talajvízmozgásoktól
Talajvízmozgásoktól refers to the various movements and dynamics of groundwater within the earth's subsurface. This phenomenon is crucial for understanding water availability, geological processes, and environmental contamination. Groundwater moves primarily due to differences in hydraulic head, which is the sum of the elevation head and the pressure head. Water flows from areas of higher hydraulic head to areas of lower hydraulic head, following the path of least resistance through porous geological materials like sand and gravel, or through fractures in solid rock.
The rate of groundwater movement is influenced by the permeability of the soil or rock. Highly permeable
Groundwater movement can occur in both horizontal and vertical directions. Vertical movement can be downward, contributing