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dc.contributor.authorNyman, P
dc.contributor.authorBox, WAC
dc.contributor.authorStout, JC
dc.contributor.authorSheridan, GJ
dc.contributor.authorKeesstra, SD
dc.contributor.authorLane, PNJ
dc.contributor.authorLanghans, C
dc.date.accessioned2020-08-05T03:36:04Z
dc.date.available2020-08-05T03:36:04Z
dc.date.issued2020
dc.identifier.issn0197-9337
dc.identifier.doi10.1002/esp.4785
dc.identifier.urihttp://hdl.handle.net/10072/396203
dc.description.abstractField 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 (<1 km2) with the Ovens River in SE Australia. We construct a sediment budget by combining new data on deposition with a sediment delivery model for post‐fire debris flows. Data on deposits were plotted alongside the slope–area curve to examine links between processes, catchment morphometry and geomorphic process domains. The results show that large deposits are concentrated in the proximity of three major channel junctions, which correspond to breaks in channel slope. Hyperconcentrated flows are more prominent towards the catchment outlet, where the slope–area curve indicates a transition from debris flow to fluvial domains. This shift corresponds to a change in efficiency of the flow, determined from the ratio of median grain size to channel slope. Our sediment budget suggests a total sediment efflux from Washington Creek catchment of 61 × 103 m3. There are similar contributions from hillslopes (43 ± 14 × 103 m3), first to third stream order channel (35 ± 12 × 103 m3) and the arterial fourth to fifth stream order channel (31 ± 17 × 103 m3) to the total volume of erosion. Deposition (39 ± 17 × 103 m3) within the arterial channel was higher than erosion (31 ± 17 × 103 m3), which means a net sediment gain of about 8 × 103 m3 in the arterial channel. The ratio of total deposition to total erosion was 0.44. For fines <63 μm, this ratio was much smaller (0.11), which means that fines are preferentially exported. This has important implications for suspended sediment and water quality in downstream rivers.
dc.description.peerreviewedYes
dc.languageen
dc.publisherWiley
dc.relation.ispartofpagefrom1155
dc.relation.ispartofpageto1167
dc.relation.ispartofissue5
dc.relation.ispartofjournalEarth Surface Processes and Landforms
dc.relation.ispartofvolume45
dc.subject.fieldofresearchGeology
dc.subject.fieldofresearchPhysical Geography and Environmental Geoscience
dc.subject.fieldofresearchcode0403
dc.subject.fieldofresearchcode0406
dc.titleDebris-flow-dominated sediment transport through a channel network after wildfire
dc.typeJournal article
dc.type.descriptionC1 - Articles
dcterms.bibliographicCitationNyman, P; Box, WAC; Stout, JC; Sheridan, GJ; Keesstra, SD; Lane, PNJ; Langhans, C, Debris-flow-dominated sediment transport through a channel network after wildfire, Earth Surface Processes and Landforms, 2020, 45 (5), pp. 1155-1167
dc.date.updated2020-08-05T03:34:50Z
gro.hasfulltextNo Full Text
gro.griffith.authorStout, Justin


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