Laserfiche WebLink
i --- - -- --�— — � KLEINPELDER <br /> Perched groundwater was encountered in our borings at depths ranging from about 82%2 to 110 <br /> feet below the existing ground surface. Our firm does not know the extent of the perched <br /> groundwater at this time. However,based on information provided by Don Pedro Drilling who <br /> services many wells in the area, including at the DSS and Teichert quarries, well soundings in <br /> the project area indicate that beneath the perched water encountered in this investigation <br /> groundwater is located at a depth greater than about 200 feet below the existing grade. <br /> 5. RECLAIMED SLOPES <br /> Based on our analysis presented in Section 6 and our previous laboratory tests, the reclaimed <br /> slopes should be compacted near the optimum moisture content to at least 85 percent relative <br /> compaction. We note that Kleinfelder previously performed a limited number of nuclear <br /> density gauge tests on reclaimed soils that had been compacted by loaded scrapers at Teichert's <br /> Vernalis Plant. Our tests indicated that the relative compaction of these soils was generally <br /> greater than 85 percent. <br /> 6. SLOPE STABILITY ANALYSIS <br /> The slope stability analyses were performed using SLOPE/W, a computer program from Geo- <br /> Slope International. The slope configuration is presented in the appendix. The soil properties <br /> used in our analyses are based on the results of the field and laboratory investigations <br /> performed for this study as well as those performed previously in the project area. <br /> Summarized in the table below are the soil properties for the four basic soils used in our <br /> analyses. - <br /> SOIL PROPERTIES <br /> Angle of Internal` Moist Unit <br /> Soil a Friction(degrees) Cohesion s Wei ht c <br /> I Cemented mixture of sand, 36 900 120 <br /> gravel, and cla <br /> II. Sandy clay 24 500 115 <br /> Weakly cemented silty sand 25 350 120 <br /> L Reclaimed soil 27 950 130 <br /> Based on our experience, slope failures in cemented soils, such as those soils encountered in <br /> the Vernalis area, tend to occur as block or wedge failures rather than deep circular failures. In <br /> other words, the likely slip surface would develop at the ground surface at the top of the slope <br /> and extend downward to a point of intersection on the face of the slope. To account for this <br /> mode of failure, various block slip surfaces were modeled to estimate the most likely failure <br /> planes as well as the minimum factors of safety. However, due to the high fines content and no r <br /> l <br /> 2900TGOUST03R1215 August 21,2003 <br /> 0 2003 Kleinfelder,Inc. Page 3 of 5 <br />