Investigation by Particle Image Velocimetry Measurements of Oblique Shock Reflection with Separation

By P. Dupont, S. Piponniau, A. Sidorenko, J. Debiève. 2008

138 citations recorded by the source corpus.

Subfields: Computational Mechanics, Ocean Engineering

View Paper: https://www.semanticscholar.org/paper/f26ec953d64f465853ebca716898259a1b8bec24

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In Computational Mechanics

In Ocean Engineering

Citations in the corpus

Low-frequency dynamics in a shock-induced separated flow (2016, background): “Due to the inflection point in the velocity profiles, the shear layer is unstable and large-scale vortical structures are formed, which have been observed in a number of STBLI studies (e.g. Dupont et al. 2008; Humble et al. 2009; Agostini et al. 2012).”
A scaling analysis for turbulent shock-wave/boundary-layer interactions (2013, background): “…four cases, the turbulent fields exhibit a resemblance: a highly turbulent region develops downstream of the foot of the reflected shock, related to the formation of large coherent scales in the mixing layer which develops downstream of this point (Dupont et al. 2006, 2008; Souverein et al. 2009).”
Large-eddy simulation of low-frequency unsteadiness in a turbulent shock-induced separation bubble (2009, methodology): “Then, we compare the obtained LES flow statistics against the available PIV data [12].”
Low-frequency unsteadiness in shock wave–turbulent boundary layer interaction (2012, background): “These observations about the shear layer profiles in a compression ramp flow agree with previous experimental observations for the reflected shock configuration (Dupont et al. 2008; Souverein et al. 2010), where it has also been shown that the shear layer profiles resemble those of a mixing layer.”
Numerical Methods for High-Speed Flows (2011, methodology): “Sample results of the calculations of Touber & Sandham (2009) are reported in Figure 5, showing a comparison between the mean LES field (in terms of streamwise velocity and turbulent shear stress), and reference experimental data (Dupont et al., 2008).”