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Ginzburg-Landau law

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Journal Article
Published: 01 August 1991
American Mineralogist (1991) 76 (7-8): 1120–1133.
... of the form Q od 2 A R ( T − T c ) = ln ⁡ t − Δ H * R T + Δ S * R − ln ⁡ τ 0 . Values of A = −2.1 × 10 −5 , T c = 2215 °C, Δ H * = 124 ± ~15 kcal/mol, and τ 0 exp(−Δ S */R) = 9 × 10 −21 s were obtained. This type of rate law can be understood in terms of solutions to the Ginzburg-Landau rate equation...
Journal Article
Published: 01 January 2003
European Journal of Mineralogy (2003) 15 (1): 7–19.
... in the linear regime between driving force, ∂G ord /∂Q̄, and ordering rate, dQ̄/dt. Under these constraints the Ginzburg-Landau equation ( Salje, 1988 ) which is based on microscopic arguments reduces to the same form. Equation (1) can be elaborated along different routes. (1) The Gibbs energy due to ordering...
FIGURES
First thumbnail for: Rate equations for non-convergent order-disorder p...
Second thumbnail for: Rate equations for non-convergent order-disorder p...
Third thumbnail for: Rate equations for non-convergent order-disorder p...
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Thermodynamic models: thin solid line is a fit to our data using O’Neill and Navrotsky (1983) model, and the dashed line is the Landau fit. Thick solid line is the calculated non-equilibrium behavior using the Ginzburg-Landau rate law with the thermodynamic driving force given by the O’Neill and Navrotsky (1983) model. The thermodynamic models show that perfect order (Q = −0.5 in inverse spinel) occurs at −273 °C and maximum disorder (Q = 0) occurs at infinite temperature.
Published: 01 January 2005
F igure 11. Thermodynamic models: thin solid line is a fit to our data using O’Neill and Navrotsky (1983) model, and the dashed line is the Landau fit. Thick solid line is the calculated non-equilibrium behavior using the Ginzburg-Landau rate law with the thermodynamic driving force given
Image
(a) Timescales for Al/Mg-inversion on the merged layer (referred as M-layer: TMgI−t+OAlI−t) within the twinned region. The time taken for inversion is calculated by integrating the Ginzburg-Landau rate law at different temperatures under isothermal conditions. The twin free energies with stable and metastable inversions (i.e., with extent of inversion same as in bulk) as a function of temperature are also shown. (b) Contours of the extent of inversion that are obtained at room temperature on the M-layer as a function of the temperature at which twinning occurred and the cooling rate. (Color online.)
Published: 01 August 2022
Figure 6. ( a ) Timescales for Al/Mg-inversion on the merged layer (referred as M-layer: T Mg I − t + O Al I − t ) within the twinned region. The time taken for inversion is calculated by integrating the Ginzburg-Landau rate law at different temperatures under
Journal Article
Published: 01 January 2005
American Mineralogist (2005) 90 (1): 219–228.
...F igure 11. Thermodynamic models: thin solid line is a fit to our data using O’Neill and Navrotsky (1983) model, and the dashed line is the Landau fit. Thick solid line is the calculated non-equilibrium behavior using the Ginzburg-Landau rate law with the thermodynamic driving force given...
FIGURES
First thumbnail for: Cation ordering in magnesioferrite, MgFe 2 O 4 , t...
Second thumbnail for: Cation ordering in magnesioferrite, MgFe 2 O 4 , t...
Third thumbnail for: Cation ordering in magnesioferrite, MgFe 2 O 4 , t...
Journal Article
Published: 01 December 2000
Mineralogical Magazine (2000) 64 (6): 971–982.
... in a significant temperature interval, or whether the data may consistently be described by a mean-field Landau model for all temperatures T < T C . Ginzburg et al. (1987) have shown that if the traditional way to fit a power law to the temperature dependence of the order parameter is followed...
FIGURES
First thumbnail for: Phase transitions in perovskites near the tricriti...
Second thumbnail for: Phase transitions in perovskites near the tricriti...
Third thumbnail for: Phase transitions in perovskites near the tricriti...
Journal Article
Published: 01 February 2006
American Mineralogist (2006) 91 (2-3): 306–312.
... by O’Neill (1994) in terms of the Mueller rate law and by Harrison and Putnis (1999) in terms of the Ginzburg-Landau rate law. The Mueller rate law is a special case of the more general Ginzburg-Landau rate law, but it only applies to homogeneous ordering. However, the Ginzburg-Landau rate law is rather...
FIGURES
First thumbnail for: Thermodynamics and kinetics of cation ordering in ...
Second thumbnail for: Thermodynamics and kinetics of cation ordering in ...
Third thumbnail for: Thermodynamics and kinetics of cation ordering in ...
Journal Article
Published: 01 March 2001
American Mineralogist (2001) 86 (3): 271–278.
... exchange equilibrium was achieved. Calculations of K were performed using the Ginzburg-Landau equation, the kinetic model of Mueller, and the mathematical formulation proposed by Sha and Chappell (1996) to check the responses of various kinetic models for a Ca-rich pyroxene on the same data set...
FIGURES
First thumbnail for: Ordering kinetics of Mg-Fe 2+ exchange in a Wo 43 ...
Second thumbnail for: Ordering kinetics of Mg-Fe 2+ exchange in a Wo 43 ...
Third thumbnail for: Ordering kinetics of Mg-Fe 2+ exchange in a Wo 43 ...
Journal Article
Published: 01 January 2000
Reviews in Mineralogy and Geochemistry (2000) 39 (1): 105–133.
... b/c ratio ( Ginzburg et al. 1987 , Redfern 1992 ). Figure 5. The dependence of the critical exponent β on the Landau coefficients. The critical exponents were calculated by least squares fitting of an equilibrium order parameter evolution from a Landau potential. The transition...
FIGURES
First thumbnail for: Order-Disorder Phase Transitions
Second thumbnail for: Order-Disorder Phase Transitions
Third thumbnail for: Order-Disorder Phase Transitions
Journal Article
Published: 01 August 2022
American Mineralogist (2022) 107 (8): 1470–1476.
...Figure 6. ( a ) Timescales for Al/Mg-inversion on the merged layer (referred as M-layer: T Mg I − t + O Al I − t ) within the twinned region. The time taken for inversion is calculated by integrating the Ginzburg-Landau rate law at different temperatures under...
FIGURES
First thumbnail for: The interplay between twinning and cation inversio...
Second thumbnail for: The interplay between twinning and cation inversio...
Third thumbnail for: The interplay between twinning and cation inversio...
Journal Article
Published: 01 October 2001
American Mineralogist (2001) 86 (10): 1170–1187.
... behavior were analyzed using a Ginzburg-Landau model giving activation energies for Mg-Ni exchange between M1 and M2 for samples of composition Mg 1.6 Ni 0.4 SiO 4 and Mg 1.0 Ni 1.0 SiO 4 of 145 ± 5 and 160 ± 5 kJ/mol, respectively. The model also shows that the characteristic time scale for re...
FIGURES
First thumbnail for: Composition and temperature dependence of cation o...
Second thumbnail for: Composition and temperature dependence of cation o...
Third thumbnail for: Composition and temperature dependence of cation o...
Journal Article
Published: 01 January 2000
Reviews in Mineralogy and Geochemistry (2000) 39 (1): 135–174.
... in a simple linear fashion with dopant concentration. This supposition can be rationalized by a Landau-Ginzburg excess Gibbs free-energy expansion ( Salje et al. 1991 ). A simple second order phase transition for phase A with the regular free energy expression (4) \batchmode \documentclass[fleqn,10pt...
FIGURES
First thumbnail for: Phase Transformations Induced by Solid Solution
Second thumbnail for: Phase Transformations Induced by Solid Solution
Third thumbnail for: Phase Transformations Induced by Solid Solution
Journal Article
Published: 01 January 2000
Reviews in Mineralogy and Geochemistry (2000) 39 (1): 65–84.
.... As the temperature increases and approaches the transition point, the transitional areas between pericline twins becomes more and more diffuse. This is in complete agreement with the predictions of the continuum Landau-Ginzburg theory, according to which the width of a domain wall increases with temperature...
FIGURES
First thumbnail for: Mesoscopic Twin Patterns in Ferroelastic and Co-El...
Second thumbnail for: Mesoscopic Twin Patterns in Ferroelastic and Co-El...
Third thumbnail for: Mesoscopic Twin Patterns in Ferroelastic and Co-El...
Journal Article
Published: 01 July 2024
American Mineralogist (2024) 109 (7): 1292–1302.
... and kinetics of Al/Si ordering in anorthite, I: Incommensurate structure and domain coarsening . American Mineralogist , 76 , 1110 – 1119 . Carpenter , M.A. ( 1991b ) Mechanisms and kinetics of Al/Si ordering in anorthite, II: Energetics and a Ginzburg-Landau rate law . American Mineralogist...
FIGURES
First thumbnail for: Local strain heterogeneity associated with Al/Si o...
Second thumbnail for: Local strain heterogeneity associated with Al/Si o...
Third thumbnail for: Local strain heterogeneity associated with Al/Si o...
Journal Article
Published: 01 March 2002
European Journal of Mineralogy (2002) 14 (2): 241–249.
... stability of polytypes ( Sassi et al., 1994 ). Redfern et al. (1997) got insights into the mechanisms governing the cation order-disorder reactions in FeMn and MgMn olivines, at high-temperature conditions, and gave an interpretation based upon the Landau-Ginzburg expansion of the associated free...
FIGURES
First thumbnail for: Neutron powder diffraction and Rietveld analysis; ...
Second thumbnail for: Neutron powder diffraction and Rietveld analysis; ...
Third thumbnail for: Neutron powder diffraction and Rietveld analysis; ...
Journal Article
Published: 01 February 2011
American Mineralogist (2011) 96 (2-3): 374–382.
... et al. 1994 ), and formation of microstructures during cation exchange processes can be rationalized, in a Landau-Ginzburg approach in which solids are treated as elastic continua , by taking into account local correlation of the order or disorder events. A theoretical interpretation of spatial...
FIGURES
First thumbnail for: Rhombic-shaped nanodomains in columbite driven by ...
Second thumbnail for: Rhombic-shaped nanodomains in columbite driven by ...
Third thumbnail for: Rhombic-shaped nanodomains in columbite driven by ...
Journal Article
Published: 01 February 2006
Mineralogical Magazine (2006) 70 (1): 65–71.
... in anorthite: I. Incommensurate structure and domain coarsening . American Mineralogist , 76 , 1110 – 1119 . Carpenter , M.A. ( 1991b ) Mechanisms and kinetics of Al,Si ordering in anorthite: II. Energetics and a Ginzburg-Landau rate law . American Mineralogist , 76 , 1120 – 1133...
FIGURES
First thumbnail for: Long-range Al,Si equilibrium configuration in Sr f...
Second thumbnail for: Long-range Al,Si equilibrium configuration in Sr f...
Third thumbnail for: Long-range Al,Si equilibrium configuration in Sr f...
Journal Article
Published: 01 January 2006
Reviews in Mineralogy and Geochemistry (2006) 63 (1): 145–170.
... towards the equilibrium order-disorder line. Using Ginzburg-Landau theory, which relates the driving force for ordering to the rate of change of order, one can obtain a kinetic description of the expected t-T- η pathway which relates to the thermodynamic description of the non-convergent disordering...
FIGURES
First thumbnail for: Neutron Powder Diffraction Studies of Order-Disord...
Second thumbnail for: Neutron Powder Diffraction Studies of Order-Disord...
Third thumbnail for: Neutron Powder Diffraction Studies of Order-Disord...
Journal Article
Published: 01 February 2009
Mineralogical Magazine (2009) 73 (1): 119–130.
... and domain coarsening . American Mineralogist , 76 , 1110 – 1119 . Carpenter , M.A. ( 1991b ) Mechanisms and kinetics of Al-Si ordering in anorthite: II. Energetics and a Ginzburg-Landau rate law . American Mineralogist , 76 , 1120 – 1133 . Carpenter , M.A. ( 1992 ) Equilibrium...
FIGURES
First thumbnail for: Cation ordering and phase transitions in feldspars...
Second thumbnail for: Cation ordering and phase transitions in feldspars...
Third thumbnail for: Cation ordering and phase transitions in feldspars...
Journal Article
Published: 01 May 1997
Russ. Geol. Geophys. (1997) 38 (5): 1038–1053.
... properties in a first approximation. Hooke’s law (a material equation connecting stresses with strains) is used with additional terms proportional to strain derivatives; the factors of proportionality are components of the gyration tensor b, the tensor of fifth rank, invariant with respect to a group...
FIGURES
First thumbnail for: SEISMIC GYROTROPY AND ITS PHYSICAL REASONS
Second thumbnail for: SEISMIC GYROTROPY AND ITS PHYSICAL REASONS
Third thumbnail for: SEISMIC GYROTROPY AND ITS PHYSICAL REASONS