Chemical exposure in flow-through sediment toxicity tests can vary
in time, between pore and overlying water, and amid free and bound
states, complicating the link between toxicity and observable concentrations
such as free pore (C
free,pore), free overlying
(C
free,over), or the corresponding dissolved
concentrations (C
diss, free + bound to
dissolved organic carbon, DOC). We introduce a numerical model that
describes the desorption from sediments to pore water, diffusion through
pores and the sediment–water boundary, DOC-mediated transport,
and mixing in and outflow from overlying water. The model explained
both the experimentally measured gap between C
free,over and C
free,pore and the
continuous decrease in overlying C
diss. Spatially resolved modeling suggested a steep concentration gradient
present in the upper millimeter of the sediment due to slow chemical
diffusion in sediment pores and fast outflux from the overlying water.
In contrast to continuous decrease in overlying C
diss expected for any chemical, C
free,over of highly hydrophobic chemicals was kept relatively
constant following desorption from DOC, a mechanism comparable to
passive dosing. Our mechanistic analyses emphasize that exposure will
depend on the chemical’s hydrophobicity, the test organism
habitat and uptake of bound chemicals, and the properties of sediment
components, including DOC. The model can help to re-evaluate existing
toxicity data, optimize experimental setups, and extrapolate laboratory
toxicity data to field exposure.