Reece, J. J., Redfern, S. A. T., Welch, M. D., Henderson, C. M. B. (2000) Mn-Mg disordering in cummingtonite: a high-temperature neutron powder diffraction study. Mineralogical Magazine, 64 (2) 255-266 doi:10.1180/002646100549166
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Mn-Mg disordering in cummingtonite: a high-temperature neutron powder diffraction study | ||
| Journal | Mineralogical Magazine | ||
| Authors | Reece, J. J. | Author | |
| Redfern, S. A. T. | Author | ||
| Welch, M. D. | Author | ||
| Henderson, C. M. B. | Author | ||
| Year | 2000 (April) | Volume | 64 |
| Page(s) | 255-266 | Issue | 2 |
| Publisher | Mineralogical Society | ||
| DOI | doi:10.1180/002646100549166Search in ResearchGate | ||
| Mindat Ref. ID | 243148 | Long-form Identifier | mindat:1:5:243148:6 |
| GUID | da5fe006-f6e0-4b79-a506-49eba46ea08b | ||
| Full Reference | Reece, J. J., Redfern, S. A. T., Welch, M. D., Henderson, C. M. B. (2000) Mn-Mg disordering in cummingtonite: a high-temperature neutron powder diffraction study. Mineralogical Magazine, 64 (2) 255-266 doi:10.1180/002646100549166 | ||
| Plain Text | Reece, J. J., Redfern, S. A. T., Welch, M. D., Henderson, C. M. B. (2000) Mn-Mg disordering in cummingtonite: a high-temperature neutron powder diffraction study. Mineralogical Magazine, 64 (2) 255-266 doi:10.1180/002646100549166 | ||
| Abstract/Notes | AbstractThe crystal structure of a manganoan cummingtonite, composition [M4](Na0.13Ca0.41Mg0.46Mn1.00) [M1,2,3](Mg4.87Mn0.13)(Si8O22)(OH)2, (Z = 2), a = 9.5539(2) Å, b = 18.0293(3) Å, c = 5.2999(1) Å, β = 102.614(2)° from Talcville, New York, has been refined at high temperature using in situ neutron powder diffraction. The P21/m to C2/m phase transition, observed as spontaneous strains +ε1 = −ε2, occurs at ˜107°C. Long-range disordering between Mg2+ and Mn2+ on the M(4) and M(2) sites occurs above 550°C. Mn2+ occupies the M(4) and M(2) sites preferring M(4) with a site-preference energy of 24.6±1.5 kJ mol−1. Disordering induces an increase in XMnM2 and decrease in XMnM4 at elevated temperatures. Upon cooling, the ordered states of cation occupancy are ‘frozen in’ and strains in lattice parameters are maintained, suggesting that re-equilibration during cooling has not taken place. | ||
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