Adequacy of laser diffraction for soil particle size analysis
Sedimentation has been a standard methodology for particle size analysis since the early 1900s. In recent years laser diffraction is beginning to replace sedimentation as the prefered technique in some industries, such as marine sediment analysis. However, for the particle size analysis of soils, wh...
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description | Sedimentation has been a standard methodology for particle size analysis since the early 1900s. In recent years laser diffraction is beginning to replace sedimentation as the prefered technique in some industries, such as marine sediment analysis. However, for the particle size analysis of soils, which have a diverse range of both particle size and shape, laser diffraction still requires evaluation of its reliability. In this study, the sedimentation based sieve plummet balance method and the laser diffraction method were used to measure the particle size distribution of 22 soil samples representing four contrasting Australian Soil Orders. Initially, a precise wet riffling methodology was developed capable of obtaining representative samples within the recommended obscuration range for laser diffraction. It was found that repeatable results were obtained even if measurements were made at the extreme ends of the manufacturer's recommended obscuration range. Results from statistical analysis suggested that the use of sample pretreatment to remove soil organic carbon (and possible traces of calcium-carbonate content) made minor differences to the laser diffraction particle size distributions compared to no pretreatment. These differences were found to be marginally statistically significant in the Podosol topsoil and Vertosol subsoil. There are well known reasons why sedimentation methods may be considered to 'overestimate' plate-like clay particles, while laser diffraction will 'underestimate' the proportion of clay particles. In this study we used Lin's concordance correlation coefficient to determine the equivalence of laser diffraction and sieve plummet balance results. The results suggested that the laser diffraction equivalent thresholds corresponding to the sieve plummet balance cumulative particle sizes of < 2 μm, < 20 μm, and < 200 μm, were < 9 μm, < 26 μm, < 275 μm respectively. The many advantages of laser diffraction for soil particle size analysis, and the empirical results of this study, suggest that deployment of laser diffraction as a standard test procedure can provide reliable results, provided consistent sample preparation is used. |
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In recent years laser diffraction is beginning to replace sedimentation as the prefered technique in some industries, such as marine sediment analysis. However, for the particle size analysis of soils, which have a diverse range of both particle size and shape, laser diffraction still requires evaluation of its reliability. In this study, the sedimentation based sieve plummet balance method and the laser diffraction method were used to measure the particle size distribution of 22 soil samples representing four contrasting Australian Soil Orders. Initially, a precise wet riffling methodology was developed capable of obtaining representative samples within the recommended obscuration range for laser diffraction. It was found that repeatable results were obtained even if measurements were made at the extreme ends of the manufacturer's recommended obscuration range. Results from statistical analysis suggested that the use of sample pretreatment to remove soil organic carbon (and possible traces of calcium-carbonate content) made minor differences to the laser diffraction particle size distributions compared to no pretreatment. These differences were found to be marginally statistically significant in the Podosol topsoil and Vertosol subsoil. There are well known reasons why sedimentation methods may be considered to 'overestimate' plate-like clay particles, while laser diffraction will 'underestimate' the proportion of clay particles. In this study we used Lin's concordance correlation coefficient to determine the equivalence of laser diffraction and sieve plummet balance results. The results suggested that the laser diffraction equivalent thresholds corresponding to the sieve plummet balance cumulative particle sizes of < 2 μm, < 20 μm, and < 200 μm, were < 9 μm, < 26 μm, < 275 μm respectively. The many advantages of laser diffraction for soil particle size analysis, and the empirical results of this study, suggest that deployment of laser diffraction as a standard test procedure can provide reliable results, provided consistent sample preparation is used.]]></description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0176510</identifier><identifier>PMID: 28472043</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Agriculture ; Australia ; Biometrics ; Calcium ; Calcium carbonate ; Carbonates ; Clay ; Correlation coefficient ; Correlation coefficients ; Diffraction ; Earth Sciences ; Ecology and Environmental Sciences ; Engineering and Technology ; Equivalence ; Extreme values ; Laser diffraction ; Lasers ; Marine sediments ; Measurement techniques ; Methods ; Models, Theoretical ; Organic carbon ; Organic soils ; Particle shape ; Particle Size ; Particle size distribution ; Physical Sciences ; Physiological aspects ; Pretreatment ; R&D ; Research & development ; Research and Analysis Methods ; Sample preparation ; Samples ; Science ; Sediment analysis ; Sedimentation ; Sediments ; Size distribution ; Soil ; Soil analysis ; Soil sciences ; Soil testing ; Soils ; Statistical analysis ; Statistical methods ; Studies ; Subsoils ; Topsoil</subject><ispartof>PloS one, 2017-05, Vol.12 (5), p.e0176510-e0176510</ispartof><rights>COPYRIGHT 2017 Public Library of Science</rights><rights>2017 Fisher et al. This is an open access article distributed under the terms of the Creative Commons Attribution License: http://creativecommons.org/licenses/by/4.0/ (the “License”), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. 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In recent years laser diffraction is beginning to replace sedimentation as the prefered technique in some industries, such as marine sediment analysis. However, for the particle size analysis of soils, which have a diverse range of both particle size and shape, laser diffraction still requires evaluation of its reliability. In this study, the sedimentation based sieve plummet balance method and the laser diffraction method were used to measure the particle size distribution of 22 soil samples representing four contrasting Australian Soil Orders. Initially, a precise wet riffling methodology was developed capable of obtaining representative samples within the recommended obscuration range for laser diffraction. It was found that repeatable results were obtained even if measurements were made at the extreme ends of the manufacturer's recommended obscuration range. Results from statistical analysis suggested that the use of sample pretreatment to remove soil organic carbon (and possible traces of calcium-carbonate content) made minor differences to the laser diffraction particle size distributions compared to no pretreatment. These differences were found to be marginally statistically significant in the Podosol topsoil and Vertosol subsoil. There are well known reasons why sedimentation methods may be considered to 'overestimate' plate-like clay particles, while laser diffraction will 'underestimate' the proportion of clay particles. In this study we used Lin's concordance correlation coefficient to determine the equivalence of laser diffraction and sieve plummet balance results. The results suggested that the laser diffraction equivalent thresholds corresponding to the sieve plummet balance cumulative particle sizes of < 2 μm, < 20 μm, and < 200 μm, were < 9 μm, < 26 μm, < 275 μm respectively. The many advantages of laser diffraction for soil particle size analysis, and the empirical results of this study, suggest that deployment of laser diffraction as a standard test procedure can provide reliable results, provided consistent sample preparation is used.]]></description><subject>Agriculture</subject><subject>Australia</subject><subject>Biometrics</subject><subject>Calcium</subject><subject>Calcium carbonate</subject><subject>Carbonates</subject><subject>Clay</subject><subject>Correlation coefficient</subject><subject>Correlation coefficients</subject><subject>Diffraction</subject><subject>Earth Sciences</subject><subject>Ecology and Environmental Sciences</subject><subject>Engineering and Technology</subject><subject>Equivalence</subject><subject>Extreme values</subject><subject>Laser diffraction</subject><subject>Lasers</subject><subject>Marine sediments</subject><subject>Measurement techniques</subject><subject>Methods</subject><subject>Models, Theoretical</subject><subject>Organic carbon</subject><subject>Organic soils</subject><subject>Particle shape</subject><subject>Particle Size</subject><subject>Particle size distribution</subject><subject>Physical Sciences</subject><subject>Physiological aspects</subject><subject>Pretreatment</subject><subject>R&D</subject><subject>Research & development</subject><subject>Research and Analysis Methods</subject><subject>Sample preparation</subject><subject>Samples</subject><subject>Science</subject><subject>Sediment analysis</subject><subject>Sedimentation</subject><subject>Sediments</subject><subject>Size distribution</subject><subject>Soil</subject><subject>Soil analysis</subject><subject>Soil sciences</subject><subject>Soil testing</subject><subject>Soils</subject><subject>Statistical analysis</subject><subject>Statistical 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of laser diffraction for soil particle size analysis</title><author>Fisher, Peter ; Aumann, Colin ; Chia, Kohleth ; O'Halloran, Nick ; Chandra, Subhash</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a715t-cf06e2de83d81b41aebda063cc28e851b4547900fd5a6e97aedab181ebf91ea73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Agriculture</topic><topic>Australia</topic><topic>Biometrics</topic><topic>Calcium</topic><topic>Calcium carbonate</topic><topic>Carbonates</topic><topic>Clay</topic><topic>Correlation coefficient</topic><topic>Correlation coefficients</topic><topic>Diffraction</topic><topic>Earth Sciences</topic><topic>Ecology and Environmental Sciences</topic><topic>Engineering and Technology</topic><topic>Equivalence</topic><topic>Extreme values</topic><topic>Laser diffraction</topic><topic>Lasers</topic><topic>Marine sediments</topic><topic>Measurement techniques</topic><topic>Methods</topic><topic>Models, Theoretical</topic><topic>Organic carbon</topic><topic>Organic soils</topic><topic>Particle shape</topic><topic>Particle Size</topic><topic>Particle size distribution</topic><topic>Physical Sciences</topic><topic>Physiological aspects</topic><topic>Pretreatment</topic><topic>R&D</topic><topic>Research & development</topic><topic>Research and Analysis Methods</topic><topic>Sample preparation</topic><topic>Samples</topic><topic>Science</topic><topic>Sediment analysis</topic><topic>Sedimentation</topic><topic>Sediments</topic><topic>Size distribution</topic><topic>Soil</topic><topic>Soil analysis</topic><topic>Soil sciences</topic><topic>Soil testing</topic><topic>Soils</topic><topic>Statistical analysis</topic><topic>Statistical methods</topic><topic>Studies</topic><topic>Subsoils</topic><topic>Topsoil</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fisher, 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Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fisher, Peter</au><au>Aumann, Colin</au><au>Chia, Kohleth</au><au>O'Halloran, Nick</au><au>Chandra, Subhash</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Adequacy of laser diffraction for soil particle size analysis</atitle><jtitle>PloS one</jtitle><addtitle>PLoS One</addtitle><date>2017-05-04</date><risdate>2017</risdate><volume>12</volume><issue>5</issue><spage>e0176510</spage><epage>e0176510</epage><pages>e0176510-e0176510</pages><issn>1932-6203</issn><eissn>1932-6203</eissn><abstract><![CDATA[Sedimentation has been a standard methodology for particle size analysis since the early 1900s. In recent years laser diffraction is beginning to replace sedimentation as the prefered technique in some industries, such as marine sediment analysis. However, for the particle size analysis of soils, which have a diverse range of both particle size and shape, laser diffraction still requires evaluation of its reliability. In this study, the sedimentation based sieve plummet balance method and the laser diffraction method were used to measure the particle size distribution of 22 soil samples representing four contrasting Australian Soil Orders. Initially, a precise wet riffling methodology was developed capable of obtaining representative samples within the recommended obscuration range for laser diffraction. It was found that repeatable results were obtained even if measurements were made at the extreme ends of the manufacturer's recommended obscuration range. Results from statistical analysis suggested that the use of sample pretreatment to remove soil organic carbon (and possible traces of calcium-carbonate content) made minor differences to the laser diffraction particle size distributions compared to no pretreatment. These differences were found to be marginally statistically significant in the Podosol topsoil and Vertosol subsoil. There are well known reasons why sedimentation methods may be considered to 'overestimate' plate-like clay particles, while laser diffraction will 'underestimate' the proportion of clay particles. In this study we used Lin's concordance correlation coefficient to determine the equivalence of laser diffraction and sieve plummet balance results. The results suggested that the laser diffraction equivalent thresholds corresponding to the sieve plummet balance cumulative particle sizes of < 2 μm, < 20 μm, and < 200 μm, were < 9 μm, < 26 μm, < 275 μm respectively. The many advantages of laser diffraction for soil particle size analysis, and the empirical results of this study, suggest that deployment of laser diffraction as a standard test procedure can provide reliable results, provided consistent sample preparation is used.]]></abstract><cop>United States</cop><pub>Public Library of Science</pub><pmid>28472043</pmid><doi>10.1371/journal.pone.0176510</doi><tpages>e0176510</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Agriculture Australia Biometrics Calcium Calcium carbonate Carbonates Clay Correlation coefficient Correlation coefficients Diffraction Earth Sciences Ecology and Environmental Sciences Engineering and Technology Equivalence Extreme values Laser diffraction Lasers Marine sediments Measurement techniques Methods Models, Theoretical Organic carbon Organic soils Particle shape Particle Size Particle size distribution Physical Sciences Physiological aspects Pretreatment R&D Research & development Research and Analysis Methods Sample preparation Samples Science Sediment analysis Sedimentation Sediments Size distribution Soil Soil analysis Soil sciences Soil testing Soils Statistical analysis Statistical methods Studies Subsoils Topsoil |
title | Adequacy of laser diffraction for soil particle size analysis |
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