硝酸盐浓度表明,存在最多数量、活性较高且具有优先性的AOB。研究结果表明,土地利用类型的变化会影响土壤氮素内部循环过程、AOB的多样性、群落和活性,进而影响土壤环境质量和生态系统的长期可持续性。

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