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[赤泥中自然土壤的成因及潜在微生物机制。]

[Natural soil genesis in red mud and underlying microbial mechanism.].

作者信息

Li Hui, Qu Yang, Yao Min-Jie, Tian Wen-Jie, Wang Xiao-Qing, Shi Ben, Cao Li-Na, Yue Ling-Fan, Cao Kai-Qin

机构信息

College of Environmental Engineering and Chemistry, Luoyang Institute of Science and Technology, Luoyang 471023, Henan, China.

College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou 350002, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2021 Apr;32(4):1452-1460. doi: 10.13287/j.1001-9332.202104.038.

Abstract

Soil genesis is important for ecological restoration of red mud disposal area. Soil genesis of red mud and the microbial mechanism were studied by analyzing the change of physicochemical and biochemical characteristics of red mud. We analyzed the microbial community structure in a red mud disposal area without any human-induced restoration through a space for time substitution approach. The results showed that, with the increases of storage time, the physical parameters of porosity, water-stable aggregates content, and mean weight diameter increased, but the bulk density decreased. The chemical parameters, including pH, electrical conductivity, acid neutralizing capacity, and exchangeable sodium percentage, decreased with increasing storage time. The bio-chemical parameters of total organic carbon, total nitrogen, available phosphorus, microbial biomass carbon and basal respiration increased, but the metabolic quotient decreased. The Shannon diversity index increased, and the dominant microflora in red mud changed from the oxygenic photosynthetic bacteria Cyanobacteria and thanaerobic anoxygenic phototrophic bacteria Chlorobi and Chloroflexi to Proteobacteria, Actinobacteria and Firmicutes. The ratio between eutrophic and oligotrophic bacteria substantially increased. The micromorphology results showed that the microorga-nism-red mud aggregates were formed through adsorption, linkage, intertwinement and package between red mud particles, microbial cells and their metabolites. The red mud biotope changed spontaneously from extreme and oligotrophic into soil-like under natural stockpiling. The soil genesis process was mediated by microbes through increasing nutrient level, decreasing alkalinity and sali-nity, and improving soil structure.

摘要

土壤发生对于赤泥堆场的生态修复至关重要。通过分析赤泥物理化学和生物化学特性的变化,研究了赤泥的土壤发生过程及其微生物机制。我们采用时空替代法,分析了一个未经任何人为修复的赤泥堆场中的微生物群落结构。结果表明,随着堆放时间的增加,孔隙度、水稳性团聚体含量和平均重量直径等物理参数增加,而容重降低。包括pH值、电导率、酸中和能力和交换性钠百分比在内的化学参数随堆放时间的增加而降低。总有机碳、总氮、有效磷、微生物生物量碳和基础呼吸等生物化学参数增加,而代谢商降低。香农多样性指数增加,赤泥中的优势微生物群落从产氧光合细菌蓝细菌、厌氧不产氧光合细菌绿弯菌门和绿菌门转变为变形菌门、放线菌门和厚壁菌门。富营养细菌与贫营养细菌的比例大幅增加。微观形态学结果表明,微生物-赤泥团聚体是通过赤泥颗粒、微生物细胞及其代谢产物之间的吸附、连接、缠绕和包裹形成的。在自然堆放条件下,赤泥生物群落自发地从极端贫营养状态转变为类土壤状态。土壤发生过程是由微生物介导的,通过提高养分水平、降低碱度和盐度以及改善土壤结构来实现。

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