Current Research:
Generally, the focus of my research is using the Uranium and
Thorium decay series nuclides (238U -> 206Pb, 235U
-> 207Pb, and 232Th -> 208Pb) to
constrain time scales of volcanic processes.
More specifically, my current investigation involves the collection and
analysis of radium and radon from hot springs and hydrothermal features in
Yellowstone National Park. The ratios of
parent to daughter nuclides (226Ra/222Rn, 223Ra/219Rn,
and 224Ra/220Rn) and the corresponding equilibrium or
disequilibrium, accordingly, can theoretically be used to constrain time scales
of hydrothermal fluid dynamics and hydrothermal fluid – rock interactions
within the Yellowstone Caldera (Sturchio et al., 1993). Potential insight(s) gained from this
investigation can augment our understanding of volcanic hydrothermal systems
and provide an analogue that can be used on a broader scale in volcanic and
magmatic processes and their associated hydrothermal systems worldwide.

Looking down in to the Crater of Mt. St. Helens, WA (6/2011)