This article is a further contribution to the discourse of ethnic ‘diffusion’ in European countries. The debate started on the pages of the Baltic Region journal by three authors — Yu. N. Gladky, I. Yu. Gladky, and K. Yu. Eidemiller [4]. We assume that Europe has been a major centre of attraction for immigrants in recent decades and a site for the rapid emergence of ethnic communities. Unlike Muslim immigration, a product of the Arab Spring and often a measure of last resort, Chinese immigration is a result of a certain convergence between the ideologies of the host countries, committed to multiculturalism, and the country of origin pursuing a ‘go global’ policy. We chose the EU countries as a ‘demonstration site’ and the Chinese diaspora as the object of research. Our aim is to describe the process of migration from China and the formation of a Chinese diaspora in European countries. We analyse the timeline and the scope of Chinese immigration, qualitative changes in the composition of immigrants, factors affecting the choice of the country of entry, and the quantitative parameters and settlement patterns of today’s Chinese diaspora in the region. We suggest grouping the EU Countries by the number and ‘age’ of their Chinese diasporas. We consider ethnic ‘diffusion’ as part of the ‘European project’ within Beijing’s global strategy.
During the operation of engineering structures made of natural stone, for industrial and civil purposes, an important parameter in monitoring their technical condition is the assessment of their reliability and safety under the influence of various external influences. In this case, high-quality monitoring of the stress–strain state of natural stone structures, its physical, mechanical and filtration properties, as well as internal structural features is necessary to study the possibility of replacing individual elements of objects that have lost their original characteristics. To assess the state of geomaterials, this article proposes using a complex of introscopic methods, including infrared radiometry and laser-ultrasound structuroscopy. An important aspect is the calculation based on the Green–Christoffel equation of the velocity of a quasi-longitudinal wave in limestone consisting of densely packed, chaotically oriented calcite grains with a small quartz content. For the first time, using laser-ultrasonic structuroscopy and standard methods for determining open porosity, both total and closed porosity were determined. This allowed us to find the values of specific heat capacities of dry and water-saturated samples. The obtained values are used to find the ratio of changes in the temperature of dry and water-saturated samples at the same stress values. The results obtained demonstrate the need to take into account changes in the intensity of thermal radiation of limestone with different moisture content under conditions of uniaxial compression, when identifying changes in the stress state of elements of stone structures in real conditions.
In relation to extraction of coal seams at significant depths, the issue of protection of safety equipment against pressure exerted by rock becomes very important. In many surveys of the effects of pressure exerted by rock it was demonstrated that the intensity of stress around the mine works increases the greater the depth of the mine works. However, surveys of technological mine works have shown that the level of deformation of the mine bracing varies in various types of rock at identical depths and no precise rule was established between the increase in pressure exerted by rock and the increasing depth of the mine works.
It is shown that one of the express-methods for studying the internal structure and phase composition of geomaterial samples is broadband acoustic spectroscopy with laser sources of ultrasound. Theoretical assessment of time profiles and spectrums of opto-acoustic signals are presented. Numerical modelling of the spectrums and time profiles of ultrasound signals generated in opto-acoustic generators made of a different material is performed. The influence of diffraction and damping in rocks on the above characteristics is studied. The amplitude spectrum and time profiles of ultrasonic pulses transmitted through samples of marble of various thicknesses in which the most part of the characteristic grain sizes lies in the range of 500 μm - 1 mm are constructed. It has been established that, according to the amplitude spectrum of the original signal and the transmitted through the sample signal, it is possible to restore the characteristic dimensions of the grains.
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