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Demonstration of X-ray Thomson scattering as diagnostics for miscibility in warm dense matter

机译:X射线汤姆森散射作为诊断诊断,如热致密物质的混溶性

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摘要

The gas and ice giants in our solar system can be seen as a natural laboratory for the physics of highly compressed matter at temperatures up to thousands of kelvins. In turn, our understanding of their structure and evolution depends critically on our ability to model such matter. One key aspect is the miscibility of the elements in their interiors. Here, we demonstrate the feasibility of X-ray Thomson scattering to quantify the degree of species separation in a 1:1 carbon-hydrogen mixture at a pressure of ~150?GPa and a temperature of ~5000?K. Our measurements provide absolute values of the structure factor that encodes the microscopic arrangement of the particles. From these data, we find a lower limit of [Formula: see text]% of the carbon atoms forming isolated carbon clusters. In principle, this procedure can be employed for investigating the miscibility behaviour of any binary mixture at the high-pressure environment of planetary interiors, in particular, for non-crystalline samples where it is difficult to obtain conclusive results from X-ray diffraction. Moreover, this method will enable unprecedented measurements of mixing/demixing kinetics in dense plasma environments, e.g., induced by chemistry or hydrodynamic instabilities.
机译:我们的太阳系中的天然气和冰巨头可以被视为高压达到数千名开尔林的高压物理物理学的自然实验室。反过来,我们对其结构和演变的理解既批判性地取决于我们模拟此类事物的能力。一个关键方面是他们内部内部元素的误解。在这里,我们证明了X射线汤姆森散射的可行性,以在〜150〜150〜150μl的压力下量化1:1碳 - 氢气混合物中的物种分离程度.GPA和〜5000Ω·k的温度。我们的测量提供了编码颗粒的微观布置的结构因子的绝对值。从这些数据中,我们发现[公式:参见文本]%的碳原子形成碳簇的下限。原则上,该程序可以用于研究行星室内内部的高压环境下任何二元混合物的混溶性行为,特别是对于非结晶样品,其中难以从X射线衍射中获得认真成果。此外,该方法将使致密等离子体环境中的混合/解剖动力学进行前所未有的测量,例如由化学或流体动力稳定性引起的。

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