Expert Centre for Methodology and Information Services, National Institute of Public Health and the Environment (RIVM), P.O. Box 1, 3720 BA Bilthoven, The Netherlands.
Water Res. 2010 Feb;44(4):1170-81. doi: 10.1016/j.watres.2010.01.002. Epub 2010 Jan 15.
An empirical formula was developed for determining the vulnerability of unconfined sandy aquifers to virus contamination, expressed as a dimensionless setback distance r(s)(*). The formula can be used to calculate the setback distance required for the protection of drinking water production wells against virus contamination. This empirical formula takes into account the intrinsic properties of the virus and the unconfined sandy aquifer. Virus removal is described by a rate coefficient that accounts for virus inactivation and attachment to sand grains. The formula also includes pumping rate, saturated thickness of the aquifer, depth of the screen of the pumping well, and anisotropy of the aquifer. This means that it accounts also for dilution effects as well as horizontal and vertical virus transport. Because the empirical model includes virus source concentration it can be used as an integral part of a quantitative viral risk assessment.
开发了一个经验公式来确定无约束砂含水层对病毒污染的脆弱性,用无量纲的后退距离 r(s)(*)来表示。该公式可用于计算保护饮用水生产井免受病毒污染所需的后退距离。该经验公式考虑了病毒和无约束砂含水层的固有特性。病毒去除由一个速率系数来描述,该系数考虑了病毒失活和附着在砂粒上的作用。该公式还包括抽水泵率、含水层的饱和厚度、抽水井的筛管深度以及含水层的各向异性。这意味着它还考虑了稀释效应以及水平和垂直的病毒迁移。由于经验模型包括病毒源浓度,因此它可以用作定量病毒风险评估的一个组成部分。