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page 2 <br /> 1604 B Street <br /> Review of the historical soil analytical data for this site indicates that, with the exception <br /> of the tank pull results at 12 to 14 feet bsg, soil contamination is present at intervals from <br /> approximately 35 to 66 feet bsg. There is no indication from the available data that there <br /> is soil contamination above 25 feet bsg in the area of the proposed SVE well. <br /> Section 5.0, Proposed Pilot Test and Rationale, states that "Airflow pathways are <br /> predicted to be radial outward from the air sparge well through the permeable sandy <br /> formation overlying the clay boundary at approximately 27 feet bsg." This statement is <br /> unclear, as the stated depth of the AS well screen interval is from 57 to 60 feet bsg. <br /> Boring logs for the site indicate a sand lens extending from approximately 23 to 27 feet <br /> bsg, with clayey silts, clayey sands and silty clay from 27 feet to approximately 53 feet <br /> bsg. Below 53 feet bsg the lithology is mostly sand to 70 feet bsg. PHS/EHD is <br /> concerned about the efficacy of a SVE well which is screened to 25 feet bsg in being <br /> able to capture vapors associated with an AS well screened at 60 feet bsg, when there is <br /> a 25 to 30 foot interval of silts and clays between them. The EPA document How to <br /> Evaluate Alternative Cleanup Technologies for Underground Storage Tank Sites, <br /> Chapter 7-Air Sparging, page VII-6, states that air sparging cannot be used to treat <br /> groundwater in a confined aquifer because the injected air would be trapped by the <br /> saturated confining layer and could not escape to the unsaturated zone. The document <br /> further states, on page VII-14, that stratified or highly variable heterogeneous soils <br /> typically create the greatest barriers to air sparging. Both the injected air and the <br /> stripped vapors will travel along the paths of least resistance (coarse-grained zones) and <br /> could travel a great lateral distance from the injection point. <br /> Section 5.0 also discusses the use of a tracer gas (helium) as an indicator compound of <br /> the radius of influence (ROI) of the injected air. Section 6.0 Pilot Test Objectives states <br /> that the first objective is to "Estimate the air sparge ROI by using tracer gas in the <br /> injected air and by monitoring vadose zone soil gas composition to detect its presence at <br /> nearby observation points." However, details of how the vadose zone soil gas will be <br /> monitored, or specifically what 'observation points' are being referred to, are not included <br /> in the work plan. These points must be clarified in writing to PHS/EHD. <br /> Further in Section 6.0, under the title "Air Sparge and Limited Vapor Extraction Test," the <br /> work plan states that"the vapor extraction unit will produce a vacuum cone of <br /> depression within the area of air injection and toward the three grouped vapor extraction <br /> wells." The meaning of this statement is also unclear. Please note that 'cone of <br /> depression' is a hydrogeologic term referring to the cone shaped lowering of the <br /> potentiometric surface of groundwater as a result of pumping influences. A statement is <br /> made that equations that will be used to calculate the AS ROI are included in the <br /> attachments [of the work plan]. However, no attachments were included in the <br /> submitted work plan. <br /> PHS/EHD approves the proposed geoprobe boring and depth discrete water sampling. <br /> This work is currently scheduled to be performed on May 22, 2001. PHS/EHD will <br /> proceed with issuance of the boring permit for this phase of the work plan. In <br /> discussions with PSI, it was agreed that the SVE well would be built to 40 feet bsg, <br /> instead of 25 feet bsg. As discussed above, PHS/EHD has serious reservations about <br /> the objectives and potential effectiveness of the proposed AS/SVE pilot test. However, if <br />