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AfcDonald's Corporation E-3G76 <br /> December 21, 1987 Page 7 <br /> percent of maximum density except for the top twelve (12) inches <br /> which should be compacted to 95 percent of maximum density. <br /> On-site soils at the time of our exploration were near the optimum <br /> moisture content and may be used as structural fill provided the <br /> grading operations are conducted in dry weather. However, the on- <br /> site soils have a significant amount of fines. Thus, compaction and <br /> grading will be difficult if the soil moistur.e increases above the <br /> optimum moisture content. Therefore, unless the moisture content <br /> can be reduced, it may be necessary to use imported granular soil as <br /> structural fill. The moisture content can be reduced by aeration in <br /> dry weather, or by using lime or cement stabilization. Ideally, <br /> structural fill which is to be placed in wet weather should consist <br /> of a yranular material with a maximum size of three inche� and no <br /> more than 5 percent fines passing the No. 200 sieve. During dry <br /> weather, any compactible non-organic soil can be used as structural <br /> fill. <br /> FIELD EXPIARATION AND LABORATORY TESTING <br /> Our field exploration was performed on November 25, 1987 . Subsur- <br /> face conditions at the site were explored by drilling five <br /> borings to a maximum depth of nineteen (19) feet below the existing <br /> grade. The borings were drilled by Associated Dril.ling using a <br /> truck-mounted drill rig. Continuous flight, hollow stem augers were <br /> used to advance and suppurt the boreholes during sampling. The <br /> locations of the borings were approximately determined by taping <br /> from existing site features. Elevations were approximately deter- <br /> mined by hand level fr.om the southeast corner of the property. The <br /> locations and elevations of the borings should be considered <br /> accurate oi:ly to the degree iMplied by the method used. These <br /> locations are shown on the Boring Location Plan, P1ate 2 . <br /> The field exploration was continuously monitored by an engineering <br /> qeologist from our firm who classified the soils encountered and <br /> maintained a log of each boring, obtained representative sai�ples, <br /> and observed pertinent site features. All samples were visually <br /> classified in accordance with the Unified Soil Classification System <br /> which is presented on Plate 3 , Legend. Logs of the borings are <br /> presented on Plates 4 through 8. The final logs represent our <br /> interpretations of the field logs and the results of the laboratory <br /> examination and tests of field samples. The stratification lines on <br /> the logs represent the approximate boundary between soil types. In <br /> actuality, the transition may be gradual . <br /> Earth Consultants, Inc. <br />