To accurately examine the mechanisms that control virus retention and trans
port in porous media, it is essential to perform experiments under environm
entally relevant conditions. Laboratory studies of virus transport are gene
rally conducted using buffered solutions. However, there are no standards f
or the concentration and composition of the solution, making comparisons be
tween different studies difficult. Our objective was to systematically inve
stigate the effects of the ionic strength and composition of buffer solutio
ns on adsorption of viruses during transport through saturated sand columns
. Two phosphate buffered saline solutions (PBS and PBS2) and one artificial
ground water (AGW) were used and experiments were conducted under saturate
d, steady state flow conditions. Bromide tracer and bacteriophages phi X174
and MS-2 were introduced into saturated sand columns as step inputs and th
eir concentrations in the outflow samples were determined. Change in ionic
strength did not affect the behavior of phi X174, whereas MS-2 was largely
removed in the high ionic strength PBS buffer (0.16 M) but moved through th
e columns in the low ionic strength PBS2 and AGW buffers (0.002 M), An addi
tional experiment conducted under an ionic strength gradient (from 0.002 to
0.2 M) using PBS indicated that the outflow concentration of MS-2 decrease
d slowly from an ionic strength of similar to 0.03 M, reached a minimum at
an apparent critical value of similar to 0.1 M, and then increased graduall
y. This study also suggests that metals or metal oxides on sand surfaces ca
n cause significant virus removal under high ionic strength conditions.