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Universality of Poisson-driven plasma fluctuations in the Alcator C-Mod scrape-off layer

Permanent link
https://hdl.handle.net/10037/14607
DOI
https://doi.org/10.1063/1.5064744
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Date
2018-12-18
Type
Journal article
Tidsskriftartikkel
Peer reviewed

Author
Theodorsen, Audun; Garcia, Odd Erik; Kube, Ralph; LaBombard, Brian; Terry, James L.
Abstract
Large-amplitude, intermittent fluctuations are ubiquitous in the boundary region of magnetically confined plasmas and lead to detrimental plasma-wall interactions in the nextgeneration, high duty cycle fusion power experiments. Using gas puff imaging data time series from the scrape-off layer in the Alcator C-Mod device, it is here demonstrated that the large-amplitude fluctuations can be described as a super-position of pulses with fixed shape and constant duration. By applying a new deconvolution algorithm on the data time series with a two-sided exponential pulse function, the arrival times and amplitudes of the pulses can be estimated and the measurement time series can be reconstructed with high accuracy. The pulse amplitudes are shown to follow an exponential distribution. The waiting times between pulses are uncorrelated, their distribution has an exponential tail, and the number of arrivals is a linear function of time. This demonstrates that pulse arrivals follow a homogeneous Poisson process. Identical statistical properties apply to both ohmic and high confinement mode plasmas, clearly demonstrating universality of the fluctuation statistics in the boundary region of Alcator C-Mod.
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This article may be downloaded for personal use only. Any other use requires prior permission of the author and AIP Publishing. This article appeared in (citation of published article) and may be found at http://doi.org/10.1063/1.5064744.
Publisher
AIP Publishing
Citation
Theodorsen, A., Garcia, O. E., Kube, R., LaBombard, B. & Terry, J. L. (2018). Universality of Poisson-driven plasma fluctuations in the Alcator C-Mod scrape-off layer. Physics of Plasmas, 25, 122309. http://doi.org/10.1063/1.5064744
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