Paper No. 33103--.
COMBINED RESULTS FROM GEOPHYSICAL LOGS AND CORE DATA OBTAINED FROM DEEP BOREHOLES AT YUCCA MOUNTAIN, NEVADA
Excerpts from these integrated borehole displays highlight a number of features of the volcanic rocks at Yucca Mountain, including: (1) the relation of the mineralogy of altered tuffs to degree of welding, (2) the downward transition from unaltered (glass-bearing) to altered (zeolitic) tuff with respect to present-day water levels, (3) volumetric estimates and spatial distribution of lithophysal zones in the Topopah Spring Tuff, (4) estimates of air-filled pore space and water saturation in the unsaturated zone, and (5) a comparison of fracture and matrix permeability. In summary, the displays provide a view of the spatial distribution of parameters relating to mineralogy, porosity, water saturation, matrix flow, and fracture flow. These data were used extensively by hydrologists to help determine flow direction and probable fate of any potential radionuclide releases.
Preferred Presentation Type: Oral
