Geodynamic models with thermodynamically self-consistent mineral physics
具有热力学自洽矿物物理的地球动力学模型
基本信息
- 批准号:41509765
- 负责人:
- 金额:--
- 依托单位:
- 依托单位国家:德国
- 项目类别:Research Grants
- 财政年份:2007
- 资助国家:德国
- 起止时间:2006-12-31 至 2008-12-31
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
We propose to combine geodynamic mantle modeling with thermodynamic models of mantle mineralogy in order to gain a better understanding of the thermal and elastic structure of Earth s mantle. For the geodynamic modeling we will use two dimensional (2-D) and three dimensional (3-D) mantle convection codes. For the thermodynamic mantle model we will apply the Gibbs-free-energy minimization method in order to compute mantle phase equilibria for a range of chemical mantle models. (1) temperature fields from mantle convection modeling will be postprocessed: we will assign to each Temperature (T) and Pressure (P) grid point value from the convection calculation its corresponding equilibrium mineral assemblage and physical properties. (2) We will then couple the convection and mineralogical model: we will use the density of the mineral assemblage to compute buoyancy forces (via the buoyancy term in the momentum equation) in the convection model. Thus densities derived from the mineralogical model establish convective flow and a thermal structure in the geodynamic model, while at the same time the P, T structure of the convection model is used in the computation of the equilibrium mineral assemblage. By combining the equation-of-state parameters with a shear wave model we will be able to study convection consistently with the underlying mineralogy. The proposed work will permit us to compare predictions of geodynamic mantle models directly to observed seismic properties. This is important because recent seismic studies of the mantle show results that are not easily understood in terms whole mantle convection. We will test the hypothesis that the seismic results can be attributed in part to complexities in the mineralogy. The mineralogical model will be made available for general use through a website, as a research and teaching tool for the geophysical and high pressure mineralogical community.
我们建议将联合收割机地球动力学地幔模拟与地幔矿物学热力学模型相结合,以便更好地了解地幔的热弹性结构。对于地球动力学模拟,我们将使用二维(2-D)和三维(3-D)地幔对流代码。对于热力学地幔模型,我们将应用吉布斯自由能最小化方法,以计算一系列化学地幔模型的地幔相平衡。(1)对地幔对流模拟的温度场进行后处理:我们将为对流计算的每个温度(T)和压力(P)网格点值分配相应的平衡矿物组合和物理性质。(2)然后,我们将耦合对流和矿物学模型:我们将使用矿物组合的密度来计算对流模型中的浮力(通过动量方程中的浮力项)。因此,从矿物学模型导出的密度在地球动力学模型中建立对流和热结构,而同时对流模型的P,T结构用于平衡矿物组合的计算。通过将状态方程参数与剪切波模型相结合,我们将能够研究与底层矿物学一致的对流。拟议的工作将使我们能够比较预测的地球动力学地幔模型直接观察到的地震属性。这一点很重要,因为最近的地幔地震研究表明,在整个地幔对流方面不容易理解的结果。我们将测试的假设,地震的结果可以部分归因于矿物学的复杂性。矿物学模型将通过一个网站供一般使用,作为地球物理和高压矿物学界的研究和教学工具。
项目成果
期刊论文数量(0)
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科研奖励数量(0)
会议论文数量(0)
专利数量(0)
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Professor Dr. Hans-Peter Bunge, Ph.D.其他文献
Professor Dr. Hans-Peter Bunge, Ph.D.的其他文献
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{{ truncateString('Professor Dr. Hans-Peter Bunge, Ph.D.', 18)}}的其他基金
Retrodiction Range of geodynamic earth models from twin experiments that account for model inconsistencies and limited resolution of present-day heterogeneity
来自孪生实验的地球动力学地球模型的回顾范围,解释了模型不一致和当今异质性的有限分辨率
- 批准号:
412338397 - 财政年份:2019
- 资助金额:
-- - 项目类别:
Research Grants
Feasibility study to identify deep Earth signals in current and future gravity field missions
在当前和未来重力场任务中识别地球深部信号的可行性研究
- 批准号:
323625017 - 财政年份:2016
- 资助金额:
-- - 项目类别:
Research Grants
Determination of current geoid trends related to deep Earth processes in the South Atlantic region
确定与南大西洋地区地球深层过程相关的当前大地水准面趋势
- 批准号:
243973216 - 财政年份:2013
- 资助金额:
-- - 项目类别:
Priority Programmes
TERRA-NEO - Integrated Co-Design of an Exascale Earth Mantle Modeling Framework
TERRA-NEO - 百亿亿次地幔建模框架的集成协同设计
- 批准号:
230862710 - 财政年份:2012
- 资助金额:
-- - 项目类别:
Priority Programmes
Mapping the upper mantle structure beneath the South Atlantic and the adjacent continents using full waveform tomography with geodynamic interpretations of hotspot flux and material transport in the asthenosphere.
使用全波形断层扫描绘制南大西洋和邻近大陆下方的上地幔结构图,并对软流圈中的热点通量和物质传输进行地球动力学解释。
- 批准号:
172686521 - 财政年份:2010
- 资助金额:
-- - 项目类别:
Priority Programmes
Seismic waveform tomography on continental scales based on the spectral-element and adjoint methods
基于谱元和伴随方法的大陆尺度地震波形层析成像
- 批准号:
73582572 - 财政年份:2009
- 资助金额:
-- - 项目类别:
Research Grants
Program management and scientific networking
项目管理和科学网络
- 批准号:
80299618 - 财政年份:2009
- 资助金额:
-- - 项目类别:
Priority Programmes
Mineralogical and Dynamic Origin of the South African Superplume
南非超羽流的矿物学和动态起源
- 批准号:
79644183 - 财政年份:2008
- 资助金额:
-- - 项目类别:
Priority Programmes
Exploring plate tectonic force balances and plate boundary forces in the South Atlantic from plate motion histories and coupled global and regional geodynamic models
从板块运动历史和耦合的全球和区域地球动力学模型探索南大西洋的板块构造力平衡和板块边界力
- 批准号:
80283908 - 财政年份:2008
- 资助金额:
-- - 项目类别:
Priority Programmes
Forward modelling of mantle density anomalies from geodynamic considerations
从地球动力学角度考虑地幔密度异常的正演模型
- 批准号:
30265607 - 财政年份:2006
- 资助金额:
-- - 项目类别:
Priority Programmes
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