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Modification of Spatial Distribution of 24-Dichlorophenoxyacetic Acid Degrader Microhabitats during Growth in Soil Columns

机译:土壤柱生长过程中24-二氯苯氧基乙酸降解物微生境的空间分布变化

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摘要

Bacterial processes in soil, including biodegradation, require contact between bacteria and substrates. Knowledge of the three-dimensional spatial distribution of bacteria at the microscale is necessary to understand and predict such processes. Using a soil microsampling strategy combined with a mathematical spatial analysis, we studied the spatial distribution of 2,4-dichlorophenoxyacetic acid (2,4-D) degrader microhabitats as a function of 2,4-D degrader abundance. Soil columns that allowed natural flow were percolated with 2,4-D to increase the 2,4-D degrader abundance. Hundreds of soil microsamples (minimum diameter, 125 μm) were collected and transferred to culture medium to check for the presence of 2,4-D degraders. Spatial distributions of bacterial microhabitats were characterized by determining the average size of colonized soil patches and the average number of patches per gram of soil. The spatial distribution of 2,4-D degrader microhabitats was not affected by water flow, but there was an overall increase in colonized patch sizes after 2,4-D amendment; colonized microsamples were dispersed in the soil at low 2,4-D degrader densities and clustered in patches that were more than 0.5 mm in diameter at higher densities. During growth, spreading of 2,4-D degraders within the soil and an increase in 2,4-D degradation were observed. We hypothesized that spreading of the bacteria increased the probability of encounters with 2,4-D and resulted in better interception of the degradable substrate. This work showed that characterization of bacterial microscale spatial distribution is relevant to microbial ecology studies. It improved quantitative bacterial microhabitat description and suggested that sporadic movement of cells occurs. Furthermore, it offered perspectives for linking microbial function to the soil physicochemical environment.
机译:土壤中的细菌过程,包括生物降解,都需要细菌与基质之间的接触。要了解和预测此类过程,必须了解细菌在三维上的三维空间分布。使用土壤微量采样策略并结合数学空间分析,我们研究了2,4-二氯苯氧基乙酸(2,4-D)降解菌微生境的空间分布,该空间分布是2,4-D降解菌丰度的函数。允许自然流动的土壤柱被2,4-D浸透,以增加2,4-D降解物的含量。收集了数百个土壤微型样品(最小直径为125μm),并转移到培养基中以检查是否存在2,4-D降解剂。通过确定定殖的土壤斑块的平均大小和每克土壤的斑块的平均数目来表征细菌微生境的空间分布。 2,4-D降解菌微生境的空间分布不受水流的影响,但是2,4-D修饰后定居斑块的大小总体增加。定殖的微量样品以低的2,4-D降解剂密度分散在土壤中,并以较高的密度聚集在直径大于0.5 mm的斑块中。在生长过程中,观察到2,4-D降解剂在土壤中的扩散和2,4-D降解的增加。我们假设细菌的传播增加了与2,4-D接触的可能性,并导致了对可降解底物的更好拦截。这项工作表明,细菌的微观空间分布特征与微生物生态学研究有关。它改善了定量细菌微生境描述,并提示细胞会发生零星运动。此外,它为将微生物功能与土壤物理化学环境联系在一起提供了前景。

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