Simplified Method for Soil Particle‐Size Determination to Accompany Soil‐Quality Analyses

Soil textural analysis is a key component of any minimum data set used for assessing soil quality and sustainability of agricultural‐management practices. However, conventional methods of soil textural analysis can be costly and time‐consuming. The objective of this study was to develop a rapid and...

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Bibliographic Details
Published in:	Soil Science Society of America journal Vol. 65; no. 3; pp. 849 - 852
Main Authors:	Kettler, T.A., Doran, J.W., Gilbert, T.L.
Format:	Journal Article Conference Proceeding
Language:	English
Published:	Madison Soil Science Society 01-05-2001 Soil Science Society of America American Society of Agronomy
Subjects:	Agronomy. Soil science and plant productions Biological and medical sciences Earth sciences Earth, ocean, space Exact sciences and technology Experiments Fundamental and applied biological sciences. Psychology Measuring instruments Methods Physical properties Physics, chemistry, biochemistry and biology of agricultural and forest soils Quality standards Sediments Soil quality Soil science Soils Structure, texture, density, mechanical behavior. Heat and gas exchanges Surficial geology United States North America America United States > US Grain size analysis Simplification Agricultural soils particulate organic matter Property of soil Soil quality Experimental study Physical properties Texture Soils Rapid technique Pedology Analysis method Soil science Method study
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Summary:	Soil textural analysis is a key component of any minimum data set used for assessing soil quality and sustainability of agricultural‐management practices. However, conventional methods of soil textural analysis can be costly and time‐consuming. The objective of this study was to develop a rapid and simple method for evaluating soil particle‐size distribution, which could be employed as a tool for initial soil‐quality assessment. The method uses a combination of sieving and sedimentation steps and is designed to be used in conjunction with analysis of particulate organic matter (POM), or as a stand‐alone textural analysis. Soils of varied texture and organic‐matter content were collected from six sites in the Great Plains. Their sand, silt, and clay contents were determined using the proposed methods and standard hydrometer and pipette techniques. Averaged across all soils, absolute differences between the proposed and standard pipette analyses were <2% for sand, silt, and clay. Relative differences were 6, −1, and −4% for sand, silt, and clay, respectively. Coefficients of variation within soil samples averaged <5% for sand, silt, and clay fractions. Regression analysis between proposed and standard pipette methods produced coefficient of determination (r2) values of 0.99, 0.98, and 0.93 for sand, silt, and clay, respectively, and 0.98 across all particle‐size ranges. The method provides an inexpensive and reliable estimate of soil texture, useful in soil‐quality assessment.
Bibliography:	Journal Series no. 13277 of the Agric. Res. Div., Univ. of Nebraska, Lincoln, NE. ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 ObjectType-Article-1 ObjectType-Feature-2
ISSN:	0361-5995 1435-0661
DOI:	10.2136/sssaj2001.653849x