RHEOLOGICAL PROPERTIES OF SOILS OF DIFFERENT LAND USE IN THE SYKTYVKAR URBAN DISTRICT OF THE KOMI REPUBLIC

L. I. ARAKELOVA, A. B. UMAROVA, D. D. KHAIDAPOVA, M. A. BUTYLKINA, Z. S. EZHELEV, A. V. FEDOTOVA
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Abstract

The mechanical characteristics of soils of the same genesis and different land use of Syktyvkar are studied: agrod- ernovo-podzolic urban-stratified soil within the city, post-frost park soil, podzolic soil of suburban territory. The analysis of their relationship with the content of organic matter and granulometric composition is carried out. In agrodern-podzolic urban-stratified soil, the strength properties are largely due to the content of large granulometric fractions (> 0.25 mm), and in podzolic soil - the content of organic matter. Rows of soils were built according to the values of rheological parameters. The strength of structural bonds, estimated by the parameter of the initial modulus of elasticity, is greatest in podzolic soil, a wide range of linear viscoelastic state distinguishes the horizons of agroderno-podzolic urban-stratified soil. Both post-frost and podzolic soil have the same average values of the starting point of the viscous flow region.
科米共和国syktyvkar城区不同土地利用方式土壤的流变特性
研究了Syktyvkar地区同一成因和不同土地利用方式土壤的力学特性:城市内农业-土壤-白垩化城市分层土壤、霜冻后公园土壤、郊区白垩化土壤。分析了它们与有机质含量和粒度组成的关系。在农灰化城市层状土中,强度特性很大程度上取决于大颗粒组分的含量(>0.25 mm),灰化土中有机质含量。根据流变参数的值建立了土壤行。由初始弹性模量参数估计的结构键强度在灰化土中最大,宽范围的线性粘弹性状态区分了土壤-灰化土城市层状土的水平。霜后土与灰化土黏性流动区起点的平均值相同。
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