This work is a preliminary pilot research aiming at defining the role of the Piechcin Diving Centre in the development of specialised tourism. Particular attention was paid to the various elements defining the quality of the services offered. The key aspects and reasons for which respondents visit the centre were also determined. Both the customer’s expectations of the organiser of this form of recreation were analysed, and research was made to help understand whether the time the customers spends at the centre facilitates a positive decision regarding the participation in diving trips in larger bodies of water, with particular consideration of the Baltic Sea. Different forms of cooperation between the centre and regional authorities in terms of promoting the region were also reviewed.
i Inżynierii Środowiska, Katedra Ekoinżynierii i Fizykochemii Środowiska STRESZCZENIA / ABSTRACTSThis paper presents an analysis of thermal and oxygen conditions of the Charzykowskie Lake in the years 2014-2016 in the period from May to August. The measurements were carried out once a month, at points representing three different basins in the lake, and the temperatures and oxygen content dissolved in the water were recorded every 1m from the surface to the bottom at the deepest point of each basin. The changes in temperatures and content of dissolved oxygen were analysed in each of the representative measurement points for particular parts of the lake. It has been shown that the deficit of oxygen dissolved in the bottom layers of the water starts occurring by the beginning of the summer stagnation period, whereas at its peak (August) the anaerobic zone includes hypolimnion and part of the metalimnion. The hypothesis that the thickness of the thermal layers varies within the lake basin was confirmed. It was also shown that the oxygen content curve at representative points, in all years of research, evolves to the form of a clinograde at the peak of summer stagnation, where the concentration of dissolved oxygen decreases with the depth. Keywords: water stratification, oxygen deficit, Lake Charzykowskie.W pracy przedstawiono analizę warunków termiczno-tlenowych Jeziora Charzykowskiego w latach 2014-2016 w okresie od maja do sierpnia. Pomiary prowadzono raz w miesiącu, w punktach reprezentujących trzy odmienne baseny w misie badanego jeziora. Wyniki pomiaru temperatury i zawartości tlenu rozpuszczonego w wodzie rejestrowano co 1m od powierzchni do dna w najgłębszym miejscu każdego basenu. Poddano analizie zmiany temperatury i zawartości tlenu rozpuszczonego w każdym z reprezentatywnych punktów pomiarowych dla poszczególnych plos jeziora. Wykazano, że deficyt tlenu rozpuszczonego w wodzie warstw naddennych występuje już na początku okresu stagnacji letniej, a w jego szczycie (sierpień) strefa beztlenowa obejmuje hypolimnion i część metalimnionu. Potwierdzono hipotezę zakładającą, że miąższość warstw termicznych jest zróżnicowana w obrębie misy jeziornej. Wykazano także, że krzywa zawartości tlenu w punktach reprezentatywnych, we wszystkich latach w których prowadzono badania, ewoluuje do postaci klinogrady w szczycie stagnacji letniej, gdzie stężenie tlenu rozpuszczonego maleje wraz z głębokością. Słowa kluczowe: stratyfikacja wód, deficyt tlenu, Jezioro Charzykowskie. В работе представлен анализ кислородно-термических условий озера Хажиковского в 2014-2016 гг в период с мая по август. Замеры проводились один раз в месяц в точках, представляющих три различных бассейна в ложе изучаемого озера. Результаты замера температуры и содержания кислорода, растворенного в воде, регистрировались каждый метр от поверхности воды до дна в самых глубоких местах бассейна. Проведен анализ изменений температуры и содержания растворенного кислорода в каждой из представленных точек замера для отдельных участков озера. Выявлено, что дефиц...
This paper characterises the concept of monolayer mobile gas adsorption on a homogeneous surface of a solid. The theoretical basis of the phenomenological variant of the description of adsorption equilibrium in the system in question are discussed. The essential features of the solutions to date are discussed, and the effect of the free surface of adsorbent on the form of the final adsorption equation is stressed.An alternative concept of the free surface based on the modified two-dimensional analogue of Reiss, Frisch and Lebowitz equations is also presented. The obtained adsorption equation was tested for critical parameters of two-dimensional condensation of the adsorption layer, and then used to describe the experimental data available in literature. The verification carried out confirmed the correctness and usefulness of the proposed concept.
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