Date of Award

5-2025

Degree Type

Thesis

Degree Name

Master of Science - Geology

Department

Geology

First Advisor

Dr. Melinda Faulkner

Second Advisor

Dr. Julie Bloxson

Third Advisor

Dr. Alyx Frantzen

Fourth Advisor

Dr. Robert Friedfeld

Abstract

The Saline Mining District of central Arkansas once led U.S. alumina production and hosts extensive bauxite and nepheline syenite deposits. With the depletion of highgrade ore, renewed interest in bauxite stockpiles has focused on critical mineral potential. Previous X-ray Fluorescence studies have identified critical elements in significant concentrations, including uranium (U), thorium (Th), gallium (Ga), molybdenum (Mo), and lanthanides (Ln). This study examines five stockpiles (SP1, Clay, SP2, SP3, and SP4) in Section 20 of the Aluminum Company of America (ALCOA) Saline County bauxite mine, using Xray Diffraction (XRD) on 25 samples to characterize mineral phases and compare them with preliminary X-ray fluorescence (XRF) data. Gibbsite and kaolinite dominate the mineralogy, with gibbsite showing strong positive correlations with zirconium (r = 0.76) and niobium (r = 0.72). Siderite, a minor mineral phase, appears associated with niobium, zirconium, and titanium, suggesting trace metal affinity. A strong inverse relationship between gibbsite and kaolinite (r = -0.96) indicates differing formation pathways. Anatase and rutile show weak correlation (r = 0.16), implying variable titanium mobility. These findings highlight geochemical heterogeneity and may guide future critical mineral exploration, provided technological and economic conditions support resource development.

Creative Commons License

Creative Commons License
This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License.

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