The chemical containment effectiveness of both the natural recovery and the
"particle broadcasting" processes for remediating contaminated bed-sedimen
ts depend upon very, thin soil and/or sand layers millimeters in depth. Con
ventional capping for in situ chemical containment of bed-sediment or dredg
ed material typically involves thick layers of 30 to 90 centimeters in dept
h. Few, studies have been conducted with thin layers of candidate natural m
aterials. A steady-state benzoic acid dissolution test apparatus and proced
ure, devised to realistically simulate bed-sediment chemodynamic conditions
, was used to measure chemical flux through thin layers (I to 8 nim) of soi
l, sand, and ideal porous media. The thin layers were found to be very effe
ctive. Flux reductions ranged from 81 to 96%, with fine sand being slightly
better than top soil. Design algorithms developed for the thick layers use
d in conventional capping design will underpredict the flux through very, t
hin layers. Advective flow, induced by, surface roughness is proposed to ex
plain the higher average measured-to-predicted flux ratio of 1.67.