Equilibrium and Reaction of Mineral-water interaction in upper crust

上地壳矿水相互作用的平衡与反应

基本信息

  • 批准号:
    14204051
  • 负责人:
  • 金额:
    $ 33.11万
  • 依托单位:
  • 依托单位国家:
    日本
  • 项目类别:
    Grant-in-Aid for Scientific Research (A)
  • 财政年份:
    2002
  • 资助国家:
    日本
  • 起止时间:
    2002 至 2004
  • 项目状态:
    已结题

项目摘要

A sample chamber for environment controlled in-situ observation was designed and made for x-ray diffraction experiments under 200℃, and under-saturated condition (up to 1.55 MPa at 200℃) to investigate mineral-vapor equilibrium and reactions. An apparatus for higher temperature and pressure was designed to investigate under-and over-saturated conditions.Experiments : Cation exchanged smectite, Kunipia F by alkali metal ion, Li+-Cs+, alkali earth metal ion, Mg2+-Ba2+ and La3+were used to investigate swelling property in terms of cations up to 150℃. The swelling behavior of smectite with various cations for temperature rage up to 150℃Molecular simulations : We made a program to produce initial structures having surfaces with fluid phase. Molecular dynamics simulation programs, MXORTO/MXDTRICL, were updated for the very large systems. Using these programs on MPI parallel PC systems, MD simulations with more than 50,000 atoms systems became possible. We performed calculations to derive excess mixing enthalpy and diffusion constant of H20 and exchangeable cations in interlayer region of clay minerals. Using these programs, we performed some multi-phase complex systems, such as smectite with edge-water/aqueous solution (NaCl,CaCl2 etc.). serpentine group minerals-water/solution systems. MD calculations of zeolite surface-ammonium gas system revealed the dynamic process of ammonium molecules at and near channel windows in zeolite structures.Analysis : Combining the data by experiments and molecular simulation results, we analyzed the relation between structural change and adsorption behavior with equilibrium and non-equilibrium processes under various physico-chemical conditions.
设计并制作了一个环境控制原位观测样品室,用于在200℃和欠饱和条件(200℃时压力高达1.55MPa)下进行X射线衍射实验,以研究矿物-蒸汽平衡和反应。设计了高温高压实验装置,研究了蒙脱石、Kunipia F、碱金属离子、Li ~+-Cs ~+、碱土金属离子、Mg ~(2+)-Ba ~(2+)、La ~(3+)等阳离子交换后的膨润土在150℃以下的溶胀性能。蒙皂石与不同阳离子在150℃温度范围内的溶胀行为分子模拟:我们编制了一个程序来产生具有流体相表面的初始结构。分子动力学模拟程序,MXORTO/MXDTRICL,更新的非常大的系统。在MPI并行PC系统上使用这些程序,超过50,000个原子系统的MD模拟成为可能。计算了H2O和可交换阳离子在粘土矿物层间区域的过量混合焓和扩散常数。使用这些程序,我们进行了一些多相复杂系统,如蒙脱石与边水/水溶液(NaCl,CaCl 2等)。蛇纹石类矿物-水/溶液系统。分子动力学计算揭示了铵分子在沸石结构中通道窗口及其附近的动力学过程。分析:结合实验数据和分子模拟结果,分析了在各种物理化学条件下,铵分子的结构变化与平衡和非平衡吸附行为的关系。

项目成果

期刊论文数量(14)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Tsuchiya, T., K.Kawamura, O.Ohtaka, H.Fukui, T.Kikegawa: "Precise measurement of equation-of-state and elastic properties for GaN up to 16 GPa"Solid State Communications. 121. 555-559 (2002)
Tsuchiya, T.、K.Kawamura、O.Ohtaka、H.Fukui、T.Kikekawa:“精确测量高达 16 GPa 的 GaN 的状态方程和弹性特性”固态通信。
  • DOI:
  • 发表时间:
  • 期刊:
  • 影响因子:
    0
  • 作者:
  • 通讯作者:
Mayumi KANEKO, Shinsuke MATSUNO, Takeshi MIKI, Masanobu NAKAYAMA, Hiromasa IKUTA, Yoshiharu UCHIMOTO, Masataka WAKIHARA, Katsuyuki KAWAMURA: "Local structural studies of LiCryMn2-y04 cathode materials for Li-ion batteries."The Journal of Physical Chemistr
Mayumi KANEKO、Shinsuke MATSUNO、Takeshi MIKI、Masanobu NAKAYAMA、Hiromasa IKUTA、Yoshiharu UCHIMOTO、Masataka WAKIHARA、Katsuyuki KAWAMURA:“锂离子电池 LiCryMn2-y04 正极材料的局部结构研究。”《物理化学杂志》
  • DOI:
  • 发表时间:
  • 期刊:
  • 影响因子:
    0
  • 作者:
  • 通讯作者:
Kenji Tateishi, Douglas du Boulay, Nobuo Ishizawa, Katsuyuki Kawamura: "Structural disorder along the lithium diffusion pathway in cubically stabilized lithium manganese spinel"J.Solid State Chemistry. 174. 175-181 (2003)
Kenji Tateishi、Douglas du Boulay、Nobuo Ishizawa、Katsuyuki Kawamura:“立方稳定锂锰尖晶石中锂扩散途径的结构紊乱”J.Solid State Chemistry。
  • DOI:
  • 发表时间:
  • 期刊:
  • 影响因子:
    0
  • 作者:
  • 通讯作者:
Diffusion of nitrogen gas in ice Ih
  • DOI:
    10.1016/j.cplett.2004.01.021
  • 发表时间:
    2004-02
  • 期刊:
  • 影响因子:
    2.8
  • 作者:
    T. Ikeda-Fukazawa;K. Kawamura;T. Hondoh
  • 通讯作者:
    T. Ikeda-Fukazawa;K. Kawamura;T. Hondoh
Stability and equation of state of MgGeO3 post-perovskite phase
  • DOI:
    10.2138/am.2005.1702
  • 发表时间:
    2005-01-01
  • 期刊:
  • 影响因子:
    3.1
  • 作者:
    Hirose, K;Kawamura, K;Sata, N
  • 通讯作者:
    Sata, N
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KAWAMURA Katsuyuki其他文献

KAWAMURA Katsuyuki的其他文献

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{{ truncateString('KAWAMURA Katsuyuki', 18)}}的其他基金

Structure and hydration of mineral crystal surfaces
矿物晶体表面的结构和水化
  • 批准号:
    21540493
  • 财政年份:
    2009
  • 资助金额:
    $ 33.11万
  • 项目类别:
    Grant-in-Aid for Scientific Research (C)
Texture and structure of hydrated and solvated clay minerals
水合和溶剂化粘土矿物的质地和结构
  • 批准号:
    19540501
  • 财政年份:
    2007
  • 资助金额:
    $ 33.11万
  • 项目类别:
    Grant-in-Aid for Scientific Research (C)
Interaction between organic molecules and clay mineral surfaces
有机分子与粘土矿物表面之间的相互作用
  • 批准号:
    17340161
  • 财政年份:
    2005
  • 资助金额:
    $ 33.11万
  • 项目类别:
    Grant-in-Aid for Scientific Research (B)
Interaction of Plate, Mantle, core and the magmatism in the earth's history
地球历史上板块、地幔、地核与岩浆作用的相互作用
  • 批准号:
    12126202
  • 财政年份:
    2000
  • 资助金额:
    $ 33.11万
  • 项目类别:
    Grant-in-Aid for Scientific Research on Priority Areas
Effect of defects, dislocations, and grain boundaries on phase transitions by means of molecular simulation methods
通过分子模拟方法研究缺陷、位错和晶界对相变的影响
  • 批准号:
    12640465
  • 财政年份:
    2000
  • 资助金额:
    $ 33.11万
  • 项目类别:
    Grant-in-Aid for Scientific Research (C)
Development of 850MPa internally heated gas medium high pressure apparatus with quenching capability
具有淬火能力的850MPa内热式气体介质高压装置的研制
  • 批准号:
    11354007
  • 财政年份:
    1999
  • 资助金额:
    $ 33.11万
  • 项目类别:
    Grant-in-Aid for Scientific Research (A)
Structure and physical properties of magma
岩浆的结构和物理性质
  • 批准号:
    05231101
  • 财政年份:
    1993
  • 资助金额:
    $ 33.11万
  • 项目类别:
    Grant-in-Aid for Scientific Research on Priority Areas
Investigation of the relation between basicity and enthalpy of mixing of multi-component silicate melts
多元硅酸盐熔体的碱度与混合热函关系的研究
  • 批准号:
    63470042
  • 财政年份:
    1988
  • 资助金额:
    $ 33.11万
  • 项目类别:
    Grant-in-Aid for General Scientific Research (B)

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高温高压下岩浆中硫的化学行为
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    2022
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高温高压合成新型铌酸锂型氮氧化物
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高温高压下微生物硫酸盐还原探索
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