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2-12 <br />Forward Composting Facility SWT Engineering <br /> Report of Composting Site Information - August 2019January 2022 <br />z:\projects\allied waste\forward\resource recovery facility\5 yr permit rvw 2019-2020\rcsi 2019\text\sec 2.doc <br />EMCON Associates in 1972. EMCON drilled a total of 17 borings ranging in depth from 38 <br />feet to 178 feet. The locations of the EMCON boreholes are shown on the Exist ing <br />Conditions Plan (Drawing 1) of that report. Another subsurface investigation was performed <br />by InsituTech in 1987 using Cone Penetration Testing (CPT) in the WMU E area. The exact <br />locations of the CPTs were, unfortunately, not surveyed by InsituTech. <br />The subsurface investigation was performed by CH2M HILL in 1992; it consisted of four soil <br />borings drilled in April and May, 199 2. The Existing Conditions Plan (Drawing 1) of that <br />report shows the approximate location of these four borings, designated as BH -1 through <br />BH-4. Pitcher Drilling Company of Palo Alto, California, was subcontracted to drill the soil <br />borings. CH2M HILL personnel specified the locations, depths of borings, and sampling <br />intervals and observed the drilling and sampling operations. All borehole logs available for <br />the site are included as an appendix in that report . <br />The CH2M HILL borings were 4 -7/8-inch diameter and extended to depths ranging from 43 <br />to 102 feet. The borings were advanced using mud rotary drilling methods with a truck - <br />mounted Failing 750 drill rig. As each boring was completed, the hole was grouted to the <br />surface using a "neat" cement grout. The borings were grouted from the bottom upward <br />using a 2-inch drill pipe as a tremie. <br />Relatively undisturbed samples were obtained using a 3 -inch outside diameter Shelby tube <br />sampler (ST samples) or Pitcher Barrel sampler (PB samples). The Pitcher Barrel sampler <br />was used to obtain samples of very stiff clay where the Shelby tubes could not be pushed. <br />This sampling was performed in general accordance with procedures for Thin-Walled Tube <br />Sampling of Soils as described by the American Society of Testing and Materials (ASTM), <br />Standard D 1587. Disturbed soil samples were obtained from the borings using a 2 -inch <br />outside diameter split -spoon sampler, driven as described for the Standard Penetration Test <br />(SPT), ASTM Standard D1586. <br />Soil recovered during the drilling program was visually classified by a CH2M HILL engineer in <br />general accordance with ASTM D2487 and D2488. The soil names on the boring logs <br />ref lect these ASTM standards. Pocket penetrometer tests were conducted on most cohesive <br />samples. Samples were then prepared for storage by placing representative portions in <br />plastic bags or by sealing the sampling tube with plastic cap and tape. Sample desc riptions, <br />blow counts recorded during the SPT, and other relevant information were recorded on the <br />soil boring logs. <br />Selected soil samples obtained by CH2M HILL from its subsurface investigation were tested <br />in the laboratory by Harding Lawson Associates (HLA) of Concord, California. Index tests <br />performed by HLA included determining the liquid limit, plastic limit, and moisture content of <br />the selected samples. Engineering property tests performed included Unconsolidated <br />Undrained (UU) triaxial compression and consolidation tests. Detailed results of the tests <br />performed are included in the Stability and Settlement Analysis of that report . <br />The soil encountered during the CH2M HILL field investigation generally consists of <br />interbedded layers of sand, silt, and lean clay. The cohesive materials are generally of very <br />stiff to hard consistency. The cohesionless materials can be characterized as dense to very <br />dense. The soil deposits at the site were found to be heterogeneous and laterally and <br />vertically discontinuous. Based on the four soil borings performed for this geotechnical <br />exploration, the subsurface soils at the site can be divided into six general layers of interest.