Hostname: page-component-586b7cd67f-vdxz6 Total loading time: 0 Render date: 2024-11-27T23:52:27.520Z Has data issue: false hasContentIssue false

Lattice defects in lawsonite: a TEM investigation

Published online by Cambridge University Press:  05 July 2018

F. Cámara*
Affiliation:
Laboratoire Structure et Propriétés de l'Etat Solide Université Sciences et Technologies de Lille, 59655 Villeneuve d'Ascq-Cedex, France
J. C. Doukhan
Affiliation:
Laboratoire Structure et Propriétés de l'Etat Solide Université Sciences et Technologies de Lille, 59655 Villeneuve d'Ascq-Cedex, France
M. A. Carpenter
Affiliation:
Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK
*

Abstract

Lattice defects in lawsonite have been studied by transmission electron microscopy. It is proposed that twinning and easy glide systems are 1/2[110] {110}; the easy glide planes are coincident with twin planes. This mineral displays high sensitivity to the electron beam, even at low temperatures. In situ precipitates appear as a consequence of beam irradiation. The precipitation takes places first on dislocations, then on twin boundaries and then in the matrix, causing ‘coffee-bean’ contrast features typical of precipitates. The studies were performed at low temperature (∼110 K) in order to investigate the low temperature displacive transitions from space group Cmcm to Pmcn and P21cn and elucidate their microscopic character. No characteristic microstructural texture, such as antiphase domains associated with the transition, were observed, however. This is probably due to the high mobility of protons under the electron beam. The development of regularly spaced dislocations along twin planes is hypothesized as the only evidence that a phase transition takes place at a nanoscale.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2001

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Footnotes

Present address: Centro di Studio per la Cristallochimica e la Cristallografia, via Ferrata 1, 27100 Pavia, Italy

References

Amelinckx, S. and Dekeyser, W. (1959) The structure and properties of grain boundaries. Solid State Phys., 8, 325499.CrossRefGoogle Scholar
Cordier, P. and Doukhan, J.C. (1989) Water solubility in quartz and its influence on ductility. Eur. J. Mineral., 1, 221–37.CrossRefGoogle Scholar
Cordier, P. and Doukhan, J.C. (1991) Water speciation in quartz; a near infrared study. Amer. Mineral., 76, 361–9.Google Scholar
Doukhan, J.C. and Trepied, L. (1985) Plastic deformation of quartz single crystals. Bull. Mineral., 108, 97123.Google Scholar
Doukhan, J.C., Doukhan, N., Koch, P.S. and Christie, J.M. (1985) TEM investigation of lattice defects in Al2SiO5 polymorphs and plasticity induced polymorphic transformations. Bull. Minèral., 108, 81–96.CrossRefGoogle Scholar
Griggs, D.T. and Blacic, J.D. (1965) Quartz: anomalous weakness of synthetic crystals. Science, 147, 292–5.CrossRefGoogle ScholarPubMed
Libowitzky, E. and Armbruster, T. (1995) Lowtemperature phase transitions and the role of hydrogen bonds in lawsonite. Amer. Mineral., 80, 1277–85.CrossRefGoogle Scholar
Libowitzky, E. and Rossman, G.R. (1996) FTIR spectroscopy of lawsonite between 82 and 325 K. Amer. Mineral., 81, 1089–91.CrossRefGoogle Scholar
McLaren, A.C., FitzGerald, J.D. and Gerresten, J. (1989) Dislocation nucleation and multiplication in synthetic quartz: relevance to water weakening. Phys. Chem. Miner., 16, 465–82.CrossRefGoogle Scholar
Meyer, H.W., Carpenter, M.A., Graeme-Barber, A. and Sondergeld, P. (2000) Local and macroscopic order parameter variations associated with low temperature phase transitions in lawsonite, CaAl2Si2O7(OH)2 H2O. Eur. J. Mineral., 12, 1139–50.CrossRefGoogle Scholar
Paterson, M.S. (1989) The interaction of water with quartz and its influence on dislocation flow; an overview. Pp. 107–42 in: Rheology of Solids and of the Earth (Karato, S.I. and Toriumi, M., editors). Oxford Science Publishers, Oxford.Google Scholar
Schmidt, M.W. (1995) Lawsonite: upper pressure stability and formation of higher density hydrous phases. Amer. Mineral., 80, 1286–92.CrossRefGoogle Scholar
Sondergeld, P., Schranz, W., Trsöster, A., Carpenter, M.A., Libowitzky, E. and Kikyk, A.V. (2000 a) Optical, elastic and dielectric studies of the phase transitions in lawsonite. Phys. Rev. B, 62, 6143–7.CrossRefGoogle Scholar
Sondergeld, P., Schranz, W., Kikyk, A.V., Carpenter, M.A. and Libowitzky, E. (2000 b) Ordering behaviour of the mineral lawsonite. Phase Trans., 71, 189203.CrossRefGoogle Scholar
Van Duysen, J.C., Doukhan, N. and Doukhan, J.C. (1985) Transmission electron microscope study of dislocations in orthopyroxene (Mg,Fe)2Si2O6 . Phys. Chem. Miner., 12, 3944.CrossRefGoogle Scholar