SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
QUICK SEARCH:   [advanced]


     

This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via ISI Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Filgueira, R. R.
Right arrow Articles by Fournier, L. L.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Filgueira, R. R.
Right arrow Articles by Fournier, L. L.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Filgueira, R. R.
Right arrow Articles by Fournier, L. L.
Related Collections
Right arrow Soil Physics
Published in Soil Sci. Soc. Am. J. 67:1703-1706 (2003).
© 2003 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA

DIVISION S-1—NOTES

TIME-MASS SCALING IN SOIL TEXTURE ANALYSIS

Roberto R. Filgueiraa,b, Yakov A. Pachepsky*,c and Lidia L. Fourniera

a Area Física Aplicada, Facultad de Ciencias Agrarias y Forestales, National University of La Plata, CC 31, 1900 La Plata, Argentina
b CONICET, Rivadavia 1917, 1033 Buenos Aires, Argentina
c Animal Waste Pathogen Lab., USDA-ARS-BA-ANRI-AWPL, Bldg. 173, Rm. 203, BARC-EAST, Powder Mill Road, Beltsville, MD 20705

* Corresponding author (ypachepsky{at}anri.barc.usda.gov).

Popular methods of textural analysis employ the relationship among time, the travel distances, and the radii of particles subject to sedimentation in a viscous liquid. The purpose of this note is to present and test an explicit relationship between time and soil suspension density in the course of the hydrometer analysis procedure applied to particles with the fractal mass-size distribution. The relationship between the logarithms of mass of particles remaining in the solution and of the observation time is linear with the slope equal to -(3 - D)/2 where D is the fragmentation fractal dimension. This relationship was tested with samples of Typic Argiudoll and 24 soils from Imperial Valley, CA, and gave good approximation of hydrometer data on sedimentation of silt fraction 2 to 50 m. Monitoring soil mass in the solution presents a way of testing the applicability of fractal fragmentation model to particle-size distributions (PSDs) and estimating the fragmentation fractal dimension.

Abbreviations: PSD, particle-size distribution






HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education		 Journal of
Environmental Quality
Copyright © 2003 by the Soil Science Society of America.