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    Wyświetlanie 1-2 z 2
    Tytuł:
    Rola terenów nadbrzeżnych i parków kieszonkowych w kształtowaniu środowiska mieszkaniowego na przykładzie osiedla Nordhavnen w Kopenhadze
    Role of waterfront areas and pocket parks in shaping of housing environment on the example of the Nordhavnen Housing Estate in Copenhagen
    Autorzy:
    Poklewski-Koziełł, D.
    Powiązania:
    https://bibliotekanauki.pl/articles/345364.pdf
    Data publikacji:
    2018
    Wydawca:
    Politechnika Krakowska im. Tadeusza Kościuszki. Wydział Architektury. Katedra Kształtowania Środowiska Mieszkaniowego
    Tematy:
    tereny nadbrzeżne
    parki kieszonkowe
    strefa buforowa
    zrównoważona mobilność
    dostępność piesza
    waterfronts
    pocket park
    edge zone
    sustainable mobility
    walkability
    Opis:
    Celem artykułu jest przedstawienie będącego obecnie w trakcie realizacji, jednego z największych projektów rozbudowy miasta jaki ma miejsce w Skandynawii, znanego pod nazwą Nordhavnen. Artykuł przybliży podstawowe założenia ideowe i strategie projektowe jakie przyświecały autorom wyłonionej w drodze międzynarodowego konkursu pracy, oraz odpowiadające im praktyczne narzędzia urbanistyczne. Artykuł przyjrzy się jak w praktyce wygląda realizacje założeń koncepcyjnych ze szczególnym uwzględnieniem terenów zielonych - parków kieszonkowych i tzw. stref buforowych - oraz wodnych - terenów nadbrzeżnych. Przeanalizowane zostaną podstawowe dane powierzchniowe w kontekście ich wpływu i roli w kreowaniu wyżej wymienionych przestrzeni.
    The goal of the article is the presentation of one of the largest city expansion projects that are currently being executed in Scandinavia, known as Nordhavnen in Copenhagen. The article will familiarise readers with the basic conceptual assumptions and design strategies that were adopted by the authors of its design, as well as the practical urban planning tools that correspond to them. The article will also explore how the implementation of the conceptual assumptions looks like in practice, with a specific emphasis on green areas - pocket parks and so-called edge zones - and those close to water - waterfronts. Basic data concerning various types of surface area in the context of their impact and role in creating the aforementioned spaces were analysed.
    Źródło:
    Środowisko Mieszkaniowe; 2018, 24; 74-81
    1731-2442
    2543-8700
    Pojawia się w:
    Środowisko Mieszkaniowe
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Warunki geologiczno-inżynierskie na obszarze strefy krawędziowej Wzgórz Warszewskich
    Autorzy:
    Seul, Cyprian
    Powiązania:
    https://bibliotekanauki.pl/articles/763303.pdf
    Data publikacji:
    2015
    Wydawca:
    Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
    Tematy:
    Szczecińskie Hills
    edge zone
    morainic plateau
    geodynamic process
    septaria clay
    geotechnical parameters
    building failures
    Wzniesienia Szczecińskie
    strefa krawędziowa
    procesy geodynamiczne
    iły septariowe
    parametry geotechniczne
    awarie budowlane
    Opis:
    Development trends of the modern city imply a reduction in the number of inhabitants in its centre, and thus the construction of dormitory suburbs on the outskirts of the city. One of the potential areas for the development of Szczecin is its northern part, i.e. the so-called Warszewo Hills. This area has both latitudinal and meridional extents of about 8 km, and is characterized by complicated engineering-geological conditions. It lies at altitudes ranging from the sea level (Odra River) to 130.9 m a.s.l. (Wielecka Góra), and has highly varied relief. Its landscape consists of hills and flat plateaux, which are cut by deep small valleys, some of them with streams (e.g. the Warszewiec stream). Geological structure is characterized by the occurrence of glacitectonically disturbed moraine deposits mixed with the Tertiary sands and clays. Taking into account geodynamic processes and their intensity, the wide edge zone of the Warszewo Hills can be divided into three main parts: plateau with the upper edge of slope (area of precipitation infiltration), slope, which is cut by small erosion valleys in places (area of surface water and groundwater flow), slope foot (area of water flow and accumulation of slope deposits). One of the most important tasks of the design-investment process is to take action in such a way as to interfere as little as possible in the natural environment and at the same time to achieve the intended purpose. Predominant occurrence of cohesive deposits in the described area (Oligocene scaled clay mixed with moraine disturbed material) results in a high susceptibility of ground to moisture changes. Strength parameters of stable slopes built of clays considerably decrease under the influence of increasing moisture and thixotropy phenomenon. Then landslide processes are triggered, as well as very slow, hardly noticeable in a short time, soil creep.The complicated arrangement of deposit layers results in spatial variability of groundwater level, and proper design of building foundation is difficult, even in the case of a small, detached house. Too much interference in the landform features (through macro-levelling, construction of streets and routes in the area with steep slopes), the decrease of water retention and increase of surface runoff contribute to an intensification of some geodynamic processes.
    Development trends of the modern city imply a reduction in the number of inhabitants in its centre, and thus the construction of dormitory suburbs on the outskirts of the city. One of the potential areas for the development ofSzczecinis its northern part, i.e. the so-called Warszewo Hills. This area has both latitudinal and meridional extents of about 8 km, and is characterized by complicated engineering-geological conditions. It lies at altitudes ranging from the sea level (OdraRiver) to 130.9 m a.s.l. (Wielecka Góra), and has very varied relief. Its landscape consists of hills and flat plateaux, which are cut by deep small valleys, some of them with streams (e.g. the Warszewiec stream). Geological structure is characterized by the occurrence of glacitectonically disturbed moraine deposits mixed with the Tertiary sands and clays. Taking into account geodynamic processes and their intensity, the wide edge zone of the Warszewo Hills can be divided into three main parts: plateau with the upper edge of slope (area of precipitation infiltration), slope, which is cut by small erosion valleys in places (area of surface water and groundwater flow), slope foot (area of water flow and accumulation of slope deposits). One of the most important tasks of the design-investment process is to take action in such a way as to interfere as little as possible in the natural environment and at the same time to achieve the intended purpose. Predominant occurrence of cohesive deposits in the described area (Oligocene scaled clay mixed with moraine disturbed material) results in a high susceptibility of ground to moisture changes. Strength parameters of stable slopes built of clays considerably decrease under the influence of increasing moisture and thixotropy phenomenon. Then landslide processes are triggered, as well as very slow, hardly noticeable in a short time, soil creep. The complicated arrangement of deposit layers results in spatial variability of groundwater level, and proper design of building foundation is difficult, even in the case of a small, detached house. Too much interference in the landform features (through macro-levelling, construction of streets and routes in the area with steep slopes), the decrease of water retention and increase of surface runoff contribute to an intensification of some geodynamic processes.   
    Źródło:
    Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia; 2015, 70, 2
    0137-1983
    Pojawia się w:
    Annales Universitatis Mariae Curie-Sklodowska, sectio B – Geographia, Geologia, Mineralogia et Petrographia
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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