Enrichment cultures obtained from soil exposed to benzene, toluene, and xyl
ene (BTX) mineralized benzene and toluene but cometabolized only xylene iso
mers, forming polymeric residues, This observation prompted us to investiga
te the metabolism of C-14-labeled BTX hydrocarbons in sail, either individu
ally or as mixtures. BTX-supplemented soil was incubated aerobically for up
to 4 weeks in a sealed system that automatically replenished any O-2 consu
med, The decrease in solvent vapors and the production of (CO2)-C-14 were m
onitored. At the conclusion of each experiment, C-14 distribution in solven
t-extractable polymers, biomass, and humic material was determined, obtaini
ng C-14 mass balances of 85 to 98%, BTX compounds were extensively minerali
zed in soil, regardless of whether they were presented singly or in combina
tions. No evidence aas obtained for the formation of solvent-extractable po
lymers from xylenes in soil, but C-14 distribution in biomass (5 to 10%) an
d humus (12 to 32%) was unusual for all BTX compounds and especially for to
luene and the xylenes, The results suggest that catechol intermediates of B
TX degradation are preferentially polymerized into the soil humus and that
the methyl substituents of the catechols derived from toluene and especiall
y from xylenes enhance this incorporation. In contrast to inhibitory residu
es formed from xylene cometabolism in culture, the humus-incorporated xylen
e residues showed no significant toxicity in the Microtox assay.