Pleistocene dune deposits along Oregon's mid-coast,
with perched groundwater seeping out along contacts with
paleosols.
Green River Formation and the Piceance Basin, NW
Colorado.The most hydrocarbon-rich acreage on Earth?
(Estimated >1.5 trillion barrels
of in-place oil shale
resources...And site of the only"atomic fracking" during
"Project Rulison", 1969).
(Images from Megan Masterson)
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My research focus is
in hydrogeology and aqueous & sedimentary
geochemistry. My students and I use a variety of
techniques including field studies, laboratory
experiments and analyses, and groundwater and
geochemical modeling to explore the interplay between groundwater and surface
waters and water-rock intereactions.
Specific
areas of current interest and some recent studies
- Groundwater
hydrology, geochemical evolution of groundwaters,
and groundwater interactions in the critical zone:
- Determining
how development and climate change affect groundwater and
secondary cements in coastal dune deposits, central Oregon coast.
- Modeling the
evolution and thermal history of geothermal waters in the Western Cascades.
- Modeling the
effects of thermal energy storage on the porosity & permeability of Columbia
River Basalt aquifers, Portland Basin.
- Assessing hydrochemical
facies and modeling the evolution of groundwater in the hydrocarbon-rich
Piceance Basin, NW Colorado.
- Determining the
hydrostratigraphy of groundwater flow systems in northern
Portland Basin, Columbia River Gorge, upper Deschutes River Basin,
and central Oregon.
- Studying the relative mobility of trace elements from weaterhing of black shales, determining their fate and transport in the surface environment.
- Determining mineralogical changes
accompanying the hydrous retorting of oil shales.
- Assessing the mobility of arsenic from
tuffs and tuffaceous sediments.
- Paleo-environmental
reconstruction using sediment geochemistry:
- Modeling paeloceanographic conditions for the formation of Devonian-Mississippian black
shales, Kentucky.
- Reconstructing
the paleoenvironmental conditions for formation of massive black-shale-hosted phosphate
deposits (Mead Peak Member, Phosphoria Formation), southern Idaho and western Wyoming.
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