Water-Physical Properties of Drained Peat Soils in the Forest-Steppe Zone of Northern Trans-Ural Region

Motorin, A. S.; Букин, А. В.

doi:10.26898/0370-8799-2017-5-1

Cited by 1 publication

(2 citation statements)

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“…The analysis and generalization of the results of field and laboratory studies were carried out using the works of K. p. Lundin [3], B. S. Maslov and others [4], A. S. Motorina, A.V. Bukin [5], and others.…”

Section: Resultsmentioning

confidence: 99%

“…The greatest destabilization of agricultural landscapes is caused by the static-destructive load [6]. In recent years, attempts have been made to generalize long-term results of observations of changes in agro-physical properties of drained hydromorphic soils in Western Siberia [5]. However, issues such as the development of these deposits, changes in their capillary and filtration properties, etc.are not covered.…”

Section: Resultsmentioning

confidence: 99%

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Monitoring of agrophysical properties of the active layer of drained long-frozen peat deposits in Western Siberia

Novokhatin

Osipova

2020

E3S Web Conf.

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In this study, the authors considered the dynamics of the main agrophysical properties of hydromorphic geosystems in Western Siberia. In the process of evolution, as well as in the conditions of technogenic impact, the soils of natural-territorial complexes, their properties are subject to significant changes. New hydromorphic geosystems are formed, the soils of which are characterized by changed agrophysical properties. Modern technologies for developing investment projects for soil reclamation of hydromorphic geosystems should be based on agrophysical characteristics of reclaimed soils, on the basis of which it is possible to create the necessary parameters of drainage systems and, as a result, provide optimal soil regimes for agricultural crops for a long period. The difficulty is that these soil characteristics are variable over time. Until recently, agrophysical characteristics of soils obtained in other regions of the country were used in the development of reclamation projects for hydromorphic soils in Western Siberia. The attempt to borrow them has led to the fact that large areas of drained soil have become completely unsuitable and to restore their project productivity, a number of agro-reclamation activities and the attraction of large financial resources are currently required. In this regard, there is a need for a comprehensive, long-term study of the main properties of hydromorphic soils used for agricultural purposes, and especially their changes over time under the influence of anthropogenic load.

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Section: Resultsmentioning

confidence: 99%

Section: Resultsmentioning

confidence: 99%