Experimental measurements of the adsorption of linear alkylbenzene sul
fonate (LAS) on soils were made at 25 degrees C using a continuous ads
orption apparatus. The adsorption of LAS on natural soils could be div
ided into two stages: linear and exponentially increasing isotherms. A
t low LAS concentration (<90 mu g ml(-1)), the adsorption isotherms we
re linear and Kd was among 1.2 to 2.0. At high LAS levels (>90 mu g ml
(-1)), cooperative adsorption was observed and the adsorption amount o
f LAS increased exponentially with the increasing of LAS concentration
in solution. LAS adsorption mechanisms on soil were mainly specific s
ire surface interactions and hydrogen bonding; The LAS adsorption capa
city of a soil significantly depended on its physical clay content. Un
der real soil environments where LAS levels are rather low, the LAS ad
sorption ability of a soil is very weak.