From: | bmolnaa@earthtech.com |
Date: | 7 Aug 2001 18:41:22 -0000 |
Reply: | cpeo-military |
Subject: | Re: [CPEO-MEF] Irvine Desalter/TCE remediation project |
The California definition of an aquifer is more stringent than EPA's. By requiring TDS to be no more than 3,000 mg/L, the state is ensuring that drinking water is provided with a TDS of <3,000. The EPA definition of an aquifer with TDS of no more than 10,000 mg/L ensures that drinking water is provided with a TDS of <10,000. As a result, the EPA definition of an aquifer is more liberal than California's. There isn't much of a difference in the yield requirement. I also wanted to comment on Doobage's remarks regarding natural attenuation. Although we may differ in our beliefs of whether or not natural attenuation is a viable remedy for sites, I do agree with the comment that "the greater percentage of natural attenuation remedies nationwide has not observed those(the EPA's) requirements." I would encourage those in the regulatory community to be aware of the EPA requirements and adopt them as minimum standards for evaluating natural attenuation. Date: Fri, 03 Aug 2001 17:00:40 -0700 From: petestrauss1@home.com Subject: Re: [CPEO-MEF] Irvine Desalter/TCE remediation project In reviewing a specific project at Moffett Field, I noted that EPA's definition of "potential drinking water" includes groundwater with a Total Dissolved Solids (TDS) concentration of 10,000 mg/L or less, and an average yield of 150 gallons per day (gpd), as compared with the California State Water Board's definition of TDS at 3,000 mg/L or less and an average yield of 200 gpd. That means that in terms of defining potential drinking water, the federal government is more stringent than California, and covers a wider swath of groundwater. EPA's definition trumps California's until the state has an EPA-endorsed Comprehensive State Groundwater Protection Program. Peter ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ | |
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