The mobility and ecology of viruses in natural environments is strongl
y influenced by the adsorption of virus particles to sand or soil surf
aces. This binding process is frequently studied by conducting batch e
xperiments in which fluid suspensions of virus particles are contacted
with the adsorbent of interest. In this report, a simple first-order
kinetic theory is presented which accounts for many of the complicated
interactions that can occur when viruses contact an adsorbent in a ba
tch system. Closed-form solutions and numerical simulations of the mod
el indicate that four classes of virus-surface interactions can be ide
ntified, including quasi-equilibrium adsorption, quasi-equilibrium ads
orption with surface sinks, quasi-equilibrium adsorption with reduced
inactivation, and direct irreversible adsorption. Based on these resul
ts, a new experimental approach for studying virus-surface interaction
s is proposed and tested using a model system consisting of bacterioph
age lambda and Ottawa sand. Fluid samples were collected from sand-con
taining and sand-free virus suspensions over the course of 5-6 days an
d analyzed for plaque forming units (PFU). These experiments were repe
ated using three different pH values and six different electrolyte com
positions. Nondimensionalization of the PFU data from the sand-free su
spension collapsed all of the data onto a single fine, as predicted by
the kinetic model. When plotted in a nondimensional format, data from
the sand-containing suspensions exhibited behavior which could readil
y be interpreted within the context of the kinetic model. These result
s suggest that the proposed approach offers a powerful alternative to
conventional methods for studying virus adsorption at the solid-liquid
interface, and for predicting the potential mobility and fate of viru
ses in porous media.