Sediment Transport

Institut for Geovidenskab og Naturforvaltning

Publikation: Bidrag til bog/antologi/rapport › Bidrag til bog/antologi › Forskning › fagfællebedømt

Standard

Sediment Transport. / Aagaard, T.; Hughes, M. G.

Treatise on Geomorphology. red. / Douglas J. Sherman. Bind 8 2. udg. Elsevier, 2022. s. 122-160.

Publikation: Bidrag til bog/antologi/rapport › Bidrag til bog/antologi › Forskning › fagfællebedømt

Harvard

Aagaard, T & Hughes, MG 2022, Sediment Transport. i DJ Sherman (red.), Treatise on Geomorphology. 2. udg, bind 8, Elsevier, s. 122-160. https://doi.org/10.1016/B978-0-12-818234-5.00064-X

APA

Aagaard, T., & Hughes, M. G. (2022). Sediment Transport. I D. J. Sherman (red.), Treatise on Geomorphology (2. udg., Bind 8, s. 122-160). Elsevier. https://doi.org/10.1016/B978-0-12-818234-5.00064-X

Vancouver

Aagaard T, Hughes MG. Sediment Transport. I Sherman DJ, red., Treatise on Geomorphology. 2. udg. Bind 8. Elsevier. 2022. s. 122-160 https://doi.org/10.1016/B978-0-12-818234-5.00064-X

Author

Aagaard, T. ; Hughes, M. G. / Sediment Transport. Treatise on Geomorphology. red. / Douglas J. Sherman. Bind 8 2. udg. Elsevier, 2022. s. 122-160

Bibtex

@inbook{de5a2c4f053443849cae61cb6159cc16,

title = "Sediment Transport",

abstract = "Sediment transport is the mechanism that translates the work of hydrodynamic processes into morphological change. Without a transport of sediment, there would be no beaches. Significant progress has been made on the topic of non-cohesive sediment transport in wave-dominated settings since the first publication of this chapter. This especially applies to the study of sheet flow, and the effects of acceleration skewness and breaker-generated turbulence on sediment mobilization. Following an introductory section, techniques for measuring sediment transport are described, providing context for the following sections. Section 3 discusses the physical mechanisms that mobilize the sediment and suspend sand into the water column. Processes resulting in cross-shore (onshore/offshore) sediment transport, and ultimately beach erosion and accretion, are described in Section 4 and longshore sediment transport in Section 5. Finally, sediment transport in the swash zone is discussed in Section 6.",

keywords = "Beach processes, Bedload transport, Cross-shore sediment transport, Longshore sediment transport, Sediment concentration, Sediment transport models, Sheet flow, Shoreface, Surf and swash zone, Suspended sediment transport",

author = "T. Aagaard and Hughes, {M. G.}",

year = "2022",

doi = "10.1016/B978-0-12-818234-5.00064-X",

language = "English",

isbn = "9780128182345",

volume = "8",

pages = "122--160",

editor = "Sherman, {Douglas J.}",

booktitle = "Treatise on Geomorphology",

publisher = "Elsevier",

edition = "2.",

}

RIS

TY - CHAP

T1 - Sediment Transport

AU - Aagaard, T.

AU - Hughes, M. G.

PY - 2022

Y1 - 2022

N2 - Sediment transport is the mechanism that translates the work of hydrodynamic processes into morphological change. Without a transport of sediment, there would be no beaches. Significant progress has been made on the topic of non-cohesive sediment transport in wave-dominated settings since the first publication of this chapter. This especially applies to the study of sheet flow, and the effects of acceleration skewness and breaker-generated turbulence on sediment mobilization. Following an introductory section, techniques for measuring sediment transport are described, providing context for the following sections. Section 3 discusses the physical mechanisms that mobilize the sediment and suspend sand into the water column. Processes resulting in cross-shore (onshore/offshore) sediment transport, and ultimately beach erosion and accretion, are described in Section 4 and longshore sediment transport in Section 5. Finally, sediment transport in the swash zone is discussed in Section 6.

AB - Sediment transport is the mechanism that translates the work of hydrodynamic processes into morphological change. Without a transport of sediment, there would be no beaches. Significant progress has been made on the topic of non-cohesive sediment transport in wave-dominated settings since the first publication of this chapter. This especially applies to the study of sheet flow, and the effects of acceleration skewness and breaker-generated turbulence on sediment mobilization. Following an introductory section, techniques for measuring sediment transport are described, providing context for the following sections. Section 3 discusses the physical mechanisms that mobilize the sediment and suspend sand into the water column. Processes resulting in cross-shore (onshore/offshore) sediment transport, and ultimately beach erosion and accretion, are described in Section 4 and longshore sediment transport in Section 5. Finally, sediment transport in the swash zone is discussed in Section 6.

KW - Beach processes

KW - Bedload transport

KW - Cross-shore sediment transport

KW - Longshore sediment transport

KW - Sediment concentration

KW - Sediment transport models

KW - Sheet flow

KW - Shoreface

KW - Surf and swash zone

KW - Suspended sediment transport

U2 - 10.1016/B978-0-12-818234-5.00064-X

DO - 10.1016/B978-0-12-818234-5.00064-X

M3 - Book chapter

AN - SCOPUS:85148832744

SN - 9780128182345

VL - 8

SP - 122

EP - 160

BT - Treatise on Geomorphology

A2 - Sherman, Douglas J.

PB - Elsevier

ER -

ID: 345371235