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The AAPG/Datapages Combined Publications Database
Environmental Geosciences (DEG)
Abstract
DOI: 10.1046/j.1526-0984.2001.84002.x
Lead Isotopes as Age-Sensitive, Genetic Markers in Hydrocarbons: 1. Copartitioning of Lead with MTBE into Water and Implications for MTBE–Source Correlations
RICHARD W. HURST 1,2, DIANA BARRON 1,MANDISSA WASHINGTON 3,
and SAMUEL A. BOWRING 3
1Department of Geological Sciences, California State University, Los Angeles,
CA 90032
2Hurst & Associates, Inc., 9 Faculty Court,
Thousand Oaks, CA 91360
3
Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute
of Technology, Cambridge, MA 02139
ABSTRACT
The potential of lead isotopes as tracers of methyl tert-butyl ether
(MTBE) in groundwater was assessed in a study that included:
an evaluation of organolead’s chemical affinity with individual
gasoline hydrocarbon constituents; gasoline/water partitioning
experiments; and site-specific investigations of MTBE-
impacted groundwater. Concentrations of organolead were correlated
with concentrations of MTBE, pentane, benzene, toluene,
xylenes, ethylbenzene, 1,2,4-trimethylbenzene, and methyl-
cyclohexane. Significant correlations (R2 > 0.98) were observed
between organolead and methylcyclohexane, MTBE, and benzene;
the latter two being the most water-soluble gasoline constituents.
To evaluate the possible role of MTBE in the transport
of organolead from a product into the aqueous
phase
, two unleaded
gasoline–aqueous partitioning experiments were performed.
Each unleaded gasoline was sequentially extracted with
fresh volumes of water over a period of ~3 weeks; a strong systematic
relationship (R2 = 0.998) was observed between lead
and MTBE in the aqueous
phase
, indicating that the organo-
lead–MTBE chemical affinity in unleaded gasoline was maintained
as these gasoline constituents partitioned into water. The
lead isotopic equilibrium between unleaded gasoline and aqueous-
phase
lead also supports this conclusion. Site-specific analyses
of groundwater impacted by MTBE corroborate the laboratory
results, showing that groundwater impacted by MTBE
releases exhibit lead isotopic ratios identical to those of unleaded
gasoline responsible for the release. Our results also suggest
that the fate/transport of MTBE plumes can be monitored
by integrated lead/MTBE data, possibly to distances exceeding
500 m from the source of the release.
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