2005 47th Annual Meeting of the Division of Plasma Physics
Monday–Friday, October 24–28, 2005;
Denver, Colorado
Session RI2: Inertial Confinement, Plasma Etch, and Plasma Thruster Technologies
2:00 PM–5:30 PM,
Thursday, October 27, 2005
Adam's Mark Hotel
Room: Plaza Ballroom EF
Chair: John Caughman, Oak Ridge National Laboratory
Abstract ID: BAPS.2005.DPP.RI2.1
Abstract: RI2.00001 : Forming Smooth Cryogenic Target Layers for OMEGA Direct-Drive ICF Implosions and Prospects for Direct-Drive Targets for the NIF
2:00 PM–2:30 PM
Preview Abstract
Abstract
Author:
D.R. Harding
(Laboratory for Laser Energetics, U. of Rochester)
More than 100 cryogenic D$_{2}$ target ice layers have been formed for
direct-drive ICF implosion experiments at LLE. While all of these layers are
smooth to several microns rms, some of them have achieved the 1-\textit{$\mu $}m rms
nonuniformity required for high-yield implosions. The largest effect on the
quality of a cryogenic target layer is the thermal uniformity of the
target's surroundings. Temperature nonuniformities at the ice that exceed
100 \textit{$\mu $}K are observable in the layers. Control of the thermal environment
determines the uniformity of the ice layer thickness and the time it takes
to form the layer. Detailed evidence for this sensitivity and the importance
of the thermal environment to the ice quality are presented. The initial
direct-drive target design for the NIF is significantly different from the
current OMEGA design with the addition of a fill tube and a refracting
``Saturn'' ring around the target equator (allows direct drive with the NIF
x-ray drive beam configuration). Progress at making these targets and a
strategy for creating a thermal environment capable of forming high-quality
ice layers in these targets will be presented. LLE is modifying its
cryogenic systems to perform DT implosions. Transitioning from pure D$_{2}$
to mixtures of D$_{2}$, DT, and T$_{2}$ adds complexity that may affect the
ice layer quality. The disparate freezing temperatures of the isotopes may
result in partial fractionation with the standard slow-cool protocol used to
form a smooth layer. The ability to enhance the layering process using
infrared heating may be affected by the inhomogeneity of the isotope
concentrations in the ice. These effects are reported for a mixture of
H$_{2}$, HD, and D$_{2}$ that is used as a proxy for D$_{2}$, DT, and
T$_{2}$ mixtures. The status of DT cryogenic operations will be presented.
This work was supported by the U.S. Department of Energy Office of Inertial
Confinement Fusion under Cooperative Agreement No. DE-FC52-92SF19460.
Contributors: M. J. Bonino, T. Duffy, D. H. Edgell, L. M. Elasky, R. Q.
Gram, D. Jacobs-Perkins, R. Janezic, S. J. Loucks, L. D. Lund, D. D.
Meyerhofer, W. Seka, W. T. Shmayda, and M. D. Wittman, \textit{LLE}.
To cite this abstract, use the following reference: http://meetings.aps.org/link/BAPS.2005.DPP.RI2.1