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The cohesionless materials can be characterized as dense to very dense. Because <br /> the sediments at the site were deposited as fluvial floodplain and channel deposits, <br /> the soil deposits at the site were found to be heterogeneous and laterally and <br /> vertically discontinuous. It is therefore difficult to characterize the subsurface soils <br /> into distinct units. <br /> Results of the most recent site investigation (GLA, 2008) indicate that under the <br /> loading of the site's design Maximum Credible Earthquake horizontal <br /> acceleration, the subsurface soils at the site are too dense to liquefy. In addition, <br /> the maximum differential settlement of subsurface soils under the proposed <br /> landfill expansion is on the order of only 0.3 percent, and dynamic settlement of <br /> subsurface soils due to a design earthquake is 0.01 to 0.2 inches with a <br /> differential settlement on the order of 0.1 inches. <br /> Two soil borrow studies (Twining, 1991 and Lewis Engineering, 2000) were <br /> conducted in a former borrow pit area within the landfill footprint. The results of <br /> these studies indicate that soils at elevations of approximately 15 to 25 feet amsl <br /> are classified as low plasticity clays (CL) based on the Unified Soil Classification <br /> System (USCS) and have laboratory permeabilities ranging from 1 x 10' to 1 x <br /> 10"$ cm/sec when compacted to above 90 percent relative compaction based <br /> on American Society for Testing Materials Method D1557 (ASTM D1557). <br /> The other soil borrow study (Twining 1996) was conducted in the borrow area <br /> north of the FL. The results of this study indicate that the soils encountered at a <br /> depth of approximately 4 to 11 feet below ground surface are classified as sandy <br /> clay and have a laboratory permeability of approximately 3 x 10-' cm/sec when <br /> compacted to above 90 percent relative compaction based on ASTM D1557. <br /> 2.5 CLIMATE <br /> The climate of the region is typical of the California Central Valley. Winters are <br /> generally cold and wet with fog, while summers are hot and dry. Representative <br /> climatologic stations were selected based on their proximity to the site and reliable <br /> period of records for the station (30 years or more). <br /> Forward Landfill-Project Description 2-6 BRYAN A.STIRRAT&ASSOCIATES <br /> j:\Allied\Forward\2007.0018 Lateral Expansion\Reports\Prof Descrip\021308 Final Proj Des\Sec 2.doc:2/13/2008) <br />