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University of Arkansas

Infrared Spectra Analysis of Thermally Altered Iron Phyllosilicates and the Implications for Mars

Abstract

dc:description.abstract

<p>This study looks at two iron-rich phyllosilicates, which may be present on Mars. The minerals, greenalite and hisingerite, are rich in iron-II and iron-III, respectively. Small samples (~0.40 grams) of each mineral were crushed and heated in a Lindberg Tube Oven for approximately twenty-four hours at temperatures selected to mimic lava flows and impact events. Following heating, each sample was placed in a Fourier Transform Infrared (FT-IR) spectrometer to collect the near- and mid-infrared spectra. The spectra allowed for these terrestrial analogs to be analyzed with regards to how their structure breaks down with increasing temperature. The samples' colors were also recorded and show varying degrees of oxidation following heating, which is expected in the oxygen-rich ambient atmosphere they were heated under. It is apparent from the spectra that for greenalite, heating at 765°C and higher breaks the mineral down into hematite and a high-temperature silica, such as cristobalite. Hisingerite exhibits the same behavior, but its basic spectra structure is retained in the 710°C sample. The near-infrared spectra were compared with spectra from different locations on Mars, collected by both Mars Express and the Mars Reconnaissance Orbiter. The spectra were also compared with each other to allow for analysis of how the iron-III polymorph of a mineral reacts differently from its iron-II counterpart. The multiple facets of the study aim to help understand the current state, history, and evolution of Mars, specifically if clay formation occurred deep in Mars' past or as the result of impact-induced hydrothermal activity more recently in its history.</p>

Degree

thesis:*
Name thesis:degree_name
Master of Science in Space & Planetary Sciences (MS)
Level thesis:degree_level
Thesis
Year dc:date.available
2013

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Bryan, William Thomas
Advisor dc:contributor.advisor
  • Chevrier, Vincent F.
Contributors dc:contributor
  • Dixon, John C.
  • Roe, Larry A.

Subjects

dc:subject × 10

Identifiers

dc:identifier.*
Repository record dc:identifier
https://scholarworks.uark.edu/etd/941
OAI identifier oai:identifier
oai:scholarworks.uark.edu:etd-1940

Chain of custody

source
Harvested from
University of Arkansas
Base URL
scholarworks.uark.edu/do/oai/
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
citation

Bryan, William Thomas. Infrared Spectra Analysis of Thermally Altered Iron Phyllosilicates and the Implications for Mars. Thesis thesis, 2013. https://scholarworks.uark.edu/etd/941