PRESSURE EFFECT ON MN, CO AND NI PARTITIONING BETWEEN IRON HYDRIDE AND MANTLE MINERALS

被引：0
|
作者：
SUZUKI, T [1 ]
AKAOGI, M [1 ]
YAGI, T [1 ]
机构：
[1] UNIV TOKYO, INST SOLID STATE PHYS, MINATO KU, TOKYO 106, JAPAN
来源：
PROCEEDINGS OF THE JAPAN ACADEMY SERIES B-PHYSICAL AND BIOLOGICAL SCIENCES | 1994年 / 70卷 / 03期
关键词：
HIGH PRESSURE; ELEMENTAL PARTITION; EARTHS CORE;
D O I：
暂无
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
Partitioning behaviors of Mn, Co and Ni between iron hydride and mantle minerals (olivine, pyroxene and magnesiowustite) under high pressure were experimentally investigated at 1400 degrees C and 3 similar to 11 GPa. The present experimental results showed that the siderophile nature of Co and Ni, and the lithophile nature of Mn decrease under high pressures: all the observed metal/mineral partition coefficients, K'=(X(i)/X(Fe))metal/(X(i)/X(Fe))(mineral), i=Mn, Co and Ni, approach 1 with increase in pressure. K' also depends on the composition of the mineral phase: K' decreases with an increase in MgO mol fraction. From these experimental results, it is expected that the observed upper mantle elemental abundance may be explained by the equilibrium between metal and silicates under extremely high pressure.
引用
收藏
页码：31 / 36
页数：6
相关论文
共 50 条
  • [1] Pressure dependence of Ni, Co and Mn partitioning between iron hydride and olivine, magnesiowustite and pyroxene
    Suzuki, T
    Akaogi, M
    Yagi, T
    [J]. PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1996, 96 (2-3) : 209 - 220
  • [2] PARTITIONING OF IRON, COBALT AND NICKEL BETWEEN MINERALS OF THE EARTHS LOWER MANTLE AT HIGH-PRESSURE AND HIGH-TEMPERATURE
    MALAVERGNE, V
    GUYOT, F
    PEYRONNEAU, J
    POIRIER, JP
    [J]. COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II, 1995, 320 (06): : 455 - 462
  • [3] Spin transition, substitution, and partitioning of iron in lower mantle minerals
    Fujino, Kiyoshi
    Nishio-Hamane, Daisuke
    Nagai, Takaya
    Seto, Yusuke
    Kuwayama, Yasuhiro
    Whitaker, Matthew
    Ohfuji, Hiroaki
    Shinmei, Toru
    Irifune, Tetsuo
    [J]. PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 2014, 228 : 186 - 191
  • [4] Element partitioning between some mantle minerals and the coexisting silicate melt under high pressure
    Suzuki, T
    Akaogi, M
    [J]. PROPERTIES OF EARTH AND PLANETARY MATERIALS AT HIGH PRESSURE AND TEMPERATURE, 1998, 101 : 261 - 270
  • [5] Water partitioning between mantle minerals from peridotite xenoliths
    Grant, Kevin
    Ingrin, Jannick
    Lorand, Jean Pierre
    Dumas, Paul
    [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 2007, 154 (01) : 15 - 34
  • [6] Water partitioning between mantle minerals from peridotite xenoliths
    Kevin Grant
    Jannick Ingrin
    Jean Pierre Lorand
    Paul Dumas
    [J]. Contributions to Mineralogy and Petrology, 2007, 154 : 15 - 34
  • [7] Iron partitioning in natural lower-mantle minerals: Toward a chemically heterogeneous lower mantle
    Kaminsky, Felix V.
    Lin, Jung-Fu
    [J]. AMERICAN MINERALOGIST, 2017, 102 (04) : 824 - 832
  • [8] The effect of pressure on partitioning of Ni and Co between silicate and iron-rich metal liquids: a diamond-anvil cell study
    Bouhifd, MA
    Jephcoat, AP
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 2003, 209 (1-2) : 245 - 255
  • [9] SC, CR, CO AND NI PARTITIONING BETWEEN MINERALS FROM SPINEL PERIDOTITE XENOLITHS
    STOSCH, HG
    [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1981, 78 (02) : 166 - 174
  • [10] PARTITIONING OF NI BETWEEN MAGNESIOWUSTITE AND METAL AT HIGH-PRESSURE - IMPLICATIONS FOR CORE MANTLE EQUILIBRIUM
    URAKAWA, S
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1991, 105 (1-3) : 293 - 313
12345