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- 10 - <br />generally 60 minutes or greater with the exception of Test A in <br />Sediment Raid RP-2, 3. Based en this information, we conclude that the • <br />in-situ sand, silt and clay mixtures are relatively impermeable. <br />LABORATORY TEST RESULTS <br />Samples obtained from our exploratory test holes were examined <br />and classified in the laboratory b~+ the project soils engineer. <br />Laboratory testing was performed on the samples to determine their <br />classification, moisture-volume change characteristics and strength. <br />A description of the laboratory test results is included in this <br />information. laboratory test results are presented in Table I and <br />Figs. B-1 through B-19. <br />Swell~onsolidation Tests: Swell-consolidation tests were conducted <br />on samples of the soils and rock from from the site in order to • <br />determine their compressibility or swell characteristics under loading <br />and saturation. Swell-consolidation tests eorx3ueted on samples of the <br />natural sand, silt and clay mixtures from the site indicate that these <br />materials have variable characteristics upon loading arc] saturation <br />(Figs. B-1 through B-7). Some of the samples showed a moderate <br />tendency to collapse, what saturated under low loads, and a moderate <br />to high consolidation upon subsequent loading. The dry unit weight of <br />the soils which collapsed upon saturation varied from 86.6 to 105.1 <br />pcf with an average of 98.4 pcf. The average rtoisture content of <br />these materials was approximately 6.58. <br />-- The remaining samples showed a low to noderate tendency to <br />expand when saturated under lover loads. These samples have somewhat <br />u <br />