Cohesive Sediment Entrainment Rate Functions: Expanding and Quantifying their Parameterizations

Abstract

The erosion characteristics of cohesive sediments in nearshore environments depend on a number of biogeochemical processes. It is standard practice to experimentally determine the entrainment rate of sediment into the water column as a function of the applied bottom shear stress and fit this data to a power law function. This work addresses the inherent problems of fitting entrainment rate data to parameterized functions, focusing on the non-uniqueness of the power law approach and its sensitivity to errors in the data. An approach for incorporating the effects of bioturbation and consolidation, thus expanding the parameter space of the entrainment function, into the standard power law formulation is examined with regard to its physical sensitivity and its expanded predictive capability of biogeochemical changes in cohesive sediments. Finally, power law and exponential entrainment functions are compared in order to illustrate the physical sensitivity of a particular entrainment parameterization.

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Document Details

Document Type
Technical Report
Publication Date
Apr 03, 2008
Accession Number
ADA479718

Entities

People

  • Mark Cobb
  • Timothy R. Keen

Organizations

  • United States Naval Research Laboratory

Tags

Communities of Interest

  • C4I
  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Boundary Layer
  • Chemical Properties
  • Climate Change
  • Data Sets
  • Environment
  • Exponential Functions
  • Layers
  • Military Research
  • New York
  • Physical Properties
  • Physics
  • Predictive Modeling
  • Seabed
  • Sedimentation
  • Shear Stresses
  • Standards
  • Two Dimensional

Readers

  • Calculus or Mathematical Analysis
  • Coastal and Marine Engineering/Sediment Transport/Hydraulic Engineering
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers

Technology Areas

  • Space
  • Space - Hall-Effect Thruster