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Fiery sighting: A new physics of eruptions that damage fusion experiments

Sudden bursts of heat that can damage the inner walls of tokamak fusion experiments are a hurdle that operators of the facilities must overcome. Such bursts, called “edge localized modes (ELMs),” occur in doughnut-shaped tokamak devices that house the hot, charged plasma that is used to replicate on Earth the power that drives the sun and other stars. Now researchers at the U.S. Department of Energy’s (DOE) Princeton Plasma Physics Laboratory (PPPL) have directly observed a possible and previously unknown process that can trigger damaging ELMs.

Working together, physicists Ahmed Diallo, an experimentalist, and Julien Dominski, a theorist, pieced together data from the DIII-D National Fusion Facility that General Atomics operates for the DOE in San Diego, to uncover a trigger for a particular type of ELM that does not fit into present models of ELM plasma destabilization. Their findings could shed light on the variety of mechanisms leading to the onset of ELMs and could broaden the portfolio of ELM suppression tools. Understanding ELM physics is crucial to developing fusion facilities that can fuse light elements in the form of plasma — the state of matter composed of free electrons and atomic nuclei — to produce a virtually inexhaustible supply of energy to generate electricity.

Puzzling data

The new observations, reported in Physical Review Letters, began as an effort to unravel puzzling data detected by probes of magnetic field and plasma density fluctuations during DIII-D experiments. The data showed the eruption of ELMs following periods of unusual quiescence. “These were special cases that didn’t follow a standard model,” said Diallo. “We started digging into this together,” Dominski said. “It was a most interesting collaboration.”

In roughly six months of joint research, the physicists uncovered previously unseen correlations of fluctuations in the DIII-D experiments. These correlations revealed the formation of two modes — or waves — at the edge of the plasma that coupled together to generate a third mode. The newcomer then moved toward the wall of the tokamak — created a radial distortion in technical terms — that triggered bursts of low-frequency ELMs.

The ELMs were a type also seen on the Joint European Torus (JET) in the United Kingdom, the ASDEX Upgrade in Germany and other fusion devices following periods of quiescence. In principle, the results could also apply to systems such as solar flares and geomagnetic storms that are suddenly unleashed, according to the paper.

Opening a door

While the findings open a door on a method for triggering ELMs, they do not fully explain the process. The two physicists thus seek to analyze more data sets. “If we can fully understand how the triggering works we can block and reverse it,” Diallo said.

Joining the PPPL researchers on the paper, for which Diallo and Dominski were first and second authors, were physicists from the University of California, Los Angeles (UCLA) and the University of Wisconsin-Madison. Support for this research comes from the DOE Office of Science. The DIII-D tokamak is an Office of Science user facility operated by General Atomics in San Diego for the U.S. Department of Energy as a collaboration between leading U.S. national laboratories, universities and private industry. For more information see: http://www.ga.com/diii-d.

PPPL, on Princeton University's Forrestal Campus in Plainsboro, N.J., is devoted to creating new knowledge about the physics of plasmas — ultra-hot, charged gases — and to developing practical solutions for the creation of fusion energy. The Laboratory is managed by the University for the U.S. Department of Energy’s Office of Science, which is the largest single supporter of basic research in the physical sciences in the United States, and is working to address some of the most pressing challenges of our time. For more information, please visit science.energy.gov.

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Princeton Plasma Physics Laboratory is a U.S. Department of Energy national laboratory managed by Princeton University.

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