University of California at Berkeley – Physics Department – Hellman Lab Application of “Calorimetry-on-a- Chip” Technology to Heat Capacities of Quenched.

Slides:



Advertisements
Similar presentations
Basic Thermochemistry
Advertisements

GOLDSCHMIDT’S RULES 1. The ions of one element can extensively replace those of another in ionic crystals if their radii differ by less than approximately.
7/12/04CIDER/ITP Short Course Composition and Structure of Earth’s Interior A Perspective from Mineral Physics.
University of California at Berkeley – Physics Department March APS Meeting, Portland, OR – March 17, 2010 Thermodynamic measurements of iron-rhodium alloys.
Introduction Table 1. Summary of excess energies to be supplied for interstitial occupancy into one of 4b sites or substitutional occupancy of a Mg site.
High Pressure Mineralogy Minerals Methods & Meaning High Pressure Mineralogy.
Pg. 25.  After Earth formed, radioactive elements decayed and heat was released  Caused melting of interior  Denser elements sank to core (iron and.
C. McCammon: Intermediate spin Fe 2+ in lower mantle perovskite Intermediate spin Fe 2+ in lower mantle perovskite C. McCammon, I. Kantor, O. Narygina,
Thermoelastic properties of ferropericlase R. Wentzcovitch Dept. of Chemical Engineering and Materials Science, Minnesota Supercomputing Institute J. F.
1 Composition of the Earth GLY 4200 Fall, Interior of the Earth Earth’s interior is divided into zones, with differing properties and compositions.
Erice, 2009 Compression Systematics in Minerals Dr Robert T Downs Department of Geosciences University of Arizona Tucson, AZ.
Interpreting Geophysical Data for Mantle Dynamics Wendy Panero University of Michigan.
Diffusion in a multi-component system (1) Diffusion without interaction (2) Diffusion with electrostatic (chemical) interaction.
Dynamic Earth Class February Volcanic Imagination (Chapter 4) Exploring the Earth’s Interior.
University of California at Berkeley – Physics Department March APS Meeting, Dallas, TX – March 23, 2011 Examining the AF > FM transition in Fe-Rh thin.
Department of Food Science
University of California at Berkeley – Physics Department March APS Meeting, Dallas, TX – March 24, 2011 Calorimetry of epitaxial thin films David W. Cooke,
Mars High-Pressure Experiments COSMOCHEMISTRY iLLUSTRATED A Martian Primary Magma Olivine compositions in Martian meteorite Y indicate crystallization.
Phase Equilibrium. Makaopuhi Lava Lake Magma samples recovered from various depths beneath solid crust From Wright and Okamura, (1977) USGS Prof. Paper,
University of California at Berkeley – Physics Department – Hellman Lab March APS Meeting – March 15, 2006 Heat capacity measurements of sub- milligram.
The Interior of Mars. Why do we need to know about the interior? Main reason: Because the chemical composition and minerals inside can tell us a lot about.
University of California at Berkeley – Physics Department – Hellman Lab March APS Meeting – March 13, 2008 Heat capacity measurements of Fe/Cr multi-layers.
Pamela Burnley, UNLV Wendy Panero, OSU Integrating Mineral Physics into Geoscience Curricula.
23 April 2001Doug Martin1 Diamond: A Story of Superlatives.
I. Minerals Definitions – Earth Materials A. Rock: naturally occurring aggregate of one or more minerals B. Mineral: naturally occurring solid with a definite.
Investigation of fluid- fluid phase transition of hydrogen under high pressure and high temperature 2014/11/26 Shimizu laboratory SHO Kawaguchi.
Bellwork Obj: SWBAT describe the layers within the earth. 1.What happens to the temperature as you move from the crust to the core of the earth?
The Third Law, Absolute Entropy and Free Energy Lecture 4.
Slide 1 Observations/Inferences: Rocky inner, icy outer solar system Asteroid differentiation temperatures heliocentrically distributed Gross zonal structure.
Phase Transitions in the Earth’s Mantle
Carbon in the Earth’s core Yingwei Fei Geophysical Laboratory Carnegie Institution of Washington.
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.
Earth Materials Minerals: The Crystalline State Minerals and Mineralogy Mineral Chemistry Atomic Structure of Minerals Minerals as indicators of the environment.
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.
Solid state chemistry of iron-nickel phosphides and the composition of the Earth core Malcolm F. Nicol, University Nevada Las Vegas, DMR Seismic.
Pressure measurements at high temperature: open issues and solutions Peter I. Dorogokupets Institute of the Earth’s Crust SB RAS, Irkutsk, Russia
Fluid, 90% iron solidified iron km ,00012,000 Mg(Fe) silicates phase changes basaltic-granitic crust chemical stratification and differentiation.
Energy, heat and temperature Olivia Jensen – 13/10/11... for 666 Module 2.
National Science Foundation X-ray vision of nano-materials Eric E Fullerton, University of California-San Diego, DMR Researcher at University of.
Diffusion in Earth’s Deep Interior: Insights from High-Pressure Experiments Jim Van Orman Department of Geological Sciences Case Western Reserve University.
Pressure-Temperature Stability Studies of Talc and 10-Å phase using x-ray diffraction. Arianna E. Gleason 1, Martin Kunz 1, Stephen Parry 2, Alison Pawley.
Structure of the Earth and Mineralogy Environmental Science Earth Science Unit Environmental Science Earth Science Unit.
1 Composition of the Earth GLY 4200 Fall, Interior of the Earth Earth’s interior is divided into zones, with differing properties and compositions.
Compres Laser Heating Activities Technical CO2 laser heating system at GSECARS Component of ID-D upgrade (in progress) Staff: Andy Campbell (50%, beginning.
Structure and chemistry of the Earth Today’s topic: The chemistry of Earth’s mantle and crust.
Fundamental Concepts of Thermodynamics First, second, and third law Entropy Heat capacity, enthalpy Reaction enthalpies and thermochemical cycles Phase.
Post-perovskite Transition in MgSiO3
Earth’s Core-Mantle Boundary: Results of Experiments at High Pressures and Temperatures Knittle& Jeanloz, Science, Vol. 251 (5000), 1991.
High pressure study on superconductor K x Fe 2-y Se 2 M1 Hidenori Fujita Shimizu group.
THERMODYNAMICS OF FORMATION AND ORDERING IN SILVER ALKANETHIOLATES: THREE DIMENSIONAL ANALOGUES TO SELF-ASSEMBLED MONOLAYERS Silver alkanethiolates are.
Basic Thermochemistry Courtesy of lab-initio.com.
Neutrons Coordinator: Nancy Ross, VT 2004 COMPRES Annual Meeting.
PREM = Preliminary Reference Earth Model So what is the Earth’s interior made of? Look for rocks at surface with Vp ~ 8 km/s and density ~ 3.5 km/s.
The Core-Mantle Boundary Region Jeanloz & Williams, 1998 Lower mantle Outer core CMB Heat flow.
MINERALS ARE EVERYWHERE. WHAT IS A MINERAL? All Minerals share the following 5 characteristics: Naturally occurring: a mineral forms by natural geologic.
Radiative Thermal Conductivity of the Lower Mantle Emma Rainey Abby Kavner Laurent Pilon.
Applications of Mössbauer Spectroscopy to Studies of the Earth’s Interior C. McCammon Bayerisches Geoinstitut Universität Bayreuth D Bayreuth,
Chapter 6 Thermochemistry: pp The Nature of Energy Energy – Capacity to do work or produce heat. – 1 st Law of Thermodynamics: Energy can.
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.
Quest for Materials for Renewable Energy Applications
Ch 6: Internal Constitution of the Earth
The Earth is differentiated
23 April 2001Doug Martin1 Diamond: A Story of Superlatives.
Minerals & Their Families
CIDER/ITP Short Course
We have been talking about minerals primarily in the earth’s crust
The Phase Diagram of FeO
Igneous Rocks Chapter 5.
We have been talking about minerals primarily in the earth’s crust
Presentation transcript:

University of California at Berkeley – Physics Department – Hellman Lab Application of “Calorimetry-on-a- Chip” Technology to Heat Capacities of Quenched High Pressure Samples David W. Cooke, Frances Hellman Department of Physics, University of California, Berkeley Alexandra Navrotsky, Maria Dorogova, Charles E. Lesher Thermochemistry Facility and Dept. of Geology, University of California, Davis COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab The Earth’s Mantle Seismic 670km Chemical change 1000km D” 1800km Wikipedia image based on elements of an illustration by USGS. Gu, et al. J. geophys. Res., 106, 11,169-11,199 (2001). COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Constituents of Mantle Primarily silicates Fe,Mg majority of composites Al,Ni,Ca,Cd,Co minority “dopants” High pressure and high temperature yields complicated phase diagram of novel crystal structures –Spinel (γ) –Modified Spinel (β) –Perovskite –Post-perovskite Navrotsky. Prog. Solid St. Chem. 17, (1987). COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Constituents of Mantle (Mg,Fe) 2 SiO 4 Spinel Fe,Mg Si O O Fe,Mg (Mg,Fe)SiO 3 Perovskite Illustrations courtesy of Dr. Helmut Föll at University of Kiel - COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Synthesizing in the Lab Multi-anvil cell (<~ 27 GPa) Diamond anvil cell (<~ 200 GPa) –X-ray/IR spectroscopy, conductivity, compressibility –P-V-T, K, μ, more The first diamond-anvil cell, fabricated by Charles Weir and Alvin Van Valkenburg NIST - Navrotsky. Prog. Solid St. Chem. 17, (1987). COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Fe v. Mg Silicates Hazen, R. Science 259, (1993). COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab “Calorimeter on a Chip” Specific heat of thin films –100nm ~= 5µg –2K - 500K –0T - 8T Information gained: –Thermodynamics Decomposition Magnetic transitions Electrical changes 2006 APS Keithley Instrumentation Award COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Device Simulation Chi^2/DoF E-8 R^ ParameterValueError y E E-5 A E-5 t E-5 COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Device Simulation COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Proof of Principle COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Proof of Principle COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab COMPRES Proposal Multi-anvil and/or diamond-anvil cell experiments –Thermal contact –Sample size –Crystal shape Magnetic transitions in high pressure minerals –Test case – Fe 2 SiO 4 spinel Data across an Mg-Fe substituted series –(Fe,Mg) 2 SiO 4 olivine and/or spinel phases –(Mg,Fe)O magnesiowustites COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab COMPRES Proposal Used indium in past –Low melting point, but not good for metastable materials Silver paint –Reproducibility? Multi-anvil and/or diamond-anvil cell experiments –Thermal contact –Sample size –Crystal shape COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab COMPRES Proposal Multi-anvil and/or diamond-anvil cell experiments –Thermal contact –Sample size –Crystal shape Sample Size –Data on large devices (CoO) Addenda (Cu/LSN) = ~50 μJ Ag Addenda = ~100 μJ Sample = ~200 μJ Sample Size –Data on regular devices Addenda (LSN) = ~3 μJ Copper Addenda = ~2 μJ Sample = ~2 μJ COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab COMPRES Proposal Multi-anvil and/or diamond-anvil cell experiments –Thermal contact –Sample size –Crystal shape Magnetic transitions in high pressure minerals –Test case – Fe 2 SiO 4 spinel Data across an Mg-Fe substituted series –(Fe,Mg) 2 SiO 4 olivine and/or spinel phases –(Mg,Fe)O magnesiowustites COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Fe 2 SiO 4 Spinel Why Fe 2 SiO 4 Spinel? –Relatively low pressure of formation (~8GPa) Larger quantity of sample Multi-anvil apparatus (Charles Lesher’s lab) –Relevant to mantle physics –Potential Mg/Fe substitutional analysis –Iron silicate – we expect a magnetic transition –Fe 2+ v. Fe 3+ – potential electronic interactions? COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Fe 2 SiO 4 Spinel K. Suito et al. Proc. 9 th AIRAPT Intl. High P. Conference (1983). COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Fe 2 SiO 4 Spinel COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Fe 2 SiO 4 Spinel COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab COMPRES Proposal Multi-anvil and/or diamond-anvil cell experiments –Thermal contact –Sample size –Crystal shape Magnetic transitions in high pressure minerals –Test case – Fe 2 SiO 4 spinel Data across an Mg-Fe substituted series –(Fe,Mg) 2 SiO 4 olivine and/or spinel phases –(Mg,Fe)O magnesiowustites COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Future Work Diamond Anvil Cell Sample Capability –Develop reliable method for ~10μg sample –Consistency of silver paint? Fe 2 SiO 4 Spinel –Can we factor out the magnetic entropy –Why is the magnetic transition so much more broad? –Substitutional (Fe,Mg) 2 SiO 4 series –Decomposition enthalpy Other materials of geophysical applications –(Mg,Fe)O magnesiowustites –(Mg,Fe)SiO 3 perovskites –High pressure phases in zirconia and titania COMPRES Calorimetry on a Chip Workshop – March 15, 2007

University of California at Berkeley – Physics Department – Hellman Lab Thanks to: Frances Hellman Alex Navrostsky Masha Dorogova Charles Lesher Department of Energy Lawrence Berkeley National Lab University of California – Berkeley University of California – Davis Oak Ridge National Laboratory Ray Jeanloz Daniel Queen Erik Helgren COMPRES Calorimetry on a Chip Workshop – March 15, 2007