The concentrations of trichloroacetic acid (TCAA) in soil and of chlorinate
d solvents in soil air from simultaneously taken samples from four sites ar
e presented. The data show that there is a significant positive correlation
between the concentrations of TCAA and chloroform - but not between TCAA a
nd other chlorinated solvents - in soil. The calculated half-life of TCAA s
hows that the contribution of decarboxylation to the chloroform concentrati
on in soil is negligible. Since TCAA and chloroform were found to be formed
from humic acids in the chloroperoxidase (CPO)-mediated reaction and CPO a
ctivity has been detected in soil, the observed correlation between the con
centrations of TCAA and chloroform provides novel support for the hypothesi
s that TCAA is formed naturally in soil. (C) 1999 Elsevier Science Ltd. All
rights reserved.