Sediment Transport and Morphological Processes at the Watershed Scale

A special issue of Hydrology (ISSN 2306-5338). This special issue belongs to the section "Surface Waters and Groundwaters".

Deadline for manuscript submissions: 30 April 2025 | Viewed by 2964

Special Issue Editors


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Guest Editor
Changjiang River Scientific Research Institute, Changjiang Water Resources Commission, Wuhan 430010, China
Interests: fine sediment dynamics; reservoir siltation; river protection

Special Issue Information

Dear Colleagues,

At a time where matters on water demand/scarcity, flood control, land degradation and sedimentation in streams and reservoirs are becoming first-line priorities for catchment managers and stakeholders, understanding hydrological processes and sediment dynamics at the watershed scale is very relevant.

In recent years, water and sediment cycles have been subjected to stresses caused by climate change and anthropogenic pressure, eventually resulting in significant basin-wide changes.

To better understand processes and drivers of such changes, a combination of innovative techniques and tools is required nowadays, integrating modelling, remote sensing, field measurements, and experimental methods.

The goal of this Special Issue is to collect papers (original research articles and review papers) to give insights on sediment transport and morphological processes at the watershed scale, showing the potential of up-to-date methods in monitoring and modelling such phenomena.

This Special Issue welcomes manuscripts that link the following themes:

  • Watershed hydrology and sediment transport;
  • State-of-the-art methods to monitor and model morphological changes at a large scale;
  • Policies and management strategies.

We look forward to receiving your original research articles and reviews.

Dr. Michael Nones
Dr. Chao Guo
Guest Editors

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Keywords

  • sediment transport
  • reservoir sediment management
  • watershed hydrology
  • morphological changes
  • landscape evolution
  • numerical modelling
  • large-scale monitoring

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Published Papers (2 papers)

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Research

16 pages, 4207 KiB  
Article
Predicting Suspended Sediment Transport in Urbanised Streams: A Case Study of Dry Creek, South Australia
by Tesfa Gebrie Andualem, Guna A. Hewa, Baden R. Myers, John Boland and Stefan Peters
Hydrology 2024, 11(11), 196; https://doi.org/10.3390/hydrology11110196 - 16 Nov 2024
Viewed by 799
Abstract
Sediment transport in urban streams is a critical environmental issue, with significant implications for water quality, ecosystem health, and infrastructure management. Accurately estimating suspended sediment concentration (SSC) is essential for effective long-term environmental management. This study investigates the relationships between streamflow, turbidity, and [...] Read more.
Sediment transport in urban streams is a critical environmental issue, with significant implications for water quality, ecosystem health, and infrastructure management. Accurately estimating suspended sediment concentration (SSC) is essential for effective long-term environmental management. This study investigates the relationships between streamflow, turbidity, and SSC in Dry Creek, South Australia, to understand sediment transport dynamics in urbanised catchments. We collected grab samples from the field and analysed them in the laboratory. We employed statistical modelling to develop a sediment rating curve (SRC) that provides insights into the sediment transport dynamics in the urban stream. The grab sample measurements showed variations in SSC between 3.2 and 431.8 mg/L, with a median value of 77.3 mg/L. The analysis revealed a strong linear relationship between streamflow and SSC, while turbidity exhibited a two-regime linear relationship, in which the low-turbidity regime demonstrated a stronger linear relationship compared to the high-turbidity regime. This is attributed to the urbanised nature of the catchment, which contributes to a first-flush effect in turbidity. This contributes to sediment hysteresis, resulting in non-proportional turbidity and SSC responses to streamflow changes. The findings demonstrate the effectiveness of a streamflow-based SRC for accurately predicting sediment discharge, explaining 97% of the variability in sediment discharge. The sediment discharge predicted using the SRC indicated a sediment load of 341.8 tonnes per year along the creek. The developed sediment rating curve provides a valuable tool for long-term sediment management in Dry Creek, enabling the assessment of downstream environmental risks. By addressing data limitations, this study contributes to a deeper understanding of sediment transport dynamics in urbanized environments, offering insights for informed decision-making and effective sediment management strategies. Full article
(This article belongs to the Special Issue Sediment Transport and Morphological Processes at the Watershed Scale)
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25 pages, 9446 KiB  
Article
Reconstruction of a Long-Term, Reach-Scale Sediment Budget Using Lateral Channel Movement Data as a Proxy: A Case Study on the Lowland Section of the Tisza River, Hungary
by Tímea Kiss, Marcell Tóth, Gergely T. Török and György Sipos
Hydrology 2024, 11(5), 67; https://doi.org/10.3390/hydrology11050067 - 9 May 2024
Cited by 1 | Viewed by 1288
Abstract
Humans have influenced the sediment transport of rivers on a centurial scale. Our goal was to use the rate of lateral channel processes as a proxy to reconstruct sediment budget (SB) changes of a lowland river (Middle Tisza, Hungary) on a historical scale [...] Read more.
Humans have influenced the sediment transport of rivers on a centurial scale. Our goal was to use the rate of lateral channel processes as a proxy to reconstruct sediment budget (SB) changes of a lowland river (Middle Tisza, Hungary) on a historical scale (1838–2017). The gross sediment budget (GSB) refers to the total area of eroded and accumulated surfaces, and the net sediment budget (NSB) indicates the sediment sink or source characteristics. At the beginning (1838–1890), the artificial cut-offs increased the slope and channel erosion, but the eroded sediment deposited in the oxbows, so the reach acted as a sediment sink (NSB: +0.1–0.8 m2/m/y). Then (1890–1929), a quasi-equilibrium state developed (NSB: −0.2 m2/m/y to +0.4 m2/m/y). Later (1929–1976), the bank protections impeded lateral erosion, so the system became a sediment sink again (NSB: +0.1–0.7 m2/m/y). Finally (1976–2017), the erosional processes accelerated due to dam construction and revetment collapses, and now the river is a sediment source (NSB: −0.03 to −0.08 m2/m/y). This study proved that (1) the actual SB could not be projected in the long term, as it was heavily modified, and (2) lateral channel changes could be used as a proxy to estimate long-term SB. Full article
(This article belongs to the Special Issue Sediment Transport and Morphological Processes at the Watershed Scale)
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