Szakadékmozgás

Szakadékmozgás is a Hungarian term that translates to "gap movement" or "crevice movement." It refers to a phenomenon observed in geological and engineering contexts, particularly concerning the movement or deformation within discontinuities in rock masses or soil structures. This can manifest as the widening or closing of existing cracks, fissures, or faults, or the initiation of new fracture planes.

The study of szakadékmozgás is crucial in understanding the stability of slopes, tunnels, foundations, and other civil engineering projects. Factors influencing szakadékmozgás include applied stress, the presence of water or other fluids, changes in temperature, and the material properties of the surrounding rock or soil. For instance, increased pore water pressure within a fissure can reduce the effective stress, leading to crack opening and potential failure. Conversely, tectonic stresses can cause fault blocks to slide past each other, a process directly related to szakadékmozgás.

Monitoring szakadékmozgás often involves in-situ measurements using extensometers, displacement transducers, or geodetic techniques. Mathematical models and numerical simulations are also employed to predict and analyze the behavior of these geological discontinuities under various conditions. Understanding and quantifying szakadékmozgás helps in assessing risks, designing appropriate mitigation measures, and ensuring the long-term safety and performance of infrastructure.