CCP 11-12-1996 - Laserfiche WebLink

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I EXPLORATION/CLASSITICATION METIIODS SamDlin" Methods Split-Spoon Samples (SS) Standard penetration (split-spoon) samples were collected in general accordance with ASTM:DI586. This method I consists of driving a 2" O.D. split barrel sampler into the in-sim soil with a 140-pound hammer dropped from a height of 30". The sampler is driven a total of 18" into the soil. After an initial set of 6". the number of hammer blows to drive the sampler the fmall2" is known as the standard penetration resistance or N-value. I Disturbed Samples (DS) Sample types described as "DS" on the boring logs are dismrbed samples. which are taken from the flights of the auger. Because the auger dismrbs the samples, possible soil layering and contact depths should be considered I approximate. Sampling Limitations I Uuless actually observed in a sample, contacts between soil layers are estimated based on the spacing of samples and the action of drilling tools. Cobbles, boulders, and other large objects generally cannot be recovered from test borings, and they may be present in the ground even if they are not noted on the boring logs. I Classification Methods Soil classifications shown on the boring logs are based on the Unified Soil Classification (USC) system. The USC system is described in ASTM:D2487 and D2488. Where laboratory classification tests (sieve analysis or Atterberg I Limits) have been performed, accurate classifications per ASTM:D2487 are possible, Otherwise, soil classifications shown on the boring logs are visual-manual judgments. Charts are attached which provide information on the USC system, the descriptive terminology, and the symbols used on the boring logs. Ie The boring logs include descriptions of apparent geology, The geologic depositional origin of each soil layer is interpreted primarily by observation of the soil samples, which can be limited. Observations of the surrounding I topography. vegetation, and development can sometimes aid this judgment. Water Level Measurements The ground water level measurements are shown at the bottom of the boring logs. The following information appears I under "Water Level Measurements" on the logs: . Date and Time of measurement I . Sampled Depth: lowest depth of soil sampling at the time or measurement . Casing Depth: depth to bottom of casing or hollow.srem auger at rime of measurement . Cave-in Depth: depm at which measuring tape stops in the borehole . Waler Level: depth in the borehole where free water is encountered I . Drilling Fluid Level: same as Water Level. except that the liquid in the borehole is drilling fluid The true location of the water table at the boring locations may be different than the water levels measured in the I boreholes. This is possible because there are several factors that can affect the water level measurements in the borehole. Some of these factors include: permeability of each soil layer in profile, presence of perched water, amount of time between water level readings, presence of drilling fluid, weather conditions, and use of borehole I casing. SamDle Storn!!e I Uuless notified to do otherwise. we routinely retain representative samples of the soils recovered from the borings for a period of 30 days, ,. Ai.\1ERlCAN ENGINEERING TESTING, INC. I --- ----- ----------