Poliovirus and reovirus were found to aggregate into clumps of up to several hundred particles when diluted 10-fold into distilled water from a stock preparation of minimal aggregation in 0.05 M phosphate buffer, pH 7.2, plus 22 to 30% sucrose. Reovirus was also found to aggregate when diluted into phosphatebuffered saline. The aggregation was concentration dependent and did not occur when either virus was diluted into water 100-fold or greater. The aggregation of poliovirus was reversible by further addition of saline and produced a dispersed preparation of virus. Reovirus aggregation was not reversible. Both viruses aggregated when diluted into buffers at pH 5 and 3, and poliovirus aggregated at pH 6, and this aggregation of both viruses was reversible when returned to pH 7. Aggregation did not occur at alkaline pH values. Aggregation at low pH could be prevented by suitable concentrations of sodium or magnesium ions, but neither caused aggregation of either virus at pH 7. Calcium ions, however, were found to aggregate both viruses at a concentration of 0.01 M.

No abstract

Quantitative electron microscopy shows that Freon-extracted poliovirus, velocity banded in a sucrose gradient, contains over 95% single particles. This well-dispersed virus reacts quite rapidly with bromine in turbulent flowing water, losing plaque titer at the rate of one log,,, unit in 10 s at pH 7, 2 C, and at a bromine concentration of 2.2 ,uM. At 10 and 20 C the rate of disinfection (log,,, plaque-forming units per second) is faster, and at both temperatures it increases in approximately linear fashion with increasing bromine concentration. At 2 C such a linear relationship is not observed.

As a first step toward the understanding of virus particle interactions in water, we have used the modified single particle analysis test to follow the aggregation of poliovirus and reovirus as induced by low pH in suspensions containing varying amounts of dissolved salts. Salts composed of mono-, di-, and trivalent cations and mono-and divalent anions were tested for their ability to reduce or increase the aggregation of these viruses in relation to that obtained by low pH alone. Mono-and divalent cations in concentrations covering those in natural waters were generally found to cause a decrease in aggregation, with the divalent cations having a much greater effectiveness than the monovalent cations. Trivalent ions (A13+), in micromolar concentrations, were found to cause aggregation over that at low pH alone. Anions, whether monovalent or divalent, had little ability to produce inhibition of viral aggregation, and thus the overall effects were due almost exclusively to the cation. This was true regardless of whether the overall charge on the virus particle was positive or negative, as determined by the relation between the isoelectric point and the pH at which the tests were carried out. Thus, whereas virus particles conform to classical colloid theory in many respects, there are specific exceptions which must be taken into account in the design of any experiment in which viral aggregation is a factor.

An apparatus is described for precise observation of the kinetics of the initial fast reaction of bromine with reovirus in turbulent flowing water. When quantitative electron microscopy shows that virus suspensions are essentially all single particles, the loss of infectivity follows first-order kinetics, the plaque titer falling at the rate of 3 log,,, units/s at pH 7, 2 C, and at a 3-AM bromine concentration. Virus suspensions containing small aggregates (2 to 10/clump) exhibit a constantly decreasing disinfection rate with bromine. At a survival level of 10-3 for single virions, the aggregated preparations have lost only 99% of their plaque titer and 10-4 is reached only after 4 s of exposure. The disinfection rate does not appear to be a simple function of the size and frequency of aggregates in the virus suspension even when the aggregates contain no foreign material. Unpurified virus preparations (crude freeze-thaw lysates of infected cells) are shown, by zonal centrifugation, to contain 50% to over 90% of the infectivity in large, fast sedimenting aggregates. Such aggregates would strongly influence the bromine resistance of virus in polluted water.