Hostname: page-component-6766d58669-6mz5d Total loading time: 0 Render date: 2026-05-18T13:55:06.341Z Has data issue: false hasContentIssue false

Application of particle image velocimetry to dusty plasma systems

Published online by Cambridge University Press:  10 May 2016

Jeremiah D. Williams*
Affiliation:
Physics Department, Wittenberg University, Springfield, OH 45504, USA
*
Email address for correspondence: jwilliams@wittenberg.edu
Rights & Permissions [Opens in a new window]

Abstract

Particle image velocimetry is a fluid measurement technique that has been used for more than 20 years to characterize the particle transport and thermal state of dusty plasma systems. This manuscript provides an overview of this diagnostic technique, highlighting the strengths and limitations that are associated with its use. Additionally, the variations of this technique that have been applied in the study of dusty plasma systems will be discussed, along with a small selection of measurements that can be made with the technique. Potential future directions for this diagnostic tool within the dusty plasma community will also be discussed.

Information

Type
Research Article
Copyright
© Cambridge University Press 2016 
Figure 0

Figure 1. Images showing representative number densities that typically present when using the (a) PTV and (b) PIV techniques.

Figure 1

Figure 2. (a) Cartoon depicting the typical camera orientations that can be used when applying the PIV technique. In the study of dusty plasmas, cameras are typically positioned perpendicular, P, to the illuminated region of the dust cloud (green rectangle). The forward, F, and back, B, scattering positions are preferable when applying stereoscopic and tomographic PIV due to the higher scattering efficiencies. The orientation (left) and images (right) depicting the physical set-up of the (b) planar and (c) stereoscopic PIV systems at Auburn University and the (d) tomographic PIV system at Wittenberg University are seen to the right. (Photos in (b) and (c) courtesy of E. Thomas, Jr., Auburn University, AL.)

Figure 2

Figure 3. (a) Representative image of a dust cloud with a $32\times 32$ pixel grid superimposed. (b) Representative interrogation regions showing a small fraction of the dust grains visible from the blue box seen in (a) and separated in time by ${\rm\Delta}t_{PIV}=t_{2}-t_{1}$. (c) The correlation map that is constructed by performing the PIV analysis on the interrogation regions seen in (b). The resulting correlation map consists of three parts, the correlation between identical particles, $R_{D}$, the correlation between random particles, $R_{F}$, and the convolution of background image intensity, $R_{C}$. Here, the average displacement is represented by the peak denoted by $R_{D}$, while $R_{F}+R_{C}$ represents the noise in the measurement.

Figure 3

Figure 4. (a) Representative image showing a pair of rotating dust tori reported in Kaur et al. (2015b), along with the (b) velocity and (c) vorticity field found using the PIV technique. (Data courtesy of M. Kaur, Institute for Plasma Research.)

Figure 4

Figure 5. Image depicting the (a) dust cloud and (d) velocity in the vertical direction (i.e. the direction of gravity) for a cloud supporting the driven dust-acoustic wave. Profile of the wave structure from the (b) image and (c) velocity data along the line profile indicated by the dashed line in (a) and (d), respectively. It is observed that the velocity field found by applying the PIV technique is able to recover the wave structure and evidence of wave activity when it not visible in the image data, as indicated by the arrows in (c).

Figure 5

Figure 6. Space–time plot constructed from (a) intensity profiles and (c) velocity in the vertical direction (i.e. the direction of gravity) from the dashed line seen in figure 5(a) and figure 5(d), respectively. Here the observed bands represent the propagation of individual wave fronts. It is noted that the transition from regular spaced bands to less regular bands that is seen around $t\sim 2~\text{s}$ corresponds to the wave mode transitioning from the driven to the naturally occurring (undriven) wave mode. The dispersion relations that are found from the space–time plots seen in (a) and (c) are seen in (b) and (d), respectively. The dashed line that is superimposed onto these plots is there to guide the eye. It is observed that the same dispersion is seen in both the image and velocity data, though the higher frequency information is not contained in the velocity field.

Figure 6

Figure 7. Plot showing the volumetric structure of the wave fronts with superimposed isosurfaces showing the (a) $x$-, (b) $y$- and (c) $z$-component of the velocity field at three spatial locations representing the right ($x=3.5~\text{mm}$), centre $(x=5.5~\text{mm})$ and left ($x=7.5~\text{mm}$) sides of the wave front. The bands that are seen in the superimposed surfaces show that the oscillations associated with the wave mode are present in each vector direction. (d) Isosurfaces revealing the three-dimensional structure of a bifurcation in the wave front near $x=5~\text{mm}$ and $y=-2~\text{mm}$.

Figure 7

Figure 8. (a) Image of the dust cloud examined. Here, the upper region of the cloud was stable, while the dust acoustic wave is observed to propagate in the lower region of the cloud. Plots of the (b) thermal energy density and (c) thermal energy transport calculated from moments of the spatially resolved phase space distribution function throughout the measurement volume. The thermal energy density is larger in the vicinity of the wave mode and largest between wave fronts while the energy transport is correlated with the observed particle motion: particles in the wave fronts move toward the bottom of the page, while particles between the wave fronts move toward the top of the page. (Analysis courtesy of R. Fisher and E. Thomas, Jr., Auburn University, AL.)

Supplementary material: File

Williams supplementary material

Williams supplementary material

Download Williams supplementary material(File)
File 202.1 KB