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Integrated Assessment Halaco Engineering Company ... - Archives

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<strong>Halaco</strong> <strong>Engineering</strong> Co. IA Section 3<br />

CAD009688052<br />

The definitive VOC results for waste samples include ten subsurface samples collected at various<br />

depths from the WMU area. Sample SW5-2/15 exhibited a detectable concentration of 5.9 ug/kg<br />

carbon disulfide. Sample SW2-1/10 exhibited an approximate concentration of 10 ug/kg<br />

tricholorofluoromethane. Sample SW2-3/15 exhibited an approximate concentration of 5.1<br />

ug/kg carbon disulfide. Sample SW3-3/5 exhibited an approximate concentration of 42 ug/kg 2-<br />

butanone. Sample locations are plotted on Figures 3-1 and 3-2.<br />

3.2.2 Water Matrix Samples<br />

WESTON® submitted ten unfiltered surface water, and fourteen unfiltered groundwater samples<br />

for definitive analysis for metals, radionuclides, and VOCs in accordance with the SAP.<br />

3.2.2.1 Definitive Metals Results<br />

Metals analyses were performed on 24 unfiltered water samples by EPA Method 6010B. Sample<br />

results are presented in Table 3-5.<br />

Results of the six surface water samples collected from the OID and the connected water body to<br />

the south of the WMU are compared to the four background surface water samples collected<br />

upgradient (north) in the OID. Four out of the six samples have results exceeding three-times the<br />

highest background concentration for at least one of the following metals: Al, Ba, Cd, Cu, Mg,<br />

Mn, V, and Zn.<br />

Results of the groundwater samples are based on a comparison of samples collected from<br />

upgradient and downgradient wells. The determination of the groundwater gradient is based on<br />

the elevations of groundwater measured in the field in June 2006, and is consistent with previous<br />

groundwater sampling performed by <strong>Halaco</strong> contractors (23). The groundwater gradient and<br />

locations of the monitoring wells are shown in Figure 3-3. Groundwater under the site flows<br />

broadly to the northeast, except in the northwestern portion of the Site. The groundwater<br />

gradient in the northwestern portion of the Site is to the north-northwest, and is interpolated<br />

largely from the anomalously low groundwater elevation observed at MW-15. Based on the<br />

overall site groundwater gradient, MW-5 is the most upgradient groundwater location on the Site.<br />

The results for the groundwater data are compared to values that are three-times those observed<br />

in the background well, MW-5. All eighteen wells yield results exceeding three-times the<br />

concentration observed in the background well for at least one of the following metals: Al, Sb,<br />

As, Ba, Be, Cd, Co, Cu, Fe, Pb, Mg, Mn, Ni, Ag, V, and Zn.<br />

3.2.2.2 Radionuclides<br />

Laboratory analysis of the target radionuclide suite was performed by EPA 901.1 for 137 Cs and<br />

40 K, and DOE EML HASL-300, Th-01-RC Modified for 228 Th, 230 Th, and 232 Th on ten surface<br />

water and thirteen groundwater samples. The target radionuclide 137 Cs was not detected in any of<br />

the water samples. The results are presented in Table 3-6 and discussed below.<br />

18

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