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    Wyświetlanie 1-16 z 16
    Tytuł:
    Landslide susceptibility assessment: a case study from Beskid Niski Mts., Carpathians, Poland
    Autorzy:
    Mrozek, T.
    Poli, S.
    Steracchini, S.
    Zabuski, L.
    Powiązania:
    https://bibliotekanauki.pl/articles/1186178.pdf
    Data publikacji:
    2004
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    mapa podatności osuwiskowej
    Beskid Niski
    landslide susceptibility map
    Beskid Niski Mts.
    Opis:
    This study involves the integration of multiple thematic datasets for landslide susceptibility assessment through spatial prediction models. The proposed methodology has been applied in the Bystrzanka-Biczyska area (Beskid Niski Mts., Carpathians Mts., Poland), characterised by a very high density of landslides. The susceptibility assessment has been based on an indirect bivariate statistical analysis ("Weights of Evidence" modelling technique, Bonham-Carter et al., 1989) performed in order to predict the occurrence of an event (landslide) where well-known evidences (predictor variables) are available. According to the relative importance of each evidence, a landslide susceptibility map has been produced. Observing final prediction results, it is concluded that the susceptibility map gives useful information both on present instability of the area and its possible future evolution in agreement with the morphological evolution of the area.
    Źródło:
    Polish Geological Institute Special Papers; 2004, 15; 13-18
    1507-9791
    Pojawia się w:
    Polish Geological Institute Special Papers
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Landslide susceptibility mapping in the Beskid Niski Mts., Western Carpathians (Dukla commune, Poland)
    Autorzy:
    Bronowski, B.
    Chybiorz, R.
    Jura, D.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059958.pdf
    Data publikacji:
    2016
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    landslide
    susceptibility map
    index of entropy
    SOPO
    Beskid Niski Mts.
    Opis:
    Landslides are one of the most prominent processes degrading the Beskidy Mts. slopes. Susceptibility assessment is based on the detailed mapping of the Dukla commune (235 km2) at the scale 1: 10,000 in frames of the project Landslide Counteracting System. The terrain affected by landslides is 19.59 km2, which is 8.34% of the researched area. The largest number of landslides can be found in the Beskid Dukielski Mts. area, where nearly 78% of all landslide areas are concentrated. Analysis of landslide-causing factors was performed using the index of entropy method. The following five factors were considered: lithology, slope inclination, slope aspect, distance to faults, and distance to drainage. The most important role in the development of mass movements in the study area is played by slope inclination (0.0079) and lithology of siliciclastic flysch (0.0066). The method applied also contributed to devising a landslide susceptibility map of considerable accuracy at 90.5%. The analyses of the landslide factors have proven that understanding of geology and landforms is not only of cognitive significance, but adds to practical applications in spatial management. The studies confirmed usefulness of large-scale mapping of landslides and applying statistical methods and GIS techniques in the spatial analysis of landform transformations. The obtained landslide susceptibility map can be a basis for assessing landslide risk. High and very high landslide susceptibility classes cover nearly 50% of the study area.
    Źródło:
    Geological Quarterly; 2016, 60, 3; 586--596
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Dendrochronological study of the Sawicki landslide activity in the Beskid Niski Mts (Polish Flysch Carpathians)
    Autorzy:
    Kiszka, K.
    Powiązania:
    https://bibliotekanauki.pl/articles/294653.pdf
    Data publikacji:
    2016
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    dendrogeomorphology
    mass movement
    landslide activity
    Sawicki landslide
    eccentricity of tree rings
    Beskid Niski Mountains
    Opis:
    The article presents the results of the dendrogeomorphological study of the activity of the Sawicki landslide, located in the Beskid Niski Mts (Polish Flysch Carpathians). The study was conducted within two study sites in the lower part of the landslide. The landslide movements were dated using the dendrogeomorphological method, basing on the eccentricity indicators calculated for the two coniferous species, i.e. Scots pine (Pinus sylvestris) and silver fir (Abies alba). It was found landslide activity in years: 1899, 1901, 1905, 1910, 1913–1914, 1920–1921, 1929–1931, 1935, 1937, 1945, 1977, 1979, 1981, 1984–1985, 1990, 1992–1993, 1997, 2003–2004, 2006, 2010–2012. The greatest activity was characterized for the northern part of the study site B and the south-western slopes of the Szklarki stream valley (study site A). Studies have shown only a partial dependence between precipitation and landslide episodes. The data were confronted with the results of dendrogeomorphological studies, conducted in the northern and central parts of the landslide. The results demonstrate the significant complexity of mass movements within large-area landslide.
    Źródło:
    Landform Analysis; 2016, 32; 9-26
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Landslide processes in a flysch massif - case study of the Kawiory landslide, Beskid Niski Mts. (Carpathians, Poland)
    Autorzy:
    Zabuski, L.
    Wójcik, A.
    Gil, E.
    Mrozek, T.
    Raczkowski, W.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059216.pdf
    Data publikacji:
    2009
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Carpathian flysch
    landslide
    monitoring
    numerical simulation
    Opis:
    Geological setting and precipitation triggers seem to be obvious parameters controlling landslides, but their relation to individual sliding processes has not been clear. We take on interdisciplinary approach (combining Earth science methods with an engineer ing-geotechnical approach) to examine sliding processes in the Kawiory landslide in the Polish Carpathians. Field parameters were obtained from inclinometer monitoring, meteorological records, piezometer data and geomechanical tests. Numerical simulation of the landslide development was performed, both for the reconstruction of the internal deformation phenomena on the slope and for approximate prediction of its future behaviour. An empirical formula describing the relationship between the depth of groundwater level (GWL) and precipitation is presented. The case study showed that for the ob served quasi-continuous creep, the depth and in particular the intensity of GWL fluctuations might be crucial.
    Źródło:
    Geological Quarterly; 2009, 53, 3; 317-332
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Some new records of Verrucaria from Beskid Niski Mts.
    Porosty z rodzaju Verrucaria z obszaru Beskidu Niskiego
    Autorzy:
    Krzewicka, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/67139.pdf
    Data publikacji:
    2009
    Wydawca:
    Polskie Towarzystwo Botaniczne
    Opis:
    Based on the historical collections of J. Motyka and J. Nowak deposited in LBL and KRARAM herbaria 26 species of Verrucaria s.l. are reported from Beskid Niski Mts. Verrucaria elaeina is reported from Poland for the first time, whereas as much as 23 species are new to the region.
    W zbiorach zielnikowych KRARAM i LBL z Beskidu Niskiego stwierdzono 26 gatunków Verrucaria s.l. (por. Appendix). V. aethiobola, V. andesiatica, V. aquatilis, V. dolosa, V. elaeina, V. elaeomelaena, V. funckii, V. hydrela, V. latebrosa, V. margacea, V. minuta, V. muralis, V. murina, V. nigrescens, V. ochrostoma, V. obfuscans, V. polysticta, V. praetermissa, V. rupestris, V. sublobulata, V. submersella, V. umbrinula, V. viridula oraz Hydropunctaria rheitrophila i Parabagliettoa cyanea (Gueiden et al. 2009) i Placopyrenium fuscellum (Navarro-Rosinés et al. 2007) wyróżniono w kolekcji zielnikowej J. Nowaka (KRAM) ze wschodniej części Beskidu Niskiego i kolekcji J. Motyki (LBL) z terenu Kąclowej koło Grybowa. Po raz pierwszy dla Polski podano gatunek Verrucaria elaeina. Pozostałe gatunki, z wyjątkiem V. nigrescens, V. polysticta i P. fuscellum (Olech 1974; Krzewicka 2009) zostały podane jako nowe dla tego terenu.
    Źródło:
    Acta Mycologica; 2009, 44, 2
    0001-625X
    2353-074X
    Pojawia się w:
    Acta Mycologica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Stopień uszkodzenia drzewostanów jodłowych Beskidu Niskiego
    Degree of damage to silver fir stands in the Beskid Niski Mts.
    Autorzy:
    Dmyterko, E.
    Bruchwald, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/989946.pdf
    Data publikacji:
    2015
    Wydawca:
    Polskie Towarzystwo Leśne
    Tematy:
    lesnictwo
    drzewostany jodlowe
    uszkodzenia drzewostanow
    jodla pospolita
    Abies alba
    uszkodzenia drzew
    korony drzew
    reakcje przyrostowe
    warunki srodowiska
    radial increment
    environmental changes
    primary crown
    secondary crown
    abies alba
    Opis:
    The main aim of the research was to study trees growth responses to the changing environmental conditions and to assess the degree of damage to trees taking into consideration their secondary crown. Based the material from plots established in 12 silver fir stands (tab.), chronologies were developed for trees in various age classes (fig. 1). 1950 saw a downward trend in the radial growth that continued till 1985, to be followed by an upturn lasting till 2000, when the radial growth stabilised. No significant changes in tree−growth were observed in the group of the youngest trees. Three types of growth response to environmental changes (positive, neutral and negative) were distinguished in the last three 15−year−long periods. In years 1970−1984 the largest proportion of firs indicated negative growth responses, while firs with positive response dominated in the period 2000−2014 (fig. 2). The period 1970−2014 saw a steady increase in the mean value of growth responses. The assessment of the top−crown growth (feature B) showed that more than 50% of the trees showed inhibited growth (fig. 3). The assessment of tree vitality (feature C) confirmed the dominance of trees with moderate crown vitality. The vitality of the secondary crowns (Zw) situated below the primary crowns (Zp) of firs was assessed on the basis of crown density and its length (formula [1]). Incorporating Zw in the assessment of tree damage (formula [2]) resulted in an increase in the vitality of the whole crown (Z) (fig. 4). Based on the defoliation, 73% of trees were found to be within damage class 2 (fig. 5). Another method of damage to trees determination was adopted (formula [3]) to assess the damage to fir stands and showed that the largest proportion of trees was with moderate damage (fig. 6). The damage index values obtained with this method were lower compared to the method that considers the defoliation exclusively. Even lower index values were obtained while using the method based on both damage index W and tree−growth response. Of the three discussed damage assessment methods, the most accurate is the method based on damage index Wz, taking into account the growth response of the entire crown (Z).
    Źródło:
    Sylwan; 2015, 159, 11; 893-904
    0039-7660
    Pojawia się w:
    Sylwan
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The structural control of the Mroczna Cave development on the slopes of Mt Kornuty (the Flysch Carpathians, Beskid Niski Mts)
    Autorzy:
    Zatorski, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/295108.pdf
    Data publikacji:
    2014
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    mass movements
    flysch Carpathians
    crevice-type cave
    structural control
    anisotropic rock massif
    Opis:
    The Mroczna Cave is one of the longest caves in the Beskid Niski Mts., located on the south-western slopes of Mt Kornuty, along the main scarp of the landslide. According to the geomechanical criterion, it is dilation cave, where extension has played a major role. Morphotectonic analysis indicates that the main gravitational movement was of a toppling nature but there were also rotation around the vertical axis as well as a backward rotation. The relatively large cave depth (15.5 m) and its shape (cross-section of its passages) indicate that it was formed along a new gravitational cutting surface of the rock massif, associated with joint sets.
    Źródło:
    Landform Analysis; 2014, 27; 55-65
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Analiza morfotektoniczna form rzeźby osuwiskowej na SW stokach góry Kornuty (Karpaty fliszowe, Beskid Niski)
    Morphotectonic analysis of the landslide relief on the SW slopes of Mt Kornuty (Flysch Carpathians, Beskid Niski Mts)
    Autorzy:
    Zatorski, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075859.pdf
    Data publikacji:
    2018
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    ruchy masowe
    analiza morfotektoniczna
    anizotropia strukturalna
    skały fliszowe
    Beskid Niski Mts.
    Polskie Karpaty zewnętrzne
    Polska Południowa
    mass movements
    morphotectonic analysis
    structural anisotrophy
    flysch rocks Beskid Niski Mts.
    Polish Outer Carpathians
    Southern Poland
    Opis:
    On the SW slopes of the Mt. Kornuty (Magura Wątkowska mountain range in the Beskid Niski Mts.) is located one of the largest landslide areas in the Polish Flysch Carpathians. The morphotectonic analysis performed using contour diagrams and rose directional diagrams, made it possible to determine the direction of gravity mass movement. In total, over than 2500 measurements of the spatial orientation of joint surfaces were made within the landslide zone. Changing the direction of the tectonic anisotropy of the in situ and ex situ forms allowed conducting the morphogenetic analysis, i.e. specifying the types of gravitational movements. Besides the commonly occurring toppling, also rockfalls, rotation around the horizontal or vertical axis, and antithetical displacements (thelistric type) were observed. The combination of several types of gravitational movements of different age allows us to unequivocally say that it is a complex type of landslide.
    Źródło:
    Przegląd Geologiczny; 2018, 66, 2; 111--117
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Charakterystyka korytarzy i ich rola w środowisku geograficznym okolic Gładyszowa w Beskidzie Niskim
    Characteristics of corridors and their role in geographic environment of Gladyszow region in the Beskid Niski Mts.
    Autorzy:
    Augustowski, K.
    Powiązania:
    https://bibliotekanauki.pl/articles/87059.pdf
    Data publikacji:
    2009
    Wydawca:
    Polska Asocjacja Ekologii Krajobrazu
    Tematy:
    Beskid Niski
    okolice Gladyszowa
    korytarze naturalne
    korytarze antropogeniczne
    typologia
    funkcje
    Źródło:
    Problemy Ekologii Krajobrazu; 2009, 23
    1899-3850
    Pojawia się w:
    Problemy Ekologii Krajobrazu
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Podstawy planowania składu gatunkowego w lasach górskich na przykładzie Beskidu Niskiego
    Basis of the species composition planning model for mountain forests on the example of Beskid Niski Mts.
    Autorzy:
    Bruchwald, A.
    Dmyterko, E.
    Mionskowski, M.
    Niemczyk, M.
    Łukaszewicz, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/972988.pdf
    Data publikacji:
    2016
    Wydawca:
    Polskie Towarzystwo Leśne
    Tematy:
    hodowla lasu
    planowanie
    czynniki siedliska
    typy siedliskowe lasu
    leśnictwo
    tereny górskie
    lasy górskie
    skład gatunkowy
    wysokość nad poziomem morza
    rzeźba terenu
    species composition
    habitats
    landforms
    mountain forests
    Opis:
    The study presents a method of planning species composition of forest stands in mountain areas on the example of Beskid Niski Mts. (south−eastern Poland). The focus was on the species composition of forest stands growing in different conditions, taking into account the type of forest habitat and terrain characteristics: altitude, exposition and slope. The research was based on data stored in the Information System of the State Forests. We used modified growth model for data processing and calculation of site index for the forests older than 60 years. The Beskid Niski Mts. are covered mostly by European beech (33.8%), silver fir (28.3%) and Scots pine (18.9%). Taking into account exclusively the productive capacity of individual forest stands, fir and spruce would be the most desirable species in analysed region. The Beskid Niski Mts. are characterized by a very small diversity of the habitat with domination of mountain fresh deciduous forest (LGśw, 92.1% of the area). We divided analysed region into four altitudinal zones that vary greatly in fraction of afforested area. Beech dominates in all zones and its share increases from the foothills to montane zone (fig. 5). Basing on a digital terrain model, the areal share of 10 landforms was determined for each stand and altitudinal zone (fig. 8). This enabled more detailed planning of species composition. However, it required the adoption of six specific assumptions including the need to maintain a suitable proportion of all tree species growing in the mountains, specifically the main forest tree species: spruce, fir and beech. The 5−stage project (preliminary, historical, current, planning, verification stages) consisting of planning species composition uses, in stage 4, detailed information on landforms. The project assumes that the fragments of forests where trees are expected to grow fast will be earmarked for endangered species. The model sees the need of planting the weaker tree species to be present in the forest ecosystems of the Beskid Niski. The proposed project will enable foresters−practitioners to plan the forest species composition for each of the forest districts in the Beskid Niski quickly. Such a programme might also be an integral part of the growth model of forests useful for forecasting and increasing timber resources.
    Źródło:
    Sylwan; 2016, 160, 03; 219-229
    0039-7660
    Pojawia się w:
    Sylwan
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zastosowania naziemnego skanera laserowego (TLS) do oceny aktywności osuwisk, na przykładzie osuwiska Bodaki (Beskid Niski)
    The use of Terrestrial Laser Scanner (TLS) to assess the activity of landslides, for example of Bodaki landslide (Beskid Niski Mts.)
    Autorzy:
    Cebulski, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/294446.pdf
    Data publikacji:
    2014
    Wydawca:
    Stowarzyszenie Geomorfologów Polskich
    Tematy:
    osuwiska
    naziemny skaning laserowy
    erozja koryt potoków
    Beskid Niski
    landslides
    terrestrial laser scanning
    stream channel erosion
    Beskid Niski Mts.
    Opis:
    W artykule przedstawiono zastosowanie naziemnego skaningu laserowego (TLS) do oceny wielkości zmian zachodzących w obrębie osuwiska Bodaki (Beskid Niski). Analiza porównawcza czterech cyfrowych modeli wysokościowych uzyskanych w wyniku skanowania pozwoliła na określenie z bardzo dużą dokładnością ilości materiału który został usunięty z osuwiska przez potok Bartniankę. Zastosowana technika pozwoliła także na określenie obszarów w największym stopniu przekształconych oraz tempa przemieszczania się wybranych fragmentów osuwiska.
    This paper presents application of Terrestrial Laser Scanning (TLS) to assess the magnitude of the changes taking place within the Bodaki landslide (Beskid Niski Mts.). The comparative analysis of four digital elevation models obtained by scanning allowed to determine with high accuracy the amount of material that was removed from landslides by the Bartnianka stream. The technique also allowed to identification the most transformed areas and the movement rate of selected parts of the landslide.
    Źródło:
    Landform Analysis; 2014, 26; 105-113
    1429-799X
    Pojawia się w:
    Landform Analysis
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zróżnicowanie i dynamika roślinności na terenie Stacji Bazowej Zintegrowanego Monitoringu Środowiska Przyrodniczego w Szymbarku (Beskid Niski)
    Differentiation and dynamics of vegetation in the Base Station of Integrated Monitoring of Natural Environment area in Szymbark (Beskid Niski Mts)
    Autorzy:
    Salachna, Anna
    Powiązania:
    https://bibliotekanauki.pl/articles/1574908.pdf
    Data publikacji:
    2020
    Wydawca:
    Polskie Towarzystwo Inżynierii Ekologicznej
    Tematy:
    dynamika roślinności
    Arrenatheretum elatioris
    Tilio cordatae-Carpinetum betuli
    wskaźniki bioróżnorodności
    vegetation dynamics
    biodiversity indicators
    Opis:
    W pracy przedstawiono wyniki badań roślinności, przeprowadzone na terenie Stacji Bazowej Monitoringu Zintegrowanego Środowiska Przyrodniczego w Szymbarku. W celu oceny tendencji dynamicznych wyróżnionych zbiorowisk roślinnych porównano dane fitosocjologiczne z 1995 i 2011 roku. Analiza DCA oraz wielozmienna analiza wariancji PERMANOVA wykazały brak istotnych statystycznie różnic w składzie gatunkowym porównywanych fitocenoz w badanym okresie. Za pomocą testu Wilcoxona dla par wiązanych odnotowano natomiast istotne statystycznie różnice w wartościach średnich bogactwa gatunkowego oraz wskaźnika jednorodności gatunkowej Pielou. Największe przeobrażenia struktury stwierdzono w zespole rajgrasu wyniosłego Arrenatheretum elatioris Br.-Bl. ex Scherr. 1925, co wynika z dużej wrażliwości tej fitocenozy na zmiany parametrów środowiskowych oraz sposobu użytkowania.
    The paper presents the results of vegetation research carried out in the Base Station of Integrated Monitoring of Natural Environment area in Szymbark. In order to assess the dynamic trends of the distinguished plant communities phytosociological data from 1995 and 2011 were compared. The DCA analysis and the multivariate PERMANOVA analysis of variance showed no statistically significant differences in the species composition of the compared phytocoenoses in the period 1995–2011. Using the Wilcoxon signed-rank test, statistically significant differences were noted in the mean values of species richness and the Pielou species homogeneity index. The greatest transformations in the structure were found in the Arrenatheretum elatioris association, which results from the high sensitivity of this phytocoenosis to changes in environmental parameters and the way of use.
    Źródło:
    Inżynieria Ekologiczna; 2020, 21, 4; 10-19
    2081-139X
    2392-0629
    Pojawia się w:
    Inżynieria Ekologiczna
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The Beloveža Formation of the Rača Unit in the Beskid Niski Mts. (Magura Nappe, Polish Flysch Carpathians) and adjacent parts of Slovakia and their equivalents in the western part of the Magura Nappe; remarks on the Beloveža Formation – Hieroglyphic Beds
    Autorzy:
    Golonka, J.
    Waśkowska, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2060514.pdf
    Data publikacji:
    2012
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    Outer Carpathians
    Eocene
    Magura Nappe
    Rača Unit
    Beloveža Formation
    lithostratigraphy
    Opis:
    Eocene thin-bedded flysch, widespread in the Alpine Tethys ocean, is present within the Magura Nappe, the largest Outer Carpathian unit in Poland and Slovakia. Thin-bedded flysch sedimentation accompanied by hemipelagic shales took place accross the entire Magura Basin during Eocene times. The lithostratigraphic position of these deposits has been a subject of considerable discussion. Different names, such as the Hieroglyphic Beds, Hieroglyphic Formation, Łabowa Shale Formation, Grzechynia Sandstones and Beloveža Beds, Beloveža Formation have been used in the Outer Carpathians literature. We show a striking resemblance of the Beloveža Beds (Formation) from its type locality to the Hieroglyphic Beds from the Beskid Wysoki area and to typical Beloveža Beds from the Hańczowa Mts. We propose to the name Beloveža Formation should be applied to thin-bedded flysch within both Bystrica and Rača units of Magura Nappe and the name Hieroglyphic Formation should be restricted to the Skole Unit. The original type locality in Beloveža near Bardejov in Slovakia is selected as type section of the Beloveža Formation
    Źródło:
    Geological Quarterly; 2012, 56, 4; 821--832
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Wtórna sukcesja roślinności w kierunku bagiennej olszyny górskiej Caltho laetae-Alnetum (Zarz. 1963) Stuchlik na dawnych łąkach Beskidu Niskiego
    Secondary succession towards grey alder bog forest Caltho laetae-Alnetum (Zarz. 1963) Stuchlik on the abandoned meadows in the Beskid Niski Mts. (Western Carpathians)
    Autorzy:
    Koczur, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/1008757.pdf
    Data publikacji:
    2012
    Wydawca:
    Polskie Towarzystwo Leśne
    Tematy:
    Beskid Niski
    laki gorskie
    laki podmokle
    sukcesja roslin
    sukcesja wtorna
    gorska olszyna bagienna
    zespol Caltho-Alnetum
    abandoned meadows
    secondary succession
    grey alder bog forest
    beskid niski mts.
    western carpathians
    Opis:
    On the abandoned wet meadows in the Beskid Niski Mts. secondary succession to the community Caltho laetae−Alnetum proceeds. In the initial phases of succession significant similarity between patches of meadows communities and grey alder bog forest in floristic composition and structure of vegetation is observed. Particular stages of succession (non−forest and forest) are characterized by occurrence of big group (43.5%) of shared species.
    Źródło:
    Sylwan; 2012, 156, 10; 784-791
    0039-7660
    Pojawia się w:
    Sylwan
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zróżnicowanie spływu powierzchniowego i spłukiwania gleby na poletkach doświadczalnych o różnej długości (Szymbark, Beskid Niski)
    The diversity of overland flow and soil wash on experimental plots of different lengths (Szymbark, Low Beskidy Mts.)
    Autorzy:
    Bochenek, W.
    Gil, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/2084663.pdf
    Data publikacji:
    2010
    Wydawca:
    Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
    Tematy:
    wies Szymbark
    Beskid Niski
    splyw powierzchniowy
    gleby
    poletka doswiadczalne
    dlugosc pola
    splukiwanie
    natezenie opadow
    wskaznik erozyjnosci opadu
    Opis:
    The study on soil wash was conducted on the experimental slope within the Scientific-Research Station of the Institute of Geography and Spatial Organization (Polish Academy of Sciences) in Szymbark in years 1990-96. Five experimental plots installed on the slope were 2m wide, had lengths of 2, 4, 8, 16, and 32m and were under black fallow. Measurements of overland flow and soil wash reveled relationships between the processes and lengths of the plots and sums and intensity of rainfall events. The volume of the surface flow increased with increasing length of the plots, from 3352 dm³ (2m) do 12153 dm³ (32m), but on the other hand this was accompanied by decrease in the flow index. The index value was highest on the shortest plot (2 m) - almost 5 times greater than on the 32m-long plot. The observed relationship is typical for the river catchments: the smaller the catchment, the higher the flow index is (pertaining to 1 km² of the area). The soil wash occurred to be more differentiated with respect to the length of the plots (from 131,6kg to 1166,4kg). The relationship between maximum intensity of rain and soil wash on all plots has a character of polynomial equations of the second degree, described by negative correlation coefficients. As the plot's length increases, the relationship is stronger. During rainfall events of a very high intensity, over 1,5 mm min⁻¹ (high kinetic energy), the soil wash is limited by aggregating soil particles due to action of the rain droplets. Agrotechnical treatments significantly influence the process of soil relocation (weeding, ploughing). Observed soil wash directly following such treatments was much more intensive in comparison with conditions of slightly compressed soil.
    Źródło:
    Prace i Studia Geograficzne; 2010, 45; 265-278
    0208-4589
    Pojawia się w:
    Prace i Studia Geograficzne
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Zapis typu ruchu osuwiska w rzeźbie terenu i jego obraz na wysokorozdzielczych numerycznych modelach terenu (NMT) na przykładzie wybranych osuwisk ze wschodniej części Beskidu Niskiego (Karpaty zewnętrzne, Polska)
    Landslide movement type record in morphology and its visualization on high resolution digital terrain models, exemplified by some landslides in the eastern part of the Low Beskid Mts. (Polish Outer Carpathians)
    Autorzy:
    Kaczorowski, J.
    Powiązania:
    https://bibliotekanauki.pl/articles/2075689.pdf
    Data publikacji:
    2017
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    osuwisko
    numeryczny model terenu
    DTM
    zsuw rotacyjny
    zsuw translacyjny
    spływ
    osuwisko złożone
    Beskid Niski
    Karpaty zewnętrzne
    landslide
    digital terrain model (DTM)
    rotational slide
    translational slide
    flow
    complex landslide
    Low Beskid Mts.
    Outer Carpathians
    Opis:
    Landslides are very common features in the Polish Outer Carpathians. In the classical cartography, landslides are recognized based on characteristic land relief: main and side scarps, toe, minor scarps, transverse ridges, recesses and cracks. Formerly, landslide mapping was carried out in the field, preceded by interpretation of topographic maps and aerial photographs. Nowadays, we use spatial data from airborne laser scanning (ALS). Spatial data reprocessing permits to achieve a high-resolution (pixel 1*1 m or more precise) digital terrain model (DTM). Exploration of land relief in search for landslides has become simpler and more accurate. DTM interpretation allows delimiting the boundaries of landslides and elements of their relief. By analysing groups oflandforms it is possible to determine the type of colluvium movement. In the eastern part of the Low Beskid Mts., four types of landslides predominate: rotational slides, translational slides, flows, and complex movements. Types of landslides are usually very well visible on the DTM. Information about types of mass movements can be useful during modelling further landslide activity and designing instrumental identification works and possibility ofstabilization.
    Źródło:
    Przegląd Geologiczny; 2017, 65, 1; 44--2
    0033-2151
    Pojawia się w:
    Przegląd Geologiczny
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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