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Satellite Drag in the Re-entry Region Brian Argrow Dept. Aerospace Engineering Sciences University of Colorado NADIR MURI 21 October 2008.

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Presentation on theme: "Satellite Drag in the Re-entry Region Brian Argrow Dept. Aerospace Engineering Sciences University of Colorado NADIR MURI 21 October 2008."— Presentation transcript:

1 Satellite Drag in the Re-entry Region Brian Argrow Dept. Aerospace Engineering Sciences University of Colorado NADIR MURI 21 October 2008

2 Focus Area VIII: Satellite Drag in the Re-Entry Region Motivation Accurate knowledge of satellite C D is essential for accurate prediction of satellite drag, and for inferring densities from accelerometer measurements Insufficient knowledge exists about C D in the transition and slip-flow regimes (i.e., < 150 km) Objective: To significantly advance understanding of satellite drag in the transition and near-continuum regimes using state-of-the art numerical modeling, and to provide C D predictions under a broadened range of conditions Brian Argrow and Jeff Forbes (CU)

3 High-Altitude Simulations with the Direct Simulation Monte Carlo (DSMC) Method 130 km 100 km Methodology –Direct Simulation Monte Carlo (DSMC) with calibrated gas-surface interaction models –Bird’s DS3V –NASA DSMC Analysis Code (DAC) –Investigate gas surface interaction models and produce calibrated modules to couple with DSMC

4 0.010.1110100 Discrete Particle or Molecular Model Continuum Model Collisionless Boltzmann Equation Boltzmann Equation Euler Eqs. Navier-Stokes Equations 0 ∞ Conservation Equations Do Not Form A Closed Set Free-Molecule Limit Inviscid Limit Local Knudsen Number Flow Regimes and Governing Equations* *Bird, G., Molecular Gas Dynamics and the Direct Simulation of Gas Flows Why DSMC? Local Kn often violates the global free-molecular flow assumption

5 Milestones and Deliverables YrMilestonesDeliverables 1DAC-based simulations of simple 3-D geometries with candidate GSI models. DSMC/GSI with atmosphere model 2Down-select/calibrate GSI models w/ satellite data DSMC/GSI w/ calibrated GSI options 3DSMC computation of transition-regime aerodynamic coefficients Code to compute C D in slip/ transition flows for range of geometries 4Create database of altitude-dependent C D for representative satellites in transition flow. Integrated simulation environment code to produce C D database 5Complete DSMC/GSI code for trajectory simulations w/ direct modeling of flow environment Integrated simulation environment code to simulate real-time application

6 DS3V Example: 1-m, 75  Delta Wing

7 Input: 75  Delta Wing,  = 2  L = 1 m V  = 7.6 km/s H = 120 km Non-reacting Air (20% O 2, 80% N 2 ) T  = 360 K Kn  = 3.3 Fully diffuse reflection T surf = 300 K Output: Total Force F x = 1.2 N F y = -1.5 × 10 -3 N F z = -9.1 × 10 -5 N Pressure F x = 1.4 × 10 -4 N F y = 2.0 × 10 -3 N F z = -5.1 × 10 -4 N Shear F x = 1.2 N F y = -4.6 × 10 -4 N F z = 4.2 × 10 -4 N

8 DSMC Example: 2-m Sphere

9 Input: L = 2 m V  = 7.6 km/s H = 120 km Non-reacting Air (20% O 2, 80% N 2 ) T  = 360 K Kn  = 1.7 Fully diffuse reflection T surf = 300 K Output: Total Force F x = 4.2 N F y = -6 × 10 -3 N F z = -1 × 10 -3 N Pressure F x = 2.3 N F y = -6 × 10 -4 N F z = -1 × 10 -3 N Shear F x = 1.9 N F y = -1 × 10 -4 N F z = 1 × 10 -3 N

10 Current Status Year 1 Summary –Hywapyong Ko, PhD candidate (started Aug 08) –Simulations of simple geometries with DS3V –Paperwork completed for DAC97 (July 08) –Dedicated 8-processor workstation Year 2 Focus –Development of DAC + gas/surface modeling –New course on Molecular Gas Dynamics (Sp 09)


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