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CAMBRIA <br /> STANDARD FIELD PROCEDURES FOR <br /> CONE PENETROMETER TESTING AND SAMPLING <br /> This document describes Cambria Environmental Technology's standard field methods for Cone Penetrometer <br /> Testing(CPT)and direct-push soil and groundwater sampling. These procedures are designed to comply with <br /> Federal, State and local regulatory guidelines. <br /> Use of CPT for logging and soil and groundwater sampling requires separate borings. Typically an initial <br /> boring is advanced to estimate soil and groundwater characteristics as described below. To collect soil samples <br /> a separate boring must be advanced using a soil sampling device. If groundwater samples are collected, <br /> another separate boring must be advanced using a groundwater sampling device. Specific field procedures are <br /> summarized below. <br /> Cone Penetrometer Testing (CPT) <br /> Cone Penetrometer Testing is performed by a trained geologist or engineer working under the supervision of a <br /> California Registered Geologist(RG)or a Certified Engineering Geologist(CEG). Cone Penetrometer Tests <br /> (CPT) are carried out by pushing an integrated electronic piezocone into the subsurface. The piezocone is <br /> pushed using a specially designed CPT rig with a force capacity of 20 to 25 tons.The piezocones are capable <br /> of recording the following parameters: <br /> Tip Resistance(Qc) <br /> Sleeve Friction (Fs) <br /> Pore Water Pressure (U) <br /> Bulk Soil Resistivity(rho) - with an added module <br /> A compression cone is used for each CPT sounding. Piezocones with rated load capacities of 5, 10 or 20 tons <br /> are used depending on soil conditions. The 5 and 10 ton cones have a tip area of 10 sq. cm. and a friction <br /> sleeve area of 150 sq. cm. The 20 ton cones have a tip area of 15 sq.cm. and a friction sleeve area of 250 sq. <br /> cm. A pore water pressure filter is located directly behind the cone tip. Each of the filters is saturated in <br /> glycerin under vacuum pressure prior to penetration. Pore Pressure Dissipation Tests(PPDT)are recorded at 5 <br /> second intervals during pauses in penetration. The equilibrium pore water pressure from the dissipation test <br /> can be used to identify the depth to groundwater. <br /> The measured parameters are printed simultaneously on a printer and stored on a computer disk for future <br /> analysis. All CPTs are carried out in accordance with ASTM D-3441. A complete set of baseline readings is <br /> taken prior to each sounding to determine any zero load offsets. <br /> The inferred stratigraphic profile at each CPT location is included on the plotted CPT logs. The stratigraphic <br /> interpretations are based on relationships between cone bearing(Qc)and friction ratio(Rf). The friction ratio <br /> is a calculated parameter(Fs/Qc)used in conjunction with the cone bearing to identify the soil type.Generally, <br /> soft cohesive soils have low cone bearing pressures and high friction ratios. Cohesionless soils(sands) have <br /> high cone bearing pressures and low friction ratios. The classification of soils is based on correlations <br /> developed by Robertson et al(1986). It is not always possible to clearly identify a soil type based on Qc and <br /> Rf alone. Correlation with existing soils information and analysis of pore water pressure measurements should <br /> also be used in determining soil type. <br /> CPT and sampling equipment are steam-cleaned or washed prior to work and between borings to prevent <br /> cross-contamination. Sampling equipment is washed between samples with trisodium phosphate or an <br /> equivalent EPA-approved detergent. Groundwater samples are decanted into appropriate containers supplied <br />