Detection of oblique shocks in a conical nozzle with a circular-arc throat.
Oblique shock detection in conical nozzle with circular arc throat, noting measurement techniques
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Oblique shock detection in conical nozzle with circular arc throat, noting measurement techniques
In the standard IAU theory for the orientation of the Earth's equator, the secular obliquity rate arises solely from the motiion of the ecliptic, not from the motion of the equator in space.
A test was conducted in the 15 cm x 15 cm supersonic wind tunnel at NASA Glenn Research Center that focused on corner effects of an oblique shock-wave/boundary-layer interaction. In an attempt to control the interaction in the corner region, eight corner fillet configurations were tested. Three parameters were considered for the fillet configurations: the radius, the fillet length, and the taper length from the square corner to the fillet radius. Fillets effectively reduced the boundary-layer thickness in the corner; however, there was an associated penalty in the form of increased boundary-layer thickness at the tunnel centerline. Larger fillet radii caused greater reductions in boundary-layer thickness along the corner bisector. To a lesser, but measureable, extent, shorter fillet lengths resulted in thinner corner boundary layers. Overall, of the configurations tested, the largest radius resulted in the best combination of control in the corner, evidenced by a reduction in boundary-layer thickness, coupled with minimal impacts at the tunnel centerline.
We report Mars Atmosphere and Volatile EvolutioN (MAVEN) mission observations of a large amplitude low-frequency plasma wave that propagated oblique to the ambient magnetic field upstream of Mars along with a non-solar-wind plasma component that had a flow velocity perpendicular to the magnetic field. We consider nine possibilities for this wave that include various combinations of its propagation direction, polarization in the solar wind frame, and ion source responsible for its generation. Using the observed wave parameters and the measured plasma parameters as constraints, we uniquely identify the wave by systematically discarding these possibilities. We determine that the wave is a right-hand polarized wave that propagated upstream in the solar wind frame. We find two possibilities for the ion source that can be responsible for this wave generation. They are either newly born pickup protons or reflected solar wind protons from the bow shock.We determine that the observed non-solar-wind component is not responsible for the wave generation, and it is likely that the non-solar-wind component was merely perturbed by the passage of the wave.
Sputtering at oblique angles of ion incidence
Gyro disturbing wave interaction with obliquely incident wanted wave in nighttime lower E region
Electromagnetic scattering by obliquely oriented cylinders, noting extinction efficiency, propagation in cylindrical waveguides and polarization reversal
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One dimensional nonisentropic MHD flow of ideal inviscid conducting compressible fluid in oblique magnetic field
Acoustic waves propagation in oblique DC magnetic fields in material with closed Fermi surface, discussing ultrasonic attenuation in metals
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Analytical model for oblique shock wave interaction with turbulent boundary layer
Downstream flow field produced by interaction of plane sound waves or plane shear waves with oblique shock front
Ring and Maxwellian transverse velocity distributions for oblique wave propagation
Analytical solution for inviscid separated jet injection at oblique angle into moving stream
Injection of attached inviscid jet at oblique angle to moving stream
Interaction of plane p-polarized electromagnetic wave obliquely incident on hot plasma half space and plasma slab