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GENERAL NOTES <br />DRILLING & SAMPLING SYMBOLS <br />SS: Split Spoon - 1-'/S" I.D., 2" O.D., unless otherwise noted HS: Hollow Stem Auger <br />ST: Thin-Walled Tube - 2" O.D., unless otherwise noted PA: Power Auger <br />RS: Ring Sampler - 2.42" I.D., 3" O.D., unless otherwise noted HA: Hand Auger <br />DB: Diamond Bit Coring - 4", N, 8 RB: Rock Bit <br />BS: Bulk Sample or Auger Sample W B: Wash Boring or Mud Rotary <br />The number of blows required to advance a standard 2-inch O.D. split-spoon sampler (SS) the last 12 inches of the total 18-inch <br />penetration with a 140-pound hammer falling 30 inches is considered the "Standard Penetration" or "N-value". <br />WATER LEVEL MEASUREMENT SYMBOLS: <br />WL: Water Level WS: While Sampling <br />WCI: Wet Cave in WD: While Drilling <br />DCI: Dry Cave in BCR: Before Casing Removal <br />AB: After Bodng ACR: After Casing Removal <br />Water levels indicated on the boring logs are the levels measured in the borings at the times indicated. Groundwater levels at other <br />times and other locations across the site could vary. In pervious soils, the indicated levels may reflect the location of groundwater, In <br />low permeability soils, the accurate determination of groundwater levels may not be possible with only short-term observations. <br />DESCRIPTIVE SOIL CLASSIFICATION: Soil classification is based on the Unified Classification System. Coarse Grained Soils have <br />more than 50% of their dry weight retained on a #200 sieve; their principal descriptors are: boulders, cobbles, grave( or sand. Fine <br />Grained Soils have less than 50% of their dry weight retained on a #200 sieve; they are principally described as clays if they are <br />plastic, and silts if they are slightly plastic ornon-plastic. Major constituents may be added as modfiers and minor constituents may be <br />added according to the relative proportions based on grain size. In addition to gradation, coarse-grained soils are defined on the basis <br />of their in-place relative density and fine-grained soils on the basis of their consistency. <br />CONSISTENCY OF FINE-GRAINED SOILS RELATIVE DENSITY OFCOARSE-GRAINED SOILS <br /> Standard <br />Unconfined Penetration or Standard Penetration <br />Compressive N-value ISS) or N-value ISS) <br />Strength. Qu. psf BlowslFt. Consistency BlowslFt. Relative Density <br />< 500 <2 Very Soft 0 - 3 Very Loose <br />500 - 1,000 2-3 Soft 4 - 9 Loose <br />1,001 - 2,000 4-6 Medium Stiff 10 - 29 Medium Dense <br />2,001 - 4,000 7-12 Stiff 30 - 49 Dense <br />4,001 - 8,000 13-26 Very Stiff 50+ Very Dense <br />8,000+ 26+ Hard <br />RELATIVE PROPORTIONS OF SAND AND GRAVEL GRAIN SIZE TERMINOLOGY <br />Descriptive Term(s) of other Percent of Major Component <br />constituents Drv Weight of Sample Particle Size <br />Trace < 15 Boulders Over 12 in. (300mm) <br />With 15 - 29 Cobbles 12 in. to 3 in. (300mm to 75 mm) <br />Modifier > 30 Gravel 3 in. to #4 sieve {75mm to 4.75 mm) <br /> Sand #4 to #200 sieve (4.75mm to 0.075mm) <br />RELATIVE PROPORTIONS OF FINES Silt or Clay Passing #200 Sieve (0.075mm) <br />Descriptive Term(s) of other Percent of PLASTICITY DESCRIPTION <br />constituents Drv Weight <br /> Term Ptasticitytndex <br />Trace < 5 Non-plastic 0 <br />With 5-12 Low 1-10 <br />Modifiers > 12 Medium 11-30 <br /> High 30+ <br /> l~~rracon _ <br />Form 108-9-00 <br />