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<br />I <br /> <br />I <br /> <br />GENERAL NOTES <br /> <br />DRILLING & SAMPLING SYMBOLS: <br /> <br />I <br /> <br />5S <br />ST <br />PA <br />08 <br />AS <br />JS <br />VS <br /> <br />I <br /> <br />I <br /> <br />Split Spoon - 1 3/8" 1.0., 2" 0.0. <br />Unless otherwise noted <br />Shelby Tube - 2: 0.0., <br />Unless otherwise noted <br />Power Auger <br />Diamond Bit -NX,BX, AX <br />Auger Sample <br />Jar Sample <br />Vane Shear <br /> <br />OS <br />HS <br />WS <br />FT <br />RB <br />5S <br />PM <br />GS <br /> <br />Osterberg Sampler - J" Shelby Tube <br />Hollow Stem Auger <br />Wash Sample <br />Fish Tail . <br />Rock Bit <br />Bulk Sample <br />Pressuremeter Test, In-Situ <br />Giddings Sampler <br /> <br />Standard "N" Penetration: Blows per foot of a 140 pound hammer falling 30 inches on a 2 inch 0.0. <br />split spoon sampler, except where otherwise noted. <br /> <br />I <br /> <br />WATER LEVEL MEASUREMENT SYMBOLS: <br /> <br />I <br /> <br />WL <br />WS <br />WD <br />A8 <br /> <br />Water Level <br />While Sampling <br />While Drilling <br />After Boring <br /> <br />WCI : <br />DCI : <br />BCR: <br />ACR: <br /> <br />Wet Cave In <br />Dry Cave In <br />Before Casing Removal <br />After Casing Removal <br /> <br />I <br /> <br />Water levels indicated on the boring logs are the levels measured in the boring at the times indicated. <br />In pervious' soils, the indicated elevations are considered reliable groundwater levels. In impervio\.lS <br />soils, the accurate determination of ground water elevations may not be possible, even after several <br />clays of observations; additional evidence of. ground water elevations must be sought. <br /> <br />I <br /> <br />GRADATION DESCRIPTION & TERMINOLOGY: <br /> <br />I <br /> <br />Coarse Grained or Granular Soils have more than 50% of their dry weight retained ona fl200 sieve; they <br />are described as: boulders, cobbles, gravel or sand. Fine Grained soils have less than 30% of their dry <br />weight retained on a /1200 sieve; they are described as: clays or clayey silts if they are cohesive and <br />silts if they are non-cohesive. In addition to gradation, granular soils are defined on the basis of their <br />relative in-place density and fine grained soils on the basis of their strength or consistency and their <br />plasticity. . . <br /> <br />Major Descriptive Term <br />Component Of Components Also Percent Of <br />Of Sample Size Range Present in Sample Drv Wei~ht <br />Boulders . Over 8 in. (200 mm) Trace 1 - 9 <br />Cobbles 8 inches to 3 inches Little 10 - 19 <br /> (200 mm to 75 mm) <br />Gravel 3 inches to 114 sieve Some 20-34 <br /> (75 mm to 4.76 mm) <br />Sand 1/4 to 11200 sieve And 35 - 50 <br /> (4.76 mm to 0.074 mm) <br />Silt Passing 11200 sieve <br /> (0.074 mm to 0.005 mm) <br />Clay Smaller than 0.005 mm <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />CONSISTENCY OF COHESIVE SOILS: <br /> <br />RELATIVE DENSITY OF GRANULAR SOILS: <br /> <br />Unconfined Compressive <br />Strength, Qu, tsf <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Consistency <br /> <br />N - Blows per ft. <br /> <br />< 0.25 <br />0.2' - 0.49 <br />0.50 - 0.99 <br />1.00 - 1.9~ <br />2.00 - 3.99 <br />4.00 - 8.00 <br />> 8.00 <br /> <br />VerY Soft <br />Soft <br />Medium (Firm) <br />Stiff <br />Very Stitf <br />Hard <br />Very Hard <br /> <br />G - 3 <br />4 - 9 <br />10 - 29 <br />30 - 4~ <br />50-&0 <br />80+ <br /> <br />SOIL TESTING SERVICES, INC. <br /> <br />Relative Density <br /> <br />Ver'l Loose <br />Loose <br />Medium Dense <br />Dense <br />Very Dense <br />Ex:remely Dense <br />