P-V equation of state for Fe2P and pressure-induced phase transition in Fe3P

High Pressure Research

Volumn 28, Issue 3, 2008, Pages 375-384

  Scott, Henry P ^a   Kiefer, Boris ^b   Martin, C David ^c   Boateng, Nana ^a   Frank, Mark R ^d   Meng, Yue ^e  

^a INDIANA UNIVERSITY SOUTH BEND   (United States)

^b NEW MEXICO STATE UNIVERSITY   (United States)

^c ARGONNE NATIONAL LABORATORY   (United States)

^d NORTHERN ILLINOIS UNIVERSITY   (United States)

^e CARNEGIE INSTITUTION OF WASHINGTON   (United States)

Author keywords

Barringerite; Bulk modulus; Equation of state; Phosphide; Planetary cores; Schreibersite

Indexed keywords

DIAMONDS; DIFFRACTION; GARNETS; GROWTH (MATERIALS); IRON; MAGNETIC MOMENTS; MAGNETISM; MATERIALS; PHASE TRANSITIONS; SILICA; SILICATE MINERALS; SYSTEM STABILITY;

BARRINGERITE; BIRCH-MURNAGHAN EQUATION OF STATE; BULK MODULUS; DIAMOND ANVIL-CELLS; EQUATION OF STATE; EXPERIMENTAL DATA; EXPERIMENTAL VALUES; FIRST-ORDER PHASE TRANSFORMATION; HIGH-PRESSURE DIFFRACTION; HUBBARD; IN SITU SYNCHROTRON X-RAY DIFFRACTION; MINERAL PHYSICS; MINOR COMPONENTS; ON-SITE CORRELATION; P SYSTEMS; PHOSPHIDE; PLANETARY CORES; PRESSURE STABILITY; PRESSURE-INDUCED PHASE TRANSITIONS; ROOM TEMPERATURES; SCHREIBERSITE; SECOND ORDERS; THEORETICAL CALCULATIONS; ZERO PRESSURE;

EQUATIONS OF STATE;

EID: 52949151182     PISSN: 08957959     EISSN: 14772299     Source Type: Journal    
DOI: 10.1080/08957950802246506     Document Type: Conference Paper

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