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V. ENGINEERING PROPERTIES OF SITE SOILS <br /> A. LABORATORY TESTING <br /> Laboratory tests were run on soil samples obtained during the field <br /> investigation. Bulk samples were classified using Atterberg Limits <br /> and percent passing the No. 200 sieve. Compaction curves and remolded <br /> permeability tests were also conducted on selected bulk samples to <br /> evaluate their suitability for use as soil liner and cover material . <br /> Undisturbed samples were evaluated for strength properties using <br /> direct shear and unconfined compressive strength tests. The strength <br /> test results will be used in future slope stability analyses specified <br /> in the Subchapter 15 regulations. Summaries of laboratory test <br /> results are presented in Appendix G. <br /> Laboratory classifications confirmed field descriptions. Testing <br /> focused on fine-grained soils with potential use in landfill construc- <br /> tion. Fine-grained soils described in the field as clays and silts <br /> were classified by testing to be primarily CL (clay) and ML (silt) , <br /> respectively. Sand content of fine-grained soils within the 0 to <br /> 20 feet interval ranged from less than 5 to 50 percent. <br /> Silty sand samples tested were found to contain between 39 and 47 per- <br /> cent fines. It should be remembered that soil materials from shallow <br /> depths at the site vary gradationally, both vertically and horizon- <br /> tally, with respect to fine-grained versus coarse-grained characteris- <br /> tics. Isolated samples do not necessarily indicate consistent lithol - <br /> ogies across the site. <br /> Samples of soils to approximately -1/2 feet from Borings P-1 and P-2 <br /> were tested for compaction characteristics and remolded permeability <br /> to ascertain the suitability of available on-site material for use as <br /> cover and in construction of retention structures. The permeability <br /> of the soils classified as ML and CL was determined to range from <br /> PJ9 9390206.00D 16 <br />