Skip to main content
SpringerLink
Log in

The logarithmic profile in wind erosion: An algebraic solution

  • Published:
Boundary-Layer Meteorology Aims and scope Submit manuscript

Abstract

This paper presents a simple algebraic approach to the interpretation of wind erosion data that allows for density variation close to the surface due to the presence of large amounts of saltating material. The effect explains nonlinearities in the logarithmic velocity profile near the surface and extends the profile into the saltating layer.

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

Access this article

Log in via an institution

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Similar content being viewed by others

References

  • Bagnold, R. A.: 1941, ‘The Physics of Blown Sand and Desert Dunes’, Methuen, London.

    Google Scholar 

  • Chepil, W. S.: 1945, ‘Dynamics of Wind Erosion: 1. Nature of Movement of Soil by Wind’, Soil Science 60, 305–320.

    Google Scholar 

  • Gerety, K. M. and Slingerland, R.: 1983. ‘Nature of the Saltating Population in Wind tunnel Experiments with Heterogeneous Size — Density Sands’, in M. E. Brookfield and T. S. Ahlbrandt (eds.), Developments in Sedimentology, 38, Eolian Sediments and Processes, Elsevier, Amsterdam.

    Google Scholar 

  • Greeley R., Williams, S. H., and Marshall, J. R.: 1983, Velocities of Windborne Particles in Saltation: Preliminary Laboratory and Field Measurements, Developments in Sedimentology, 38, Ibid.

  • Nickling, W. G.: 1978, ‘Eolian Sediment Transport During Dust Storms: Slims River Valley, Yukon Territory’, Can. J. Earth Sci. 15, 1069–1084.

    Google Scholar 

  • Owen, P. R.: 1964, ‘Saltation of Uniform Grains in Air’, J. Fluid Mech. 20, 225–242.

    Google Scholar 

  • Scott, W. D. and Summers, K. J.: 1984, ‘Saltation and Associated Dust Generation: Mathematical Model’, submitted to the J. Applied Math. Modelling.

  • Sutton, O. C.: 1977, ‘Micrometeorology: A Study of Physical Processes in the Lowest Layer of the Earth's Atmosphere’, Kriegen, NY.

    Google Scholar 

  • Zingg, A. W.: 1953, ‘Wind Tunnel Studies of the Movement of Sedimentary Material’, Iowa University, Studies in Engineering, Bulletin No. 34, 111–135.

    Google Scholar 

Download references

Author information

Authors and Affiliations

  1. School of Environmental and Life Sciences, Murdoch University, Murdoch, Western Australia, Australia

    W. D. Scott

  2. Division of Resource Management, Department of Agriculture, South Perth, Western Australia, Australia

    D. J. Carter

Authors
  1. W. D. Scott
    View author publications

    You can also search for this author in PubMed Google Scholar

  2. D. J. Carter
    View author publications

    You can also search for this author in PubMed Google Scholar

Rights and permissions

Reprints and permissions

About this article

Cite this article

Scott, W.D., Carter, D.J. The logarithmic profile in wind erosion: An algebraic solution. Boundary-Layer Meteorol 34, 303–310 (1986). https://doi.org/10.1007/BF00122384

Download citation

  • Revised:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF00122384

Keywords

Search

Navigation