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Association of Fecal Coliforms With Soil Aggregates: Effect of Water Content and Bovine Manure Application

机译:粪大肠菌群与土壤团聚体的关系:水分和牛粪施用的影响

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Manure-borne microorganisms and organic particles can move in soils in large interconnected pores or in long macropores. These pathways in structured soils are located between soil aggregates or peds. Therefore, interaction with soil aggregates may substantially affect the ability of macropores to serve as bacterial conduits.The study tested the hypothesis that fecal coliform, (FC) association with soil aggregates is affected by aggregate size, water content, and bovine manure application.Tyler loam soil aggregates were separated into three fractions. Air-dried and water-saturated aggregates were submerged in water-FC and water-manure-FC suspensions with concentrations of 10(3), 10(4), or 10(5) CFU mL(-1) for 24 h. The maximum association of FC with aggregates was observed in the experiments with air-dried aggregates in the water-FC suspensions; no measurable FC amount was associated with the saturated aggregates in the same suspension. In the water-manure-FC Suspension, about 2.5 times more FC were associated with the air-dried soil aggregates than with the water-saturated aggregates. The FC amount associated with air-dried aggregates in the water-manure-FC suspension was about 300 times less compared with the amount in the water-FC suspension. The FC association with the aggregates was not affected by aggregate size. Increased water content of soil aggregates and presence of manure in water-FC suspensions decreased FC association with soil aggregates. Because FC transport in soil generally occurs through interaggregate pores after rainfalls after manure applications, a decrease in bacteria-soil association with aggregates can enhance bacterial mobility and increase risk of groundwater contamination.
机译:粪便传播的微生物和有机颗粒可以在相互连通的大孔隙或长大孔中的土壤中移动。结构化土壤中的这些途径位于土壤聚集体或土壤之间。因此,与土壤团聚体的相互作用可能会大大影响大孔作为细菌管道的能力。这项研究检验了以下假设:粪便大肠菌群(FC)与土壤团聚体的结合受团粒大小,含水量和牛粪肥施用的影响。壤土的土壤聚集体分为三个部分。将风干和水饱和的骨料浸入浓度为10(3),10(4)或10(5)CFU mL(-1)的水-FC和水-粪肥-FC悬浮液中24小时。在水-FC悬浮液中风干的骨料的实验中,观察到了FC与骨料的最大关联。在同一悬浮液中,没有可测量的FC量与饱和骨料相关联。在水肥FC悬浮液中,风干土壤团聚体的FC含量是水饱和团聚体的2.5倍。与水肥FC悬浮液中的风干骨料相关的FC量比水FC悬浮液中的FC量少约300倍。 FC与聚集体的关联不受聚集体大小的影响。土壤团聚体中水分含量的增加和水-FC悬浮液中粪便的存在降低了FC与土壤团聚体的缔合。由于FC在土壤中的运输通常通过施用肥料后的降雨后通过集聚体的孔隙发生,因此细菌-土壤与集聚体的缔合减少会增强细菌的活动性并增加地下水污染的风险。

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