Skip to main content

Abstract

Granulometric studies of sediment samples from different geomorphic units (e.g. mid-channel bars or flood-tidal delta, river mouth bars or ebb-tidal deltas, point bars, swash platforms, wash-over flats and riverbanks (levee) of the Thakuran basin have revealed the prevailing hydrodynamic condition at the time of their deposition. A coarsening of graphic mean size (MZ), betterment of sorting (σ1) and negative to positive skewness (SK1) have been noticed, progressively from the seaward point and in the landward direction. Variations of these textural parameters are related to decreasing energy levels in the same direction. A bipartite-granulometric model of sedimentation, which has a sand-to-mud transition from the seaward point of the tidal creek and in the landward direction, has been discerned. This is in contrast to a tripartite-granulometric model typical of estuaries.

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 84.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 109.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 109.99
Price excludes VAT (USA)
  • Durable hardcover 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

References

  • Das GK (2015) Estuarine morphodynamics of the Sunderbans. Coastal research library, vol 11. Springer, Switzerland, 211p

    Google Scholar 

  • DeMaeyer P, Wartel S (1988) Relation between superficial sediment grain size and morphological features of the coastal ridges off the Belgian coast. In: DeBoer PL et al (eds) Tide-influenced sedimentary environment and facies. D Reidel Publication Company, pp 91–100 (530p)

    Google Scholar 

  • Evans G (1965) Intertidal flat sedimentation and their environment of deposition in the wash. Q J Geol Soc 121:209–241

    Article  Google Scholar 

  • Flemming BW (1999) Mass physical properties of muddy intertidal sediments: some applications, misapplications and non-applications. Intertidal mudflats; properties and processes. Plymouth, England

    Google Scholar 

  • Folk RL (1954) Sedimentary rock nomenclature. J Geol 62:345–351

    Article  Google Scholar 

  • Folk RL, Ward W (1957) Brazos river bar-A study in the significance of grain size parameters. J Sediment Petrol 27:3–26

    Article  Google Scholar 

  • Friedman GM (1967) Dynamic processes and statistical parameters compared for size frequency distribution of beach and river sands. J Sediment Petrol 37:327–354

    Article  Google Scholar 

  • McLaren P (1981) An interpretation in grain size measurements. J Sediment Petrol 51:611–624

    Google Scholar 

  • Middleton GV (1976) Hydraulic interpretation of sand size distributions. J Geol 84:405–426

    Article  Google Scholar 

  • Moiola RJ, Weiser D (1968) Textural parameters: an evaluation. J Sediment Petrol 38:45–53

    Google Scholar 

  • Pejrup M (1988) The triangular diagram used for classification of estuarine sediments: a new approach. In: DeBoer PL, Van Gelder A, Nio SD (eds) Tide-influenced sedimentary environments and facies, D Reidel Publication Company. Holland, pp 289–300 (530p)

    Google Scholar 

  • Rahmani RA (1988) Estuarine tidal channel and nearshore sedimentation of a late Cretaceous epicontinental sea, Drumheller, Alberta, Canada. In: de Boer PL, Van Gelder A, Nio SD (eds) Tide-influenced sedimentary environments and facies. D Reidel Publishing Company. Holland, pp 433–471 (530p)

    Google Scholar 

  • Sagoe KMO, Visher GS (1977) Population breaks a grain size distribution of sand. A theoretical model. J Sediment Petrol 47:215–310

    Google Scholar 

  • Shepard FP (1954) Nomenclature based on sand-silt-clay ratio. J Sediment Petrol 24:151–158

    Article  Google Scholar 

  • Spencer DW (1963) The interpretation of grain size distribution curves of clastic sediments. J Sediment Petrol 33:180–190

    Google Scholar 

  • Tanner WF (1959) Sample components obtained by the method of differences. J Sediment Petrol 29:408–411

    Google Scholar 

  • Visher GS (1969) Grainsize distribution and depositional processes. J Sediment Petrol 39:1074–1106

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Gautam Kumar Das .

Rights and permissions

Reprints and permissions

Copyright information

© 2017 Springer International Publishing Switzerland

About this chapter

Cite this chapter

Das, G.K. (2017). Sediment Texture. In: Tidal Sedimentation of the Sunderban's Thakuran Basin. Springer, Cham. https://doi.org/10.1007/978-3-319-44191-7_6

Download citation

Publish with us

Policies and ethics