HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS		QUICK SEARCH:   [advanced] Author: Keyword(s): Year:  Vol:  Page:

This Article Figures Only Full Text Free Full Text (PDF) Free Alert me when this article is cited Alert me if a correction is posted Services Similar articles in this journal Similar articles in Web of Science Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via Web of Science (1) Citing Articles via Google Scholar Google Scholar Articles by Shirazi, M. A. Articles by Johnson, C. B. Search for Related Content PubMed Articles by Shirazi, M. A. Articles by Johnson, C. B. GeoRef GeoRef Citation Agricola Articles by Shirazi, M. A. Articles by Johnson, C. B. Related Collections Structure and Properties Soil Analysis

DIVISION S-1-SOIL PHYSICS

Particle-Size Distributions

Comparing Texture Systems, Adding Rock, and Predicting Soil Properties

^a Western Ecology Division, NHEERL, U.S. Environmental Protection Agency, 200 SW 35th Street, Corvallis, OR 97333
^b Dept. of Crop and Soil Science, ALS 3017, Oregon State Univ., Corvallis, OR 97331-7306
^c OAO Corporation, 200 Sw 35th Street, Corvallis, OR 97333

Corresponding author (safa{at}mail.cor.epa.gov)

Conventional soil texture classification systems use different definitions of particle-size distributions (PSDs). For example, sand in the International Soil Science Society (ISSS) system equals the combined separate limits of coarse silt and sand in the USDA system. Because relationships between texture and other soil properties are affected by these differences, the ability to merge survey data in environmental studies is limited. Previous research calculated two PSD statistics, namely the geometric mean particle diameter (dg) and its standard deviation (g), which do not depend on separate limits. We expanded the development of the PSD statistics dg and g to compare the USDA and ISSS systems, develop relationships with soil properties, include rock fragments, and simplify the USDA texture classification to facilitate the use of soil survey data in environmental research. We found that (i) for equal clay and sand fractions, the texture of a soil sample as described by the USDA system has larger dg and g values than in ISSS; (ii) for equal clay and sand fractions, soil samples have larger values of cation-exchange capacity (CEC) in the ISSS than in the USDA system; (iii) small differences between some of the traditional 12 USDA classes are reflected in the dg and g values for samples containing rocks, thereby presenting a rationale for simplification; and (iv) with this rationale, the 12 USDA classes were aggregated into five classes.

Abbreviations: CEC, cation-exchange capacity • ISSS, International Soil Science Society • PSD, particle-size distribution • SC, soil characteristic • STATSGO, State Soil Geographic Data Base • WSPSD, whole soil particle-size distribution • USDA5, aggregated USDA classes • USDA12, original 12 USDA classes

This article has been cited by other articles:

				M. A. Shirazi, C. B. Johnson, J. M. Omernik, D. White, P. K. Haggerty, and G. E. Griffith Quantitative Soil Descriptions for Ecoregions of the United States J. Environ. Qual., March 1, 2003; 32(2): 550 - 561. [Abstract] [Full Text] [PDF]