стрес-режим

Personnel management is an activity that creates many new challenges for managers who implement it at the enterprise. Today, one of these challenges is personnel management under martial law. In the conditions of martial law, a person's mental state is especially vulnerable, which is accompanied by a change in behavior, a low level of information perception, and an aggressive attitude towards others. All these negative processes are formed under the influence of stress in which people are, in particular, employees in organizations under martial law.

Deformation processes in media with fractal structure have been studied. At present, research on the construction of mathematical methods and models of interconnected deformation-relaxation and heatmass transfer processes in environments with a fractal structure is at an early stage. There are a number of unsolved problems, in particular, the problem of correct and physically meaningful setting of initial and boundary conditions for nonlocal mathematical models of nonequilibrium processes in environments with fractal structure remains unsolved.

There are considered the technological ability to manage residual stress during machining by correcting the distorted structure of the treated surface det-lei new vector machines cutting speed for roughing and finishing operations processing.

The periodicity, dynamics and kinematics of unadequately studied Cenozoic activities in the Donets intraplate foldbelt (“the Donbass”) and in its neighbourhood were considered. It have been demonstrated that two independent orogenies divided by a tectonic pause in the Eocene-Oligocene took places there, the Laramic one (the terminal Maestrichtian – Paleocene) of an early Alpine tectonic epochs and conventiolly neotectonic one (Early Miocene – Quaternary) of a late Alpine epoch.

Purpose. The aim of the research is to estimate parameters for seismic dislocations, for example of strong earthquakes in the Turan platform and adjacent mountainous part of Western Tien-Shan, as well as identifying the relationship between the magnitudes and lengths of breaks for pleistoseist zones. Methodology.