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Kaye Savage Ph.D. Stanford University, 2001
Environmental Geochemistry
Email: k.savage@vanderbilt.edu Office: 6702 General Interests Kaye Savage is interested in physical and geochemical processes which control the distribution and speciation of trace elements at and near the earth’s surface, particularly in mineralized environments. Characterization of soils, sediments, and weathering rock, and waters in contact with these materials, are her primary focus. This type of research aids efforts to remediate contaminated mine sites, as well as providing fundamental information about interactions between mineral surfaces and aqueous environments. Current Research Savage’s
recent work has concentrated on gold mine sites in California, examining
arsenic geochemistry within tailings piles, mineralized outcrops, and an open
pit mine lake. Because the toxicity of arsenic is related to its chemical
form, understanding the behavior of arsenic in natural systems is critical for
assessing its potential health effects and mitigating its hazards in watershed
and storage areas. In the Mother Lode Gold Mining District of California,
located along the western foothills of the Sierra Nevada mountains, arsenic is
found in naturally occurring sulfide minerals such as pyrite ("fool's
gold") and arsenopyrite. These minerals are concentrated in mine
tailings, composed of waste rock and ore that has undergone varying degrees of
crushing and chemical processing. When the arsenic minerals decompose during
weathering, arsenic is released into more soluble minerals and into lake and
river waters which react with the mine waste. Differences in the mode of
arsenic uptake, mineral solubilities, and stabilities in different types of
aqueous environments have significant consequences for release of arsenic to
surface and ground waters.
Distribution of arsenic in an open mine
pit lake over time. Hot colors represent seasonally high arsenic
concentrations, up to about 1100 µg/L.
Atomic structure of pyrite showing
arsenic substitution for sulfur in its structure, based on X-ray absorption
spectroscopy undertaken at the Stanford Synchrotron Radiation Laboratory. Other ongoing and new
projects include studies of arsenic uptake in sulfate minerals, potential
environmental impacts to soils from smelter fallout in the Pacific Northwest,
oxidation rates of arsenian pyrite, and impacts
of mining in the southeastern U.S. What Students Do
There are opportunities for students with a wide assortment of
interests and backgrounds to participate in environmental geochemistry/water
resources research. The use of information at different spatial scales, from
field maps to molecular interactions, provides a means of introducing students
to a variety of environmental geochemistry approaches. Students use a variety
of techniques to address environmental problems: field mapping and sampling,
spectroscopic analysis, wet chemical experimentation with model analogs to
field conditions, and predictive modeling using equilibrium concepts and
irreversible reaction paths. Students interested in public policy or economics
will also find opportunities to explore, since many sites with significant
contamination are also targets of public interest and government action. Selected Publications Savage,
K.S., Tingle, T.N., O'Day, P.A., Waychunas, G.A., and Bird, D.K. (2000)
Arsenic speciation in pyrite and secondary weathering phases, Southern Mother
Lode Gold District, Tuolumne County, California. Applied
Geochemistry 15(8):1219-1244. Savage,
K.S., Bird, D.K., and Ashley, R. A. (2000) Legacy of the California gold rush:
environmental geochemistry of arsenic in the southern Mother Lode Gold
District. International Geology Review
42(5):385-415. Ashley, R.A. and Savage, K.S.
(2001) Analytical data for waters of the Harvard open pit, Jamestown Mine,
Tuolumne County, California, March 1998 – September 1999. USGS Open File
Report OF-01-74 v. 1.0 Savage, K.S., Ashley, R.A., and
Bird, D.K. (2000) Wall rock geochemical contributions to a high-arsenic,
alkaline pit lake at the Jamestown Mine, California. Eos,
Transactions, American Geophysical Union, 81(48):F525. Savage, K. S., Bird, D.K., and
O’Day, P.A. (2000) Arsenic distribution in iron sulfate minerals associated
with pyrite oxidation: natural and synthetic samples. Geological Society of America Abstracts with Programs, 32(7):A109 Savage, K. S., Bird, D.K., O’Day, P.A. and Mehta, A. (1999) Characterization of synthetic and natural arsenian jarosite using synchrotron x-ray techniques. Eos, Transactions, American Geophysical Union 80(46):F378. Field Trips
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