EAR-PF: An Experimental Investigation of the Effect of Pressure, Mineralogy and Water on the Rheological Properties of the Upper Mantle: Implications for Mantle Dynamics

Janelle洪堡博士被授予NSF地球科学博士后奖学金，在明尼苏达大学开展研究和教育计划。这项工作将调查矿物组成（橄榄石/辉石模态丰度），水含量和压力对地球上地幔强度的影响，以更好地了解大规模的动态地幔过程。为此，本研究的一个重要目标是利用实验工作来开发流动定律（应力和应变率之间的关系），其中包括成分，水和压力的影响。将利用D-DIA（一种高压变形装置）对橄榄石/辉石聚集体（“辉石岩”）进行实验。D-DIA的最新发展将使这项研究能够研究以前在实验室中无法获得的高压条件（3-12 GPa），并且更能代表整个上地幔的变形条件。 除了分析每个实验的力学数据外，还将通过许多不同的技术（红外光谱，电子背散射衍射和透射电子显微镜）分析运行产品，以更深入地了解变形中涉及的微观物理过程。虽然浅部地球的力学行为被认为是相对较好的理解，很大的不确定性仍然存在于更深的部分上地幔（深度大于100公里）的变形行为。这种情况在很大程度上是由于在D-DIA出现之前，实验室中可获得的压力范围相当有限。在这项研究中计划的一系列实验将允许更好地了解整个上地幔的地球材料的变形行为，并通过扩展，更好地了解各种关键的地球动力学过程，如俯冲。除了发展J.洪堡的技能作为一个研究人员，这个奖学金将使她能够发展作为一个教育工作者在课堂上和外展设置。她将协助教授地质学课程，并指导明尼苏达大学的本科生和研究生。 她还将参与明尼苏达科学博物馆科学教育项目的开发。

Dr. Janelle Homburg has been awarded an NSF Earth Science Postdoctoral Fellowship to carry out a research and education plan at the University of Minnesota. This work will investigate the effects of mineralogical composition (olivine/pyroxene modal abundance), water content and pressure on the strength of Earth's upper mantle in order to better understand large-scale dynamic mantle processes. To this end, an important goal of this study is to utilize experimental work to develop flow laws (relationships between stress and strain rate) that incorporate the effects of composition, water and pressure. Experiments will be preformed on olivine/pyroxene aggregates ("harzburgite" rocks) utilizing the D-DIA, a high-pressure deformation apparatus. The recent development of the D-DIA will allow this study to investigate high-pressure conditions (3-12 GPa) that have previously been unobtainable in the lab and are more representative of deformation conditions throughout the upper mantle. In addition to analyzing the mechanical data from each experiment, the run products will be analyzed by a number of different techniques (infrared spectroscopy, electron backscatter diffraction, and transmission electron microscopy) in order to develop a deeper understanding of the microphysical processes involved in deformation. While the mechanical behavior of the shallow Earth is thought to be relatively well understood, great uncertainty still remains in the deformation behavior of the deeper portion of the upper mantle (depths greater then ~100 km). This situation is due in large part to the fact that prior to the advent of the D-DIA, the range of pressures accessible in the lab was fairly limited. The series of experiments planned in this research will allow for better understanding of the deformation behavior of earth materials throughout the entire upper mantle and, by extension, better understanding of a wide variety of key geodynamic processes, such as subduction.In addition to developing J. Homburg's skills as a researcher, this fellowship will allow her to develop as an educator both in classroom and outreach settings. She will assist in teaching geology courses and in mentoring undergraduate and graduate students at the University of Minnesota. She will also be involved in the development of science education programs at the Science Museum of Minnesota.