Effectiveness of Random Field Approach in Serviceability Limit State Analysis of Strip Foundation     

Winkelmann  Karol  Żyliński  Kamil  Korzec  Aleksandra  Górski  Jarosław 《Geotechnical and Geological Engineering》2022,40(9):4705-4720

Geotechnical and Geological Engineering - This work conducts a probabilistic inquiry on how the variability of the parameter defining soil deformability affects the settlement of the foundation...  相似文献   

Different Borders‐Different Cooperation? Transborder Cooperation in Poland          下载免费PDF全文

Sylwia Dołzbłasz  Andrzej Raczyk 《Geographical review》2015,105(3):360-376

The aim of this paper was to analyze the role of border and borderland type in transborder cooperation. To this end, 591 projects under six Interreg IIIA Programs in which Polish border regions participated from 2004 to 2006 were examined. These programs were compared to identify the various factors influencing projects in different border regions. Although research on cooperation usually focuses on a national scale, actual cooperation depends largely on regional and local conditions, which are the focus of this study. Despite a common legal and institutional framework, the Interreg projects were not all realized in the same way. Different local conditions had impacts on programs and implementation. Therefore, the effectiveness and achievement of transborder cooperation objectives depended on the modification of each program to specific regional conditions.  相似文献   

Snow Accumulation on a Small High‐Arctic Glacier Svenbreen: Variability and Topographic Controls          下载免费PDF全文

Jakub Małecki 《Geografiska Annaler: Series A, Physical Geography》2015,97(4):809-817

One of the main controls on the net mass change of land‐terminating Arctic glaciers is the magnitude and distribution of snow accumulation. In Dickson Land, region of Svalbard with the greatest distance to the sea, the issue has not been receiving much scientific attention for decades. In this paper, new snow accumulation data are presented from Svenbreen in Dickson Land from end‐of‐winter surveys. The measured winter balance was 0.42 ± 0.15 m w.e. in 2010, 0.50 ± 0.10 m w.e. in 2011 and 0.62 ± 0.10 cm w.e. in 2012. Snow depth and water equivalent have been analysed in the background of altitude, slope and aspect extracted from the digital elevation model of the glacier. On steep northern slopes (>15°) accumulation was the highest, whereas it was decreased on southern slopes with moderate inclination (9–12°). Elevation, which on many glaciers proved to be highly correlated with snow depth, explained only 17–34% of snow depth variability due to complex interplay between local climate and geometry of a small valley.  相似文献   

Phytoplankton response to the environmental and climatic variability in a temperate lake over the last 14,500 years in eastern Latvia     

N. Stivrins  P. Kołaczek  T. Reitalu  H. Seppä  S. Veski 《Journal of Paleolimnology》2015,54(1):103-119

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Eemian environmental changes recorded in lake deposits from Rzecino (NW Poland): Cladocera,isotopic and selected geochemical data     

Monika Niska  Joanna Mirosław-Grabowska 《Journal of Paleolimnology》2015,53(1):89-105

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Search of visually similar microscopic rock images     

Magdalena Ładniak  Mariusz Młynarczuk 《Computational Geosciences》2015,19(1):127-136

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Selected Spectral Characteristics of Turbulence over an Urbanized Area in the Centre of Łódź, Poland     

Krzysztof Fortuniak  Włodzimierz Pawlak 《Boundary-Layer Meteorology》2015,154(1):137-156

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Observed changes in SAT and GDD and the climatological suitability of the Poland-Germany-Czech Republic transboundary region for wine grapes cultivation     

Maciej Kryza  Mariusz Szymanowski  Marek Błaś  Krzysztof Migała  Małgorzata Werner  Mieczysław Sobik 《Theoretical and Applied Climatology》2015,122(1-2):207-218

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Frost peat mounds on Hermansenøya (Oscar II Land,NW Svalbard) – their genesis,age and terminology     

Tomasz Jaworski  Władysław Niewiarowski 《Boreas: An International Journal of Quaternary Research》2012,41(4):660-672

Here we present research on previously uninvestigated frost peat mounds occurring on a peat bog in the southern part of Hermansenøya, NW Svalbard. Detailed characteristics are given of the environmental conditions of the peat bog and of the morphological features and surface structure of the frost peat mounds, as well as an analysis of the internal structure of one mound. Three types of frost peat mounds have been distinguished: disc‐shaped mounds (low), mid‐sized mounds with gentle sides, and high mounds with steep sides. Radiocarbon dating of the peat within the frost peat mound performed for the first time on Svalbard and a detailed analysis of the deposits demonstrated that in the high mound (1.3 m) there is an ice‐peat core and peat cover without ice. There are three layers of peat of different ages separated by at least two hiatuses. A generalized history of the development of the peat bog from about 8 ka BP is established. The studied mound displays two development cycles unknown elsewhere. The older relict part of the peat mound was formed during a climatic cooling about 3.0–2.5 ka BP, while the younger part originated during the Little Ice Age (c. AD 1550–1850). Despite certain similarities of these mounds to some palsas, this term should not be applied to the mounds because they are smaller and their cores consist mostly of layers of massive injection ice, the presence of which indicates a pressurized system in their genesis.  相似文献   

Modelling of hydrogeochemical potential of three lake catchments in Polesie region (Eastern Poland)     

Jarosław Dawidek  Beata Ferencz  Wojciech Sobolewski 《水文研究》2013,27(12):1773-1780

Total dissolved solids (TDS) in lake and catchment water is a result of geological structure, as well as duration of rock and water contact and human activity. In this paper, a potential dissolved solids (PtDS) in three ??czna–W?odawa Lake catchments was determined using extraction and computer software (GIS and AquaChem). Human pressure on water quality was estimated as a difference of the TDS and a catchment hydrogeochemical potential (TPtDS, total potential dissolved solids). TPtDS coefficient included hydrogeological features of the aquifer, soil cover impact on infiltrated water quality, and sediments susceptibility to denudation. The main advantage of the model is a possibility of its employment for every catchment or other areas (e.g. administrative) on both microscale and mesoscale. The highest TPtDS occurred in the catchment, favoured with underground supply, which was located in the vicinity of the Cretaceous mesoregional unit (Che?m Hills). The lowest value was observed in the catchment built with organogenic sediments and coarse material. A seasonal constancy of TPtDS values proved a stability of the lake‐catchment systems under study. Copyright © 2012 John Wiley & Sons, Ltd.  相似文献