Collaborative Research: An Experimental Investigation of Reactive Melt Channelization in Partially Molten Rocks

融化发生在板块构造边界带和火山热点之下，如夏威夷和冰岛。迁移的熔体和周围岩石之间的物理和化学相互作用决定了行星如何随着时间的推移而演变。然而，在地球深处形成的熔融物向上迁移到地表，在地壳岩浆房中喷发或缓慢冷却的方式还不清楚。地质学家想知道行星的整体成分是如何演变成地壳岩石的，这些岩石与下面的地幔岩石具有根本不同的矿物学。这些信息巩固了关于地球内部和表面之间化学交换程度的知识。这项研究的特点是一个早期的职业科学家与成熟的专家合作，实施新的实验室技术，首先，应该产生的结果，可以与无法进入的自然系统。随着实验程序的完善，将开发新的本科生实验室练习。他们将使用玻璃珠和盐，并向学生介绍技术，使研究系统的物理和化学之间存在反馈的复杂过程成为可能。熔体提取影响地幔，地壳和大气之间的大部分化学交换。地球化学、地球物理和地质证据表明，在熔体提取的某个阶段，熔体必须分离成高渗透性通道。这些通道必须足够隔离，以保持化学不平衡，并具有足够的渗透性，以允许快速熔融提取，以保持放射性不平衡。在自然界中，熔体偏析被推断为由于反应和变形之间的相互作用而发生。实验研究提供了关键的见解熔体迁移过程中发生的，并激励进一步的理论发展。最近开发的实验方法再现了反应渗透不稳定性。由于孔隙压力的梯度可以在这些实验中控制，因此可以独立地控制熔体速度和熔体-固体反应性。因此，渗透率随时间的演变可以探索的反应修改岩石微观结构，由于通道化的熔体流量的增加可以量化，熔体迁移制度可以记录为物理和化学驱动力的函数。第一组实验将在高温高压下对橄榄石与单斜辉石和斜方辉石的双组分样品进行。第二组将联合收割机橄榄石与两种辉石结合在一个样品中。这项研究还将开发新的方法来分析所产生的微观结构和测试/完善参数，允许将实验室数据扩展到自然环境。

Melting occurs beneath the plate tectonic boundary zones as well as volcanic hotspots, such as Hawaii and Iceland. The physical and chemical interactions between the migrating melt and the surrounding rock determine how planets evolve over time. However, the means by which melt formed deep in the Earth migrates upward to the surface to either erupt or cool slowly in a crustal magma chamber are not well understood. Geologists want to know how bulk planetary composition evolves to produce crustal rocks that have fundamentally different mineralogy than the underlying mantle rock. Such information underpins knowledge about the extent of chemical exchange between the Earth's interior and surface. This study will feature an early career scientist working with established experts to implement new laboratory techniques that, for the first, should produce results that can be related to the inaccessible natural system. As the experimental procedures are honed, new undergraduate lab exercises will be developed. They will employ glass beads and salt and introduce students to techniques that make is possible to investigate complex processes where there are feedbacks between the physics and chemistry of the system.Melt extraction affects much of the chemical exchange between mantle, crust and the atmosphere. Geochemical, geophysical and geological evidence suggests that, at some stage of melt extraction, melt must segregate into high permeability channels. These channels must be isolated enough to preserve chemical disequilibrium and permeable enough to allow fast melt extraction in order to preserve radiogenic disequilibrium. In nature, melt segregation is inferred to occur due to an interplay between reaction and deformation. Experimental investigations provide key insights into the processes occurring during melt migration and motivate further theoretical developments. A recently developed experimental methodology has reproduced the reaction infiltration instability. Since the gradient in pore pressure can be controlled in these experiments, it is possible to independently control melt velocity and melt-solid reactivity. Thus, the evolution of permeability with time can be explored as the reaction modifies the rock microstructure, the increase in melt flux due to channelization can be quantified, and melt migration regimes can be documented as a function of physical and chemical driving forces. A first set of experiments will be conducted on dual composition samples of olivine with clinopyroxene, and with orthopyroxene at high temperature and pressure. A second set will combine olivine with both pyroxenes in a single sample. This study will also develop new methods for analyzing the resulting microstructures and test/refine parameters that allow for scaling of laboratory data to natural environments.