Use and limitations of second-derivative diffuse reflectance spectroscopy in the visible to near-infrared range to identify and quantify Fe oxide minerals in soils

Clays and Clay Minerals

Volumn 46, Issue 5, 1998, Pages 528-536

  Scheinost, A C ^a,c   Chavernas, A ^b   Barron V ^b   Torrent, J ^b  

^a PURDUE UNIVERSITY   (United States)

^b UNIVERSITY OF CÓRDOBA   (Spain)

^c UNIVERSITY OF DELAWARE   (United States)

Author keywords

Crystal field bands; Diffuse reflectance spectroscopy; Goethite; Hematite; Intervalence charge transfer; Iron oxides; Magnetite

Indexed keywords

CHARGE TRANSFER; ELECTRON ENERGY LEVELS; ELECTRON TRANSITIONS; INFRARED SPECTROSCOPY; IRON OXIDES; MAGNETITE; SOILS; X RAY DIFFRACTION ANALYSIS;

CRYSTAL FILED BAND; DIFFUSE REFLECTANCE SPECTROSCOPY; GOETHITE; HEMATITE;

OXIDE MINERALS;

INFRARED SPECTROSCOPY; IRON OXIDE; REFLECTANCE; SOIL; SPECTROSCOPY;

EID: 0032194394     PISSN: 00098604     EISSN: None     Source Type: Journal    
DOI: 10.1346/CCMN.1998.0460506     Document Type: Article

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