The ability of the soil cover system at the Equity Silver Mine to limit oxy
gen and water fluxes to underlying waste rock was evaluated using a detaile
d instrumentation program. Field instrumentation was installed to monitor t
emperature, gaseous oxygen, and gaseous carbon dioxide in the waste rock pi
les. Lysimeters were constructed at the base of the soil cover system to mo
nitor infiltration across the soil cover. Sensors to measure matric suction
, soil temperature, and water content were installed. An automated weather
station was also installed to monitor climate conditions at the mine site.
The field data indicates that the lower compacted layer maintained a high d
egree of saturation (i.e., 90% or higher) during 3 years of data collection
(August 1992 to August 1995). This is a positive result, since the lower c
ompacted layer was designed as an oxygen limiting barrier. The average meas
ured infiltration from lysimeters placed at the base of the soil cover syst
em was 5% of precipitation (from October 1992 to August 1993). The measured
matric suction data indicates that the hydraulic gradient within the soil
cover system is predominantly upward except for relatively short periods of
heavy rainfall and snow melt in late fall and early spring.