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This article in SSSAJ

  1. Vol. 60 No. 1, p. 72-76
     
    Received: Dec 27, 1994
    Published: Jan, 1996


    * Corresponding author(s): barak@calshp.cals.wisc.edu
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doi:10.2136/sssaj1996.03615995006000010013x

Self-Similitude and Fractal Dimension of Sand Grains

  1. Phillip Barak ,
  2. Kevin McSweeney and
  3. Cathy A. Seybold
  1. Dep. of Soil Science, Univ. of Wisconsin, 1525 Observatory Dr., Madison, WI 53706-1299
    Virginia State Univ., P.O. Box 9081, Petersburg, VA 23806

Abstract

Abstract

Fractal theory postulates that geological materials possess a noninteger, fractal dimension describing length-surface-volume relations and particle-size distribution. We examined sand grains, composed largely of quartz, from several horizons of Wisconsin soils derived from glacial outwash for fractal dimension using image analysis of reflected light micrographs with NIH Image software. No evidence was found to support other than a Euclidean, i.e., regular dimension, relating the geometric properties of: (i) measured particle perimeter as a function of magnification or (ii) particle area and perimeter. In addition, particle-size distributions were better fit by lognormal distribution than by a fractal fragmentation dimension. Fractal theory would not appear to provide a useful description for these soil materials.

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