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Technology Status Report: In Situ Flushing - CLU-IN

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<strong>In</strong> <strong>Situ</strong> <strong>Flushing</strong> Project Summaries<br />

GWRTAC Case Study Database<br />

GWRTAC ID: FLSH0078<br />

Project Name: PPG Plant, Lake Charles, LA<br />

City: Lake Charles State/Province: LA<br />

Primary GWRTAC Personal<br />

Communication Source<br />

(Name/Organization):<br />

<strong>Report</strong>(s)/Publication(s) (GWRTAC Source):<br />

"Surfactant-Enhanced DNAPL Remediation at a Highly Heterogeneous Site", John Fountain,<br />

Geology Department, State University of New York at Buffalo, presented May 6, 1998 at<br />

GWRTAC/U.S. EPA TIO "Advances in Ground-Water Remedation Conference", San Francisco, CA<br />

Project Summary:<br />

The following text was excerpted from "Surfactant-Enhanced DNAPL Remediation at a Highly<br />

Heterogeneous Site", John Fountain, Geology Department, State University of New York at<br />

Buffalo, presented May 6, 1998 at GWRTAC/U.S. EPA TIO "Advances in Ground-Water<br />

Remedation Conference", San Francisco, CA:<br />

At the PPG Plant in Lake Charles, Louisiana, a site with known DNAPL (primarily dichloroethane -<br />

EDC) contamination, a pilot test was undertaken to effect DNAPL source zone remediation. The<br />

site is underlain by a thick sequence of interbedded clays and thin sands of fluvial-deltaic and<br />

marine origin (Holocene and Pleistocene aged Beaumont or Prarie Formation). The site<br />

hydrostratigraphy is thus complex, and a regional aquifer (Chicot Aquifer) is present at depth.<br />

The surfactant field test was conducted in 1997-1998, only in the shallowest water-bearing unit, the<br />

"10 foot sand", which had been consistently found beneath the site at about 10 feet bgs. DNAPL<br />

was likely present in the sand layer based on cone penetrometer testing and analysis of<br />

groundwater samples collected from monitoring wells. The DNAPL primarily consists on<br />

dichloroethane, or EDC. A sand layer at 20 feet was also contaminated. Grain size analysis<br />

showed that a one foot sand zone was present at 10.5 feet bgs, and another foot of silty sand was<br />

present beneath this one foot sand zone. Permeameter tests on core samples revealed hydraulic<br />

conductivities ranging from 6 x 10-3 cm/sec in sand to

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