Abstract To search for a possible atmosphere on Pluto and Triton, spectra of these objects as well as comparison stars were obtained with a three-stage Varo image tube for the spectral region from 6800 to 9000 A. Ratio spectra indicate an absorption feature near 8900 A, although the steeply diminishing response of the image tube at that wavelength casts some doubt on the reality of this feature. The feature appears more definitive in the spectrum of Pluto and less certain in the spectrum of Triton. The absorption was analyzed using our recently determined band-model parameters for methane. Under the assumption of a pressure higher than 0.01 atm an abundance of 3 m-amagat was determined. For pressures limited by the methane abundance itself, an abundance of 50 m-amagat and a pressure of 10 −3 atm was derived (using g = 0.20 g ⊕ for both Pluto and Triton). This pressure is close to the pressure that can be expected from the equilibrium vapor pressure of a methane frost. If the absorption at 8900 A is spurious, our analysis will be applicable as an upper limit for the presence of methane gas on Pluto or Triton.
[1]
D. Morrison,et al.
Pluto: Evidence for Methane Frost
,
1976
.
[2]
JOHN S. Lewis.
Satellites of the Outer Planets: Their Physical and Chemical Nature
,
1971
.
[3]
G. Kuiper.
The atmospheres of the earth and planets.
,
1952
.
[4]
Gerard P. Kuiper,et al.
Titan: a Satellite with an Atmosphere.
,
1944
.
[5]
Uwe Fink,et al.
Photoelectric absorption spectra of methane /CH4/, methane and hydrogen /H2/ mixtures, and ethane /C2H6/
,
1977
.
[6]
T. Martin.
Saturn and Jupiter : a study of atmospheric constituents
,
1975
.
[7]
H. Spinrad.
LACK OF A NOTICEABLE METHANE ATMOSPHERE ON TRITON
,
1969
.
[8]
M. H. Hart.
A possible atmosphere for Pluto
,
1974
.
[9]
U. Fink,et al.
Band model analysis of laboratory methane absorption spectra from 4500 to 10500 A
,
1977
.
[10]
J. S. Neff,et al.
A MEASUREMENT OF THE RELATIVE REFLECTANCE OF PLUTO AT 0.86 MICRON.
,
1976
.