Rc. Blanchard et al., SHUTTLE UPPER-ATMOSPHERE MASS-SPECTROMETER EXPERIMENTAL FLIGHT RESULTS, Journal of spacecraft and rockets, 31(4), 1994, pp. 562-568
Calibrated pressure measurements for species with mass-to-charge ratio
s up to 50 amu/e- were obtained from the shuttle upper atmosphere mass
spectrometer experiment during re-entry on the STS-35 mission. The pr
incipal experimental objective is to obtain measurements of freestream
density in the hypersonic rarefield flow flight regime. Data were col
lected from 180 to about 87 km. However, data above 115 km were contam
inated from a source of gas emanating from pressure transducers connec
ted in parallel to the mass spectrometer. At lower altitudes, the pres
sure transducer data are compared to the mass spectrometer total press
ure with excellent agreement. Near the orifice entrance, a significant
amount of CO2 was generated from chemical reactions. The freestream d
ensity in the rarefield flow flight regime is calculated using an orif
ice pressure coefficient model based upon direct simulation Monte Carl
o results. This density, when compared with the 1976 U.S. Standard Atm
osphere model, exhibits the wavelike nature seen on previous flights u
sing accelerometry. Selected spectra are presented at higher altitudes
(320 km) showing the effects of the ingestion of gases from a forward
fuselage fuel dump.