Autor: Szczucinski, P. - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Czynniki i bariery rozwoju a peryferyjność województwa lubuskiego
Factors and barriers of development versur peripherality of Lubuskie Voivodeship
Autorzy:: Szczucinski, P.
Powiązania:: https://bibliotekanauki.pl/articles/1811806.pdf
Data publikacji:: 2017
Wydawca:: Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Wydawnictwo Szkoły Głównej Gospodarstwa Wiejskiego w Warszawie
Tematy:: województwo lubuskie
region peryferyjny
rozwój społeczno-ekonomiczny
system osadniczy
infrastruktura
analiza statystyczna
Lubuskie Voivodeship
peripheral region
social and economic development
settlement system
infrastructure
statistical analysis
Opis:: Do podstawowych cech współczesnej gospodarki należą zróżnicowanie przestrzenne i jej zmienność w czasie. Obserwuje się, że jedne regiony i kraje rozwijają się szybciej, inne wolniej. Ramy teoretyczne badania ich rozwoju określa koncepcja peryferyjności regionalnej. Nawiązując do tej koncepcji, w artykule poddano ocenie możliwości rozwoju województwa lubuskiego. W badaniach empirycznych uwzględniono 39 wskaźników diagnostycznych opisujących następujące grupy uwarunkowań: położenie geograficzne i system osadniczy, gospodarkę i jej strukturę, czynniki demograficzno-społeczne, infrastrukturę regionu. Wykorzystując dane za 2014 rok, przeprowadzono analizę rozwoju województwa na tle gospodarki polskiej z uwzględnieniem wybranych aspektów rozwoju obszarów wiejskich. Wyniki przeprowadzonych badań wskazują, że w wielu przypadkach województwo lubuskie charakteryzują procesy typowe dla regionów peryferyjnych.
The basic features of the contemporary economy include spatial diversity and its variation in time. It can be observed that some regions and countries develop faster and others slower. The theoretical framework of research into their development is specified by the concept of regional peripherality. In line with this concept, the possibilities for development of Lubuskie Voivodeship were assessed in the article. There were 39 diagnostic indicators considered in empirical research, describing the following groups of determinants: geographical location and settlement system, economy and its structure, demographical and social factors as well as infrastructure of the region. With the use of the data for 2014, the analysis of the voivodeship development was carried out in relation to Polish economy. Selected aspects of development of rural areas were considered. The results of the research indicate that Lubuskie Voivodeship is in many cases characterized by processes typical for peripheral regions.
Źródło:: Roczniki Naukowe Ekonomii Rolnictwa i Rozwoju Obszarów Wiejskich; 2017, 104, 1; 72-82
2353-4362
Pojawia się w:: Roczniki Naukowe Ekonomii Rolnictwa i Rozwoju Obszarów Wiejskich
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Sedimentary evidence of extreme storm surge or tsunami events in the southern Baltic Sea (Rogowo area, NW Poland)
Autorzy:: Piotrowski, A.
Szczuciński, W.
Sydor, P.
Kotrys, B.
Rzodkiewicz, M.
Krzymińska, J.
Powiązania:: https://bibliotekanauki.pl/articles/2060594.pdf
Data publikacji:: 2017
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: tsunami deposits
storm surge deposits
grain size analysis
geochemistry
radiocarbon dating
Baltic Sea
Opis:: The Baltic Sea is not typically considered as an area affected by tsunamis. However, during the Late Pleistocene and Holocene several tsunami events have been interpreted from the sedimentary record, mainly in Sweden and Estonia. Furthermore, on the southern coast of the Baltic Sea, there are historical accounts of catastrophical marine floodings called “der Seebär” (“the Sea Bear”). Their descriptions reveal many features typical for tsunami, but their genesis remained unknown and sedimentary evidence for such events has not been found. Here we provide evidence of sandy event layers from the area of Rogowo, NW Poland – the area of historical catastrophic storms as well as “der Seebär” events. The study area is a low-lying coastal plain with an average elevation of –0.5 to +0.5 m a.s.l., protected from the open sea by beach and coastal dune systems up to 5 m high. Sedimentological, micropalaeontological and geochemical analyses along with AMS 14C dating were applied to sedimentary successions seen in 5 major trenches and 198 sediment cores up to 1.5 m long. Two sandy layers were identified in the peat deposits that developed on the plain during the last ~2000 years. They reveal a number of typical features of tsunami deposits (significant lateral extent and thickness, rip-up clasts, chemical and micropalaeontological evidence of marine origin), however, 14C dating along with the historical accounts revealed that the major layer, extending at least 1.2 km from the modern coasts, was probably deposited by arguably the largest storm surge during the last 2000 years, which took place in 1497 AD. These storm deposits were likely formed during inundation of the low-lying coastal plain after major breaching of coastal dunes resulting in tsunami – like flow pattern and thus similar sedimentological effects. A discontinuous sand layer of younger age (18th century) and sharing similar properties to the previous one may be related to “der Seebär” event or another storm surge. The study revealed that the southern Baltic Sea coast may be affected by much greater coastal flooding than known from more recent accounts and observations. Thus, the presented geological record should be taken as an example of a worst-case scenario in coastal zone risk assessment from natural hazards. These events left sedimentary deposits that resemble tsunami deposits. It is likely that, in similar settings where storm surges cause unidirectional inundation of a coastal plain, it may not be possible to establish whether the resulting deposits were laid down from storms or tsunamis.
Źródło:: Geological Quarterly; 2017, 61, 4; 973--986
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki