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Suspended sediment budget and intra-event sediment dynamics of a small glaciated mountainous catchment in the Northern Caucasus

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dc.contributor.author Tsyplenkov A.
dc.contributor.author Vanmaercke M.
dc.contributor.author Golosov V.
dc.contributor.author Chalov S.
dc.date.accessioned 2021-02-25T20:43:06Z
dc.date.available 2021-02-25T20:43:06Z
dc.date.issued 2020
dc.identifier.issn 1439-0108
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/162297
dc.description.abstract © 2020, Springer-Verlag GmbH Germany, part of Springer Nature. Purpose: The sediment dynamics of (peri-)glacial catchments can be highly variable and complex. Understanding these dynamics and their underlying causes is not only of interest from a scientific perspective but also required to address the practical problems with which they are often associated. In order to better understand the sediment dynamics of glaciated mountainous catchments, suspended sediment fluxes in the 9.1 km2 Djankuat catchment (North Caucasus, Russia) were monitored intensively during the 2017 ablation season. Materials and methods: The intra-event suspended sediment dynamics were studied using a newly proposed simple hysteresis index (SHI), quantifying to what extent evolutions in sediment concentration are characterized by a clockwise or anticlockwise hysteresis loop. Results and discussion: The resulting catchment suspended sediment yield was 1033 t km−2 year−1, with the glacier itself contributing 72% of the suspended sediment load. However, during rainfall events, also hillslope erosion in the proglacial area became a very significant sediment source. Clockwise hysteresis loops occurred in 61.8% of the events, while anticlockwise in 11.8%. On the other hand, only 47.8% of the total suspended sediment flux was transported during clockwise events. Our observations clearly indicate that events showing a stronger clockwise pattern (i.e., a higher SHI) are associated with a larger sediment input from the proglacial area. Conclusions: Overall, our results provide data and insights on sediment dynamics in an understudied environment. They illustrate that the type and characteristics of sediment concentration hysteresis loops are to some extent linked to the dominant sediment sources during the event. As such, the proposed methodology and SHI may also help with a better understanding of sediment dynamics in other environments.
dc.relation.ispartofseries Journal of Soils and Sediments
dc.subject Hysteresis
dc.subject Mountain hydrology
dc.subject Sediment budget
dc.subject Sediment yield
dc.subject Suspended sediments
dc.title Suspended sediment budget and intra-event sediment dynamics of a small glaciated mountainous catchment in the Northern Caucasus
dc.type Article
dc.relation.ispartofseries-issue 8
dc.relation.ispartofseries-volume 20
dc.collection Публикации сотрудников КФУ
dc.relation.startpage 3266
dc.source.id SCOPUS14390108-2020-20-8-SID85084826586


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  • Публикации сотрудников КФУ Scopus [24551]
    Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.

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