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Published on: July 1, 2019
ICE CHEMISTRY ON OUTER SOLAR SYSTEM BODIES: ELECTRON RADIOLYSIS OF N2-, CH4-, AND CO-CONTAINING ICES
Christopher K Materese1,2, Dale P Cruikshank1, Scott A Sandford1
1NASA Ames Research Center, MS 245-6, Moffett Field, CA 94035-1000, USA.
Radiation processing of simple ices on outer Solar System bodies creates complex organic molecules. These nitrogen-rich refractory materials, including urea and carboxylic acids, are key to understanding prebiotic chemistry on icy worlds.
Area of Science:
- Astrochemistry
- Planetary Science
- Organic Chemistry
Background:
- Surface ices on outer Solar System bodies are processed by radiation.
- This radiation processing is hypothesized to create complex organic molecules.
- These molecules may contribute to the observed colors of icy bodies.
Purpose of the Study:
- To analyze refractory materials produced from electron irradiation of simple ices.
- To simulate cosmic ray bombardment effects on Pluto's surface ices.
- To identify the composition and chemical nature of radiation-produced organics.
Main Methods:
- Electron bombardment of low-temperature N2-, CH4-, and CO-containing ices.
- Analysis of refractory materials using Fourier-transform infrared spectroscopy (FTIR).
- X-ray absorption near-edge structure (XANES) spectroscopy and gas chromatography-mass spectrometry (GC-MS).
Main Results:
- Electron irradiation of simple ices produced complex oxygen- and nitrogen-bearing organic molecules.
- FTIR and XANES indicated the presence of alcohols, carboxylic acids, amines, amides, urea, and nitriles.
- XANES analysis revealed highly nitrogen-rich residues (N/C ~ 0.9).
Conclusions:
- Radiation processing of simple ices can generate complex organic molecules relevant to astrobiology.
- The identified molecules, including urea and carboxylic acids, are significant for prebiotic chemistry.
- This study provides insights into the chemical evolution of icy bodies in the outer Solar System.
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