Influence of the hyporheic zone on the phosphorus dynamics of a large gravel-bed river, Garonne River, France

Hydrological Processes

Volumn 23, Issue 12, 2009, Pages 1801-1812

  Vervier, Philippe ^a,b   Bonvallet Garay, Sonia ^a,b   Sauvage, Sabine ^a,b   Valett, H Maurice ^c   Sanchez Perez, José Miguel ^a,b  

^a CNRS   (France)

^b UNIVERSITÉ DE TOULOUSE   (France)

^c VIRGINIA POLYTECHNIC INSTITUTE AND STATE UNIVERSITY   (United States)

Author keywords

Hyporheic zone; Interstitial water; Large river; Phosphorus; Sediments

Indexed keywords

DISSOLVED PHOSPHORUS; DOWN-WELLING; FINE SEDIMENTS; GRAVEL-BED RIVERS; HYDRAULIC GRADIENTS; HYPORHEIC; HYPORHEIC ZONE; INTERSTITIAL WATER; LARGE RIVER; LARGE RIVERS; PHOSPHORUS DYNAMICS; SAMPLING DATES; SOLUBLE REACTIVE PHOSPHORUS; TOTAL DISSOLVED PHOSPHORUS; TOTAL PHOSPHORUS; TOULOUSE; WASTEWATER TREATMENT PLANTS;

CONCENTRATION (PROCESS); DISSOLUTION; GRAVEL; HOLOGRAPHIC GRATINGS; RIVERS; SEDIMENTOLOGY; STREAM FLOW; WASTEWATER; WASTEWATER RECLAMATION; WASTEWATER TREATMENT; WATER TREATMENT PLANTS;

PHOSPHORUS;

BIOAVAILABILITY; CONCENTRATION (COMPOSITION); DISSOLVED MATTER; GRAVEL BED STREAM; HYPORHEIC ZONE; NUTRIENT DYNAMICS; PHOSPHORUS; POREWATER;

EURASIA; EUROPE; FRANCE; GARONNE RIVER; WESTERN EUROPE;

EID: 65949084480     PISSN: 08856087     EISSN: 10991085     Source Type: Journal    
DOI: 10.1002/hyp.7319     Document Type: Article

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