Fersiynau electronig

Dogfennau

  • Baas et al (2018) revised ms

    Llawysgrif awdur wedi’i dderbyn, 4 MB, dogfen-PDF

    Embargo yn dod i ben: 4/04/20

Dangosydd eitem ddigidol (DOI)

  • Jacobus Baas
  • Megan Baker
  • Jonathan Malarkey
  • S.J. Bass
    School of Marine Science and Engineering, Plymouth University
  • A.J. Manning
    School of Marine Science and Engineering, Plymouth University
  • J.A. Hope
    Institute of Marine Science, The University of Auckland
  • Jeff Peakall
    Leeds University
  • Ian Lichtman
  • L. Ye
    Department of Geography, Environment and Earth Sciences, University of Hull
  • Alan Davies
  • D.R. Parsons
    Department of Geography, Environment and Earth Sciences, University of Hull
  • D.M. Paterson
    Scottish Oceans Institute, School of Biology, University of St. Andrews
  • P.D. Thorne
    National Oceanography Centre, Liverpool
The shape and size of sedimentary bedforms play a key role in the reconstruction of sedimentary processes in modern and ancient environments. Recent laboratory experiments have shown that bedforms in mixed sand–clay develop at a slower rate and often have smaller heights and wavelengths than equivalent bedforms in pure sand. This is generally attributed to cohesive forces that can be of physical origin, caused by electrostatic forces of attraction between clay minerals, and of biological origin, caused by ‘sticky’ extracellular polymeric substances (EPS) produced by micro-organisms, such as microalgae (microphytobenthos) and bacteria. The present study demonstrates, for the first time, that these laboratory experiments are a suitable analogue for current ripples formed by tidal currents on a natural mixed sand–mud–EPS intertidal flat in a macrotidal estuary. Integrated hydrodynamic and bed morphological measurements, collected during a spring tide under weak wave conditions near Hilbre Island (Dee Estuary, north-west England), reveal a statistically significant decrease in current ripple wavelength for progressively higher bed mud and EPS contents, and a concurrent change from three-dimensional linguoid to two-dimensional straight-crested ripple planform morphology. These results agree well with observations in laboratory flumes, but the rate of decrease of ripple wavelength as mud content increased was found to be substantially greater for the field than the laboratory. Since the formation of ripples under natural conditions is inherently more complex than in the laboratory, four additional factors that might affect current ripple development in estuaries, but which were not accounted for in laboratory experiments, were explored. These were current forcing, clay type, pore water salinity, and bed EPS content. These data illustrate that clay type alone cannot explain the difference in the rate of decrease in ripple wavelength, because the bed clay contents were too low for clay type to have had a measurable effect on bedform development. Accounting for the difference in current forcing between the field and experiments, and therefore the relative stage of development with respect to equilibrium ripples, increases the difference between the ripple wavelengths. The presence of strongly cohesive EPS in the current ripples on the natural intertidal flat might explain the majority of the difference in the rate of decrease in ripple wavelength between the field and the laboratory. The effect of pore water salinity on the rate of bedform development cannot be quantified at present, but salinity is postulated herein to have had a smaller influence on the ripple wavelength than bed EPS content. The common presence of clay and EPS in many aqueous sedimentary environments implies that a re-assessment of the role of current ripples and their primary current lamination in predicting and reconstructing flow regimes is necessary, and that models that are valid for pure sand are an inappropriate descriptor for more complex mixed sediment. This study proposes that this re-assessment is necessary at all bed clay contents above 3%.

Allweddeiriau

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Dynodwyr Gwrthrych Digidol (DOIs)
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