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Proposed Bridgestone April 20, 2011<br />

NWC of Vance St. & W. Center Ave. PSI Project No. 532281<br />

Lakewood, Colorado Page 3 of 15<br />

sedimentary bedrock in the borings at depths of 5 ½ to 8 feet below the existing grade<br />

and consisted of brown, red, brown, and light brown, moist, hard, sandy claystone. The<br />

following table present the materials encountered during our investigation.<br />

Material / Property<br />

Thickness Encountered<br />

Dry Density (pcf)<br />

Moisture Content (%)<br />

*Percent Swell (%)<br />

Liquid Limit (%)<br />

Plastic Limit (%)<br />

Blows per foot<br />

Sandy<br />

Range 0 ft 100 – 112 13 – 20 1.6 – 11.2 54 – 60 21 – 22 21 – 58<br />

Clay Average 0 ft 105 17 7.4 58 22 38<br />

Sandy<br />

Claystone<br />

Bedrock<br />

Range 5 ½ - 8 100 – 107 19 – 26 0.3 – 1.2 - - 50+<br />

Average 8 ft 103 22 0.9 - - 50+<br />

PSI performed Denver Swell Testing on selected samples collected during our field<br />

investigation. The testing yielded swell percentages ranging from 0.3 to 11.2 percent<br />

when wetted under a 250, 500, or 1,000 psf surcharge pressure. Based on these swell<br />

percentages, PSI has classified this site as having “high” swell potential. The<br />

development at this site will need to be designed for high swelling soils.<br />

The Boring Logs illustrated in Figures 3 through 11 should be reviewed for specific<br />

information at individual boring locations. These records include soil descriptions,<br />

stratifications, penetration resistances, locations of the samples and laboratory test data.<br />

3.2.2 Groundwater Conditions<br />

Groundwater was not encountered during our drilling operations. However, it should be<br />

noted that it is possible for the groundwater table to fluctuate during the year depending<br />

upon climatic and rainfall conditions and changes to surface topography and drainage<br />

patterns. Also, based on our laboratory data, the sandy claystone may be saturated.<br />

Discontinuous zones of perched water may also exist, or develop, within the overburden<br />

materials subsequent to the construction of the pump station. The groundwater levels<br />

presented in this report are the levels that were measured at the time of our field<br />

activities.

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