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Water
Special Issues
Monitoring and Assessment of Suspended Sediment Transport at Catchment Scale
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Special Issue "Monitoring and Assessment of Suspended Sediment Transport at Catchment Scale"

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Water Erosion and Sediment Transport".

Deadline for manuscript submissions: closed (20 December 2022) | Viewed by 10719

Special Issue Editors

Dr. María Luz Rodríguez-Blanco

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Guest Editor
Área de Geografía Física, Grupo GEAAT, Campus de Ourense (UVigo), 32004 Ourense, España
Interests: hydrology; soil erosion; sediment and nutrient dynamics; hydrology modeling; climate change
Special Issues, Collections and Topics in MDPI journals
Dr. Núria Martínez-Carreras

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Guest Editor
Luxembourg Institute of Science and Technology (LIST), Esch-sur-Alzette, Luxembourg, Luxembourg
Interests: sediment transport; sediment tracing; catchment hydrology
Dr. Estela Nadal-Romero

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Guest Editor
Instituto Pirenaico de Ecología, IPE-CSIC, Zaragoza, Spain
Interests: badlands; hydrological dynamics; soil erosion; sediment transport; soil properties; land use change

Special Issue Information

In many rivers, suspended sediment has been identified as one of the leading causes of river impairment. Therefore, a deeper understanding of suspended sediment transport mechanisms and dynamics, as well as an accurate quantification of suspended sediment fluxes, is important for sustainable water and sediment management purposes.

In this Special Issue, we invite papers that investigate suspended sediment transport at catchment scale. Papers should improve our knowledge on factors controlling suspended sediment transport mechanisms across different landscapes and provide robust diagnoses and guidelines to decision makers. We especially encourage contributions dealing with long-term monitoring datasets, comparative studies, and those that attempt high-resolution monitoring across multiple temporal and spatial scales. In addition, we welcome studies using new technologies and innovative methods for monitoring suspended sediment transport, and those investigating the impact of global change on sediment transport by rivers.

Dr. María Luz Rodríguez-Blanco
Dr. Núria Martínez-Carreras
Dr. Estela Nadal-Romero
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Water is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2600 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • sediment transport
  • catchment scale
  • long-term monitoring
  • high resolution

Published Papers (3 papers)

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Research

25 pages, 11167 KiB  
Article
Fluvial Response to Climate Change in the Pacific Northwest: Skeena River Discharge and Sediment Yield
by
Amanda Lily Wild
,
Eva Kwoll
,
D. Gwyn Lintern
and
Shannon Fargey
Water 2023, 15(1), 167; https://doi.org/10.3390/w15010167 - 31 Dec 2022
Cited by 1 | Viewed by 1628
Abstract
Changes in climate affect the hydrological regime of rivers worldwide and differ with geographic location and basin characteristics. Such changes within a basin are captured in the flux of water and sediment at river mouths, which can impact coastal productivity and development. Here, [...] Read more.
Changes in climate affect the hydrological regime of rivers worldwide and differ with geographic location and basin characteristics. Such changes within a basin are captured in the flux of water and sediment at river mouths, which can impact coastal productivity and development. Here, we model discharge and sediment yield of the Skeena River, a significant river in British Columbia, Canada. We use HydroTrend 3.0, two global climate models (GCMs), and two representative concentration pathways (RCPs) to model changes in fluvial fluxes related to climate change until the end of the century. Contributions of sediment to the river from glaciers decreases throughout the century, while basin-wide overland and instream contributions driven by precipitation increase. Bedload, though increased compared to the period (1981–2010), is on a decreasing trajectory by the end of the century. For overall yield, the model simulations suggest conflicting results, with those GCMs that predict higher increases in precipitation and temperature predicting an increase in total (suspended and bedload) sediment yield by up to 10% in some scenarios, and those predicting more moderate increases predicting a decrease in yield by as much as 20%. The model results highlight the complexity of sediment conveyance in rivers within British Columbia and present the first comprehensive investigation into the sediment fluxes of this understudied river system. Full article
(This article belongs to the Special Issue Monitoring and Assessment of Suspended Sediment Transport at Catchment Scale)
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19 pages, 7039 KiB  
Article
Did the Construction of the Bhumibol Dam Cause a Dramatic Reduction in Sediment Supply to the Chao Phraya River?
by
Matharit Namsai
,
Warit Charoenlerkthawin
,
Supakorn Sirapojanakul
,
William C. Burnett
and
Butsawan Bidorn
Water 2021, 13(3), 386; https://doi.org/10.3390/w13030386 - 02 Feb 2021
Cited by 5 | Viewed by 3753
Abstract
The Bhumibol Dam on Ping River, Thailand, was constructed in 1964 to provide water for irrigation, hydroelectric power generation, flood mitigation, fisheries, and saltwater intrusion control to the Great Chao Phraya River basin. Many studies, carried out near the basin outlet, have suggested [...] Read more.
The Bhumibol Dam on Ping River, Thailand, was constructed in 1964 to provide water for irrigation, hydroelectric power generation, flood mitigation, fisheries, and saltwater intrusion control to the Great Chao Phraya River basin. Many studies, carried out near the basin outlet, have suggested that the dam impounds significant sediment, resulting in shoreline retreat of the Chao Phraya Delta. In this study, the impact of damming on the sediment regime is analyzed through the sediment variation along the Ping River. The results show that the Ping River drains a mountainous region, with sediment mainly transported in suspension in the upper and middle reaches. By contrast, sediment is mostly transported as bedload in the lower basin. Variation of long-term total sediment flux data suggests that, while the Bhumibol Dam does effectively trap sediment, there was only a 5% reduction in sediment supply to the Chao Phraya River system because of sediment additions downstream. Full article
(This article belongs to the Special Issue Monitoring and Assessment of Suspended Sediment Transport at Catchment Scale)
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23 pages, 5046 KiB  
Article
Effect of the Three Gorges Dam on Total Suspended Sediments from MODIS and Landsat Satellite Data
by
Antonio Di Trapani
,
Chiara Corbari
and
Marco Mancini
Water 2020, 12(11), 3259; https://doi.org/10.3390/w12113259 - 20 Nov 2020
Cited by 5 | Viewed by 4683
Abstract
Total suspended matter (TSM) concentration is an extremely important parameter for water quality definition. The aim of this work is the evaluation of the effect of the Three Gorges Dam on total suspended sediments using remote sensing data at different temporal and spatial [...] Read more.
Total suspended matter (TSM) concentration is an extremely important parameter for water quality definition. The aim of this work is the evaluation of the effect of the Three Gorges Dam on total suspended sediments using remote sensing data at different temporal and spatial resolutions. TSM is estimated for the middle Yangtze river, China, before and after the construction of the Three Gorges Dam. The retrieved values are correlated to ground daily discharge values, finding relations between the physical quantities and discharge. Then, the application of the obtained relations to the discharge dataset provides continuous daily estimations of TSM values, also covering the days for which satellite scenes were lacking. This daily dataset will allow us to estimate the annual volume of river solid sediments. According to this work, both low spatial resolution MODIS (Moderate Resolution Imaging Spectroradiometer) data and high-resolution. Landsat 5 and 7 are able to detect the changes in TSM distribution over space and time induced by the building of the Three Gorges Dam, with a variation of even 50 mg/L over summer season. The confrontation of solid discharge with daily estimated TSM values shows that the single band MODIS algorithm performs better for medium-low concentrations, while the dual-band algorithm for MODIS and the selected Landsat algorithm perform better with high concentrations. Full article
(This article belongs to the Special Issue Monitoring and Assessment of Suspended Sediment Transport at Catchment Scale)
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