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Thermoelastic Properties of Iron‐Rich Ringwoodite and the Deep Mantle Aerotherm of Mars

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1029/2024GL109666· OSTI ID:2514542
 [1];  [2];  [2];  [3];  [4];  [5];  [6];  [6];  [2]
  1. Department of Earth and Planetary Sciences Northwestern University Evanston IL USA, Bayerisches Geoinstitut University of Bayreuth Bayreuth Germany
  2. Department of Earth and Planetary Sciences Northwestern University Evanston IL USA
  3. Hawai'i Institute of Geophysics and Planetology School of Ocean and Earth Science and Technology University of Hawai'i at Manoa Honolulu HI USA
  4. Bayerisches Geoinstitut University of Bayreuth Bayreuth Germany, Advanced Light Source Lawrence Berkeley National Laboratory Berkeley CA USA
  5. Department of Geological Sciences University of Colorado Boulder CO USA
  6. Advanced Photon Source Argonne National Laboratory Argonne IL USA

Abstract

The Martian mantle is considered to have a higher Fe/Mg ratio than the Earth's mantle. Ringwoodite, γ‐(Mg,Fe) 2 SiO 4 , is likely the dominant polymorph of olivine in the core‐mantle boundary (CMB) region of Mars. We synthesized anhydrous iron‐rich ringwoodite with molar Mg/(Mg + Fe) = 0.44 and determined its thermal equation of state up to 35 GPa and 750 K by synchrotron X‐ray diffraction. Using a third order Birch‐Murnaghan equation of state, we obtain K T 0  = 182 (3) GPa, K′ = 4.6 (2), and α 0  = 3.18 (6) × 10 −5  K −1 . Using these results and an updated mineralogical model with an iron‐rich composition of Mg/(Mg + Fe) = 0.75 for the Martian mantle, we estimate ∼1900 K for the temperature of the D1000 seismic discontinuity inside Mars. The resulting adiabat predicts a warm aerotherm, which could explain the presence of partial melt at the CMB of Mars recently detected with seismic data from the 2019 InSight mission.

Sponsoring Organization:
USDOE
Grant/Contract Number:
FG02-94ER14466; AC02-06CH11357
OSTI ID:
2514542
Alternate ID(s):
OSTI ID: 2530561
OSTI ID: 2551887
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 3 Vol. 52; ISSN 0094-8276
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English

References (48)

Comparative compressibility of hydrous wadsleyite and ringwoodite: Effect of H 2 O and implications for detecting water in the transition zone journal December 2015
Crystal structures of Ni2SiO4 and Fe2SiO4 as a function of temperature and heating duration journal July 1986
The bulk composition of Mars journal December 2013
Computation of phase equilibria by linear programming: A tool for geodynamic modeling and its application to subduction zone decarbonation journal July 2005
Hydrogen partitioning between iron and ringwoodite: Implications for water transport into the Martian core journal October 2009
Sound velocities of hydrous ringwoodite to 16GPa and 673K journal May 2012
High water solubility of ringwoodite at mantle transition zone temperature journal February 2020
Geophysical and cosmochemical evidence for a volatile-rich Mars journal January 2022
High pressure-temperature single-crystal elasticity of ringwoodite: Implications for detecting the 520 discontinuity and metastable ringwoodite at depths greater than 660 km journal February 2022
Thermal equation of state of (Mg0.91Fe0.09)2SiO4 ringwoodite journal June 2004
Sound velocities and elastic constants of iron-bearing hydrous ringwoodite journal June 2004
Thermal expansion of wadsleyite, ringwoodite, hydrous wadsleyite and hydrous ringwoodite journal June 2004
The effect of iron on the elastic properties of ringwoodite at high pressure journal December 2006
Adiabatic temperature profile in the mantle journal November 2010
New accurate compression data for γ-Fe2SiO4 journal December 2010
Anhydrous ringwoodites in the mantle transition zone: Their bulk modulus, solid solution behavior, compositional variation, and sound velocity feature journal June 2016
Monochromatization of synchrotron radiation for nuclear resonant scattering experiments journal January 2000
CONUSS and PHOENIX: Evaluation of nuclear resonant scattering data journal March 2000
Mantle solidus: Experimental constraints and the effects of peridotite composition: MANTLE SOLIDUS journal October 2000
Single-crystal elasticity of γ-(Mg 0.91 Fe 0.09 ( 2 SiO 4 to high pressures and to high temperatures journal November 2001
On protons, iron and the high-pressure behavior of ringwoodite journal January 2002
Thermal expansion of Mg2SiO4 ringwoodite at high pressures journal December 2004
The geodynamic equation of state: What and how: GEODYNAMIC EQUATION OF STATE-WHAT AND HOW journal October 2009
High pressure, high temperature equation of state for Fe 2 SiO 4 ringwoodite and implications for the Earth's transition zone: THE EQUATION OF STATE OF FE-RINGWOODITE journal April 2011
Extending the Solidus for a Model Iron‐Rich Martian Mantle Composition to 25 GPa journal October 2018
A Revised Adiabatic Temperature Profile for the Mantle journal February 2022
Marsquake Locations and 1‐D Seismic Models for Mars From InSight Data journal September 2022
Observation of a Core‐Diffracted P‐Wave From a Farside Impact With Implications for the Lower‐Mantle Structure of Mars journal November 2022
Mineralogy of the Martian interior up to core-mantle boundary pressures journal March 1997
Sound velocities and elastic properties of Fe-bearing wadsleyite and ringwoodite journal September 1998
Single-crystal elastic properties of the spinel phase of Mg 2 SiO 4 journal September 1984
Hydrous mantle transition zone indicated by ringwoodite included within diamond journal March 2014
Toward an internally consistent pressure scale journal May 2007
Compressional and shear wave velocities of Fe2SiO4 spinel at high pressure and high temperature journal September 2008
The COMPRES/GSECARS gas-loading system for diamond anvil cells at the Advanced Photon Source journal September 2008
DIOPTAS : a program for reduction of two-dimensional X-ray diffraction data and data exploration journal May 2015
New Thermodynamic Models and Calculated Phase Equilibria in NCFMAS for Basic and Ultrabasic Compositions through the Transition Zone into the Uppermost Lower Mantle journal July 2013
Equations of state of six metals above 94 GPa journal September 2004
EosFit7-GUI : a new graphical user interface for equation of state calculations, analyses and teaching journal June 2016
Unit cell refinement from powder diffraction data: the use of regression diagnostics journal February 1997
The Upper Mantle and Transition Zone journal June 2008
Physical contradictions and remedies using simple polythermal equations of state journal November 2009
Effect of iron on the compressibility of hydrous ringwoodite journal May 2010
Compressibility and thermal expansion of hydrous ringwoodite with 2.5(3) wt% H2O journal March 2012
Effect of Water on the Equation of State of Nominally Anhydrous Minerals journal January 2006
Quantification of water in hydrous ringwoodite journal January 2015
High Pressure Single Crystal Diffraction at PX^2 journal January 2017
Thermoelastic properties of iron-rich ringwoodite and the deep mantle aerotherm of Mars dataset January 2024

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