NASA Logo

NTRS

NTRS - NASA Technical Reports Server

Back to Results
Thermal Analysis, Compressibility, and Decomposition of Synthetic Bastnäsite-(La) to Lanthanum OxyfluorideUnderstanding basic material properties of rare earth element (REE) bearing minerals such as their phase stability and equations of state can assist in understanding how economically viable deposits might form. Bastnäsite is the most commonly mined REE bearing mineral. We synthesized the lanthanum-fluoride end member, bastnäsite-(La) (LaCO3F), and investigated its thermal behavior and decomposition products from 298 K to 1173 K under ambient pressure conditions through thermogravimetric analysis, differential scanning calorimetry, evolved gas analysis, and high temperature powder X-ray diffraction. We also investigated the compressibility of bastnäsite-(La) via single crystal X-ray diffraction in diamond anvil cells at an ambient temperature up to 11.3 GPa and from 4.9 GPa to 7.7 GPa up to 673 K. At ambient pressure, bastnäsite-(La) was stable up to 598 K in air, where it decomposed into CO2 and tetragonal γ-LaOF. Above 948 K, cubic α-LaOF is stable. High temperature X-ray diffraction data were used to fit the Fei thermal equation of state and the thermal expansion coefficient α(sub 298) for all three materials. Bastnäsite-(La) was fit from 298 K to 723 K with V(sub 0) = 439.82 Å(exp 3), α(sub 298) = 4.32 × 10(exp -5) K(exp -1), a(sub 0) = −1.68 × 10(exp -5) K(exp -1), a(sub 1) = 8.34 × 10(exp -8) K(exp -1), and a(sub 2) = 3.126 K(exp -1). Tetragonal γ-LaOF was fit from 723 K to 948 K with V(sub 0) = 96.51 Å(exp 3), α(sub 298) = 2.95×10(exp -4) K(exp -1), a(sub 0) = −2.41×10(exp -5) K(exp -1), a(sub 1) = 2.42×10(exp -7) K(exp -1), and a(sub 2) = 41.147 K(exp -1). Cubic α-LaOF was fit from 973 K to 1123 K with V(sub 0) = 190.71 Å(exp 3), α(sub 298) = −1.12×10(exp -5) K(exp -1), a(sub 0) = 2.36×10(exp -4) K(exp -1), a(sub 1) = −1.73 × 10(exp -7) K(exp -1), and a(sub 2) = −17.362 K(exp -1). An ambient temperature third order Birch–Murnaghan equation of state was fit with V(sub 0) = 439.82 Å(exp 3), K(sub 0) = 105 GPa, and K’ = 5.58.
Document ID
20205002769
Acquisition Source
Johnson Space Center
Document Type
Accepted Manuscript (Version with final changes)
Authors
Richard L Rowland, II ORCID
(Los Alamos National Laboratory Los Alamos, New Mexico, United States)
Barbara Lavina
(University of Nevada, Las Vegas Las Vegas, Nevada, United States)
Kathleen E Vander Kaaden ORCID
(Jacobs (United States) Dallas, Texas, United States)
Lisa R Danielson
(Los Alamos National Laboratory Los Alamos, New Mexico, United States)
Pamela C Burnley
(University of Nevada, Las Vegas Las Vegas, Nevada, United States)
Date Acquired
May 27, 2020
Publication Date
February 27, 2020
Publication Information
Publication: Minerals
Publisher: MDPI
Volume: 10
Issue: 3
Issue Publication Date: March 1, 2020
e-ISSN: 2075-163X
Subject Category
Geosciences (General)
Funding Number(s)
CONTRACT_GRANT: DE-AC02- 06CH11357
CONTRACT_GRANT: EAR 1157758
CONTRACT_GRANT: EAR-1128799
CONTRACT_GRANT: DEFG02- 94ER1466
CONTRACT_GRANT: NNJ13HA01C
WBS: 811073
CONTRACT_GRANT: DE-NA0001982
CONTRACT_GRANT: EAR-1220548
Distribution Limits
Public
Copyright
Use by or on behalf of the US Gov. Permitted.
Technical Review
External Peer Committee
Keywords
Bastnäsite
Equation of state
Rare earth element
No Preview Available