Field and laboratory investigations of inactivation of viruses (PRD1 and MS2) attached to iron oxide-coated quartz sand

被引:118
作者
Ryan, JN [1 ]
Harvey, RW
Metge, D
Elimelech, M
Navigato, T
Pieper, AP
机构
[1] Univ Colorado, Dept Civil Environm & Architectural Engn, Boulder, CO 80309 USA
[2] US Geol Survey, Div Water Resources, Boulder, CO 80303 USA
[3] Yale Univ, Dept Chem Engn, Environm Engn Program, New Haven, CT 06520 USA
关键词
D O I
10.1021/es011285y
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Field and laboratory experiments were conducted to investigate inactivation of viruses attached to mineral surfaces. In a natural gradient transport field experiment, bacteriophage PRD1, radiolabeled with (32)p, Was injected into a ferric oxyhydroxide-coated sand aquifer with bromide and linear alkylbenzene sulfonates. In a zone of the aquifer contaminated by secondary sewage infiltration, small fractions of infective and P-32-labeled PRD1 broke through with the bromide tracer, followed by the slow release of 84% of the P-32 activity and only 0.011% of the infective PRDI. In the laboratory experiments, the inactivation of PRDI, labeled with 35S (protein capsid), and MS2, dual radiolabeled with 35S (protein capsid) and 32p (nucleic acid), was monitored in the presence of groundwater and sediment from the contaminated zone of the field site. Release of infective viruses decreased at a much faster rate than release of the radiolabels, indicating that attached viruses were undergoing surface inactivation. Disparities between P-32 and (35) S release suggest that the inactivated viruses were released in a disintegrated state. Comparison of estimated solution and surface inactivation rates indicates solution inactivation is similar to3 times as fast as surface inactivation. The actual rate of surface inactivation may be substantially underestimated owing to slow release of inactivated viruses.
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页码:2403 / 2413
页数:11
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