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• W1989729135 abstract "The particle-size distribution (PSD) is one of the most important soil characteristics used in soil science. Numerous studies on the laser diffraction method (LDM) suggest that the PSD obtained by the LDM differs from that obtained by sieve sedimentation methods (SSMs). The aim of this study was to determine the potential causes of errors in PSD measurements using the LDM, especially in the context of conflicting reports regarding the over/underestimation of finer fractions in comparison with SSMs. Mixtures of two fractions of glass beads (15–50 and 1000–1180 μm) were measured with two differently constructed dispersion units (Hydro MU and Hydro G) and using two continuous phases (H2O, density 0.998 Mg m−3, and CsCl, density 1.582 Mg m−3). The error in the measurements using the LDM (the most extreme overestimation of the coarse fraction was approximately 275%) was attributed to insufficient homogenization of the soil suspension in the dispersion units. The degree of over- or underestimation depended on the ratio between the contents of each fraction. It is difficult to indicate clearly which dispersion unit construction was better in these investigations. The Hydro MU appeared to be slightly more suitable when the content of the given fractions features a wider range in relation to the content of the other fractions. However, Hydro G may be better suited to soils with relatively fewer sand fraction particles. The knowledge of the causes of the errors should help to minimize errors in PSD measurements by the LDM and lead to better interpretations of the results." @default.
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• W1989729135 date "2014-12-16" @default.
• W1989729135 modified "2023-10-18" @default.
• W1989729135 title "The Reasons for Incorrect Measurements of the Mass Fraction Ratios of Fine and Coarse Material by Laser Diffraction" @default.
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• W1989729135 doi "https://doi.org/10.2136/sssaj2013.07.0286n" @default.
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