skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Evaluation of a predictive ground-water solute-transport model at the Idaho National Engineering Laboratory, Idaho. US Geological Survey water-resources investigation 82-25

Technical Report ·
OSTI ID:5247353

In 1973, a digital chemical solute-transport modeling study at the Idaho National Engineering Laboratory (INEL) had been used to project chloride and tritium waste plumes for 1980. The model indicated that for the conditions assumed, the wastes would be at or near the INEL southern boundary by 1980. Eight wells were drilled during the summer of 1980 near the southern boundary to fill existing gaps in the INEL hydrogeological data base, to delineate the leading edge of the waste plumes, and to monitor for first arrivals of aqueous wastes at the existing boundary of the INEL. The data from the eight wells were used to evaluate the accuracy of the predictive model, and the assumptions used. The subsurface geology in the southwestern INEL vicinity is dominated by thin basalt flows interbedded with layers of sediment and silicic rocks are penetrated only in those wells near the INEL's southern boundary. The Arco volcanic rift zone was found to have a marked effect on the regional ground-water flow regimen, and perhaps, on water quality. This same subsurface geologic structure appears to have lower water-yielding and transmitting capabilities than the surrounding aquifer matrix and retards the movement of aqueous wastes. The leading edges of the chloride and tritium waste plumes are 2 to 3 miles upgradient from the southern boundary of the INEL, and higher-than-background specific conductance values are measurable at about the same upgradient distance. As expected, the waste plumes projected by the computer model for 1980 extended somewhat further downgradient than indicated by well data due to conservative worst-case assumptions in the model input and inaccurate approximations of subsequent waste discharge and aquifer recharge conditions.

Research Organization:
Geological Survey, Idaho Falls, ID (USA). Water Resources Div.
OSTI ID:
5247353
Report Number(s):
IDO-22062; ON: DE82012698
Resource Relation:
Other Information: Portions of document are illegible
Country of Publication:
United States
Language:
English