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~, <br /> <br /> <br /> <br />LJ <br /> <br /> <br /> <br /> <br />1 <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />1 <br />-lz- <br />we recommend the following shet:r strength parameters: <br />Soil Type <br />Sl. sandy clay (natural) <br />S1. sandy clay (natural) <br />S1. Sandy clay (remolded) <br />Silty to clayey sand and <br />silt (natural) <br />Silty to clayey sand <br />silt (remolded) <br />TABLE A <br />Soil Conditions <br />Unconsolidated, undrained <br />Consolidated, undrained <br />Consolidated, undcained <br />Consolidated, drained <br /> Cohesion <br />(d (ksf) <br />5° 2.5 <br />34° 0.25 <br />29° 0.5 <br />33° 0.1 <br />Consolidated, drained 30° 0.1 <br />The above values essentially represent effective stress para- <br />meters. Total stress parameters for the clays can be obtained from <br />triaxial shear tests presented on Figs. 11 and 12. Differentiation <br />between total and effective conditions cannot be accurately made for <br />the direct shear testing procedures. <br />Earthcork: We recommend all embankment fill material consisting of <br />on-site clays and silty to sandy soils be compacted to at least 958 of <br />standard Proctor density (ASTM D-698) at.a moisture content 28 below <br />to 78 above optimum rtuisture. This degree of con action has been <br />utilized to derive shear strength parameters. The predominant embank- <br />ment constituent should have a percent passing the U200 sieve in <br />excess of 358 and maximum size of 6 ind~es. It may be possible for <br />large equipment to ~.ork rock fragmented soils to meet these specifica- <br />lions. However, the contractor should be prepared to selectively <br />place or stockpile unsuitable material as required. Due to the drier <br />condition of the deeper clays, some difficulties in obtaining optimum <br />rtuisture may be experienced. 'getting of the borrow area prior to <br />cutting may be helpful. bb borrow should be removed from below the <br /> <br />