Methods for determining the actual water levels of the buzz
DOI:
https://doi.org/10.32523/y94nev64Keywords:
soil evaporation, filtration coefficient, fertility, irrigated land, air exchange zone, soil densityAbstract
The shortage of water in irrigated lands and the processes of water movement in cultivated fields is examined based on specific research. Methods for identifying factors influencing the rise of water levels in these fields are presented using empirical data. Statistical analysis was performed on data obtained from groundwater level monitoring. It was established that the average rate of groundwater rise directly depends on the depth of its occurrence. The dynamics of water levels are significantly affected by the moisture coefficient, soil density and porosity, filtration properties, and infiltration volume. Depending on the soil structure – specifically its thickness, density, and salinity – the mineralization level of groundwater, seasonal evaporation rates, capillary rise height, and potential threshold levels were determined. These research results are based on experimental data from agricultural fields, where the rise in groundwater levels plays a crucial role in land reclamation. The study shows that the hydrogeological justification of field investigations encompasses irrigation system regimes, reclamation planning, and the integrated use of water resources. These measures are based on hydrodynamic and hydrochemical forecasts of groundwater regimes and the water-salt balance of the aeration zone. Furthermore, the findings highlight the importance of systematic monitoring to ensure the sustainable productivity of irrigated lands. This scientifically grounded analysis optimizes reclamation measures and reduces the risk of secondary soil salinization. Ultimately, the study confirms that rational water resource management is a critical factor for regional environmental safety.
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