Collaborative Research: COMPRES Grand Challenge for Experimental Study of Plastic Deformation under Deep Earth Conditions

Karato0136181地球材料的定量流变学测量仅在相对较低的压力条件下进行，对应的深度为~60千米或更小。该项目的主要目的是通过技术发展，将这一界限扩大到至少800公里，不仅覆盖上地幔，而且覆盖过渡带和下地幔。我们建议通过利用国家设施和教育项目的运营基础设施，与COMPRES(地球科学材料特性研究联合会)协调建立一个新的机构间计划，我们将为更广泛的科学界扩大这些设施的能力。通过机构间的合作，我们将开发两种新的设备(改进的立方体设备(D-DIA)和旋转Drickamer设备(RDA))，此外还将进一步改进使用多砧板设备(MA)的成熟的变形技术。D-DIA和RDA(以及MA)都可以很容易地安装到同步辐射设施中，以允许在高压和温度条件下对应力和应变进行定量测量。D-DIA适合于包括剪切局部化和由此产生的不稳定性在内的定量流变学测量，而RDA具有独特的高压大应变变形实验能力，这是研究晶格择优取向的重要特征。这些设备将被用来获得第一组关于地球和行星材料在高压、高温条件下(~15-25 Gpa，~2000K)的流变性和形变诱导的微观结构的定量数据集。这些测量结果将有助于更好地了解(I)整个地幔的流变性质的径向和横向变化，(Ii)流变行为与包括相变在内的化学反应的相互作用，以及(Iii)变形诱导的微结构的性质，如晶格择优取向(导致地震各向异性)。这样开发的独特设施将可供大型矿物和岩石物理界使用，并将大大加强矿物和岩石物理研究对广泛的固体地球科学的贡献。

Karato0136181Quantitative rheological measurements on Earth materials have been conducted only under relatively low-pressure conditions corresponding to the depth of ~60 km or less. The main thrust of this project is to extend this limit, through technical developments, at least to ~800 km covering not only the upper mantle but also the transition zone and the lower mantle. We propose to establish a new inter-institutional program coordinated with COMPRES (Consortium for Materials Property Research in the Earth Sciences) by utilizing the infrastructure for operation of national facilities and educational program, and we will expand the capabilities of these facilities for the broader scientific community. Through inter-institutional collaboration, we will develop two new types of apparatus (a modified cubic apparatus (D-DIA) and a rotational Drickamer apparatus (RDA)) in addition to further improvements to the well-established deformation techniques using a multianvil apparatus (MA). Both D-DIA and RDA (as well as MA) can readily be fitted to synchrotron radiation facilities to allow quantitative measurements of stress and strain at high-pressure and temperature conditions. D-DIA is suited for quantitative rheology measurements including shear localization and resultant instabilities while RDA has a unique capability of large strain deformation experiments at high-pressures, an important feature for study of lattice preferred orientation. These apparatus will be used to obtain the first quantitative data set on rheological properties and deformation-induced microstructures of Earth and planetary materials under high-pressure, high-temperature conditions (to ~15-25 GPa, ~2000 K). The results of such measurements will contribute to better understand (i) the radial and lateral variation of rheological properties for whole mantle, (ii) the interaction of rheological behavior with chemical reactions including phase transformations, and (iii) the nature of deformation-induced microstructures such as lattice preferred orientation (which causes seismic anisotropy). The unique facility thus developed will be accessible to a large mineral and rock physics community and will significantly enhance the contribution of mineral and rock physics research to a wide range of solid Earth sciences.