Cover Page/Proposal Summary
ROSS-99 NRA 99-OSS-01
Date Due: 5/3/99
This proposal shall be used and disclosed for evaluation purposes only, and a copy of this Government notice shall be applied to any reproduction or abstract thereof. Any authorized restrictive notices that the submitter places on this proposal shall also be strictly complied with. Disclosure of this proposal for any reason outside the Government evaluation purposes shall be made only to the extent authorized by the Government. |
Proposal Type: New Proposal |
Proposal Category: Laboratory |
Major Equipment Proposal? No |
Do you intend to submit an Education/Public Outreach (E/PO) proposal? No |
Proposal Title: |
The Temperature Dependence of Energy Transfer in Planetary Molecules |
Abbreviated Proposal Title: |
Temperature-Dependent Molecular Energy Transfer |
Principal Investigator: |
Dr. John Allen
Jr. Laboratory for Extraterrestrial Physics CODE 691 NASA's Goddard Space Flight Center Greenbelt, MD 20771-0001 Phone: 301-286-5896 Fax: 301-286-0212 E-mail: john.e.allen@gsfc.nasa gov |
Signature | Date |
_____________________________________ | ____________ |
Co-Investigators and Collaborators: | |||
Type | Name | Affiliation | |
Sci Co-I | Dr. Benjamin Patrick Michael | NRC-GSFC | patrick.mic hael@gsfc.nasa.gov |
Sci Co-I | Dr. John W. Keller | GSFC | john.w.keller@gs fc.nasa.gov |
Proposal Summary:
Interpretation of planetary observations and modeling of planetary atmospheres are dependent on accurate laboratory data for the properties and processes of various atmospheric constituents. It is important that these data be taken over the appropriate range of parameters, e.g., temperature and composition; however, temperature-dependent laboratory data for most properties or processes of relevant species are particularly meager. This proposal addresses the needs of the planetary atmospheres community for temperature-dependent molecular relaxation rates which serve as input for thermal-structure models of planetary atmospheres. In the absence of low-temperature measurements, modelers must extrapolate high-temperature data to the temperatures of interest. These extrapolations can cover large temperature ranges, thus introducing significant errors in the models. We propose to measure relaxation rates for several light hydrocarbons at temperatures appropriate for the outer planets and their satellites (90 to 300 K). Temperature-dependent vibrational-to-translational relaxation of methane by helium, argon, normal and ortho/para hydrogen, and nitrogen will be determined using a photoacoustic apparatus specifically constructed for these experiements, and similar data will then be acquired for acetylene. A pump-probe technique will be implemented to measure vibrational-to-translational rates for larger hydrocarbons as well as vibrational-to-vibrational or vibrational-to-rotational transfer rates for both small and large hydrocarbons. Results from these experiments will be of immediate use in atmospheric models constructed to guide the engineering development of, planning for, and interpretation of data from a variety of planetary missions: the Kuiper/Pluto Express, Cassini/Huygens, and the Galileo Orbiter/Probe.