Laserfiche WebLink
Page 4 <br /> Tracy Tire Fire <br /> Celeste Temple,Project Officer <br /> Environmental Sciences Consultants (N&M) in Irvine, California for analysis of permeability <br /> using American Society for Testing Materials Method D5084 (ASTM D5084), Atterberg Limits <br /> (ASTM D4318-95), and Sieve Analysis (ASTM D422-63). The results are summarized in Table <br /> 1 below. <br /> Table 1 <br /> Geotechnical Analytical Results Summar <br /> Atterberg Limits <br /> Sample Permeability USCS Soil Type <br /> LL PL I PI (cm/sec) <br /> G-1 (1'9"-2'9") 47 24 23 2.5 x 10-8 CL <br /> G-1 (6'0"-7'0") 45 24 21 3.8 x 10-7 CL <br /> G-1 (7'0"-7'8") 44 22 22 CL <br /> G-2 (5'0"-6'0") 39 21 18 CL <br /> G-2 (11'0"-12'0") — — — SW-SM <br /> __J <br /> Where: <br /> LL=Liquid Limit PI=Plasticity Index CL=Low-plasticity clay <br /> PL=Plastic Limit cm/sec=centimeters per second SW-SM=Well graded to silty sand <br /> N&M was unable to test the permeability of three of the five samples submitted, due to low <br /> sample volume. N&M was able to test the permeability of the two samples listed above, because <br /> a significantly smaller volume was required for testing of those consolidated, predominantly fine- <br /> grained samples. Thus, the permeability values shown in the table should represent the lowest of <br /> the soils. Because the samples were also classified as sand and gravel (see Attachment B), the <br /> permeability can be much greater, possibly as great as 1 x 10-' cm/sec. It is important to note that <br /> the permeability of the geologic materials varies widely, and that several clay layers may act to <br /> retard the transmission of groundwater infiltrating from the surface. <br /> In addition to the GeoprobeTM sampling, IWMB personnel excavated trenches using a trackhoe to <br /> provide an exposed cross-section for the START geologist to observe. The geologic materials <br /> observed were consistent with the samples collected using the GeoprobeTM: interbedded gravel, <br /> sand, silt, and clay. However, one trench was excavated to a depth of approximately 20 feet, and <br /> groundwater was observed at a depth of approximately 15 feet in the trench. At the request of <br /> the OSC, a groundwater sample (T-1) was collected and submitted to the laboratory of Curtis & <br /> Tompkins, Ltd. in Berkeley, California and analyzed for the contaminants of concern: volatile <br /> organic compounds (VOCs), semi-volatile organic compounds (SVOCs), phenols, and metals. <br /> No VOC, SVOC, or phenol constituent was detected. Some metals of concern were detected. <br /> Laboratory analytical results indicated that the levels of arsenic and lead in the groundwater <br /> exceed the EPA Region 9 Preliminary Remediation Goals (PRGs) for these metals; however, no <br /> 1:\000610\SF389_0339TTRZXX\ITTzur30.799.wpd <br /> 10/17/99 6:56 PM <br />