Yates M V, Ouyang Y
Department of Soil and Environmental Sciences, University of California, Riverside 92521.
Appl Environ Microbiol. 1992 May;58(5):1609-16. doi: 10.1128/aem.58.5.1609-1616.1992.
As a result of the recently proposed mandatory groundwater disinfection requirements to inactivate viruses in potable water supplies, there has been increasing interest in virus fate and transport in the subsurface. Several models have been developed to predict the fate of viruses in groundwater, but few include transport in the unsaturated zone and all require a constant virus inactivation rate. These are serious limitations in the models, as it has been well documented that considerable virus removal occurs in the unsaturated zone and that the inactivation rate of viruses is dependent on environmental conditions. The purpose of this research was to develop a predictive model of virus fate and transport in unsaturated soils that allows the virus inactivation rate to vary on the basis of changes in soil temperature. The model was developed on the basis of the law of mass conservation of a contaminant in porous media and couples the flows of water, viruses, and heat through the soil. Model predictions were compared with measured data of virus transport in laboratory column studies and, with the exception of one point, were within the 95% confidence limits of the measured concentrations. The model should be a useful tool for anyone wishing to estimate the number of viruses entering groundwater after traveling through the soil from a contamination source. In addition, model simulations were performed to identify parameters that have a large effect on the results. This information can be used to help design experiments so that important variables are measured accurately.
由于最近提出了对饮用水供应中的病毒进行灭活的强制性地下水消毒要求,人们对病毒在地下的归宿和运移越来越感兴趣。已经开发了几种模型来预测病毒在地下水中的归宿,但很少有模型考虑病毒在非饱和带中的运移,并且所有模型都要求病毒灭活速率恒定。这些都是模型中的严重局限性,因为已有充分记录表明,在非饱和带中会发生大量病毒去除,而且病毒的灭活速率取决于环境条件。本研究的目的是开发一种非饱和土壤中病毒归宿和运移的预测模型,该模型允许病毒灭活速率根据土壤温度变化而变化。该模型是基于多孔介质中污染物的质量守恒定律开发的,并将水、病毒和热量在土壤中的流动耦合起来。将模型预测结果与实验室柱实验中病毒运移的实测数据进行了比较,除了一个点外,预测结果均在实测浓度的95%置信区间内。该模型对于任何希望估算病毒从污染源穿过土壤后进入地下水数量的人来说都应该是一个有用的工具。此外,还进行了模型模拟以识别对结果有重大影响的参数。这些信息可用于帮助设计实验,以便准确测量重要变量。