Skip to main content

Fine Sediment Particle Transport in Estuaries

  • Conference paper
Physical Processes in Estuaries

Abstract

The main sedimentary feature indicative of fine sediment transport in estuaries is the turbidity maximum. This is a dynamic feature within which suspended sediment concentrations vary with tidal state, with the lunar cycle, with river discharge, and seasonally. The turbidity maximum is a feature through which sediment is continually exchanged from one part of the estuary to another with small amounts being added from the rivers and the sea; though these inputs are on average balanced by accumulation. Individual particles may undergo many cycles of deposition and re-entrainment during their life in the turbidity maximum. The feature depends in a complex way on a combination of the tidal dynamics, the residual estuarine circulation, and the erosion and deposition of sediment, which depend upon the bed shear stress, as well as the erodability of the bed sediment. Examination of the suspended sediment fluxes in five estuaries leads to the conclusion that the major factor in generating and supporting the turbidity maximum is the phase lag with the current produced by entrainment and suspension of sediment.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 129.00
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 169.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

Preview

Unable to display preview. Download preview PDF.

Unable to display preview. Download preview PDF.

References

  • Allen GP (1973) Etude des processes sédimentaires dans l’estuaire de la Gironde. Mem Inst Geol Bassin D’Aquitaine No. 5

    Google Scholar 

  • Allen GP, Salomon JC, Bassoulet P, Du Penhoat Y, DeGrandpre C (1980) Effects of tides on mixing and suspended sediment transport in macrotidal estuaries. Sediment Geol 26:69–90

    Article  Google Scholar 

  • Ariathurai R, Arulanandan K (1978) Erosion rates of cohesive soils. J Hydraul Div ASCE 104 HY2:279–283

    Google Scholar 

  • Aubrey DG, Speer PE (1983) Sediment transport in a tidal inlet. Woods Hole Oceanogr Inst Tech Rep WHO1-83–20

    Google Scholar 

  • Been K, Sills GC (1981) Self weight consolidation of soft soils: an experimental and theoretical study. Geotechnique 31:519–535

    Article  Google Scholar 

  • Boon JD (1975) Tidal discharge asymmetry in a salt marsh drainage system. Limnol Oceanogr 20:71–80

    Article  Google Scholar 

  • Boon JD, Byrne RJ (1981) On basin hypsometry and the morphodynamic response of coastal inlet systems. Mar Geol 40:27–48

    Article  Google Scholar 

  • Brown WS, Trask RP (1980) A study of tidal energy dissipation and bottom stress in an estuary. J Phys Oceanogr 10:1742–1754

    Article  Google Scholar 

  • De Jonge VN (1985) The occurrence of “epipsammic” diatom populations: a result of interaction between physical sorting of sediment and certain properties of diatom species. Estuarine Coastal Mar Sci 21:607–622

    Article  Google Scholar 

  • Dobereiner C, McManus J (1983) Turbidity maximum migration and harbour siltation in the Tay Estuary. Can J Fish Aquat Sci 40:117–129

    Article  Google Scholar 

  • Dronkers J (1986) Tide-induced residual transport of fine sediment. In: Van de Kreeke J (ed) Physics of shallow estuaries and bays, Springer, Berlin Heidelberg New York, pp 228–244

    Google Scholar 

  • Dyer KR (1974) The salt balance in stratified estuaries. Estuarine Coastal Mar Sci 2:273–281

    Article  Google Scholar 

  • Dyer KR (1978) The balance of suspended sediment in the Gironde and Thames estuaries. In: Kjerfve BJ (ed) Estuarine transport processes. Belle W Baruch Libr Mar Sci 7:331

    Google Scholar 

  • Dyer KR (1986) Coastal and estuarine sediment dynamics. John Wiley, Chichester, p 342

    Google Scholar 

  • Einstein HA, Krone RB (1962) Experiments to determine modes of cohesive sediment transport in salt water. J Geophys Res 67:1451–1461

    Article  Google Scholar 

  • Festa JF, Hansen DV (1978) Turbidity maxima in partially mixed estuaries: a two-dimensional numerical model. Estuarine Coastal Mar Sci 7:347–359

    Article  Google Scholar 

  • Fischer HB (1972) Mass transport mechanisms in partially stratified estuaries. J Fluid Mech 53:672–687

    Article  Google Scholar 

  • Frostick LE, McCave IN (1979) Seasonal shifts of sediment within an estuary mediated by algal growth. Estuarine Coastal Mar Sci 9:569–576

    Article  Google Scholar 

  • Green FHW (1957) Tidal phenomena: with special reference to Southampton and Poole. Dock Harbour Auth 32:143–148

    Google Scholar 

  • Groen P (1967) On the residual transport of suspended matter by an alternating tidal current. Neth J Sea Res 3:564–574

    Article  Google Scholar 

  • Halliwell AR, O’Connor BA (1966) Suspended sediment in a tidal estuary. Proc 10th Coastal Eng Conf New York, pp 687–706

    Google Scholar 

  • Hansen DV (1965) Currents and mixing in the Columbia River estuary. Trans Joint Conf Ocean Sci Ocean Eng, pp 943–955

    Google Scholar 

  • HRS (1981) The Severn estuary: silt monitoring April 1980—March 1981. Hydraul Res Stat Rep EX 995

    Google Scholar 

  • Jackson WH (1964) An investigation into silt in suspension in the River Humber. Dock Harbour Auth 45:526

    Google Scholar 

  • James AE, Williams DJA (1982) Flocculation and rheology of kaolinite/quartz suspensions. Rheol Acta 21:176–183

    Article  Google Scholar 

  • Kirby R, Parker WR (1981) Settled mud deposits in Bridgwater Bay, Bristol Channel. Inst Oceanogr Sci Rep 107:67

    Google Scholar 

  • Lewis R, Lewis JO (1986) Shear stress variations in an estuary. Estuarine Coastal Shelf Sci 25:621–635

    Article  Google Scholar 

  • McCave IN (1974) Discussion on Meade RH, net transport of sediment through the mouths of estuaries: seaward or landward? Mem Inst Geol Bassin D’Aquitaine 7:207–213

    Google Scholar 

  • Murray SP, Siripong A (1978) Role of lateral gradients and longitudinal dispersion in the salt balance of a shallow well mixed estuary. In: Kjerfve BJ (ed) Estuarine transport processes. Belle W Baruch Libr Mar Sci 7:331

    Google Scholar 

  • Nichols MM (1977) Response and recovery of an estuary following a river flood. J Sediment Petrol 47:1171–1186

    Google Scholar 

  • Nichols MM, Biggs RB (1985) Estuaries. In: Davis RA Jr (ed) Coastal sedimentary environments. Springer, Berlin Heidelberg New York

    Google Scholar 

  • Officer CB (1981) Physical dynamics of estuarine suspended sediments. Mar Geol 40:1–14

    Article  Google Scholar 

  • Postma H (1961) Transport and accumulation of suspended matter in the Dutch Wadden Sea. Neth J Sea Res 1:148–190

    Article  Google Scholar 

  • Rattray M, Dworski JG (1980) Comparison of methods for analysis of the transverse and vertical circulation contributions to the longitudinal advective flux in estuaries. Estuarine Coastal Mar Sci 11:515–536

    Article  Google Scholar 

  • Schubel JR (1969) Distribution and transport of suspended sediment in Upper Chesapeake Bay. Chesapeake Bay Institute Johns Hopkins Univ Tech Rep 60, 69–13

    Google Scholar 

  • Schubel JR, Carter HH (1984) The estuary as a filter for fine-grained suspended sediment. In: Kennedy V (ed) The estuary as a filter. Academic Press, New York

    Google Scholar 

  • Soulsby RL, Salkield AP, LeGood GP (1985) Measurements of the turbulence characteristics of sand suspendend by a tidal current. Continent Shelf Res 3:439–454

    Article  Google Scholar 

  • Su J, Wang K (1986) The suspended sediment balance in Changjiang estuary. Estuarine Coastal Shelf Sci 23:81–98

    Article  Google Scholar 

  • Thorn MFC, Parsons JG (1980) Erosion of cohesive sediments in estuaries: an engineering guide. Proc 3rd Int Symp Dredging Tech, pp 349–358

    Google Scholar 

  • Uncles RJ, Elliott TCA, Weston SA (1984) Lateral distributions of water, salt and sediment transport in a partly mixed estuary. Proc 19th Coastal Eng Conf Houston, pp 3067–3077

    Google Scholar 

  • Uncles RJ, Elliott RCA, Weston SA (1985a) Observed fluxes of water, and suspended sediment in a partly mixed estuary. Estuarine Coastal Shelf Sci 20:147–167

    Article  Google Scholar 

  • Uncles RJ, Elliott RCA, Weston SA (1985b) Dispersion of salt and suspended sediment in a partly mixed estuary. Estuaries 8:256–269

    Article  Google Scholar 

  • van Straaten LMJU, Kuenen PLH (1958) Tidal action as a cause of clay accumulation. J Sediment Petrol 28:406–413

    Google Scholar 

  • Wellershaus S (1981) Turbidity maximum and mud shoaling in the Weser Estuary. Arch Hydrobiol 92:161–198

    Google Scholar 

  • Zarillo GA (1985) Tidal dynamics and substrate response in a salt-marsh estuary. Mar Geol 67:13–35

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 1988 Springer-Verlag Berlin Heidelberg

About this paper

Cite this paper

Dyer, K.R. (1988). Fine Sediment Particle Transport in Estuaries. In: Dronkers, J., van Leussen, W. (eds) Physical Processes in Estuaries. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-73691-9_16

Download citation

  • DOI: https://doi.org/10.1007/978-3-642-73691-9_16

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-73693-3

  • Online ISBN: 978-3-642-73691-9

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics