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The Ways to Develop Soil Textural Classification for Laser Diffraction Method

  • SOIL PHYSICS
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Abstract

The existing classifications of soil texture are based on the sedimentation data. The aim of this article is to consider the ways to develop soil textural classification on the basis of particle-size distribution (PSD) data obtained by the laser diffraction method. A detailed comparison of PSD data obtained by the classical pipette method and the method of laser diffractometry has been performed. We have shown the reproducibility of the laser diffraction method and the effect of the oxidation stage on the soil texture class. This study is based on eight genetic soil types (overall, 32 full-profile soil pits) forming a zonal soil sequence from Podzols (Subpolar Urals) to ferrallitic soil (southwest Oceania) and differing in their mineralogical compositions, textures, and elementary pedogenetic processes. The direct use of the Kachinskii and USDA classifications with the data of the laser diffraction method leads to mistakes in determining the soil texture class in 43 and 65% of cases, respectively. The increasing complexity of recalculation, introduction of new variables, and accounting for interlaboratory errors allow us to determine correctly the texture class according to the Kachinskii and USDA classifications in no more than 70 and 72% of soil samples, respectively. The most simple and effective approach to solve the classification problem for the laser diffraction method is to calibrate existing classifications directly on the basis of data on soil samples, for which the texture class was determined by the field method.

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ACKNOWLEDGMENTS

The authors are grateful to D.V. Dubovik, A.Yu. Aidiev, and V.M. Lazarev for the opportunity to work on the territory of the Kursk Federal Agrarian Center and the Kursk Research Institute of Agricultural Production; to A.A. Vlasov and O.V. Ryzhkov for the opportunity to work on the territory of the V.V. Alekhin Central Chernozemic State Reserve; to A.F. Stulin for the opportunity to work on the territory of the Voronezh Department of the All-Russia Research Institute of Corn. The authors are especially grateful to Dr. Nikolay Khitrov for valuable comments and advice on improving the paper.

Funding

This study supported by the Russian Foundation for Basic Research, project nos. 18-34-00825 and 18-316-00139. It was performed using the equipment of the Collective Use Center “Functions and Properties of Soils and Soil Cover” of the Dokuchaev Soil Science Institute (laser diffractometer Microtrac Bluewave) and the Skolkovo Institute of Science and Technology (the pipetting apparatus Eijkelkamp, Netherlands, and vortex Reax Top Heidolph, Germany).

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Authors and Affiliations

  1. Dokuchaev Soil Science Institute, per. Pyzhevskii 7, 119017, Moscow, Russia

    A. V. Yudina, D. S. Fomin, I. A. Valdes-Korovkin, N. A. Churilin, I. V. Kovda & E. Yu. Milanovskiy

  2. Lomonosov Moscow State University, 119991, Moscow, Leninskie gory, Russia

    I. A. Valdes-Korovkin, M. S. Aleksandrova, Yu. A. Golovleva & E. Yu. Milanovskiy

  3. Izrael Institute of Global Climate and Ecology, 107258, Moscow, Russia

    M. S. Aleksandrova

  4. Institute for Biological Problems of the Cryolithozone, Siberian Branch of the Russian Academy of Sciences, 677007, Yakutsk, Russia

    N. V. Phillipov

  5. Institute of Biology, Komi Science Center, Ural Branch of the Russian Academy of Science, 167982, Syktyvkar, Komi Republic, Russia

    A. A. Dymov

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  1. A. V. Yudina
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  2. D. S. Fomin
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  4. N. A. Churilin
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  6. Yu. A. Golovleva
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Correspondence to A. V. Yudina.

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Yudina, A.V., Fomin, D.S., Valdes-Korovkin, I.A. et al. The Ways to Develop Soil Textural Classification for Laser Diffraction Method. Eurasian Soil Sc. 53, 1579–1595 (2020). https://doi.org/10.1134/S1064229320110149

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