Possibilities of using rheological parameters as physical indicators of soil structural changes
https://doi.org/10.19047/0136-1694-2020-103-108-148
Abstract
The rheological parameters of structured soddy-podzolic soils (Albic Glossic Retisols (Lomic, Cutanic)) and chernozems (Haplic Chernozems (Loamic, Pachic)) in their natural state and involved in agricultural use were studied by the oscillation amplitude sweep test. Shear resistance parameters of the studied soils (shear stress at the end of the linear viscoelasticity range – LVE-range tL, shear stress tF at the Crossover point and maximum shear stress tmax) were more informative and indicated pronounced differences between soil genetic horizons in contrast to viscoelasticity parameters (deformation γL at the end of the LVE-range and the integral zone Z) when comparing natural and arable soils. The agricultural land use resulted in decreased organic carbon content and, as a consequence, reduced viscoelasticity and shear resistance of the soils. At the same time, the higher bulk density of arable horizons and the redistribution of fine soil particles (physical clay) could explain maximal values of the rheological parameters in the upper arable horizons and their slight differentiation with depth. Further development in the application of the proposed and studied rheological parameters can give insight into the nature and strength evaluation of interparticle bonds, the soil processes under the impact of agricultural machinery, and can also be integrated into the system of physical indicators of soil structural changes.
About the Authors
V. V. Klyueva
Federal Research Centre “V.V. Dokuchaev Soil Science Institute”
Russian Federation
7 Bld. 2 Pyzhevskiy per., Moscow 119017
Russian Federation
7 Bld. 2 Pyzhevskiy per., Moscow 119017
D. D. Khaydapova
Lomonosov Moscow State University
Russian Federation
12 Bld. 1 Leninskie Gori, Moscow 119234
Russian Federation
12 Bld. 1 Leninskie Gori, Moscow 119234
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96. Reynolds D., Bowman B.T., Drury C.F., Tan C.S., Lu X., Indicators of good soil physical quality : density and storage parameters, Geoderma, 2002, Vol. 110, pp. 131–146.
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101. Ye C., Guo Z., Cai C.,Wang J., Deng J., Effect of water content, bulk density, and aggregate size on mechanical characteristics of Aquults soil blocks and aggregates from subtropical China, Journal of Soils and Sediments, 2016, Vol. 17, No. 1, pp. 210–219.
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103. Zhang H.Q., Hartge K.H., Cohesion in unsaturated sandy soils and the influence of organic matter, Soil Technology, 1990, No. 3, pp. 311–326.
104. Shukla M.K., Lal R., Ebinger M., Determining soil quality indicators by factor analysis, Soil Tillage Research, 2006, Vol. 87, pp. 194–204.
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106. Six J., Bossuyt H., Degryze S., Denef K.A., History of research on the link between (micro) aggregates, soil biota, and soil organic matter dynamics, Soil Tillage Research, 2004, Vol. 79, pp. 7–31.
107. Stoppe N., Horn R., Microstructural strength of tidal soils – A rheometric approach to develop pedotransfer functions, Journal of Hydrology and Hydromechanics, 2018, Vol. 66, No. 1, pp. 87–96.
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110. Zhang H.Q., Hartge K.H., Cohesion in unsaturated sandy soils and the influence of organic matter, Soil Technology, 1990, No. 3, pp. 311–326.
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Klyueva V.V., Khaydapova D.D. Possibilities of using rheological parameters as physical indicators of soil structural changes. Dokuchaev Soil Bulletin. 2020;(103):108-148. (In Russ.) https://doi.org/10.19047/0136-1694-2020-103-108-148
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