Abstract
In the olivine crystal structure, cations are distributed over two inequivalent octahedral sites, M1 and M2. Kinetics of cation exchange between the two octahedral sites in (Co0.1Mg0.9)2SiO4 single crystal have been studied in the temperature range from 600 to 800°C by monitoring the time evolution of the absorbance of Co2+ ions in M1 or M2 sites using optical spectroscopy after rapid temperature jumps. It was found from such temperature-jump induced relaxation experiments that with increasing temperature the absorbance of Co2+ ions in the M1 site decreases while that in the M2 site increases. This indicates a tendency of Co2+ cations to populate the M2 site with increasing temperatures and vice versa. The experimental relaxation data can be modeled using a triple exponential equation based on theoretical analysis. Activation energies of 221 ± 4 and 213 ± 10 kJ/mol were derived from relaxation experiments on the M2 site and M1 site, respectively, for the cation exchange processes in (Co0.1Mg0.9)2SiO4 olivine. Implications for cation diffusion at low temperatures are discussed.
Similar content being viewed by others
References
Akamatsu T, Kumazawa M (1993) Kinetics of intracrystalline cation redistribution in olivine and its implication. Phys Chem Miner 19:423–430
Bäckermann J, Becker KD (1998) The mechanism of cation equilibration in nickel aluminate spinel, NiAlO4. Z Phys Chem 206:26–31
Becker KD, Rau F (1987) High-temperature ligand field spectra in spinels: cation disorder and cation kinetics in NiAl2O4. Ber Bunsenges Phys Chem 91:1279–1282
Becker KD, Bäckermann J (1995) Kinetics of order-disorder processes in spinels. Phase Trans 55:181–197
Boström D (1989) Single crystal diffraction studies of synthetic (Co,Mg)-olivine solid solutions. Acta Chem Scand 43:121–127
Brown WE, (1980) Olivines and silicate spinels. In: Ribbe PH (ed) Orthosilicates. Rev Mineral 5:275–365
Buening DK, Buseck PR (1973) Fe–Mg lattice diffusion in olivine. J Geophys Res 78:6852–6862
Coogan LA, Hain A, Stahl S, Chakraborty S (2006) Experimental determination of diffusion coefficient of calcium in olivine between 900°C and 1500°C. Geochim Cosmochim Acta 69:3683–3694
Chakraborty S, Farver JR, Yund RA, Rubie DC (1994) Mg tracer diffusion in synthetic forsterite and San Carlos olivine as a function of P, T and fO2. Phys Chem Miner 21:489–500
Chakraborty S (1997) Rates and mechanism of Fe-Mg interdiffusion in olivine at 980–1300°C. J Geophys Res B6 102:12317–12331
Figgis BN, Hitchman MA (2000) Ligand field theory and its applications, chap 8. Wiley-VCH, New York
Garsche M (1994) Spektroskopische und strukturelle Untersuchungen zur Intrakristallinen Ni–Mg-Verteilung in Olivinen, (Mg1−x Ni x )2SiO4. PhD Thesis, Technische Universitaet Berlin
Ghose S, Wan C (1974) Strong site preprence of Co2+ in olivine Co1.1Mg0.90SiO4. Contr Mineral Petrol 47:131–140
Henderson CMB, Rederfern SAT, Smith RI, Knight KS, Charnock JM (2001) Composition and temperature dependence of cation ordering in Ni–Mg olivine solid solutions: a time-of-flight neutron powder diffraction and EXAFS study. Am Mineral 86:1170–1187
Hermeling J, Schmalzried H (1984) Tracerdiffusion of the Fe-cations in olivine (Fe x Mg1−x )2SiO4(III). Phys Chem Miner 11:161–166
Ito M, Yurimoto H, Morioka M, Nagasawa H (1999) Co2+ and Ni2+ diffusion in olivine determined by secondary ion mass spectroscopy. Phys Chem Miner 26:435–431
Ito M, Ganguly J (2006) Diffusion kinetics of Cr in olivine and 53Mn–53Cr thermochronology of early solar system objects. Geochim Cosmochim Acta 70:799–809
Miyake M, Nakamura H, Kojima H, Marumo F (1987) Cation ordering in Co-Mg olivine solid solution series. Am Mineral 72:594–598
Morioka M (1980) Cation diffusion in olivine—I. Cobalt and magesium. Geochim Cosmochim Acta 44:759–762
Morozov M, Brinkmann Ch, Lottermoser W, Tippelt G, Amthauer G, Kroll H (2005) Octrahedral cation partitioning in Mg, Fe2+-olivine. Mössbauer spectroscopic study of synthetic (Mg0.5Fe0.5)2SiO4(Fa50). Eur J Mineral 17:495–500
Müller-Sommer M, Hock R, Kirfel A (1997) Rietveld refinement study of the cation distribution in (Co, Mg)-olivine. Phys Chem Miner 24:17–23
Nakamura A, Schmalzried H (1983) On the nonstoichiometry and point defects of olivine. Phys Chem Miner 10:27–37
Petry C, Chakraborty S, Palm H (2004) Experimental determination of Ni diffusion coefficients and their dependence on temperature, composition, oxygen fugacity and crystallographic orientation. Geochim Cosmochim Acta 68:4179–4188
Rinaldi R, Gatta GD, Artioli KS, Knight KS, Geiger CA (2005) Crystal chemistry, cation ordering and thermoelastic behavior of CoMgSiO4 olivine at high temperature as studied by in situ neutron powder diffraction. Phys Chem Miner 36:655–664
Schmitz-DuMont O, Friebel C (1967) Farbe und Konsitution bei anorganischen Feststoffen, 15. Mitteilungen: Die Lichtabsorption des zweiwertigen Cobalts in Silikaten vom Olivintypus. Mh Chem 4:1583–1602
Schwier G, Dieckmann R, Schmalzried H (1973) Punktfehlstellen in Oxidmischphasen (I) Fehlstellenthermodynamik der Mischphasen (Co x Mg1−x )O und (Co x Mg1−x )2SiO4. Ber Bunsenges Phys Chem 77:402–408
Stocker RL, Smith DM (1978) Effect of enstatite activity and oxygen partial pressure on the point-defect chemistry of olivine. Phys Earth Planet Int 16:145–156
Taran MN, Koch-Müller M (2006) Octahedral cation ordering in Mg, Fe2+-olivine: an optical absorption spectroscopic study. Phys Chem Miner 33:511–518
Taran MN, Rossman GR (2001) Optical spectra of Co2+ in three synthetic silicate minerals. Am Mineral 86:889–891
Tsai TL, Diekmann R (1997) Point defects and transport of matter and charge in olivines, (Fe x Mg1−x )2SiO4. Mater Sci Forum 239(24):399–402
Tsai TL, Diekmann R (2002) Variation of the oxygen content and point defects in olivines, (Fe x Mg1−x )2SiO4. Phys Chem Miner 29:680–694
Ullrich K, Langer K, Becker KD (2001) Temperature dependence of the polarized electronic absorption spectra of olivines. Part I—fayalite. Phy Chem Miner 29:409–419
Ullrich K, Ott O, Langer K, Becker KD (2004) Temperature dependence of the polarized electronic absorption spectra of olivines. Part II—Cobalt-containing olivines. Phys Chem Miner 31:247–260
Acknowledgments
The authors would like to thank Dr. S. Kipp, M. Schrader, S. Dlugocz and A. Tiefnig for their help during this work. Thanks are also due to Prof. P. G. Jones’s group for performing single crystal diffraction experiments and Dr. J. Koepke, University of Hanover, for electron microprobe analysis. Financial support from Deutsche Forschungsgemeinschaft (DFG) is greatly acknowledged.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Shi, J., Ebbinghaus, S.G. & Becker, K.D. Temperature-jump induced cation exchange kinetics in (Co0.1Mg0.9)2SiO4 olivine: an in situ optical spectroscopic study. Phys Chem Minerals 35, 1–9 (2008). https://doi.org/10.1007/s00269-007-0187-1
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00269-007-0187-1