Is iron redox cycling in a high altitude watershed photochemically or thermally driven?

Chemical Geology

Volumn 269, Issue 1-2, 2010, Pages 33-39

  Borman, Christopher J ^a   Sullivan, B Patrick ^a   Eggleston, Carrick M ^a   Colberg, Patricia J S ^a  

^a UNIVERSITY OF WYOMING   (United States)

Author keywords

Aqueous iron; Dissolved organic matter; DOM; Ferric DOM complexes; Humics; Photochemical iron reduction

Indexed keywords

AQUEOUS IRON; DISSOLVED ORGANIC MATTERS; DOM; FERRIC-DOM COMPLEXES; HUMICS; PHOTOCHEMICAL IRON REDUCTION;

CHARGE TRANSFER; EXPERIMENTS; IRON; OXIDATION; PHOTOOXIDATION; RATE CONSTANTS; SURFACE WATERS; WATERSHEDS;

IRON COMPOUNDS;

CONCENTRATION (COMPOSITION); DISSOLUTION; EXPERIMENTAL STUDY; HYDROCHEMISTRY; IRON; PH; PHOTOCHEMISTRY; REACTION KINETICS; REACTION RATE; REDOX CONDITIONS; WATERSHED;

EID: 79952901976     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2009.07.011     Document Type: Article

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