Title Information
Title
Tracing Planetary Scale Volatile Cycling with Inert Gases: A Combined Experimental and Numerical Approach
Name: Personal
Name Part
Krantz, John A
Role
Role Term: Text
creator
Name: Personal
Name Part
Parman, Stephen
Role
Role Term: Text
Advisor
Name: Personal
Name Part
Saal, Alberto
Role
Role Term: Text
Reader
Name: Personal
Name Part
Cooper, Reid
Role
Role Term: Text
Reader
Name: Personal
Name Part
Huber, Christian
Role
Role Term: Text
Reader
Name: Personal
Name Part
Barry, Peter
Role
Role Term: Text
Reader
Name: Corporate
Name Part
Brown University. Department of Earth, Environmental, and Planetary Sciences
Role
Role Term: Text
sponsor
Origin Information
Copyright Date
2019
Physical Description
Extent
xii, 177 p.
digitalOrigin
born digital
Note: thesis
Thesis (Ph. D.)--Brown University, 2019
Genre (aat)
theses
Abstract
Abstract of Tracing Planetary Scale Volatile Cycling with Inert Gases: A Combined Experimental and Numerical Approach, by John A. Krantz, Ph.D., Brown University, May 2020. To better understand the origin of Earth’s volatiles, this thesis represents the results of experiments and numerical models. Despite being physically and biologically important, volatiles like water and carbon dioxide are challenging subjects for analytical investigation. They readily react with any number of other materials and have limited potential for isotopic analysis. There are, however, other volatiles which are less reactive and have a greater variety of isotopic information available. At the extreme opposite end of reactivity are the nominally inert noble gases. The noble gases experience the same physical processes which the major, life-essential volatiles experience without the complexity of chemical interactions. As such, this thesis focuses on improving our understanding of how the noble gases interact with geological materials—particularly during subduction—and the implications thereof. Experimentally-measured solubilities for the full suite of noble gases in natural serpentinite are presented. Serpentinite fractionates the heavy noble gases, with solubilities increasing from Ar to Kr to Xe. Kr/Ar and Xe/Ar ratios in MORB are quite like those predicted for subducted serpentinite, consistent with most heavy noble gases in the MORB-source coming from subducted serpentinite. The results of our model constrain the degree to which the mantle has been processed. The constraints from the coupled N-Xe system are also used to model the evolution of H. These results show that volatile input to the mantle increased during the Archean, consistent with models of the onset of subduction. We also explore the long-term effects of ingassing and outgassing on a planet without subduction. Where the surface of the Earth has been repeatedly processed through mantle melting and subduction, the Martian surface has been, effectively, preserved since its earliest formation. Hydrous minerals, especially clays, produced in the crust in the presence of an early steam atmosphere and hydrosphere could have incorporated and sequestered substantial amounts of Xe. This Xe could be reintroduced to the atmosphere over billion-year timescales, producing the 129Xe anomaly seen today.
Subject (fast) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/01756663")
Topic
Igneous rocks
Subject (fast) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/00938685")
Topic
Gases, Rare
Subject
Topic
Planets--Geology (Planetary geology)
Subject (fast) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/01065128")
Topic
Planets--Atmospheres
Language
Language Term (ISO639-2B)
English
Record Information
Record Content Source (marcorg)
RPB
Record Creation Date (encoding="iso8601")
20200720
Access Condition: rights statement (href="http://rightsstatements.org/vocab/InC/1.0/")
In Copyright
Access Condition: restriction on access
Collection is open for research.
Type of Resource (primo)
dissertations