Debris‐flow‐dominated sediment transport through a channel network after wildfire

Debris‐flow‐dominated sediment transport through a channel network after wildfire

Field studies that investigate sediment transport between debris‐flow‐producing headwaters and rivers are uncommon, particularly in forested settings, where debris flows are infrequent and opportunities for collecting data are limited. This study quantifies the volume and composition of sediment dep...

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Veröffentlicht in:Earth surface processes and landforms 2020-04, Vol.45 (5), p.1155-1167
Hauptverfasser: Nyman, Petter, Box, Walter A.C., Stout, Justin C., Sheridan, Gary J., Keesstra, Saskia D., Lane, Patrick N.J., Langhans, Christoph
Format: Artikel
Sprache:eng
Schlagworte:
Catchment area
Catchments
channel network
Coastal inlets
Creeks
Data collection
Debris flow
Deposition
Detritus
Domains
Efflux
Fluvial deposits
Fluvial sediments
Geomorphology
Grain size
Headwaters
Morphometry
Outlets
Ovens
Rivers
Sediment
sediment budget
sediment deposition
Sediment transport
Slopes
Soil erosion
Stream order
Suspended sediments
Water quality
wildfire
Wildfires
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Beschreibung
Zusammenfassung:Field studies that investigate sediment transport between debris‐flow‐producing headwaters and rivers are uncommon, particularly in forested settings, where debris flows are infrequent and opportunities for collecting data are limited. This study quantifies the volume and composition of sediment deposited in the arterial channel network of a 14‐km2 catchment (Washington Creek) that connects small, burned and debris‐flow‐producing headwaters (
ISSN:0197-9337
1096-9837
DOI:10.1002/esp.4785