Infiltration experiments: Realization and evaluation

Červeňanská, Michaela; Janík, Adam; Baroková, Dana

doi:10.1556/606.2018.13.1.12

Cited by 3 publications

(2 citation statements)

References 12 publications

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“…The retention capacity and potential of water in the soil affects the water regime of the landscape (Tall and Gomboš, 2013). Retention soil capacity and soil water availability for the crops is different in various soil types (Červeňanská et al, 2016;Červeňanská et al, 2018;Šoltész and Baroková, 2011;Constantin, 2016). Soil types are defined by texture.…”

Section: Introductionmentioning

confidence: 99%

Influence of soil type on statistical characteristics and graphical results interpretation of the water storage distribution monitoring along the vertical of the soil profile

Gomboš¹,

Tall²,

Kandra³

et al. 2021

AHS

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The results of authors of submitted article are based on knowledge that soil retention capacity and soil water availability for plants is different in various soil types. Soil types are defined by texture. It is expected that different retention capacity of soil and different availability of soil water for plants is reflected in changes of moisture regime in space and time. Moisture regime monitoring results captures these changes. Changes can be statistically and graphically analysed and interpreted. The results gained from three localities of East Slovakian Lowland (ESL) of the year 2015 extreme drought period were selected for presentation. Examined localities differs by texture compound. Localities are representing the heaviest clay soils, lighter clay-loam-silty soils and the lightest loam soils. Soil volume humidity was monitored into the depth of 1.00 m by layers of 0.10 m. All samples were taken in the same day in examined localities. Descriptive statistics method was used for data processing. Graphical representation is processed in form of chronoizophlets, line and column graphs. Different monitoring results of volume moisture and water storage in different soil types are quantified in the article. Winter water refill of soil profile, soil water storage, vertical scatter of soil profile moisture volume, temporal and spatial moisture regime changes and availability of soil water for plant cover was analysed within this quantification. The results of analysis and interpretation of moisture regime in different soil environments are necessary for water management of the country and for the design of adaptive measures for the periods of soil drought.

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Section: Introductionmentioning

confidence: 99%

Influence of soil type on statistical characteristics and graphical results interpretation of the water storage distribution monitoring along the vertical of the soil profile

Gomboš¹,

Tall²,

Kandra³

et al. 2021

AHS

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“…After World War II, a network of drainage channels and Pumping Stations (PS) was built by Slovak Water Management Enterprise (SWME) on both sides of the Ondava River. Landscaping was carried out in order to develop agriculture [1][2][3].…”

Section: Introductionmentioning

confidence: 99%

Measures for flood discharge transformation on the Ondava River

Mydla

Šoltész

Orfánus

2021

Pollack

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The contribution is dealing with run-off conditions on the lower part of the Ondava River as the capacity of the river bed is insufficient at high flow rates. The reason for the proposed research was the flood situations when protection dikes were breached. For mathematical modeling of flood wave progress, the HEC-RAS software has been applied coupling 1D and 2D modeling procedures. Results of the mathematical model of the surface water level regime in the Ondava River were compared with measured values and afterwards it was used to design further flood protection measures utilizing the existing drainage channel system and pumping stations, as well.

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Evaluation of Water Content in Soils of Žitný Ostrov from the Point of View of Its Exploitation for Biosphere

Rehák¹,

Stradiot²,

Abaffy³

2021

IOP Conf. Ser.: Earth Environ. Sci.

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The lithospheric zone between the soil surface and the first ground water horizon, respectively the ground water table, has a character of three-phase system. It consists of solid phase having fine to rough disperse granularity. This creates a structure of porous environment with characters that can be physically determined. The water occurs in pores in different forms of state and its bond with solid phase. Its energetic bond is clearly quantified by means of moisture retention curve. The gas phase fills pores with the water up to the value of the full porosity, i.e. it fills the part of pores that is not saturated with water. Therefore, this lithospheric zone is called the soil aeration zone. The volume of water occurring in the soil aeration zone corresponds to the concentration of water in the framework of hydrological cycle components. This water serves as the water resource for the vegetation cover. The data used for calculation were particular soil types in the area, depth of ground water table, hydrolimits (wilting point, point of decreased availability, field water capacity) and aeration zone thickness. The water content in the soil aeration zone between hydrolimits field water capacity (FWC) and wilting point (WP) is the critical interval of water content for vegetation cover in a given locality. Water from this interval is available for the vegetation cover. This water has no properties of free water, and plants have to have a developed root system and such suction pressure, that is able to overcome the bond between water and soil. Calculated results were verified with the help of monitored water content. Both calculated and measured values of soil water content in the aeration zone show that the water content is affected by appurtenant soil type. The human activity in a landscape directly affects the dynamics of this water resource, either from quantitative or qualitative viewpoint. This affect is demonstrated by changes of the ground water regime, i.e. changes of ground water table and amplitude of its fluctuation. The paper brings results of water content evaluation in the soil aeration zone in the Žitný ostrov area.

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Infiltration experiments: Realization and evaluation

Cited by 3 publications

References 12 publications

Influence of soil type on statistical characteristics and graphical results interpretation of the water storage distribution monitoring along the vertical of the soil profile

Influence of soil type on statistical characteristics and graphical results interpretation of the water storage distribution monitoring along the vertical of the soil profile

Measures for flood discharge transformation on the Ondava River

Evaluation of Water Content in Soils of Žitný Ostrov from the Point of View of Its Exploitation for Biosphere

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