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Mineralogical evidence of galvanic corrosion in drinking water lead pipe joints Michael K. DeSantis, Simoni Triantafyllidou, Michael Schock, and Darren A Lytle Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.7b06010 • Publication Date (Web): 15 Feb 2018 Downloaded from http://pubs.acs.org on February 16, 2018
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Environmental Science & Technology
Mineralogical Evidence of Galvanic Corrosion in Drinking Water Lead Pipe Joints
Michael K. DeSantis*,1, Simoni Triantafyllidou2, Michael R. Schock2, Darren A. Lytle2 1
ORISE Post-Doctoral Fellow at the U.S Environmental Protection Agency, Cincinnati, Ohio
45268 2
National Risk Management Research Laboratory, U.S. Environmental Protection Agency, 26 W.
Martin Luther King Dr., Cincinnati, OH 45268 *Corresponding author’s contact information: 26 West Martin Luther King Drive, Cincinnati, Ohio 45268, United States, Phone: +1 513 569 7939; E-mail:
[email protected] Abstract Galvanic corrosion as a mechanism of toxic lead release into drinking water has been under scientific debate in the U.S. for over 30 years. Visual and mineralogical analysis of 28 lead pipe joints, excavated after 60+ years from 8 U.S. water utilities, provided the first direct view of three distinct galvanic corrosion patterns in practice: (1) no evidence of galvanic corrosion; (2) galvanic corrosion with lead cathode; (3) galvanic corrosion with lead anode. Pattern 3 is consistent with empirical galvanic series (leadbrasscopper in order of increasing nobility) and poses the greatest risk of Pb exposure. Pattern 2 is consistent with galvanic battery reversion. The identification of copper-sulfate minerals (Pattern 2), and lead-sulfate and lead-chloride minerals (Pattern 3) in galvanic zones illustrated the migration of chloride and sulfate toward the anode. Geochemical modeling confirmed the required pH drop from the bulk water level to at least pH 3.0-4.0 (Pattern 2) and pH
