An investigation of the phase transitions in bornite (Cu<sub>5</sub>FeS<sub>4</sub>) using neutron diffraction and differential scanning calorimetry (1998)

Other| December 01, 1998 An investigation of the phase transitions in bornite (Cu 5 FeS 4 ) using neutron diffraction and differential scanning calorimetry Benjamin A. Grguric; Benjamin A. Grguric University of Cambridge, Department of Earth Sciences, Cambridge, United Kingdom Search for other works by this author on: GSW Google Scholar Andrew Putnis; Andrew Putnis Search for other works by this author on: GSW Google Scholar Richard J. Harrison Richard J. Harrison Search for other works by this author on: GSW Google Scholar American Mineralogist (1998) 83 (11-12_Part_1): 1231–1239. https://doi.org/10.2138/am-1998-11-1211 Article history first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Benjamin A. Grguric, Andrew Putnis, Richard J. Harrison; An investigation of the phase transitions in bornite (Cu 5 FeS 4 ) using neutron diffraction and differential scanning calorimetry. American Mineralogist 1998;; 83 (11-12_Part_1): 1231–1239. doi: https://doi.org/10.2138/am-1998-11-1211 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyAmerican Mineralogist Search Advanced Search Abstract Bornite (Cu 5 FeS 4 ) exists in three polymorphic forms related by superstructuring, with structural transitions at 200 and 265 degrees C. The phase transitions and structural behavior in two natural bornite samples were investigated as a function of temperature using differential scanning calorimetry (DSC) to characterize the thermal anomalies associated with each transition and in-situ high-resolution neutron powder diffraction to determine the variation in superlattice intensity and lattice parameters. These two methods, carried out over the temperature range 50-350 degrees C, provided insight into the short- and long-range interactions, respectively, and a comparison of measurements taken up-T and down-T enabled thermal hysteresis effects to be quantified. The high to intermediate transition at 265 degrees C involves long-range cation ordering and vacancy clustering, resulting in a doubling of the high-temperature cubic unit cell (m3m). The square of both the spontaneous strain and the 2a superlattice intensity varied linearly with temperature, indicating that the transition is tricritical in character. Loss of long- and short-range order occurred simultaneously during heating, whereas during cooling, the reappearance of 2a superlattice reflections was depressed some 50 degrees C below the short-range transition recorded by DSC due to the formation of antiphase domains. The presence of antiphase domains also caused the discontinuity in the strain associated with the transition to occur at a different temperature to the appearance of superlattice intensity. The intermediate-low transition associated with the development of a 2a4a2a orthorhombic superlattice (Pbca) is strongly first-order and exhibits a large intrinsic hysteresis (38 degrees C). The down-T transition temperature of the intermediate-low transition is shown to be dependent on the degree of order attained in the intermediate phase. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.