T Thirty M Meter Telescope T Wind Tunnel Testing of a Generic Telescope Enclosure Tait S. Pottebaum Douglas G. MacMynowski* California Institute of Technology June 2004 *formerly D. MacMartin macmardg@cds.caltech.edu Experiment • Model: – Empty telescope enclosure – Square opening • size appropriate for roughly f/1.3 – 30° Zenith angle (fixed) – Diameter = 0.83m, ~1% scale • Turbulent flow at M2 location • Probably not turbulent at M1 location • Data: – Flow visualization – Digital particle image velocimetry (DPIV) data in a vertical plane containing the telescope axis near the dome opening – Hot-wire anemometer data along the axis of the telescope T Thirty Meter Telescope M T Scaling Dimensionless parameters Re UL Re exp 106 Re fs (12 ms 1 )( 32m) 34 1 Re exp (35ms )( 0.32m) where L is the side length of the opening Convective frequency scaling U f0 L f 0,exp, 35ms 1 109s1 f 0,fs ,12ms 1 0.37s1 Helmholtz frequency scaling T c L fH 2 V Thirty Meter where Telescope M T fH,exp 62s 1 fH,f s 0.57s 1 V is the enclosed volume and c is the speed of sound Experimental Setup • • • • • Clear Lucite dome with opening Camera and mirror for visualization & DPIV Hotwire mounted on traverse Mirror and optics for laser sheet Lucas adaptive wall wind tunnel – 5’ by 6’ un-adapted • Mounted on turn-table T Thirty Meter Telescope M T Large scale flow, 0° and 180 ° T Thirty Meter Telescope M T Smoke Visualization • 0° azimuth • Smoke injected from outside the dome T Thirty Meter Telescope M T U∞ Velocity (hot-wire) spectrum inside enclosure data at 0°, r/R = 0.934 Dominant 1st peak Large 2nd peak -5/3 slope 35m/s 20m/s fH T Thirty Meter Telescope M T Shear layer modes: • Frequency: f ~ 0.65nU/L • Present for AZ ≤ 90° • Mode n depends on speed; influenced by Helmholtz mode fH DPIV data • Focus on area near the opening • Principle of measurements – – – – – Seed flow with tracer particles (water droplets) Illuminate a thin sheet with a laser (vertical plane on centerline of dome) Synchronize laser with the camera Record images in pairs with small time separation Correlate small regions of image to determine displacement • Weaknesses x u t – In regions of steep gradients, velocity is typically underestimated – Scales smaller than the interrogation regions cannot be resolved – Only the in-plane components of velocity are measured • Obtain mean and statistics from large number of image pairs – 2400 pairs for 0° – 4495 pairs for 180° T Thirty Meter Telescope M T Sample data image: 1st snapshot T Thirty Meter Telescope M T Sample data image: 2nd snapshot T Thirty Meter Telescope M T Mean in-plane velocity, 0° T Thirty Meter Telescope M T u Uinf In-plane rms fluctuation, 0° u 2 T Thirty Meter Telescope M T v2 1/2 Uinf Mean in-plane velocity, 180° T Thirty Meter Telescope M T u Uinf In-plane rms fluctuation, 180° u 2 T Thirty Meter Telescope M T v2 1/2 Uinf Profiles on telescope axis T Thirty Meter Telescope M T Conclusions • Upwind viewing – Shear layer across enclosure opening periodically rolls up into large vortices • Frequencies are well described by convection velocity of shear layers and a mode number • Mode selection may be influenced by coupling of the shear layer instability with Helmholtz oscillations – Large fluctuation velocities are likely to exert significant unsteady forces on the secondary mirror and support structure • Downwind viewing – Opening is inside the wake recirculation – Mean velocity local maximum exists inside the dome – Fluctuation levels are low, so most forces are likely to be steady T Thirty Meter Telescope M T Further analysis • Data being used for comparison with CFD (Konstantinos Vogiatzis, AURA NIO) • Additional testing done with venting; data analysis in progress. – Significant attenuation of shear layer modes T Thirty Meter Telescope M T