Diel stream geochemistry, Taylor Valley, Antarctica

Hydrological Processes

Volumn 27, Issue 3, 2013, Pages 394-404

  Fortner, Sarah K ^a,b   Lyons, W Berry ^a,b   Munk, Leeann ^c  

^a OHIO STATE UNIVERSITY   (United States)

^b OHIO STATE UNIVERSITY   (United States)

^c UNIVERSITY OF ALASKA ANCHORAGE   (United States)

Author keywords

Antarctica; Diel; Major ions; Streams; Trace elements

Indexed keywords

ANDERSONS; ANTARCTICA; DIEL; DYNAMIC NATURE; EOLIAN SEDIMENTS; FLOW VARIATIONS; GLACIAL MELTWATER; HYDROGRAPHS; MAJOR IONS; MAXIMUM FLOWS; MINIMUM FLOW; PROGLACIAL; PROGLACIAL STREAMS; SOLUTE CONCENTRATIONS; STREAM CHANNELS; STREAMS; VALLEY FLOOR;

FLOORS; GROUNDWATER; GROUNDWATER GEOCHEMISTRY; LANDFORMS; MATERIALS PROPERTIES; SEDIMENTOLOGY; SEDIMENTS; STREAM FLOW; TRACE ELEMENTS;

BIOLOGICAL MATERIALS;

DIURNAL VARIATION; EOLIAN PROCESS; GEOCHEMISTRY; GLACIER; MELTWATER; PROGLACIAL ENVIRONMENT; STREAM CHANNEL; TRACE ELEMENT;

ANTARCTICA; EAST ANTARCTICA; MCMURDO DRY VALLEYS; TAYLOR VALLEY;

EID: 84872181498     PISSN: 08856087     EISSN: 10991085     Source Type: Journal    
DOI: 10.1002/hyp.9255     Document Type: Article

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