Laboratory studies were conducted to evaluate flumetsulam adsorption a
nd mobility in seven Mississippi soils of different organic matter con
tent, pH, and texture. Adsorption isotherms were determined for all so
ils using a 1:1 (soil:water) technique. In six of seven soils, Freundl
ich n constants were close to unity, suggesting a partitioning-like ad
sorption mechanism for flumetsulam. Mobility was examined using packed
soil columns. C-14-flumetsulam recoveries in leachate ranged from 1 t
o 70% and were influenced by both organic matter content and soil pH.
However, the effects of organic matter content and soil pH were not in
dependent. Consequently, clear relationships between flumetsulam mobil
ity and either organic matter content or soil pH were not established
across all soils. However, among soils of similar pH (7.5 +/- 0.3), mo
bility decreased linearly (R-2 = 0.75) as organic matter content incre
ased from 0.7 to 3.6%. Across soils with similar organic matter conten
t (3.9 +/- 0.3%), mobility increased linearly (R-2 = 0.98) as soil pH
increased from 5.3 to 7.2. Net adsorption constants (K-d) provided a m
ore accurate assessment of flumetsulam mobility across all soils than
K-oc.