Paulina Mareczka’s research while affiliated with University of the National Education Commission, Krakow and other places

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Publications (6)


Cechy uziarnienia osadów eolicznych w rejonie jeziora Piaski (Równina Wkrzańska)
  • Conference Paper
  • Full-text available

June 2022

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127 Reads

Anna Dykas

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Patrycja Dziewit

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[...]

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Sesja naukowa "Paleogeografia Schyłku Vistulianu", Popów 2022

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Location of study area: (a) localization of maps (b,c); (b) map of peat bogs in the Orawa-Nowy Targ Basin; (c) 3D model of the central part of the Polish Carpathian Mountains with location of the peat bogs.
Map of the Baligówka peat bog.
Scheme of workflow in the study.
(a) Division of the Baligówka peat bog; (b) topographic profile along non-exploited part of the peat dome; (c) topographic profile along drainage system area; (d) topographic profile along industrial peat exploitation area.
Distribution of vegetation height classes in the Baligówka peat bog.

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Assessment of Peat Extraction Range and Vegetation Succession on the Baligówka Degraded Peat Bog (Central Europe) Using the ALS Data and Orthophotomap

June 2022

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90 Reads

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3 Citations

The Baligówka peat bog is one of the peat bogs of the Orawa-Nowy Targ Basin—the largest complex of wetlands in the Polish Carpathians. Its area has declined in the past as a result of drainage and peat exploitation, which caused a bad hydrological condition and it is gradually overgrown by non-peat bog medium and high vegetation. The research uses models derived from airborne laser scanning (ALS) and an orthophotomap to delimit the bog and divide it into parts and assess the range of drainage ditches and vegetation. The area of the peat dome along with 3 sites of peat exploitation is currently 159.6 ha, while the ecotone zone is 105.9 ha. Both sections are separated by a steep post-mining slope. The medium and high vegetation areas cover 44% of the peat bog; its location is related to the dense drainage system in the southern part of the dome. The parameters of the Baligówka peat bog: area, size and extent of drainage system, and the degree of overgrowth by high vegetation, are the subject of research towards the protection under the Natura 2000 network (PLH120016) and the establishment of a plan for restoration activities.


Geochemical analyses of recent sediments from Lake Morzycko against selected physiographic parameters of the Słubia River catchment (Western Poland)

December 2021

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130 Reads

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2 Citations

Acta Geographica Lodziensia

This paper presents the results of a study on the content of lithogeochemical components (organic matter, Na, K, Mg, Ca, Mn, Fe, Cu and Zn) and grain-size composition of mineral matter in the bottom sediments of Morzycko Lake (Myślibórz Lakeland, NW Poland). This lake is large (342.7 ha) and deep (69 m). The catchment has a typical forested character (mainly in the middle part of the Słubia River valley) with agricultural area (mainly in the upland areas north of the lake). The diversity of concentrations of metals was analysed based on 44 samples from 22 representative sites, including surface sediments and sediments from 5 cm below the current lake bed. The results showed that the chemical composition and granulometry of bottom sediments depends on contemporary morphogenetic processes in the catchment of the Słubia River. Geochemical and grain-size indices varied due to changes in biological productivity, intensity of weathering of postglacial material making up the catchment, and potential for migration of metals to the lake with surface or underground runoff. An important aspect in assessing the degree of enrichment of the sediments in trace elements is the location of shallow parts of the lake near the tourist districts of Moryń.


Figure 2. Location of the study area in Poland (A), in the Orawa -Nowy Targ Basin (B) and near the village of Ludźmierz (C).
Figure 3. Ludźmierz Bog. A: slope map of study area; B: division of the bog into domes and cutover areas; C: 3D model of the study area showing natural colours.
Figure 4. The borders between peat dome remnants and cutover areas. A: map showing the different types of border; B: diagram showing the proportions of different border types.
Figure 5. Characteristics of vegetation on the Ludźmierz bog from ALS data and the orthophotomap of Poland. A: differential model of vegetation height on the bog; B: vegetation types occurring on the bog; C: diagram showing the shares of different vegetation types on the dome and cutover areas; D: cumulative graphs of the relative (%) surface areas of domes and cutover occupied by vegetation of given stature (m).
Figure 6. Vegetation characteristics on the dome from satellite data. A: Colour Infrared (CIR) satellite image of the study area; B: map of NDVI values; C: spectrum diagram of the vegetation types mapped in Figure 5B (bands RED and IR); D: cumulative curves of NDVI for the peat domes and peat extraction areas.
Using remote sensing materials to assess the effects of peat extraction on the morphology and vegetation cover of a raised bog (Ludźmierz near Nowy Targ, Southern Poland)

December 2020

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243 Reads

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3 Citations

Mires and Peat

The Orawa-Nowy Targ Basin is one of only a few areas in the Polish Carpathians with high relative cover of peatlands (12 %). This fraction is declining progressively due to several centuries of peat exploitation for fuel, gardening and balneology. The peatland at Ludźmierz near Nowy Targ is regionally important for its high biodiversity but has been scarred by historical and contemporary peat extraction. The current area and fragmentation of peat domes on Ludźmierz Bog were assessed, along with the characteristics and condition of the vegetation. Also, topographical changes across areas of peat extraction were analysed using a combination of remote sensing and field study methods in order to identify the locations of modern peat extraction and natural mass movements. The condition of the raised bog and changes in its boundaries were thus deduced, paying attention to the bog's exceptional environmental and landscape values. The area covered by the bog is currently 39 ha and it is divided into three separate domes which are drained by a network of ditches and through discontinuities of the water table at peat extraction areas. The vegetation on extraction areas currently has a higher biomass growth rate than the plant cover on the domes, and is in better condition on the basis of NDVI assessment.


Mokradła i torfowiska jako temat zajęć terenowych w edukacji geograficznej

December 2020

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179 Reads

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1 Citation

Annales Universitatis Paedagogicae Cracoviensis Studia Geographica

Mokradła i torfowiska jako temat zajęć terenowych w edukacji geograficznej Streszczenie Celem artykułu jest charakterystyka torfowisk Kotliny Orawsko-Nowotarskiej jako miejsca do przeprowadzenia zajęć terenowych z geografii i przyrody. Wskazano unikatowość mo-kradeł oraz pełnione przez nie funkcje w środowisku geograficznym. W oparciu o kwerendę literatury przygotowano zestaw wiadomości o mokradłach i torfowiskach. Podczas badania terenowego opisano obiekty dydaktyczne istniejące na torfowiskach obszaru badań-ścieżkę w rezerwacie przyrody "Bór na Czerwonem" oraz ścieżkę "Torfowisko Baligówka", położone w Kotlinie Orawsko-Nowotarskiej. Szlaki te oceniono pod kątem dostępności komunikacyj-nej i stanu infrastruktury, a także treści merytorycznych oraz różnorodności krajobrazowej. Opisywane trasy i położone wzdłuż nich obiekty stanowią przykład wartościowego materia-łu dydaktycznego, który warto wykorzystać podczas wycieczki szkolnej na zajęciach z geo-grafii i przyrody. W końcowej części opracowania wskazano elementy, o których nauczyciel powinien wiedzieć i zwrócić na nie uwagę uczniom podczas takich zajęć. Wetlands and peat bogs as theme for field geography education Abstract The purpose of this article is to characterize the peat bog objects of Orawa-Nowy Targ Basin as a destination to conduct field geography and natural science lesson. The uniqueness of wetlands and peat bogs as well as their functions in the environment were indicated in the text. In the text was conducted compilation of knowledge about wetlands and peatlands, based on literature research. During the field study, educational trails already existing on the peatlands of the study area were described-they were the educational trails in the "Bór on Czerwonem" nature reserve and "Torfowisko Baligówka", located in Orawa-NowyTarg Basin. These routes were evaluated in terms of communication aspect and the state of its


Fig. 2. Distribution of landscape pieces in study area: 1 -border of study area, 2 -border of PNP, 3 -development areas, 4 -agriculture areas (cereal crops), 5 -agriculture areas (other crops), 6 -grasslands (meadows, pastures), 7 -grasslands (other areas), 8 -forests, 9 -bare soils and rocks, 10 -water bodies. Source: own elaboration
Fig. 3. Diagrams of the structure of landscape pieces for study area: A: Pieniny Mts.; B: PNP; C: Pieniny without PNP. 1 -development areas, 2 -agriculture areas (cereal crops), 3 -agriculture areas (other crops), 4 -grasslands (meadows, pastures), 5 -grasslands (other areas), 6 -forests, 7 -bare soils and rocks, 8 -water bodies. Source: own elaboration
Fig. 8. Cumulative curves of landscape pieces area (x axis) in relation to TRI index (y axis): A -Pieniny Mts.; B -PNP; C -Pieniny without PNP. 1 -development areas, 2 -agriculture areas (cereal crops), 3 -agriculture areas (other crops), 4 -grasslands (meadows, pastures), 5 -grasslands (other areas), 6 -forests, 7 -bare soils and rocks, 8 -water bodies. Source: own elaboration
Struktura pozioma i pionowa krajobrazu Pienin polskich i Pienińskiego Parku Narodowego [Horizontal and vertical landscape mosaic of the Polish part of the Pieniny range and the Pieniny National Park]

November 2018

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182 Reads

The article contains the study on the structure of the landscape of the Polish Pieniny Mountains. Two types of remote sensing data were used during the research: Sentinel-2A satellite land cover data and airborne laser scanner data. There were calculated 4 indicators chosen by literature review to define the current landscape diversity-the structure, variety and shape indexes of landscape pieces for horizontal aspect as well as topographic ruggedness index for vertical landscape aspect. Afterwards, the area of the Pieniny National Park (PNP) was separated from the range and all steps of the study were repeated. In the end, indicator results for Pieniny Mountains and PNP were compared.

Citations (4)


... NDVI and spectral information were used to identify five plant cover types that indicate hydrological differences and degradation intensity of extraction areas compared to the remnant peat dome. Jucha et al. (2022) used lidar data and an orthophoto-based map (< 1 m) to analyze degradation at another Polish peat bog (160 ha) after peat extraction. They differentiated vegetation height classes, peat extraction areas, and drainage, and evaluated the relationship between vegetation height and distance to drainage. ...

Reference:

Remote sensing of peatland degradation in temperate and boreal climate zones -A review of the potentials, gaps, and challenges
Assessment of Peat Extraction Range and Vegetation Succession on the Baligówka Degraded Peat Bog (Central Europe) Using the ALS Data and Orthophotomap

... According to Borówka (2007), the most important of these processes are: terrigenic sedimentation (the supply of allochthonous mineral matter, mainly from the catchment), biogenic sedimentation (e.g. the accumulation of amorphous organic matter or the sedimentation and decomposition of diatom shells, molluscs, etc.) and chemogenic sedimentation (the dissolving and precipitation of crystalline and amorphous substances such as calcium carbonate, hydroxides, sulphides or phosphates). All these processes are variable in space and time (Bojakowska, Sokołowska 1997;Apolinarska et al. 2012;Kittel et al. 2020;Adamek et al. 2021;Pleskot et al. 2022;Sojka et al. 2022), and their intensity can increase markedly depending on the nature and degree of human impact (Kosiński et al. 1994;Korzeniowski et al. 2020;Cybul, Okupny 2021;Płóciennik et al. 2021Płóciennik et al. , 2022. In this respect, strongholds, defensive settlements and urban centres are special; though they contain historically valuable features, they also constitute an irreplaceable testing ground for geoarchaeology, which also includes environmental geochemistry (Wardas-Lasoń et al. 2007;Hildebrandt-Radke 2011;Galas, Jaeger 2016;Kittel et al. 2018;Twardy et al. 2018). ...

Geochemical analyses of recent sediments from Lake Morzycko against selected physiographic parameters of the Słubia River catchment (Western Poland)

Acta Geographica Lodziensia

... This area can be very wet with swamps, rushes and shallow water bodies fed by water outflows from the peat dome, sometimes with renewing peat bog vegetation. The post-mining site may also be occupied by a birch grove [25] or a coniferous swamp [28]. It can also be drained and incorporated into agricultural land-in this situation, the ecotone zone disappears ( Figure 2). ...

Mokradła i torfowiska jako temat zajęć terenowych w edukacji geograficznej

Annales Universitatis Paedagogicae Cracoviensis Studia Geographica

... Notably, using this algorithm they derived six site conditions (reflecting a disturbance gradient) from Sentinel-2 data, enhancing its potential utility. Jucha et al. (2020) combined lidar, orthophotos, and Sentinel-2 imagery to analyze a small (68 ha) peat bog in Poland with ongoing peat extraction with < 1 m spatial resolution. They identified different peat extraction types (mechanical vs. hand-cut) and vegetation cover variety (e.g. ...

Using remote sensing materials to assess the effects of peat extraction on the morphology and vegetation cover of a raised bog (Ludźmierz near Nowy Targ, Southern Poland)

Mires and Peat