Managing in Local Government 1994
DOI: 10.1007/978-1-349-23650-3_3
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Cited by 6 publications
(9 citation statements)
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“…The quartz Hugoniot was previously established by the OMEGAlaser experiments to have a linear U s -U p relation given by U sQ = a 0 +a 1 (U pQ −β), where a 0 = 20.57±0.15, a 1 = 1.291 ± 0.036, and β = 12.74 23,26 . This formula is valid at the pressure over 200 GPa and in good agreement with the Kerley-7360 EOS model 27 . Impedance-matching occurs at the intersection of the hydrogen Rayleigh line and the release isentrope of quartz.…”
Section: Results: Shock Velocitiessupporting
confidence: 72%
“…The quartz Hugoniot was previously established by the OMEGAlaser experiments to have a linear U s -U p relation given by U sQ = a 0 +a 1 (U pQ −β), where a 0 = 20.57±0.15, a 1 = 1.291 ± 0.036, and β = 12.74 23,26 . This formula is valid at the pressure over 200 GPa and in good agreement with the Kerley-7360 EOS model 27 . Impedance-matching occurs at the intersection of the hydrogen Rayleigh line and the release isentrope of quartz.…”
Section: Results: Shock Velocitiessupporting
confidence: 72%
“…Also shown in the figures are data from Simakov and Trunin, 51 and Vildanov et al 52 The solid line is the predicted U s − u p response from a quartz EOS model, Sesame 7360, 44 with the initial density set at 200 mg/ cc ͑ϳ13.25 times expanded͒. 4 and 5.…”
Section: Aerogel Hugoniot Experimentsmentioning
confidence: 99%
“…The rectangular flyer plate, approximately 12 ϫ 25 mm in lateral dimension by ϳ300 m in effective thickness 42 was accelerated across a nominal 3-to 4-mm vacuum gap by the magnetic field. Due to the considerable porosity of the aerogel sample, shock compression resulted in a significant increase in temperature; the temperature of the silica aerogel on the Hugoniot between ϳ30 and 75 GPa is estimated to be approximately 30 000-70 000 K. 44,45 Thus the shocked aerogel emits a copious amount of visible light, providing a convenient way of diagnosing shock propagation in the sample. The flyer plate velocity was directly measured using a conventional velocity interferometry 43 velocity interferometer system for any reflector ͑VISAR͒ to an accuracy of typically ϳ1% to 2%.…”
Section: Aerogel Hugoniot Experimentsmentioning
confidence: 99%
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“…PIMC simulations and the Sesame EOS predict a relatively stiff behavior at high pressures while the LM and FVT + id models yield a more compressible EOS. The application of the various hydrogen EOS to Giant Planets and the comparison of their predicted internal structure with observational parameters is an alternative test besides laboratory experiments, see [51,52] for reviews. Giant Planets like Jupiter consist of roughly 10% helium and 90% hydrogen, forming a cold molecular fluid in the outer envelope and a pressure ionized plasma in the deeper interior as indicated by the existance of a magnetic field.…”
Section: Eos and Hugoniot Curvesmentioning
confidence: 99%