Six anions which showed potential as tracers of soil water movement were evaluated in laboratory and field experiments. The anions included iodide (I ‐ ), thiocyanate (SCN ‐ ), and four fluorobenzoates: m ‐(trifluoromethyl)benzoic acid ( m ‐TFMBA), o ‐(trifluoromethyl)benzoic acid ( o ‐TFMBA), pentafluorobenzoic acid (PFBA) and 2,6‐difluorobenzoic acid (2,6‐DFBA). The sorption and mobility characteristics of the six potential tracers were compared to those of bromide (Br ‐ ), which served as an index tracer in all experiments. Initial tracer concentrations ranged from 20 to 100 mg L −1 . The anions were quantified simultaneously in sub‐mL samples of soil solution using a high performance liquid chromatography technique. Batch equilibrations (28 d), and breakthrough curves (7 to 10 d) in a 2.5‐m column of loamy sand, under both ponded and trickle‐irrigated conditions, indicated that all the tracers except SCN ‐ were conservative and were not sorbed. SCN ‐ was not retarded in the column studies but did show a negative mass balance, most likely due to chemical and/or biological transformation. Distribution of a tracer solution applied to a field soil was monitored for 69 d in soil water from suction samplers (1.0‐ and 1.8‐m depth) and in extracts from core samples. SCN ‐ , I ‐ , and m ‐TFMBA showed reduced concentrations relative to Br ‐ at all sampling times and depths; o ‐TFMBA, PFBA, and 2,6‐DFBA had distributions similar to that of Br ‐ . These latter three fluorobenzoates show promise as laboratory and field tracers of soil water, particularly where multiple tracing tests or totally exotic tracers are required.
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Robert S. Bowman (1984) studied this question.