METHANE PRODUCTION AND CONSUMPTION MONITORED BY STABLE H AND C ISOTOPE RATIOS AT A CRUDE-OIL SPILL SITE, BEMIDJI, MINNESOTA

Stable isotopic ratios of C and H in dissolved CH4 and C in dissolved inorganic C in the ground water of a crude-oil spill near Bemidji, Min nesota, support the concept of CH4 production by acetate fermentation with a contemporaneous increase in HCO3- concentration. Methane concen trations in the saturated zone decrease from 20.6 mg L(-1) to less tha n 0.001 mg L(-1) along the investigated flow path. Dissolved N-2 and A r concentrations in the ground water below the oil plume are 25 times lower than background; this suggests that gas exsolution is removing d issolved CH4 (along with other dissolved gases) from the ground water. Oxidation of dissolved CH4 along the flow path seems to be minimal be cause no measurable change in isotopic composition of CH4 occurs with distance from the oil body. However, CH4 is partly oxidized to CO2 as it diffuses upward from the ground water through a 5- to 7-m thick uns aturated zone; the delta(13)C of the remaining CH4 increases, the delt a(13)C of the CO2 decreases, and the partial pressure of CO2 increases . Calculations of C fluxes in the saturated and unsaturated zones orig inating from the degradation of the oil plume lead to a minimum estima ted life expectancy of 110 years. This is a minimum estimate because t he degradation of the oil body should slow down with time as its more volatile and reactive components are leached out and preferentially ox idized. The calculated life expectancy is an order of magnitude estima te because of the uncertainty in the average linear ground-water veloc ities and because of the factor of 2 uncertainty in the calculation of the effective CO2 diffusion coefficient.