1989
DOI: 10.1016/0043-1354(89)90095-x
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Survival of viruses in groundwater

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Cited by 41 publications
(39 citation statements)
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“…Based on our experimental analysis and previous reports in the literature (15,24,25,56), first-order kinetics of viral infectivity reduction was assumed. Plaque assay-based infectivity reduction rates (log 10 PFU/day) were obtained for all virus-seeded samples.…”
Section: Resultsmentioning
confidence: 99%
“…Based on our experimental analysis and previous reports in the literature (15,24,25,56), first-order kinetics of viral infectivity reduction was assumed. Plaque assay-based infectivity reduction rates (log 10 PFU/day) were obtained for all virus-seeded samples.…”
Section: Resultsmentioning
confidence: 99%
“…Penetration to depths as great as 67 m and horizontal migration as far as 408 m in glacial till and 1,600 m in fractured limestone have been reported (38,50). Viruses can persist for several months in soils and groundwater when temperatures are low and soils are moist (35,50,58,65). Enteric viruses are shed in enormous quantities in feces (10 9 to 10 10 /g) and have an infectious dose on the order of tens to hundreds of virions (23,44), so that even an 8-log reduction in virus concentration during transport could still result in infectious virus present in potable groundwater.…”
mentioning
confidence: 99%
“…Temperature is the most important factor that influences virus inactivation (Hurst et al,1980;Yates et al, 1985Yates et al, , 1987. Inactivation rates increase with temperature (Hurst et al, 1980;Yates et al, 1985;Jansons et al, 1989;Nasser et al, 1993;Yahya et al, 1993;Blanc and Nasser, 1996). (2000) compared the dependence of the inactivation rate coefficient on temperature for a number of bacteriophages, using data from several studies.…”
Section: Inactivation a Virus Inactivation During Saturated Subsurfamentioning
confidence: 98%