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Advances in the investigation of shock-induced reflectivity of porous carbon

Published online by Cambridge University Press:  02 July 2013

Dimitri Batani*
Affiliation:
University Bordeaux, CEA, CNRS, CELIA (Centre Laser Intense at Applications), UMR 5107, Talence, France
Stefano Paleari
Affiliation:
Dipartimento di Fisica G.Occhialini, Università di Milano Bicocca, Milan, Italy
Tommaso Vinci
Affiliation:
Laboratoire pour l'Utilisation des Lasers Intenses, UMR 7605 CNRS-CEA-Ecole Polytechnique-Paris VI, Palaiseau, France
Roberto Benocci
Affiliation:
University Bordeaux, CEA, CNRS, CELIA (Centre Laser Intense at Applications), UMR 5107, Talence, France
Keisuke Shigemori
Affiliation:
Institute of Laser Engineering, Osaka University, Suita City, Osaka, Japan
Yoichiro Hironaka
Affiliation:
Institute of Laser Engineering, Osaka University, Suita City, Osaka, Japan
Toshihiko Kadono
Affiliation:
Institute of Laser Engineering, Osaka University, Suita City, Osaka, Japan
Akiyuki Shiroshita
Affiliation:
Institute of Laser Engineering, Osaka University, Suita City, Osaka, Japan
*
Address correspondence and reprint requests to: Dimitri Batani, Centre Lasers Intenses et Applications, Universit_e Bordeaux 1, Cours de la Liberation 351, 33405 Talence cedex, France. E-mail: batani@celia.u-bordeaux1.fr

Abstract

We studied the behavior of porous carbon compressed by laser-generated shock waves. In particular, we developed a new design for targets, optimized for the investigation of carbon reflectivity at hundred-GPa pressures and eV/k temperatures. Specially designed “two-layer-two materials” targets, comprising porous carbon on transparent substrates, allowed the probing of carbon reflectivity and a quite accurate determination of the position in the P, T plane. This was achieved by the simultaneous measurement of shock breakout times, sample temperature (by optical pyrometry) and uid velocity. The experiments proved the new scheme is reliable and appropriate for reflectivity measurements of thermodynamical states lying out of the standard graphite or diamond hugoniot. An increase of reflectivity in carbon has been observed at 260 GPa and 14,000 K while no increase in reflectivity is found at 200 GPa and 20,000 K. We also discuss the role of numerical simulations in the optimization of target parameters and in clarifying shock dynamics.

Information

Type
Research Article
Copyright
Copyright © Cambridge University Press 2013 
Figure 0

Fig. 1. (Color online) Shock planarity is provided by the large focal spot (1 mm diameter) and KPP smoothing. SOP images show intense shock fronts from 100 μm to 250 μm wide with a time lag of 0.2 ns between the center and the wings.

Figure 1

Fig. 2. (Color online) Experiment layout showing the “two-layer–two material” target design. The main laser pulse produces a shock wave propagating from the porous carbon through the substrate. The shock breakout in the transparent material is imaged by a streaked optical pyrometer (SOP) and a streaked spectrograph (SSOP) while a secondary laser reflects on the back of the target and the light is collected by two VISAR interferometers.

Figure 2

Fig. 3. (Color online) Shock dynamics in the case of thick carbon layer (≳25 µm). Pressure vs. space and time is plotted. The high pressure state is maintained for 1–2 ns, while, at the arrival of the rarefaction wave, pressure drop to zero.

Figure 3

Fig. 4. (Color online) Shock dynamics in the case of thin carbon layer (≲25 µm). The high pressure state is maintained only for a fraction of ns. On the other hand, the rarefaction wave is generated when the laser pulse is at full intensity, thus the pressure of the release wave can still exceed 100 GPa.

Figure 4

Fig. 5. (Color online) Graphical resume of the main experimental outcomes. In each of the three columns, the first plot on top shows the light reflected back from the target. The reflectivity is integrated on the central portion of the VISAR images, averaging out the fringe intensities. The corresponding images are displayed immediately below, with the fringe pattern evidenced by red lines. At the bottom, the plots present the spectral temperature calculated from the SSOP images, the brightness temperature from the SOP diagnostic, and the temperature predicted by the MULTI simulations. Due to the finite size of the spectrograph slit and the image smoothing, the time resolution of the experimental spectra is reduced to about 1 ns and the time profiles are rounded out. Simulations otherwise predict a very sharp step. As reported in the text, in the first shot from the left (no. 33083) the maximum pressure was about 200 Gpa and no increase in reflectivity was observed. In the middle, the most interesting shot (no. 33062) shows a reflectivity peak (shaded in yellow) after breakout (shaded in red), vanishing as pressure drops. The pressure predicted by simulations is plotted in red. On the right, an intense shot (no. 33065) produced a reflective shock front propagating into the SiO2 substrate.

Figure 5

Fig. 6. (Color online) Hydrodynamic and equation of state relationships connect fluid velocity U with pressure P at a shock discontinuity. As the shocked carbon surface proceeds at the same speed of the compressed LiF substrate and the pressure is continuous across the interface, the measurement of the speed of the carbon surface yields the pressure, knowing the shock polar of LiF. The graph on the left shows the interface velocity calculated from fringe shift recorded by Visar; higher and lower bounds are given; one fringe jump is considered at breakout. The presence of the window material and the change of its index of refraction under compression has been considered (Setchell, 2002; Clérouin et al., 2006). On the right, lithium fluoride shock polar is plotted on the P-U plane; according to the Visar, the fluid velocity is 6.8 ± 0.7 Km/s, thus the relation yields P = 2.6 ± 0.4 Mbar (260 ± 40 GPa), as shown graphically on the right.

Figure 6

Fig. 7. (Color online) When the shock wave is strong enough to metallize the otherwise transparent substrate, the shock front becomes reflective. In shot 33065 the velocity calculated from VISAR is consistent with the shock velocity D predicted by Multi simulations while the fluid velocity U is appreciably lower, as shown in the left plot. One fringe jump is considered at shock breakout. The Hugoniot curve for SiO2 allows to obtain the pressure starting from D: to a velocity of 11.8 ± 0.7 Km/s corresponds a pressure of 1.7 ± 0.2 Mbar(170 ± 20GPa), as shown graphically on the right.

Figure 7

Fig. 8. (Color online) Increase in reflectivity in high-pressure carbon is confirmed also by a different laser induced shock-compression experiment, performed with porous carbon steps deposited on aluminum. The reflectivity of the rear target face, recorded with a streak camera and shown at the bottom, presents bright Al stripes and opaque carbon areas before shock arrival. At breakout the converse situation is observed, the aluminum reflectivity drops due to unloading of the material into vacuum while at the carbon sites a peak is observed (indicated by the white arrow). Above, carbon signal (in blue) is compared to the aluminum (in red).

Figure 8

Fig. 9. (Color online) Phase diagram of carbon in the high pressure and temperature regime, after Grumbach & Martin (1996); the solid line (blue in the web version of this article) shows the porous carbon Hugoniot, the dashed black line indicates the graphite Hugoniot and the experimental points of reflective and non-reflective carbon are indicated by the squares; due to reflection of the shock at the interface, these points lie well above the Hugoniot; the regimes of stability of the graphite (G), diamond (D) and conductive BC-8 phases of carbon are indicated in gray, blue and yellow respectively.