Monday,
October 14, 2024
6:00 - 7:30 pm
Note: ETGS members will receive an email with info for logging into the meeting.
October Presentation
Pyrite Oxidation in Rocks: From Atomic Observation to Global Implications
By
Xin Gu
Geochemist
Oak Ridge National Laboratory (ORNL)
Abstract
Pyrite oxidation is a crucial reaction influencing
geochemical cycles of iron, sulfur, carbon, and oxygen. To interpret
pyrite oxidation throughout Earth's geologic history, we must first
understand the current controls on its oxidation rate. We propose a
model for pyrite oxidation across various scales: grain, clast,
borehole, and watershed. At the atomic scale, the oxidation rate is
limited by the interfacial reaction between oxygen and sulfide. At
the pyrite grain scale, evidence suggests that oxygen diffusion to
the oxidation front limits the rate. At the pedon scale, diffusion
is constrained by fracture formation rates. Finally, at the borehole
scale, the rate at which oxygenated water reaches unoxidized pyrite
at depth is limited by the erosive removal of overlying soil and
weathered rock. Thus, as the scale of observation increases, the
rate-limiting step for pyrite oxidation transitions from chemical
reaction → diffusion → fracturing → erosion.
Biography
Xin Gu is a broadly trained critical zone scientist with degrees in Environmental Engineering (B.E., Tsinghua University), Forest Resources (M.S., Penn State University), and Geosciences and Biogeochemistry (Ph.D., Penn State University). From 2018 to 2021, he worked at the Earth and Environmental Systems Institute at Penn State as a PostDoc and later as an Assistant Research Professor. Since 2021, he has been an experimental geochemist in the Environmental Division at Oak Ridge National Laboratory. His research focuses on how geochemical reactions at pore scales drive macroscopic processes such as chemical weathering, watershed hydrology, and landscape evolution.
Greetings, and welcome to the October 14, 2024 ETGS
hybrid meeting.
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