Environmental conditions which define boundaries for biofilm production could provide useful ecological information for biofilm models. A practical use of defined conditions could be applied to the high-level nuclear waste repository at Yucca Mountain. Data for temperature and humidity conditions indicate that decreases in relative humidity or increased temperature severely affect biofilm formation on three candidate canister metals.Biofilms create microenvironments for a consortium of bacteria residing on a substrate. These microenvironments include variations in pH, nutrient concentrations, and oxygen levels (17, 24). On a surface such as metal, biofilms allow for a variety of microorganisms with differing redox potential requirements to reside in close proximity. Microorganisms that carry out microbially influenced corrosion (MIC) can occur in and are facilitated by biofilms (7,8,9). MIC also includes production of microbial metabolites at one location which diffuse to a corrosion site, possibly at another location (15). MIC of metal surfaces results in pitting, crevice corrosion, under-deposit corrosion, and selective leaching. The ability of endolithic and contaminating microbes to form biofilms can ultimately affect performance of structures such as those in the Yucca Mountain repository.Metal biocorrosion occurs in the presence of biofilms; therefore, this study was designed to determine boundary conditions for biofilm formation. Our study had two objectives that address the potential for biofilm production: (i) to determine relative humidity (RH) limits for biofilm formation, and (ii) to determine the boundary limits of biofilm formation on the basis of temperature.Yucca Mountain is located at the Nevada Test Site, 100 miles northwest of Las Vegas, Nevada. Mined Yucca Mountain tuff was collected near the north portal entrance. The surface layer of the tunnel wall was removed by using flamesterilized tools, and the newly exposed rock was collected into sterile, plastic bags and was placed on ice. The rock was transported to the laboratory within 6 h and was stored at Ϫ20°C (14). It was later aseptically crushed into fine grains by using flame-sterilized mortars and pestles.One-centimeter-square coupons were constructed from the following metals: C22 nickel alloy, N-316 stainless steel, and titanium (Metal Samples, Mumford, Ala.). Aseptically crushed rock was transferred to sterile glass petri plates, metal coupons were placed within the crushed rock, and microcosms were placed in chambers held to specific RH and temperature values.To achieve different RH levels, specific saturated salt solutions were placed in the bottom reservoirs of the microcosm chambers (Nalgene Autoclavable Desiccators, Rochester, N.Y.). The salt solutions included KCl (83.6% RH), KI (67.9% RH), and MgCl 2 (32.4% RH). Distilled water was used to create 100% RH. Petri plate microcosms were placed above the salt solution reservoir. Chambers were sealed with highvacuum grease (Dow Corning, Midland, Mich.), and RH levels were checked by ...