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�I Providence Family Services Center 9-91 M-12723-0 <br /> August 25, 1999 Page 7 <br /> � <br /> IOur geotechnical laboratory tests revealed that the on-site scils have a fines(silt and clay)content <br /> on the order of 23 to 32 percent, and a moisture content on the order of 9 to 13 percent. We <br /> I interpret these soils to be currently near or above their optimum moisture contents,and to be highly <br /> sensitivetomoisturecontentvariations. TheenclosedlaboratoytestingsheetsgraphicaU�•r�esent <br /> our test results, and Table 3 summarizes these results. <br /> TABLE 3 <br /> LABORATORY TEST RESULTS FOR NON-0RGANIC ONSITE SOILS <br /> Sample lNoisture Gravel Sand SiltlClay <br /> i Soil Type and Source Depth Content Content Content Content <br /> (feet) (percent) (percent) (parcent) (percent) <br /> Upper SAND (B-10/S-4) 12'/:to 14 13 9 59 �2 <br /> I Weathered Till (B-10/S-5) 17'/: to 19 11 3 65 32 <br /> Glacial Till B-10/S-6 22'/�to 24 9 c19 58 23 <br /> ( 4.5 Groundwater Conditions <br /> ( At the time of drillirg (January 1999), none of our explorations encountered groundwater within <br /> their termination depths of 14 to 44 feet. Because our explorations were performed during an <br /> extended period of generally wetweather,groundwater conditions may closeiy represent the yearly <br /> ( high levels; somewhat lower levels probably occur during the summer and early fall months. <br /> However, perched groun�Hater may form atop the glacial till horizon during periods of heavy <br /> rainfall. It should also be noted that throughout the year,groundwater levels wouid likely fluctuate <br /> � in response to changing precipitation patterns, off-site construction activities, and site utilization. <br /> 4.6 Seismic Conditions <br /> � Based on our analysis of subsurface exploration logs and our review of published geologic maps, <br /> we interpret the on-site soil conditions to correspond to seismic soil profile type S-C as defined by <br /> Table 16-J of the 1997 Uniform Building Code (UBC). Curcent (1996) National Seismic Hazard <br /> ( Maps prepared by the U.S. Geological Survey indicate that a peak Cedrock site acceleration <br /> coefficient of about 0.28 is appropriate for an earthquake having a 10-percent probability of <br /> exceedance in 50 years,which corresponds to a retum interval of 475 years. According to Figure <br /> � 16-2 of the 1997 UBC, the site lies within seismic risk zone 3. If a future version of the UBC is to <br /> be used for structural design purposes,we can a�aist the project structural engineer in deveioping <br /> appropriate seismic criteria. <br /> I4.7 Environmental Conditlons <br /> Our on-site geotechnical explorations did not disclose any obvious indications of petroleum orother <br /> I environmental contaminants in the subsurface soils. However, because a specific assessment of <br /> on-site environrrsntal conditions was not included in our scope of work, no substantiated opinions <br /> can be drawn in regards to whether contaminants are present. <br /> I� 5 �S�OFOPROC'�99Pmiects�5eai0e��700Cs�.'.':]RoOmsonWrowEenceHosp�iip�woC ,Q <br /> I <br />