Thermochemical relaxation behind a normal shock in Mars and Titan gas mixtures is simulated using a CFD solver, DPLR, for a hemisphere of 1 m radius; the thermochemical relaxation along the stagnation streamline is considered equivalent to the flow behind a normal shock. Flow simulations are performed for a Titan gas mixture (98% N2, 2% CH4 by volume) for shock speeds of 5.7 and 7.6 km/s and pressures ranging from 20 to 1000 Pa, and a Mars gas mixture (96% CO2, and 4% N2 by volume) for a shock speed of 8.6 km/s and freestream pressure of 13 Pa. For each case, the temperatures and number densities of chemical species obtained from the CFD flow predictions are used as an input to a line-by-line radiation code, NEQAIR. The NEQAIR code is then ...
This paper presents simulations of the radiative heat flux imparted on the after-body of vehicles en...
CO concentration and gas temperature distribution are diagnosed behind a strong shock wave simulatin...
When vehicles re-enter the Earth's atmosphere at hyper-velocity, gas radiative heat will increas...
This thesis investigates the modelling of radiating shock layers encountered during atmospheric entr...
An update to a collisional-radiative model developed by Magin1 for Huygens Titan atmospheric entry i...
A model for simulating nonequilibrium radiation from Mars entry shock layers is presented. A new che...
This paper reports on the measurement of radiative heating for shock heated flows which simulate con...
Detailed spectrally and spatially resolved radiance has been measured in the Electric Arc Shock Tube...
This paper details the experimental work conducted at the University of Queensland to measure the no...
The X2 facility at the University of Queensland was modified to allow experimentation at low pressur...
Radiative heating computations are performed for a range of high speed Earth entry experiments condu...
For reentry operations into atmospheres such as Titan, accurate, reliable radiation data is essentia...
A computational platform was developed to study radiation of high-temperature gases during atmospher...
International audienceNonequilibrium infrared emission spectra representative of a Mars atmospheric ...
This work represents ongoing efforts to study high-enthalpy carbon dioxide flows in anticipation of ...
This paper presents simulations of the radiative heat flux imparted on the after-body of vehicles en...
CO concentration and gas temperature distribution are diagnosed behind a strong shock wave simulatin...
When vehicles re-enter the Earth's atmosphere at hyper-velocity, gas radiative heat will increas...
This thesis investigates the modelling of radiating shock layers encountered during atmospheric entr...
An update to a collisional-radiative model developed by Magin1 for Huygens Titan atmospheric entry i...
A model for simulating nonequilibrium radiation from Mars entry shock layers is presented. A new che...
This paper reports on the measurement of radiative heating for shock heated flows which simulate con...
Detailed spectrally and spatially resolved radiance has been measured in the Electric Arc Shock Tube...
This paper details the experimental work conducted at the University of Queensland to measure the no...
The X2 facility at the University of Queensland was modified to allow experimentation at low pressur...
Radiative heating computations are performed for a range of high speed Earth entry experiments condu...
For reentry operations into atmospheres such as Titan, accurate, reliable radiation data is essentia...
A computational platform was developed to study radiation of high-temperature gases during atmospher...
International audienceNonequilibrium infrared emission spectra representative of a Mars atmospheric ...
This work represents ongoing efforts to study high-enthalpy carbon dioxide flows in anticipation of ...
This paper presents simulations of the radiative heat flux imparted on the after-body of vehicles en...
CO concentration and gas temperature distribution are diagnosed behind a strong shock wave simulatin...
When vehicles re-enter the Earth's atmosphere at hyper-velocity, gas radiative heat will increas...