The research group of NIFS together with collaborators in the United States applied the “heat pulse modulation method” in the magnetic island produced intentionally in the tokamak “Doublet III-D.” Temperature gradient inherent in the magnetically confined plasma causes turbulence while there is no turbulence in the magnetic island because of the absence of the gradient. That the turbulence propagates has now been demonstrated for the first time by investigating turbulence in the magnetic island.
In seeking to achieve fusion energy, research on magnetic field confinement of high-temperature plasma is being conducted around the world. In a high-temperature plasma there is a temperature gradient. When the temperature gradient becomes steep, turbulence is generated. Because the high-temperature regions and the low temperature areas are mixed due to the turbulence, the core temperature cannot be effectively raised. Thus, research on the generation and on the suppression of turbulence is being performed around the world on experimental devices of magnetically confined plasma (tokamaks and helical devices). In research to date, numerous turbulences have been observed. It was very difficult to distinguish whether that turbulence occurred at that place or whether it occurred at another place and propagated to that place. That the turbulence generated expands into other regions, that is, the phenomenon called “turbulence propagation” has been predicted theoretically, but has not been observed experimentally.
The research group of Professor Katsumi Ida and Professor Tatsuya Kobayashi of the National Institutes of Natural Sciences (NINS) National Institute for Fusion Science (NIFS) and United States collaborators conducted research on turbulence propagation in the Doublet III-D tokamak of General Atomics, in the United States. By applying “heat pulse modulation method” conceived in the Large Helical Device (LHD) at NIFS to measure turbulence in a special region, the “magnetic island,” where turbulence should not be generated because there is no temperature gradient in the magnetic island. They discovered that the turbulence exists in the magnetic island, and propagates faster toward the center of the magnetic island, which is called the O-point, than the modulated temperature change. Thus “turbulence propagation” was observed for the first time in the world.
This result is valuable because of the experimental demonstration of a new way of thinking regarding the suppression of turbulence using the idea of “propagation of turbulence.” And that an article has been published in the famous academic journal Physical Review Letters is evidence of the high level of world class research.
In the future we will continue to improve high-performance plasma through accumulating further knowledge on the suppression of turbulence.
Image 1: Propagation of turbulence inside the magnetic island
(left) There is no or small turbulence due to the almost zero temperature gradient inside the crescent-shaped magnetic island. (right) Turbulence propagates inside the magnetic island faster than the heat pulse.
Image 2: Idea of turbulence suppression
(top) Idea to date: To suppress the turbulence in a high-temperature plasma region it was thought that the turbulence should be suppressed in a large area.
(bottom) New idea: It is thought that the turbulence propagation is needed to suppress.
Movie : Propagation of heat pulse and turbulence
Heat pulse is generated approximately at the normalized minor radius x=0.0. Flat blue line means no temperature gradient inside the magnetic island (x=0.6～0.8). Turbulence (in red) propagates faster than the heat pulse.
When plasma is heated, while the temperature gradient increases, small eddies appear. Because this small eddy is of various sizes and it is aligned irregularly, this disturbed state is called turbulence. When turbulence occurs, the increase of the temperature gradient is suppressed.
In order to confine plasma, it is necessary to form a nested magnetic container. The form of the cross section of the container resembles concentric rings, such as tree rings. In this experiment, a small magnetic field from outside was purposely added to the intrinsic magnetic field for making magnetic field configuration with a crescent shape similar to a grain. This structure is called a magnetic island because it resembles an island in the middle of a river. Inside the magnetic island, the plasma has no temperature gradient and turbulence is not predicted to be generated forming a unique region.
Grant-in-Aid for Scientific Research of JSPS Japan (No. JP15H02336)
Formation of International Scientific Base and Network program of NIFS/NINS (KEIN1111, KEIN1113)
US Department of Energy program (DE-FC02-04ER54698, DE-FG03-97ER54415, and DE-AC05-00OR22725)
Dr. Katsumi Ida
National Institutes of Natural Sciences,
National Institute for Fusion Science, Japan