A model has been developed to simulate the dynamics of decomposers and substrates in grasslands. Sub~trates r~presented are humic material, feces, and dead plant and animal remains. Exc~pt for humic ma~enal, sub_strates are fur!her divid_ed _into a rapidly and a slowly decomposing f~actwn. The proportiOn of rapidly decomposmg matenal m a substrate is predicted from its initial mtroge_n content. The bel_owground P?r~ion of ~he system is divided into layers because temperature and soil water.' the most Important dnvmg vanables for the model, vary with depth. Decomposition rates are pr~dicted from temperature, water tension, and inorganic nitrogen concentration.T~xon?mic groups o~ decomposers are not distinguished, but a distinction is made between active an~ m_active states, which differ in respiration rate, in death rate, and in that only active decomposers assimilate substrate.The model's pre~ictions comp~re favora~ly t? data on COz evolution and to litter bag experiments, but not to ATP esti~ates of active microbial biOmass. The model indicates a profound influence of depth o~ _decompositiOn rates and on decomposer biomass dynamics, growth yield, and secondary productivity.