Natural SciencesAerospace EngineeringMechanical EngineeringComputational Fluid DynamicsFluid DynamicsHeat TransferConvection DynamicsEntrainment ProcessesHeat FlowPlanetary Boundary LayerChemical NonequilibriumEntryEnvironmental SurveyMars Atmospheric EntryMars EntryPhysical ModelsStagnation PointsStagnation-point Heating
Computational fluid dynamics models for the thermodynamics and transport properties used in an equilibrium version of the Langley Aerothermodynamics Upwind Relaxation Algorithm (LAURA) for Martian Atmospheric entries are described. In addition, the physical models used in a nonequilibrium version of LAURA for Martian-entry flows are described. Uncertainties exist in defining constants used in the transport properties for the equilibrium model and in many of the physical models for the nonequilibrium version. Solutions from the two codes using the best available constants are examined at the Martian-entry conditions characteristic of the Mars Environmental Survey (MESUR) mission. While the flowfields are near thermal equilibrium, chemical nonequilibrium effects are present in the entry cases examined. Convective heating at the stagnation point for these flows (assuming fully catalytic wall boundary conditions) is approximately 100 W/sq cm. Radiative heating is negligible.
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A Viscosity Equation for Gas Mixtures
C. R. Wilke · The Journal of Chemical Physics · 1950 · 2.6K citations
Natural Sciences, Chemistry, Physics +14
60. Approximate formula for the thermal conductivity of gas mixtures.
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