To assess the impact of microbial metabolism of the organic substituents of low level radioactive wastes on radionuclide mobility in disposal sites, the nature of the microbial transformations involved in this metabolism and the effect of the prevailing environmental parameters on the quantities and types of metabolic intermediates accumulated were examined. Since both aerobic and anaerobic periods can occur during trench ecosystem development, oxidation capacities of the microbial community in the presence and absence of oxygen were analyzed. Results of gas studies performed at three commercial low level radioactive waste disposal sites were reviewed. Several deficiencies in available data were determined. Further research needs are suggested. The predominant microbial transformations involved with organic matter decomposition processes in the low-level radioactive waste disposal trench are anaerobic, i.e., they occur in the absence of molecular oxygen. This conclusion is supported by detection of methane gas evolution from trench sites, by the nature of the organic substances accumulated in trench waters, and by analysis of trench construction procedures. Methane is only synthesized biologically under extremely reducing (anaerobic) atmospheres. Placement of the trench within the soil profile and, in many cases, the water saturated conditions existent within the trench cavity, preclude significant oxygen diffusion to the active microbial communities. Major metabolic products detected in trench waters result from fermentation, anaerobic respiration, and 6-oxidation of various waste components. These reactions yield organic acids, alcohols, etc. Under proper conditions, the organic acids serve as substrates for methane and carbon dioxide synthesis. Actually, because of the heterogeneous placements of waste materials within the trench, methane may be the terminal metabolic product at one site, while organic acids accumulate at an adjacent site within the same trench. Thus, significant quantities of organic acids are detected in trench waters collected from a methane producing site. This results from the localized occurrence of conditions inhibitory to methane synthesis. At sites which vn are not water saturated, conditions may not be favorable for significant methane synthesis. The terminal metabolic products would then be organic acids and amines. These products, under proper conditions, may transport nuclides from the site in trench gases or drainage waters. The majority of the water-soluble organic compounds detected in trench waters are postulated to be products of anaerobic metabolic processes. These include several straight and branched chain organic acids. The aromatic acids found in trench waters may originate in the primary waste material or be formed by partial metabolism of more complex aromatic compounds. The aromatic nuclei of these compounds accumulate in the waters due to their relative biodegradation resistance under anaerobic conditions. Other organic compounds which are recalcitrant in the anaerob...