The geodynamic equation of state: What and how

By J. A. Connolly. 2009

1,013 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/ba8685c3e30136eb7ff0909cd09278222bdc5a77

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In Geophysics

1. J. A. Connolly
2. L. Stixrude
3. C. Lithgow‐Bertelloni
4. Paul J. Tackley
5. Mark A. Wieczorek
6. Cian R. Wilson
7. Y. Podladchikov
8. J. C. Afonso

Citations in the corpus

• Thermodynamics of mantle minerals - II. Phase equilibria (2011, background): “For example, Legendre transformation to the internal energy U(S, V ) = F (V, T ) + TS is important in geodynamic applications (Connolly 2009).”
• The nature of the TRAPPIST-1 exoplanets. (2018, methodology): “The silicate-mantle model of Connolly (2009) is used to compute equilibrium mineralogy and density profiles for a given bulk mantle composition.”
• How contact metamorphism can trigger global climate changes: Modeling gas generation around igneous sills in sedimentary basins (2010, methodology): “The thermal solver is coupled to mineralogy by phase equilibrium modeling (Connolly, 2009).”
• High Accuracy Mantle Convection Simulation through Modern Numerical Methods. II: Realistic Models and Problems (2017, methodology): “One may use a thermodynamic calculation package, such as Perple X [Connolly(2009)] or BurnMan [Cottaar et al.(2014)] to compute p -”
• Fluid flow in subduction zones: The role of solid rheology and compaction pressure (2014, methodology): “To calculate the bound-water fraction in each layer, F , we use tabulated phase diagrams calculated using Perple_X (Connolly, 2009) and described by Hacker (2008).”
• Can we constrain the interior structure of rocky exoplanets from mass and radius measurements (2015, methodology): “The equilibrium mineralogy and, consequently its density, is computed as a function of pressure, temperature, and bulk composition by Gibbs energy minimization (Connolly 2009).”
• The composition of Mars (2019, methodology): “Mineralogy, radial density distribution and seismic velocity profiles in the Martian mantle were computed using the Gibbs free energy minimization method that is employed in the thermodynamic modeling code Perple X version 6.8.6 (Connolly, 2009).”
• The seismicity of Mars (2020, methodology): “Here, Martian mineralogy and physical properties are assumed to be governed by thermodynamic equilibrium and computed for a given model pressure, temperature, and bulk composition along self-consistent adiabats by Gibbs free-energy minimization (Connolly, 2009) using the thermodynamic formulation an”
• 3‐D multiobservable probabilistic inversion for the compositional and thermal structure of the lithosphere and upper mantle. I: a priori petrological information and geophysical observables (2013, methodology): “…ultramafic lithologies (i.e., eclogite, pyroxenites, and peridotites) and their relevant physical properties are computed with components of the software Perple_X [Connolly, 2009] within the CFMAS system using the database and thermodynamic formalism of Stixrude and Lithgow-Bertelloni [2011].”