Search results for "MOA"
showing 3 items of 103 documents
Preparation, crystal structure at 298 and 90 K and phase transition in (C2H5NH3) 2[SbBr5] studied by the single crystal X-Ray diffraction method
2004
The reaction of antimony(III) oxide with ethylamine, in molar ratios from 1:1 to 1:10, in concentrated hydrobromic acid leads to the formation of one product – bis(ethylammonium) pentabromoantimonate(III). The structure of (C2H5NH3)2[SbBr5] was determined at 298 and 90 K, below and above the phase transition that occurs at about 158.5 K. The orthorhombic system was found in both phases, space groups Cmca and Pbca at 298 and 90 K, respectively. At both temperatures the structure consists of [SbBr6] 3− octahedra connected via cis bromine atoms forming one-dimensional zig-zag [{SbBr5}2−]n chains. The ethylammonium cations fill the space between polyanionic chains. The organic and inorganic sub…
Poczucie jakości życia osób z kadry kierowniczej w świetle Modelu Osobowościowo-Aksjologicznego MOA
2016
The paper attempte to present issues coming from the raanagement and personality psychology, including their implications for company management practices and for their impact on spocialists well-being and a ąuality of life. The research, based on Ryan and Deci concept, cuncerns the psychological needs, adaptation (Rotter) and hierarchical valucs (Rokeach) of spocialists. It was assumed that the sense of the quality of life would reveal asignificant relationahip with personality-relatcd and axiological dimensions among spocialists. It was hypothesized that a positive correlation between independent porsonolity-related variables distinguished in the personality and axiologica) MOA model for …
First Evidence of Contourite Drifts in the North-Western Sicilian Active Continental Margin (Southern Tyrrhenian Sea)
2021
We present the results of an integrated geomorphological and seismo-stratigraphic study based on high resolution marine data acquired in the north-western Sicilian continental margin. We document for the first time five contourite drifts (marked as EM1a, EM2b, EM2, EM3a, and EM3b), located in the continental slope at depths between ca. 400 and 1500 m. EM1a,b have been interpreted as elongated mounded drifts. EM1a,b are ca. 3 km long, 1.3 km wide, and have a maximum thickness of 36 m in their center that thins northwards, while EM1b is smaller with a thickness up to 24 m. They are internally characterized by mounded seismic packages dominated by continuous and parallel reflectors. EM2 is loc…