To more fully understand the potential for transport of nitroaromatic compo
unds in soils and subsoils,the adsorption of a series of para- and meta-sub
stituted nitrobenzenes (SNBs) by K-smectite clay was measured. Adsorption i
sotherms were fit to the Freundlich equation, and the resultant Freundlich
adsorption coefficients (log(K-f)) were positively correlated with the Hamm
ett substituent constant (r(2) = 0.80). This relationship and a positive re
action constant (rho = 1.15) indicate that the adsorption reaction is favor
ed by electron-withdrawing substituents. These results are consistent with
an electron donor (smectite)-acceptor (substituted nitrobenzene) mechanism
offered previously. However, quantum calculations did not reveal any system
atic relationship between the Hammett constant and the electron density on
the aromatic ring, which would explain a donor-acceptor relationship. Rathe
r, electron density donated by a second substituent on nitrobenzene appears
to be appropriated by the nitro group leaving ring electron density unchan
ged. Fourier transform infrared spectroscopy revealed shifts in the -NO2 vi
brational modes of 1,3,5-trinitrobenzene (TNB) upon adsorption to K+-smecti
te that were consistent with the complexation of K+ by -NO2 groups. Such TN
B vibrational shifts were not observed for SWy-1 saturated with more strong
ly hydrated cations (i.e., Na+, Mg2+, Ca2+, and Ba2+). The simultaneous int
eraction of multiple -NO2 groups with exchangeable K+ was indicated by mole
cular dynamic simulations. Adsorption of SNBs by smectite clays appears to
result from the additive interactions of -NO2 groups and secondary substitu
ents with interlayer K+ ions. Adsorption occurs to a greater or lesser exte
nt depending on the abilities of substituents to complex additional interla
yer cations and the water solubilities of SNBs. We conclude that the adsorp
tion trends of SNBs on K-SAz-1 can be explained without recourse to hypothe
tical electron donor-acceptor complexes.