Changes in the mineralogy and chemistry of a lateritic soil due to a bushfire at Wundowie, Darling Range, Western Australia

Geoderma

Volumn 191, Issue , 2012, Pages 140-150

  Yusiharni, E ^a   Gilkes, R J ^a  

^a UNIVERSITY OF WESTERN AUSTRALIA   (Australia)

Author keywords

Ash; Dehydroxylation; Fire; Mineralogy; Soil heating

Indexed keywords

AMORPHOUS PHASE; ARID CONDITIONS; AUSTRALIA; BUSHFIRES; CHEMICAL BEHAVIOR; CRYSTALLINE COMPOUNDS; DEHYDROXYLATIONS; EUCALYPTUS MARGINATA; GIBBSITES; LATERITIC SOILS; METAKAOLINITE; NATIVE PLANTS; PLANT ASH; SOIL HEATING; SOIL MINERALS; SOIL SAMPLE; WESTERN AUSTRALIA; XRD PATTERNS;

AMORPHOUS SILICON; ASHES; CRYSTALLINE MATERIALS; CRYSTALLOGRAPHY; FIRES; HEATING; KAOLINITE; MINERALOGY; MINERALS; QUARTZ;

SOILS;

ARID REGION; ASH; CALCITE; CHEMICAL COMPOSITION; HEATING; LATERITE; MINERALOGY; NATIVE SPECIES; PH; SEASONALITY; SOIL ANALYSIS; SOIL CHEMISTRY; TRANSFORMATION; WILDFIRE;

AUSTRALIA; DARLING RANGE; WESTERN AUSTRALIA; WUNDOWIE;

EUCALYPTUS; EUCALYPTUS MARGINATA; XANTHORRHOEA;

EID: 84868362867     PISSN: 00167061     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.geoderma.2012.01.030     Document Type: Article

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