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<br />. <br /> <br />Woodward.Clyde Consultants <br /> <br />-. rl i""\ r) <br />UJ~':' <br /> <br />. <br /> <br />For 54 tests on composited materials having permeability <br /> <br />rates of less than 10 feet/year, the average permeability value <br />w~s abuut 0.6 feet/year (6 x 10-7 cm/sec--very low <br /> <br />. <br /> <br />permeability). For the only 3 tests on composited materials <br />having permeability rates of greater than 10 feet/year, the <br /> <br />permeability values were about 10 to 60 feet/year (very low to <br /> <br />. <br /> <br />low permeability). From our review of the tests and test pit <br /> <br />logs it is apparent that the proposed Zone 2 borrow areas <br /> <br />contain extremely variable soils with respect to location and <br /> <br />. <br /> <br />depth, and will have very low permeability in the embankment. <br /> <br />The friction coefficient, Tan 0, the cohesive strength at <br /> <br />. <br /> <br />optimum moisture, Co, and the saturated cohesive strength, Cs, <br /> <br />which we assigned to the Zone 2 materials are given in Table 2. <br /> <br />4. Filter-Drain Zone <br /> <br />Although not specifically described in Table 1, we were <br /> <br />. <br /> <br />later informed that the pervious filter-drain material, now <br /> <br />proposed, is to be processed material secured from Borrow Area <br /> <br />A, apparently with materials from Borrow Areas B, C, Land M <br /> <br />. <br /> <br />also being available. The processing is to remove the fine <br /> <br />fraction so that less than 5% will pass the 200 mesh screen. <br /> <br />The filter materials were classified by the Bureau (Table 1) as <br /> <br />. <br /> <br />silty sand (SM) with 31% gravel and 69% sand, without an amount <br /> <br />of fines indicated. After processing the classification will <br /> <br />be well graded sand-gravel and poorly graded sands (GW-SW-SP) <br /> <br />. <br /> <br />with an approximate dry density of 127 pcf at 70% relative <br /> <br />- 13 - <br /> <br />. <br /> <br />., <br />