Can electron energy-loss spectroscopy (EELS) be used to quantify hydrogen in minerals from the O K edge?

American Mineralogist

Volumn 95, Issue 1, 2010, Pages 92-97

  Garvie, Laurence A J ^a  

^a ARIZONA STATE UNIVERSITY   (United States)

Author keywords

Beam damage; EELS; Hydrogen; TEM

Indexed keywords

DISSOCIATION; ELECTRON BEAMS; ELECTRON EMISSION; ELECTRON ENERGY LEVELS; ELECTRON IRRADIATION; ELECTRON SCATTERING; ELECTRONS; ENERGY DISSIPATION; HYDROGEN; MINERALS; TRANSMISSION ELECTRON MICROSCOPY;

ANHYDROUS MINERALS; BEAM DAMAGE; ELECTRON BEAM DAMAGE; FLUENCE RATES; FLUENCES; O K-EDGES; PRE-PEAK; RADIATION-INDUCED;

ELECTRON ENERGY LOSS SPECTROSCOPY;

CONCENTRATION (COMPOSITION); CRYSTAL CHEMISTRY; CRYSTAL STRUCTURE; ELECTRON SPIN RESONANCE; HYDROGEN; IRRADIATION; QUANTITATIVE ANALYSIS; TRANSMISSION ELECTRON MICROSCOPY;

EID: 77249092743     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am.2010.3290     Document Type: Article

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