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病毒在饱和流和非饱和流状态下在土壤中的移动。

Virus movement in soil during saturated and unsaturated flow.

作者信息

Lance J C, Gerba C P

出版信息

Appl Environ Microbiol. 1984 Feb;47(2):335-7. doi: 10.1128/aem.47.2.335-337.1984.

Abstract

Virus movement in soil during saturated and unsaturated flow was compared by adding poliovirus to sewage water and applying the water at different rates to a 250-cm-long soil column equipped with ceramic samplers at different depths. Movement of viruses during unsaturated flow of sewage through soil columns was much less than during saturated flow. Viruses did not move below the 40-cm level when sewage water was applied at less than the maximum infiltration rate; virus penetration in columns flooded with sewage was at least 160 cm. Therefore, virus movement in soils irrigated with sewage should be less than in flooded groundwater recharge basins or in saturated soil columns. Management of land treatment systems to provide unsaturated flow through the soil should minimize the depth of virus penetration. Differences in virus movement during saturated and unsaturated flow must be considered in the development of any model used to simulate virus movement in soils.

摘要

通过将脊髓灰质炎病毒添加到污水中,并以不同速率将污水施用于一个250厘米长、在不同深度配备陶瓷采样器的土柱,比较了饱和流和非饱和流期间病毒在土壤中的移动情况。污水在土柱中进行非饱和流时病毒的移动量远小于饱和流时。当污水施用量小于最大入渗速率时,病毒不会移动到40厘米以下的深度;用污水淹没的土柱中病毒渗透深度至少为160厘米。因此,用污水灌溉的土壤中病毒的移动量应小于在淹没式地下水回灌盆地或饱和土柱中的移动量。对土地处理系统进行管理,以使污水通过土壤进行非饱和流,应能将病毒渗透深度降至最低。在开发用于模拟土壤中病毒移动的任何模型时,都必须考虑饱和流和非饱和流期间病毒移动的差异。

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本文引用的文献

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