Providing more than child's play, sandpile avalanches are offering
insights into achieving optimal conditions in tokamaks, donut-shaped
devices designed to produce energy from nuclear fusion. The first priority
in a tokamak is to maintain a high-density, high-temperature plasma,
especially an optimal configuration called the H-mode. But it is not
completely understood how to get fusion plasmas into this state.
Sandpiles may provide some clues. Researchers (Sandra Chapman, University
of Warwick, Sandra.Chapman@astro.warwick.ac.uk
, 011-44-2476-523390) simulate avalanches in a sandpile by devising
a computer model for redistributing sand and observing the ensuing avalanches.
The occurrence of avalanches at all size scales is a hallmark of self-organized
criticality (SOC). Since the mid-1990s, a sizeable body of research
has found evidence of SOC in tokamak plasmas, where particles and energy
are rapidly redistributed, at all size scales, to other areas of the
plasma For some reason this "transport"seems to occur faster
than ordinary diffusion allows.
But there's a twist: SOC behavior, by itself, would tend to produce
a plasma with poor confinement of its particles. The new modeling suggests
that the desirable H-mode occurs when some, but not all, of the conditions
of SOC are met. The researchers have hopes that the H mode can be achieved
by manipulating the plasma so that the "fast transport" only
takes place at the short length scales. (Chapman,
Dendy, and Hnat, Physical Review Letters, 26 March 2001.)