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Final Second Five-Year Review Report Fort Ord Superfund Site ...

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and 0.098 ppbv). Both the indoor and outdoor samples collected at Lexington Court were within the<br />

range of background concentrations 0.067 ppbv and 0.13 ppbv measured in outdoor air during the <strong>Fort</strong><br />

<strong>Ord</strong> outdoor air monitoring. These results then support the conclusion that groundwater contamination<br />

appears to be an insignificant contributing source of VOCs to indoor air in the source area<br />

(MACTEC, 2006b).<br />

11.1.2 Groundwater<br />

The upper three aquifers at the former <strong>Fort</strong> <strong>Ord</strong>, none of which are currently used as a drinking water<br />

source within the OUCTP, have been found to contain concentrations above MCLs for CT and other<br />

VOCs within the OUCTP. The aquifer cleanup levels are listed in Table 7. The presence of CT in these<br />

three aquifers is described below.<br />

A-Aquifer Groundwater<br />

The length of the CT plume in the A-Aquifer is approximately 1.6 miles, and ranges from 500 to 750 feet<br />

in width along the length of the plume (see Plate 3). The State MCL for CT in groundwater is 0.5 μg/L,<br />

and the maximum historic detected concentration in the A-Aquifer since groundwater monitoring was<br />

initiated in 1992 was 19 μg/L. The most recent maximum concentration of CT detected in the A-Aquifer<br />

was 15 μg/L. Low levels of PCE and TCE have also been identified in the A-Aquifer within the OUCTP.<br />

Hydraulic communication between this A-Aquifer and underlying aquifers is limited to those areas west<br />

of the OUCTP where the <strong>Fort</strong> <strong>Ord</strong>-Salinas Valley Aquiclude clay unit pinches out, or where it has been<br />

penetrated by wells without adequate sanitary seals. Two such vertical conduits have been identified and<br />

have resulted in the migration of CT from the A-Aquifer to the underlying Upper and Lower 180-Foot<br />

Aquifers. All identified vertical conduits have been destroyed (grouted and sealed) eliminating hydraulic<br />

communication between the A-Aquifer and the underlying aquifers.<br />

Upper 180-Foot Aquifer<br />

There are two narrow, parallel plumes in this aquifer as shown on Plate 3. The western CT plume in the<br />

Upper 180-Foot Aquifer is approximately 0.7 miles in length and 400 feet in width. The eastern CT<br />

plume in the Upper 180-Foot Aquifer is approximately 0.9 miles in length and ranges from 200 to 600<br />

feet in width. The maximum historic detected concentration in the Upper 180-Foot Aquifer since<br />

groundwater monitoring was initiated was 9.8 μg/L. The most recent maximum concentration of CT<br />

detected in the Upper 180-Foot Aquifer was 3.5 μg/L.<br />

Lower 180-Foot Aquifer<br />

There are two separate plumes in this aquifer. The northern CT plume in the Lower 180-Foot Aquifer is<br />

approximately 0.75 miles in length and 1,000 feet in width. The maximum historic detected<br />

concentration in the Lower 180-Foot Aquifer since groundwater monitoring was initiated was 6.95 μg/L.<br />

The most recent maximum concentration of CT detected in the Lower 180-Foot Aquifer was 3.6 μg/L.<br />

Low levels of 1,2-DCA have also been detected in the Lower 180-Foot Aquifer.<br />

11.2 Remedial Actions<br />

11.2.1 Remedy Selection<br />

The following four alternatives were evaluated in the FS (MACTEC, 2006b).<br />

<strong>Final</strong><br />

11-2<br />

FORMER FT ORD 5YR REVIEW 2007_FINAL United States Department of the Army

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