First Principles Thermoelasticity of Mantle Minerals Renata M. M. Wentzcovitch Department of Chemical Engineering and Materials Science U. of Minnesota,

Slides:



Advertisements
Similar presentations
7/12/04CIDER/ITP Short Course Composition and Structure of Earth’s Interior A Perspective from Mineral Physics.
Advertisements

12/14/2009 MR-14A-06 1 Some remarks on micro-physics of LPO (plastic anisotropy) some tutorials Shun-ichiro Karato Yale University Department of Geology.
The Earth’s Structure Seismology and the Earth’s Deep Interior The Earth’s Structure from Travel Times Spherically symmetric structure: PREM - Crustal.
High Pressure Mineralogy Minerals Methods & Meaning High Pressure Mineralogy.
Deformation of Diopside Single Crystals at Mantle P and T E. AMIGUET 1, P. RATERRON 1, P. CORDIER 1,H. COUVY 2, AND J. CHEN 2 1Laboratoire Structure et.
Thermoelastic properties of ferropericlase R. Wentzcovitch Dept. of Chemical Engineering and Materials Science, Minnesota Supercomputing Institute J. F.
Seismological Tests (and Implications) of Post-Perovskite Presence in the Deep Mantle In collaboration with Ed Garnero, Alex Hutko John Hernlund In collaboration.
Europa Scenarios: Physical Models Ice-cracks on surface consistent with either “warm-ice” or water beneath the surface Near infrared mapping consistent.
Geophysics, Mineral Physics, and QMC Lars Stixrude [University of Michigan] 2007 Summer School on Computational Materials Science Quantum Monte Carlo:
12/15MR22B-01 1 Some remarks on seismic wave attenuation and tidal dissipation Shun-ichiro Karato Yale University Department of Geology & Geophysics.
Lowermost Outer Core and the ICB Bin Chen, Vernon Cormier, Shan Dou, Garrett Euler, Lili Gao, David Gubbins, Kuang He, Svetlana Kharlamova, Jie Li, Hongfeng.
Constraints on Mantle Composition from 1D Earth Models 2007 Vlab/EGC Workshop ESS Building SUNY Stony Brook Stony Brook, NY Baosheng Li Supported.
Seismic tomography: Art or science? Frederik J Simons Princeton University.
Seismic tomography Tomography attempts to determine anomalous structures within the Earth as revealed by deviations from “average” seismic properties at.
Interpreting Geophysical Data for Mantle Dynamics Wendy Panero University of Michigan.
3D seismic imaging of the earth’s mantle Barbara Romanowicz Department of Earth and Planetary Science U.C. Berkeley.
Diffusion in a multi-component system (1) Diffusion without interaction (2) Diffusion with electrostatic (chemical) interaction.
University of California at Berkeley – Physics Department – Hellman Lab Application of “Calorimetry-on-a- Chip” Technology to Heat Capacities of Quenched.
The Nuts and Bolts of First-Principles Simulation
March 2, 2010Global Network Symposium 1 Physics of compression of liquids Implication for the evolution of planets Shun-ichiro Karato Yale University Department.
VLab development team UNIVERSITY OF MINNESOTA Indiana University Florida State Louisiana State University Thermoelastic Properties within VLab.
The role of first principles calculations in geophysics
Continental lithosphere investigations using seismological tools Seismology- lecture 5 Barbara Romanowicz, UC Berkeley CIDER2012, KITP.
Mineral physics and seismic constraints on Earth’s structure and dynamics Earth stucture, mineralogy, elasticity.
Seismology – Lecture 2 Normal modes and surface waves Barbara Romanowicz Univ. of California, Berkeley CIDER Summer KITP.
First Principles Thermoelasticity of Minerals: Insights into the Earth’s LM Problems related with seismic observations T and composition in the lower mantle.
Department of Geology & Geophysics
Renata M. Wentzcovitch Dept. of Chemical Engineering and Materials Science, Minnesota Supercomputing Institute UNIVERSITY OF MINNESOTA Phase transitions.
Chemical and Clapeyron- induced buoyancy at the 660 km discontinuity D.J. Weidner & Y. Wang 1998.
Invariant MD w/ Variable Cell Shape R. Wentzcovitch U. Minnesota Vlab Tutorial -Simulate solids at high PTs -Useful for structural optimizations -Useful.
Phase Transitions in the Earth’s Mantle
Geology 5640/6640 Introduction to Seismology 15 Apr 2015 © A.R. Lowry 2015 Read for Fri 17 Apr: S&W (§3.6) Last time: Structure of the Deep Earth’s.
Probing Earth’s deep interior using mantle discontinuities Arwen Deuss University of Cambridge, UK also: Jennifer Andrews, Kit Chambers, Simon Redfern,
Spin transition in ferrous iron in MgSiO 3 perovskite under pressure Koichiro Umemoto  Spin transition of Fe 2+ Displacement of low-spin Fe Change of.
Seismological observations Earth’s deep interior, and their geodynamical and mineral physical interpretation Arwen Deuss, Jennifer Andrews University of.
Virtual Laboratory for Earth and Planetary Materials, VLab Renata Wenztcovitch, Yousef Saad, Ilja Siepmann, Don Truhlar, Dave Yuen (Minnesota), Philip.
Equation of State Thermal Expansion Bulk Modulus Shear Modulus Elastic Properties.
First-Principles study of Thermal and Elastic Properties of Al 2 O 3 Bin Xu and Jianjun Dong, Physics Department, Auburn University, Auburn, AL
Fluid, 90% iron solidified iron km ,00012,000 Mg(Fe) silicates phase changes basaltic-granitic crust chemical stratification and differentiation.
First Principles Calculations in Mineral Physics Overview of methods Amorphization of quartz under pressure Structural transitions in ruby and the ruby.
Global seismic tomography and its CIDER applications Adam M. Dziewonski KITP, July 14, 2008.
Beyond Elasticity stress, strain, time Don Weidner Stony Brook.
Seismological studies on mantle upwelling in NE Japan: Implications for the genesis of arc magmas Junichi Nakajima & Akira Hasegawa Research Center for.
Partitioning of FeSiO 3 and FeAlO 3, Fe-spin state and elasticity for bridgmanite and post-bridgmanite C.E. Mohn 1 R.G. Trønnes 1,2 1 Centre for Earth.
Quasiharmonic Thermodynamic Properties of Minerals Renata M. M. Wentzcovitch Department of Chemical Engineering and Materials Science Minnesota Supercomputer.
GEO 5/6690 Geodynamics 21 Nov 2014 © A.R. Lowry 2014 Read for Mon 1 Dec: T&S Last Time: The Lithosphere Revisited There are several different processes.
Post-perovskite Transition in MgSiO3
Chapter 12: Earth’s Interior
Constraints on the observation of mantle plumes using global seismology Arwen Deuss University of Cambridge, UK.
Structural and Optical transitions in ruby Collaborators: W. Duan (U. of MN), G. Paiva (USP), & A. Fazzio (USP) Support: NSF, CNPq, and FAPESP Renata Wentzcovitch.
First Principles Thermoelasticity of Minerals: Insights into the Earth’s LM Seismic observations and the nature of the LM T and composition in the lower.
Shear velocity of olivine Data from Kumazawa & Anderson [1969] Seismic Anisotropy.
Composition of the Earth’s core from ab-initio calculation of chemical potentials Department of Earth Sciences & Department of Physics and Astronomy, Thomas.
Anisotropy. Vocabulary 1 Isotropy ahy-saht-trah-pee ahy-so-troh-pee Isotropic ahy-suh-trahp-ik ahy-so-troh-pik.
Spin Transitions in Lower Mantle Minerals? Concentrate on ferropericlase as more likely to have a big effect.
The Core-Mantle Boundary Region Jeanloz & Williams, 1998 Lower mantle Outer core CMB Heat flow.
Materials Theory and Mineral Physics Overview of methods Amorphization of quartz under pressure Structural transitions in ruby and the ruby pressure scale.
Elasticity of MgO- Frequency Dependence Hoda Mohseni and Gerd Steinle-Neumann 1. Introduction Fig 2. MgO crystal structure 3. Experimental methods used.
Insight into the lithospheric structure and deformation in Eastern Tibet from splitting and traveltime variations of core phases S. Sol, A. Meltzer, B.
Han Hsu (徐翰) Department of Chemical Engineering & Materials Science
Fe-Mg partitioning in the lower mantle: in-situ XRD and quantitative analysis Li Zhang a, Yue Meng b, Vitali Prakapenka c, and Wendy L. Mao d,e a Geophysical.
Spin Transitions in Lower Mantle Minerals?
Constraints on flow in the deepest mantle from seismic anisotropy (and other observations) Maureen D. Long1 With contributions from: Heather Ford1,2, Neala.
Formation and Composition of Earth’s Core Beyond the Current Paradigms
Deep Earth dynamics – numerical and fluid tank modelling
CIDER/ITP Summer School
Seismic velocity gradients across the transition zone
CIDER/ITP Short Course
“Phonon” Dispersion Relations in Crystalline Materials
Asthenosphere flow and mantle lithosphere instabilities below continental rifts and rifted margins Jolante van Wijk (University of Houston) Jeroen van.
Presentation transcript:

First Principles Thermoelasticity of Mantle Minerals Renata M. M. Wentzcovitch Department of Chemical Engineering and Materials Science U. of Minnesota, Minneapolis Research in the early 90’s (first principles MD) Current research (NSF/EAR funded) Geophysical motivation Thermoelasticity Some inferences about the lower mantle Research tomorrow

First Principles Thermoelasticity of Mantle Minerals Renata M. M. Wentzcovitch Department of Chemical Engineering and Materials Science U. of Minnesota, Minneapolis Research in the early 90’s (first principles MD) Current research (NSF/EAR funded) Geophysical motivation Thermoelasticity Some Inferences about the Lower Mantle Research tomorrow

Research in the early nineties Development of a variable cell shape (VCS) molecular dynamics (MD) method (Wentzcovitch, PRB,1991) Development of first principles MD I. Self-consistent method with iterative diagonalization used in MD simulations (Wentzcovitch and Martins, SSC,1991) II. Implementation of finite temperature DFT (Wentzcovitch, Martins, and Allen, PRB,1992) Some original applications of combined methodologies Collaborators: J. L. Martins (INESC, Lisbon) and P. B. Allen (SUNY-Stony Brook, CHiPR)

First Principles VCS-MD (Wentzcovitch, Martins, Price, PRL 1993) Damped dynamics P = 150 GPa MgSiO 3

Acknowledgements David Price (UCL-London) Lars Stixrude (U. of Michigan, Ann Arbor) Shun-ichiro Karato (U. of Minnesota/Yale) Bijaya B. Karki (Louisiana S. U.) Boris Kiefer (Princeton U.)

The Contribution from Seismology Longitudinal (P) waves Transverse (S) wave from free oscillations

PREM (Preliminary Reference Earth Model) (Dziewonski & Anderson, 1981) P(GPa)

Mantle Mineralogy SiO MgO 37.8 FeO 8.1 Al 2 O CaO 3.6 Cr 2 O Na 2 O 0.4 NiO 0.2 TiO MnO 0.1 (McDonough and Sun, 1995) Pyrolite model (% weight) Depth (km) P (Kbar) V % Olivine perovskite  -phase spinel MW garnets opx cpx (Mg 1--x,Fe x ) 2 SiO 4 (‘’) MgSiO 3 (Mg,Al,Si)O 3 (Mg,Fe) (Si,Al)O 3 (Mg 1--x,Fe x ) O (Mg,Ca)SiO 3 CaSiO 3

Mantle convection

Intermediate Model of Mantle Convection (Kellogg, Hager, van der Hilst, Science, 1999)

3D Maps of V s and V p V s V  V p ( Masters et al, 2000)

(MLDB-Masters et al., 2000) (KWH-Kennett et al., 1998) (SD-Su & Dziewonski, 1997) (RW-Robertson & Woodhouse,1996) Lateral variations in V S and V P (Karato & Karki, JGR 2001)

Anisotropy   isotropic transverse azimuthal V P V S1 = V S2 V P (  ) V S1 (  )  V S2 (  ) V P ( ,  ) V S1 ( ,  )  V S2 ( ,  )

Anisotropy in the Earth (Karato, 1998)

Mantle Anisotropy SH>SV SV>SH

Slip system Zinc wire F Slip systems and LPO

Lattice Preferred Orientation (LPO) Shape Preferred Orientation (SPO) Mantle flow geometry LPOSeismic anisotropy slip system C ij Anisotropic Structures

+ Mineral sequence II Lower Mantle (Mg x,Fe (1-x) )O(Mg x,Fe (1-x) )SiO 3 + CaSiO 3

+ Mineral sequence II Lower Mantle (Mg x,Fe (1-x) )O(Mg (1-x),Fe x )(Si (1-y),Al y )O 3 + CaSiO 3

Crystal ( Pbnm ) equilibrium structure  kl re-optimize  kl  ij c ijkl (i,j) m Elastic constant tensor 

Yegani-Haeri, 1994 Wentzcovitch et al, 1995 Karki et al, 1997 within 5% S-waves (shear) P-wave (longitudinal) n propagation direction Elastic Waves

Cristoffel’s eq.: with is the propagation direction Wave velocities in perovskite (Pbnm) (Wentzcovitch, Karki, Karato, EPSL 1998)

Anisotropy P-azimuthal: S-azimuthal: S-polarization: (Karki, Stixrude, Wentzcovitch, Rev. Geophys. 2002)

Voigt: uniform strain Reuss: uniform stress Voigt-Reuss averages: Poly-Crystalline aggregate

Polarization anisotropy in transversely isotropic medium High P, slip systems MgO: {100} ? MgSiO 3 pv: {010} ? Seismic anisotropy Isotropic in bulk LM 2% V SH > V SV in D’’ (SH-SV)/S Anisotropy (%) (Karki et al., JGR 1997; Wentzcovitch et al EPSL1998 ) (Karki, Stixrude, Wentzcovitch, Rev. Geophys. 2002)

Acoustic Velocities of Potential LM Phases (Karki, Stixrude, Wentzcovitch, Rev. Geophys. 2002)

T M of mantle phases Core T Mantle adiabat solidus HA Mw (Mg,Fe)SiO 3 CaSiO 3 peridotite P(GPa) T (K) (Zerr, Diegler, Boehler, Science1998)

Method Density Functional Perturbation Theory for phonons xxxxxxxxxxxxxxxxxx (Gianozzi, Baroni, and de Gironcoli, 1991) Thermodynamic method: VDoS and F(T,V) within the QHA N-th order finite strain EoS (N=3,4,5…)

equilibrium structure  kl re-optimize (Thermo) Elastic constant tensor 

Phonon dispersions in MgO Exp: Sangster et al (Karki, Wentzcovitch, de Gironcoli and Baroni, PRB 61, 8793, 2000) -

Phonon dispersion of MgSiO 3 perovskite Calc Exp Calc: Karki, Wentzcovitch, de Gironcoli, Baroni PRB 62, 14750, 2000 Exp: Raman [Durben and Wolf 1992] Infrared [Lu et al. 1994] 0 GPa 100 GPa - -

Zero Point Motion Effect Volume (Å 3 ) F (Ry) MgO Static 300K Exp (Fei 1999) V (Å 3 ) K (GPa) K´ K´´(GPa -1 )

MgSiO 3 -perovskite and MgO Exp.: [Ross & Hazen, 1989; Mao et al., 1991; Wang et al., 1994; Funamori et al., 1996; Chopelas, 1996; Gillet et al., 2000; Fiquet et al., 2000]

Thermal expansivity of MgO and MgSiO 3 (Karki, Wentzcovitch, de Gironcoli and Baroni, Science 1999) (Karki, Wentzcovitch, de Gironcoli and Baroni, GRL 2001)  (10 -5 K -1 )

Elasticity of MgO (Karki et al., Science 1999)

Adiabatic bulk modulus at LM P-T (Karki, Wentzcovitch, de Gironcoli and Baroni, GRL, 2001 )

LM geotherms

Elastic constant tensor (Wentzcovitch, Karki, & Coccociono, 2002)

Velocities

Effect of Fe alloying (Kiefer, Stixrude,Wentzcovitch, GRL 2002) (Mg 0.75 Fe 0.25 )SiO ||

Comparison with PREM Along B&S-geotherm perovskite pyrolite

Summary Building a consistent body of knowledge obout LM phases We have adequate methods (DFT, QHA) to examine elasticity of major mantle phases The objective is to interpret seismic observations (1D, 3D, anisotropy) in terms of composition, temperature, ``flow’’…

Summary Building a consistent body of knowledge obout LM phases We have adequate methods (DFT, QHA) to examine elasticity of major mantle phases The objective is to interpret seismic observations (1D, 3D, anisotropy) in term of composition, temperature, ``flow’’… Seismology Mineral Physics Geodynamics

Acknowledgements Bijaya B. Karki (LSU) Stefano de Gironcoli, Matteo Coccocioni (SISSA, Italy)