LRO Diviner Soil Composition Measurements - Lunar Sample Ground TruthThe Diviner Lunar Radiometer Experiment on the Lunar Reconnaissance Orbiter [1,2] includes three thermal infrared channels spanning the wavelength ranges 7.55-8.05 microns 8.10-8.40 microns, and 8.38-8.68 microns. These "8 micron" bands were specifically selected to measure the "Christiansen feature". The wavelength location of this feature, referred to herein as CF, is particularly sensitive to silicate minerals including plagioclase, pyroxene, and olivine the major crystalline components of lunar rocks and soil. The general trend is that lower CF values are correlated with higher silica content and higher CF values are correlated with lower silica content. In a companion abstract, Greenhagen et al. [3] discuss the details of lunar mineral identification using Diviner data.
Document ID
20100009427
Acquisition Source
Johnson Space Center
Document Type
Extended Abstract
Authors
Allen, Carlton C. (NASA Johnson Space Center Houston, TX, United States)
Greenhagen, Benjamin T. (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Paige, David A. (California Univ. Los Angeles, CA, United States)
Date Acquired
August 25, 2013
Publication Date
March 1, 2010
Subject Category
Lunar And Planetary Science And Exploration
Report/Patent Number
JSC-CN-19976Report Number: JSC-CN-19976
Meeting Information
Meeting: 41st Lunar and Planetary Science Conference
Location: The Woodlands, TX
Country: United States
Start Date: March 1, 2010
End Date: March 5, 2010
Sponsors: NASA Johnson Space Center, Lunar and Planetary Inst.