Relations between local, nonlocal, discrete and continuous models of bioturbation
By Filip Meysman, B. Boudreau, Jack J. Middelburg. 2003
164 citations recorded by the source corpus.
Subfields: Civil and Structural Engineering, Environmental Engineering, Water Science and Technology
View Paper: https://www.semanticscholar.org/paper/400192a8602f81136e084221eea0e0d64582af7c
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In Civil and Structural Engineering
In Environmental Engineering
In Water Science and Technology
Citations in the corpus
- A comparison of sediment reworking rates by the surface deposit-feeding bivalve Abra ovata during summertime and wintertime, with a comparison between two models of sediment reworking (2007, unknown): “Assuming that particles are mixed infinitely fast over infinitely small distances, bioturbation can be represented as a diffusive process (Boudreau, 1986; Meysman et al., 2003), and the governing conservation equation for the luminophore concentration C thus becomes”
- Reviews and syntheses: to the bottom of carbon processing at the seafloor (2017, background): “Particle transport is not only due to steady particle deposition but also due to sediment reworking by animals (bioturbation, Boudreau, 1997; Aller, 1994, 2013; Rice, 1986; Meysman et al., 2003, 2006, 2010).”
- Quantification of sediment reworking rates in bioturbation research: a review (2010, methodology): “This striking contradiction between modelling theory and field practice has been referred to as the ‘biodiffusion paradox’ (Meysman et al. 2003).”
- Effects of population density on the sediment mixing induced by the gallery-diffusor Hediste (Nereis) diversicolor O.F. Muller, 1776 (2006, background): “The biotransport coefficient (r) represents a non-local mixing pattern associated with a biologically induced transfer of particles from one place to another in a discontinuous pattern (i.e. a non-continuous transport; Boudreau, 1986; Meysman et al., 2003).”
- Sediment reworking by marine benthic species from the Gullmar Fjord (Western Sweden): Importance of faunal biovolume (2007, background): “The biotransport coefficient (r) represents a non-local mixing pattern associated with a biologically induced transfer of particles from one place to another in a discontinuous pattern (i.e. a non-continuous transport; Boudreau, 1986; Meysman et al., 2003).”