Elution of atrazine and metolachlor residues from a long-contaminated
soil under saturated flow was compared to elution of freshly-injected
compounds from the same soil. The mobility of the injected herbicide w
as far greater than the native. A two-compartment diffusion sorption m
odel-having a fast compartment S1 in rapid exchange with water and a s
low compartment S2 with exchange by radial diffusion kinetics-gave goo
d simultaneous fits to native and injected elution curves and predicte
d flow rate effects and postleaching soil herbicide profiles. An analo
gous model with first-order kinetics was less successful. The diffusio
n model parameters indicated that (i) at apparent equilibrium, the bul
k (82-92%) of the sorbate was in S2; (ii) the short-term (24-h) batch
partition coefficient greatly underestimates the apparent true value a
nd instead reflects partitioning into S1; and (iii) the time scale for
sorption is many months. The absence of particle-size size effects on
desorption rates suggests that the diffusive medium of S2 is micropar
ticles or microstructures (less-than-or-equal-to 1 mum) distributed am
ong all particle-size fractions.