Six phyllosilicates were progressively dehydrated under controlled conditions in an effort to study the spectral effects of their dehydration. The spectra obtained at each level of hydration provide information that may be used in future spectroscopic observations of the planets, as well as a data set which compliments the existing body of terrestrial soil knowledge.
Spectral effects of dehydration on phyllosilicates
1987-05-01
Miscellaneous
No indication
English
Phyllosilicates in Apollo 11 samples
NTRS | 1970
|NTRS | 1964
|Online Contents | 2008