Phosphorus-31 nuclear magnetic resonance (31P NMR) was used to follow the decomposition of chlorpyrifos (an organothiophosphate pesticide) adsorbed on soil, humic acid, partially hydrated kaolin clay, and partially hydrated montmorillonite clay at high concentration (typically 2-10 wt %). Solid-state 31P NMR (using magic-angle spinning and cross polarization or direct polarization) and liquid-solution 31P NMR of DMSO and acetone extracts indicate that chlorpyrifos is initially physisorbed, appearing by solid-state 31P NMR to exhibit significant motion on the molecular level, which results in almost liquidlike solid-state spectra. Over periods ranging from hours to years, the signals due to unreacted chlorpyrifos sorbed on the clays diminish and are replaced by new 31P NMR peaks resulting from hydrolysis, isomerization, mineralization, and oxidation reactions. The 31P NMR signal characteristics indicate that these decomposition products are much more tightly bound to the clay than is chlorpyrifos. Solid-state 13C and 27AI NMR spectra were less useful for following the decomposition of chlorpyrifos than those obtained by 31P NMR. Solid-state 31P NMR results indicate that a chlorpyrifos loading level of 10% by weight, used in some of the samples to facilitate 31P NMR detection of less-than-dominant decomposition products, exceeds the adsorption capacity of the soil, humic acid, and kaolinite tested, but not Ca2+ -exchanged montmorillonite. This pattern is consistent with intercalation into the montmorillonite, but only surface adsorption on kaolinite.