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<br />I <br />I AET #93-1379 - Page 8 <br />,. Review of Soil Prooerties <br />I . Strength/Stability - Opinions relative to subgrade strength and stability have been <br /> generally discussed in the previous Site Conditions section which describes the soil <br />I encountered at each individual street location. Generally, much of the soil subgrade <br /> appears to be reasonably stable with more obvious exceptions within the upper 3' zone <br />I noted at Boring #4, #5, and #8. Conditions at Boring #6 are also somewhat unstable, <br /> - although sample review suggests the condition is not a severe as the other described <br />I locations. Please note that soil conditions encountered are mixed and variable, and we <br />I expect stability properties will also be variable along the roadways such that some local <br /> or "spotty" zones of instability will exist. <br />I . Compressibility - Without a significant grade increase, and assuming upper soils are <br />.. corrected as needed for strength reasons, compressibility of the subgrade soils will not <br /> be a problem at this site. <br />I . Drainage Properties - Most of the subgrade soils are clayey, which are relatively poor <br />I draining materials. These soils can allow for perching or trapping of water within the <br /> base and sub grade. The main exceptions to the above are as follows: <br />I - The silty sand layer within the upper 3' along Keithson Drive meet the <br />I requirements of a granular borrow. These soils are judged to be moderately fast <br /> to moderate draining. <br />I The sand layer noted from 3' to 4' deep at Boring #12 is a silty sand which is also <br /> - <br />I at least moderately draining. This particular layer was found to include trapped <br /> water, which resulted in a measurable water level within the borehole. <br />I <br />i' <br />I <br />