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粪源大肠杆菌在河床沉积物中的存活:温度和沉积物特性的影响。

Survival of manure-borne E. coli in streambed sediment: effects of temperature and sediment properties.

机构信息

USDA-ARS Environmental Microbial and Food Safety Laboratory, BARC-EAST, U.S. Department of Agriculture, 10300 Baltimore Avenue, Beltsville, MD 20705, USA.

出版信息

Water Res. 2010 May;44(9):2753-62. doi: 10.1016/j.watres.2010.02.011. Epub 2010 Feb 13.

Abstract

Escherichia coli bacteria are commonly used as indicator organisms to designate of impaired surface waters and to guide the design of management practices to prevent fecal contamination of water. Stream sediments are known to serve as a reservoir and potential source of fecal bacteria (E. coli) for stream water. In agricultural watersheds, substantial numbers of E. coli may reach surface waters, and subsequently be deposited into sediments, along with fecal material in runoff from land-applied manures, grazing lands, or wildlife excreta. The objectives of this work were (a) to test the hypothesis that E. coli survival in streambed sediment in the presence of manure material will be affected by sediment texture and organic carbon content and (b) to evaluate applicability of the exponential die-off equation to the E. coli survival data in the presence of manure material. Experiments were conducted at three temperatures (4 degrees C, 14 degrees C, and 24 degrees C) in flow-through chambers using sediment from three locations at the Beaverdam Creek Tributary in Beltsville, Maryland mixed with dairy manure slurry in the proportion of 1000:1. Indigenous E. coli populations in sediments ranged from ca. 10(1) to 10(3)MPNg(-1) while approx 10(3) manure-borne E. coli MPNg(-1) were added. E. coli survived in sediments much longer than in the overlaying water. The exponential inactivation model gave an excellent approximation of data after 6-16 days from the beginning of the experiment. Slower inactivation was observed with the increase in organic carbon content in sediments with identical granulometric composition. The increase in the content of fine particles and organic carbon in sediments led not only to the slower inactivation but also to lower sensitivity of the inactivation to temperature. Streambed sediment properties have to be documented to better evaluate the role of sediments as reservoirs of E. coli that can affect microbiological stream water quality during high flow events.

摘要

大肠杆菌细菌通常被用作指示生物,以指示受损的地表水,并指导管理实践的设计,以防止粪便污染水。溪流沉积物已知是粪便细菌(大肠杆菌)的储存库和潜在来源,用于溪流水。在农业流域,大量的大肠杆菌可能会到达地表水,并随着粪便物质一起沉积到沉积物中,这些粪便物质是从土地施用的肥料、放牧地或野生动物排泄物中的径流中产生的。这项工作的目的是:(a) 测试假设,即在存在粪肥物质的情况下,大肠杆菌在河床沉积物中的存活将受到沉积物质地和有机碳含量的影响;(b) 评估指数衰减方程在存在粪肥物质的情况下对大肠杆菌存活数据的适用性。实验在三个温度(4°C、14°C 和 24°C)下进行,使用来自马里兰州贝尔茨维尔 Beaverdam Creek 支流的三个地点的沉积物,与 1000:1 的比例混合乳制品粪肥浆。沉积物中土著大肠杆菌种群的数量范围约为 10(1) 到 10(3)MPNg(-1),而添加的约 10(3)粪肥携带的大肠杆菌 MPNg(-1)。大肠杆菌在沉积物中的存活时间比在覆盖层水中长得多。指数失活模型在实验开始后 6-16 天对数据进行了很好的近似。在具有相同粒度组成的沉积物中,随着有机碳含量的增加,观察到失活速度变慢。沉积物中细颗粒和有机碳含量的增加不仅导致失活速度变慢,而且使失活对温度的敏感性降低。必须记录河床沉积物的特性,以更好地评估沉积物作为大肠杆菌储库的作用,这些大肠杆菌可能会在高流量事件期间影响微生物地表水水质。

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