2015
DOI: 10.1134/s106422931506006x
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Contact angles of wetting and water stability of soil structure

Abstract: From the soddy podzolic soils and typical chernozems of different texture and land use, dry 3-1 mm aggregates were isolated and sieved in water. As a result, water stable aggregates and water unstable particles composing dry 3-1 mm aggregates were obtained. These preparations were ground, and contact angles of wet ting were determined by the static sessile drop method. The angles varied from 11° to 85°. In most cases, the values of the angles for the water stable aggregates significantly exceeded those for the… Show more

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Cited by 17 publications
(7 citation statements)
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“…The drying-wetting cycle was always followed by the pooling and separation of the soil aggregate into various size classes (Kholodov, 2013). A wetting method is an approach used in detecting the resistance capacity of a macroaggregate structure to water strength (Kholodov et al, 2015). Under the wet conditions, the aggregate was formed and distributed into five aggregate size classes (Figure 2).…”
Section: Discussionmentioning
confidence: 99%
“…The drying-wetting cycle was always followed by the pooling and separation of the soil aggregate into various size classes (Kholodov, 2013). A wetting method is an approach used in detecting the resistance capacity of a macroaggregate structure to water strength (Kholodov et al, 2015). Under the wet conditions, the aggregate was formed and distributed into five aggregate size classes (Figure 2).…”
Section: Discussionmentioning
confidence: 99%
“…Wetting and dewetting are fundamental processes in many applications, including inkjet printing 1 , coating 2 , lubrication 3,4 , and soil science 5,6 . These applications usually involve dynamic conditions, e.g., drop impingement on substrates 7 , requiring further consideration of the rate effects among multiple phases, i.e., gas, liquid and solid.…”
Section: Introductionmentioning
confidence: 99%
“…Adjacent to the Kund, there is a dug well, in which the water level is 5.59 meters below to the ground level having a water column thickness of 8.26. According to Capillary Height Formula/Jurin's law (Kholodov et al, 2015)…”
Section: Hydrogeological Methodsmentioning
confidence: 99%