Abstract

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 2{4}_{-7}^{+6}% 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.

Highlights

  • 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

  • Whereas previous analysis has established diamond formation in these samples with X-ray diffraction (XRD) from diamond crystallites[15,23], here, we present a quantitative analysis of species separation applying X-Ray Thomson scattering (XRTS) that does not rely on the presence of crystalline structures

  • The observed results are in good agreement with XRD data recorded in the same experiment which show the formation of nanodiamonds induced by the second shock wave[15,23]

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Summary

Introduction

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. We find a lower limit of 24þÀ67% 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 highpressure environment of planetary interiors, in particular, for non-crystalline samples where it is difficult to obtain conclusive results from X-ray diffraction. The current state of the large bodies in our solar system is an essential benchmark for our understanding how planetary systems form and evolve Modern planetary probes such as the Juno mission[1] provide a growing wealth of data, such as magnetic field configurations[2], gravitational moments[3] and zonal winds[4], even for distant planets like Jupiter. To move beyond such simple models, dedicated laboratory experiments are needed to determine the properties of mixtures in this parameter regime

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