4 research outputs found

    Phase contrast imaging measurements and modeling of short wavelength turbulence in the DIII-D tokamak

    Get PDF
    Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Physics, 2010.This electronic version was submitted by the student author. The certified thesis is available in the Institute Archives and Special Collections.Cataloged from student submitted PDF version of thesis.Includes bibliographical references (p. 203-212).The DIII-D phase contrast imaging (PCI) diagnostic has been upgraded and used to measure turbulence in the outer plasma region (0.7 < r/a < 1). These upgrades extended its operational range to high frequencies (10 kHz - 10 MHz), short wavelength (2 - 30 cm-1), and improved the signal-to-noise ratio by 10X, as well as provided a novel rotating mask to measure turbulence as a function of propagation angle about the PCI chord. Turbulent fluctuations that propagate perpendicular to the magnetic field direction can be localized by making use of the variation of the magnetic field component perpendicular to the viewing chord as a function of chord height. Long wavelength (IkI . 12 cm-1) turbulence is shown to be a branch in frequency and wave-number space, and is localized to within the instrumental width of the last closed flux surface (LCFS) (r/a & 0.9). Three classes of turbulence with finite (and theoretically unexpected) kII have been identified: (i) modes that are localized in wave-number and mask angle (the high-k and medium-k modes), (ii) a broad (in mask angle) background turbulence, and (iii) a low-k "wing" that smears the main branch structure. These modes are seen to propagate at angles as large as kII/k ~ 0.1 - 0.4. ECH heating is observed to increase the spectral power density in the high-k mode (-24 < k < -18 cm-1), and the parallel wave-numbers are measured to be as large as kII/k ~ 0.15. The applied heating is shown to increase the electron temperature gradient drive (inverse scale-length, 1/LTe) and decrease the ion temperature and density gradient drives (1/LTi and 1/Ln). Using a basic temperature gradient driven drift-wave model in slab geometry, it is shown that finite (and relatively high) kII modes could interact resonantly with ions through the ion cyclotron Doppler resonance terms [xi]±1i = (w± [omega]i)/(kIIvti) ~ 1. These m = / \ 0 terms in the dispersion relation are not included in the derivation of the gyrokinetic equations.by James Robert Dorris III.Ph.D

    Phase Contrast Imaging Measurements and Modeling of Short Wavelength Turbulence in the DIII–D Tokamak

    Get PDF

    On Two-Dimensional Maximum Entropy Spectral Estimation

    Get PDF
    A novel method of two-dimensional (2-D) spectral estimation, which we introduced recently using the Radon transform and a one dimensional (1-D) autoregressive model, led us to investigate the maximization of entropy subject to the correlation matching constraints in the Radon space. Instead of solving the 2-D maximum entropy spectral estimation problem, we convert it into a problem which is easier to solve. It is shown that a radial slice of the 2-D ME spectrum can be obtained by 1-D AR modeling of the projections (Radon transform) of a stationary random field (SRF). The advantages and limitations of using this new duality relation to estimate the complete 2-D ME spectra on a polar raster are discussed

    On Two-Dimensional Maximum Entropy Spectral Estimation

    No full text
    A novel method of two-dimensional (2-D) spectral estimation, which we introduced recently using the Radon transform and a one dimensional (1-D) autoregressive model, led us to investigate the maximization of entropy subject to the correlation matching constraints in the Radon space. Instead of solving the 2-D maximum entropy spectral estimation problem, we convert it into a problem which is easier to solve. It is shown that a radial slice of the 2-D ME spectrum can be obtained by 1-D AR modeling of the projections (Radon transform) of a stationary random field (SRF). The advantages and limitations of using this new duality relation to estimate the complete 2-D ME spectra on a polar raster are discussed
    corecore