Thorium has been frequently used as a tracer of particulate carbon removal
from the ocean surface mixed layers. Although coagulation is known to be im
portant in the process, models used to interpret measurements have been lim
ited to simple descriptions of coagulation. We present results from a coupl
ed adsorption-aggregation model for Th-234 scavenging. The aggregation comp
onent models the particle size spectrum from colloidal particles to particl
es of about 100 mu m in size and incorporates details of the physical mecha
nisms that bring particles together. We make comparisons between an adsorpt
ion model that has a constant mass specific adsorption rate and one that is
purely transport limited, the former of which is shown to be unphysical fo
r larger particles. The combined model reproduces the observed inverse depe
ndence of POC/Th-234 On particle size. Comparison with observational result
s is made by simulating a series of filtrations using the model results. Th
e filtered values are determined by the maximum of the particle distributio
n within the relevant size range, and consequently affect the comparison be
tween observed values and model output. This stresses the importance of the
particle size spectrum in the scavenging process and suggests that measure
ments using more particle size classes should be made to accurately determi
ne kinetic rates. (C) 1999 Elsevier Science Ltd. All rights reserved.