2017
DOI: 10.21515/1999-1703-69-118-123
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Degradation change of the physical state of soils of Azov-Kuban plains

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“…-alluvial deposits with hydromorphous soils, with average density and porosity; -degraded loesslike, deluvial, tertiary marine deposits and saline soils with zonal and intrazonal soils that characterized by high density and low porosity [4,6].…”
Section: Resultsmentioning
confidence: 99%
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“…-alluvial deposits with hydromorphous soils, with average density and porosity; -degraded loesslike, deluvial, tertiary marine deposits and saline soils with zonal and intrazonal soils that characterized by high density and low porosity [4,6].…”
Section: Resultsmentioning
confidence: 99%
“…The hydromorphous soils belonging to alluvial types have formed in the existing natural conditions: alluvial bog (humus-gley, slimy-peat-gley, slimy-peat), alluvial meadow-bog and alluvial meadow saturated (stratified, normal, black) soils [4,5,9].…”
Section: Introductionmentioning
confidence: 99%
“…At present, it is not known how far the transformation of the properties of the former rainfed soils, now used in rice crop rotations, has gone. This raises questions of developing methods for restoring the properties and fertility of soils in rice fields [1,3].…”
Section: Introductionmentioning
confidence: 99%