Cf. Benson et Rs. Bowman, TRI-FLUOROBENZOATES AND TETRAFLUOROBENZOATES AS NONREACTIVE TRACERS IN SOIL AND GROUNDWATER, Soil Science Society of America journal, 58(4), 1994, pp. 1123-1129
Several fluorinated derivatives of benzoic acid (fluorobenzoate, FBA)
have proven their usefulness as nonreactive soil and groundwater trace
rs. In this study, four previously untested trifluorobenzoates (TFBA)
and two tetrafluorobenzoates (TEFBA) were examined for their suitabili
ty as water tracers in saturated and unsaturated environments. Negativ
e log acid dissociation constants (pK(a)) determined by base titration
ranged from 2.71 to 3.54 at 298 K. Some sorption of FBAs was observed
in batch equilibration experiments with lower pH, high organic C frac
tion soils. An algorithm was developed for calculating a linear partit
ion coefficient (K(D)) for each FBA isomer based on pK(a), soil organi
c C, pH, and an average organic C-based partition coefficient for prot
onated FBA (K(OC)). K(OC)* was estimated to be 18 200 +/- 6 300 L kg-
1 when total FBA solution concentration is less than 5 mg L-1. Column
mobility experiments in sandy media under saturated and unsaturated co
nditions yielded breakthrough curves for TFBA and TEFBA isomers that w
ere indistinguishable from Br-. The results presented herein suggest t
hat all 16 ring-substituted FBAs can serve as nonreactive water tracer
s.