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Tytuł:
Etapy i zakres prac badawczych realizowanych w ramach zintegrowanego systemu monitorowania wód podziemnych w Gdańsku i Sopocie w latach 2011–2014
Stages and scope of the research work carried out in the framework of integrated groundwater monitoring system in Gdańsk and Sopot in 2011–2014
Autorzy:
Lidzbarski, M.
Kordalski, Z.
Powiązania:
https://bibliotekanauki.pl/articles/2075479.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
monitorowanie wód podziemnych
wody podziemne
pobrzeże
monitorowanie
Gdańsk
Sopot
regional integrated groundwater monitoring system
groundwater monitoring
monitoring
Opis:
This paper synthetically describes the stages and methods used in the course of research carried out within the integrated groundwater monitoring system in Gdańsk and Sopot in 2011–2014. The study was divided into 3 stages: surveillance, operational and research monitoring. Surveillance monitoring, implemented in 2011–2012, involved comprehensive assessment of the groundwater state. Operational monitoring, carried out in 2013, was intended to confirm the previously identified hydrogeochemical anomalies and to establish ongoing trends in quality changes. The third stage of the research was conducted in post-industrial and urban areas of Gdańsk, where groundwater contamination had been identified. The work focused on the determination of the type, extent, concentration and rate of transport of contaminants. Another task was to prepare a tool enabling efficient use of collected information. It was decided to create a platform for hydrogeological information exchange (environmental database) in the form of geoMonitoring web application.
Źródło:
Przegląd Geologiczny; 2016, 64, 6; 382--388
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Monitoring zagrożenia sejsmicznego obszaru Polski
Monitoring seismic hazards in Poland
Autorzy:
Trojanowski, J.
Plesiewicz, B.
Guterch, A.
Grad, M.
Powiązania:
https://bibliotekanauki.pl/articles/2066182.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
zagrożenie sejsmiczne
monitoring
Polska
Źródło:
Przegląd Geologiczny; 2009, 57, 2; 133-137
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wyznaczenie przemieszczeń powierzchniowych na osuwisku w Kłodnem (gmina Limanowa, południowa Polska)
Determination of surface displacement on the landslide in Kłodne (Limanowa community, southern Poland)
Autorzy:
Ćwiąkała, P.
Stanisz, J.
Wróbel, A.
Kaczmarczyk, R.
Drwal, P.
Grabek, P.
Daroch, M.
Pękala, M.
Świątek, M.
Zierkiewicz, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075554.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Karpaty fliszowe
osuwiska
monitoring geodezyjny
Kłodne
flysch Carpathians
landslides
geodetic monitoring
Opis:
Examination of the landslide in Kłodne was carried out in 2013 and 2014. The work was divided into two parts: geological engineering investigations (mapping of the external borders of the landslide) and geodetic surveying (photogrammetric studies and monitoring of surface movements). The boundaries of the landslide were marked using a Garmin eTrex GPS receiver and a geological compass (Freiberg). The boundaries have not changed and is convergent with previous studies. In the south-western part of the landslide the boundary is blurred as a result of anthropogenic transformation of the area. In the south-eastern part (as at May17, 2014) about 200 m3 of the colluvial material has been moved. Photogrammetric studies were based on the analysis of aerial photos from May 26, 2009 (prior tothe landslide formation) and on the orthophotomap created from images taken in July 2010, after the formation of the landslide. Displacement vectors were determined by comparing the locations of specific terrain details in the pictures taken before and after the mass movements occurred. In the upper part of the landslide the maximum horizontal displacement value was 87.7 m, the minimum was 6.2, and the average – 84.5 m. In the lower part of the landslide the horizontal displacements amounted to 65.5 m, had a minimum value of 10.3, and an average of 54.8 m. In the last stage of the study the base measurement network was created. It consisted of 68 points stabilized in the ground. The measurements were performed using the static GNSS observations method and linear-angular measurements carried out with a precise total station. In 2013, horizontal displacements ranged from 1 to 8.1 mm, and vertical ones ranged from –9.8 to 13.5 mm. In 2014, there were displacements observed in the vicinity of the main slope. They were directed to the south. The horizontal displacement vector has reached values from 2 to 94 mm, and the vertical vector was from –63 to 16 mm.
Źródło:
Przegląd Geologiczny; 2016, 64, 2; 122--130
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Jednorodność sieci monitoringowej wód podziemnych w rejonie kompleksu składowisk odpadów w Strzemieszycach
The homogeneity of the groundwater monitoring network in the region of the landfills’ system in Strzemieszyce
Autorzy:
Dąbrowska, D
Sołtysiak, M.
Kucharski, R.
Powiązania:
https://bibliotekanauki.pl/articles/2075410.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
monitoring wód podziemnych
reprezentatywność danych
składowiska odpadów
groundwater monitoring
data representativeness
landfill sites
Opis:
The correct assessment of the groundwater chemical status in the region of the real or potential contamination sources is possible due to reliable and representative results of monitoring researches. The homogenously-designed monitoring network allows us to get the data from the whole specified area. This paper shows calculations of the representativity index and the nearest neighborhood index to determine the homogeneity of the monitoring network of the landfills’ system in Strzemieszyce (D¹browa Górnicza). There were taken into account piezometers intaking Quaternary and Triassic aquifer. In particular, it has been determined if an existing number of monitoring points is sufficient for this area and optimal for the assessment of the groundwater threat.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/1; 657--660
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Możliwości identyfikacji suszy hydrogeologicznej na podstawie monitoringu i modelowania GIS na przykładzie regionu Dolnej Odry i Przymorza Zachodniego
Identification of hydrogeological drought based on monitoring and GIS modelling on the example of the Lower Odra and Western Pomerania region
Autorzy:
Gurwin, J.
Powiązania:
https://bibliotekanauki.pl/articles/2075394.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
susza hydrologiczna
monitoring wód podziemnych
modelowanie GIS
hydrogeological drought
groundwater monitoring
GIS modelling
Opis:
The paper presents the problem of spatial analysis capabilities of hydrogeological drought based on long-term observations of groundwater table fluctuations in the national monitoring network and multi-criteria modelling using GIS tools. An uncomplicated as possible scheme was developed, allowing for rapid qualitative assessment of spatial variability of susceptibility and exposure to drought. The mean values were determined from the annual lowest states of water table for every monitoring point being accepted for analysis. And drought periods were established. Afterwards the map of spatial distribution of drought was created and put in GIS modelling as the input layer together with other appropriate weighted overlay function parameters.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/1; 738--742
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Dynamika przemieszczeń wybranych osuwisk w Karpatach
The dynamics of displacements of selected landslides in the Carpathians
Autorzy:
Warmuz, Bartłomiej
Nescieruk, Piotr
Powiązania:
https://bibliotekanauki.pl/articles/2075947.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
osuwiska
monitoring instrumentalny
opad atmosferyczny
otwór geologiczny
andslides
instrumental monitoring
precipitation
geological basement
Opis:
The paper presents the activity ofselected landslides where instrumental monitoring has been carried out within the Framework of Landslide Counteracting System (SOPO). The temporal relationships between subsurface dynamics (displacements) and geological structure with respect to atmospheric precipitation are discussed. In order to expose these relationships, the landslides were divided into two groups: the first one is located in the areas where the bedrock is made up of flysch formations with the predominance of clay rocks. The second group is located in areas with the prevalence of sandstones in the bedrock. The analysis of the 10-year record shows that, in the areas where the geological structure is dominated by clays, the landslides present continuous activity with displacements not exceeding a dozen mm/year. In the areas where in the geological foundation (bedrock) sandstones are dominated, landslide movements were usually more impulsive. Dislocations were recorded mainly after intense, long-lasting precipitation or heavy rainstorms. In extreme situations the large displacements caused total destruction of the measuring column.
Źródło:
Przegląd Geologiczny; 2019, 67, 5; 326--331
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zastosowanie modelowania geochemicznego jako elementu wspomagającego monitoring przyrodniczych obszarów chronionych
Geochemical modeling as an element of protected area monitoring
Autorzy:
Jóźwiak, K.
Krogulec, E.
Powiązania:
https://bibliotekanauki.pl/articles/2074435.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
park narodowy
monitoring wód podziemnych
monitoring wód powierzchniowych
geochemia
modelowanie
Kampinoski Park Narodowy
national park
groundwater monitoring
geochemical modelling
Kampinoski National Park
Opis:
Groundwater in the Kampinoski National Park (KPN) area is usually of fresh and ultrafresh type with mineralisation lower than 493.36 mg/dm3. The variation of groundwater types is mainly caused by low ability of the system to buffer the acid accumulation and contamination as well as by the lack of isolation. The aim of the monitoring system at the KPN is to prevent anthropogenic contamination of the system. Geochemical modeling is one of the most important elements of the monitoring. Description of geochemical speciations present in groundwater can be used for characterizing a variation of groundwaters’ natural and athropogenic chemistry. Not only speciation modeling (which can reveal speciation of particular elements in groundwater) should be a part of monitoring system, but also inverse modeling, allowing us to reconstruct processes cocurring in the system and their intensity.
Źródło:
Przegląd Geologiczny; 2006, 54, 11; 987-992
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Fotogrametria bliskiego zasięgu i skaning laserowy jako metody monitoringu zmian geodynamicznych na przykładzie skarpy w Płocku
Close range photogrammetry and laser scanning as the methods of monitoring geodynamic changes on the example of the scarp in Płock
Autorzy:
Przyłucka, M.
Klimkowska, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075515.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
fotogrametria bliskiego zasięgu
naziemny skaning laserowy
monitoring osuwiska
close-range photogrammetry
terrestrial laser scanning
landslides monitoring
Opis:
Landslides are a phenomenon commonly found on the slopes of valleys and water bodies, as well as areas of rivers, embankments and slopes of excavations. Sudden landslides in these areas can be monitored using photogrammetric technique. The aim of this paper is to present the possibility of close-range photogrammetry (CRP) and terrestrial laser scanning (TLS) to conduct monitoring of surface changes that have taken place due to geodynamic processes. The studies were conducted on a 22-m section of the Vistula River scarp in P³ock. Terrestrial images, taken three times every six months, as well as terrestrial laser scanner measurements were used to determine the morphological changes occurring on a portion of the Vistula River scarp in Płock in one year. Based on the measurements, a thick cloud of points and a three-dimensional terrain model of the area of interest were obtained each time. Next, a comparative analysis of models taken at different times was carried out. Results of measurements allowed demonstrating the overall stability of the slope, i.e. the lack of morphological changes in the analysed period, with minor changes in some of its regions (loss of soil mass in the northern part and the growth in the southern part of the test area). The study shows that, in morphologically difficult areas, CRPcan provide information about the direction and magnitude of deformation, when changes are formed rapidly and contribute to large (at least several-decimetre) geodynamic changes.
Źródło:
Przegląd Geologiczny; 2016, 64, 7; 504--512
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Monitoring fotogrametryczny z wykorzystaniem bezzałogowego statku powietrznego na przykładzie osuwiska zlokalizowanego na zboczach poeksploatacyjnego zbiornika wodnego w KWB Adamów
Photogrammetric monitoring with the use of an unmanned aerial vehicle : case study of a landslide located on the slopes of a post-mining water reservoir in the KWB Adamów Mine
Autorzy:
Karwacki, Krzysztof
Powiązania:
https://bibliotekanauki.pl/articles/20064891.pdf
Data publikacji:
2022
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
monitoring osuwisk
fotogrametria UAV
odkrywkowa kopalnia węgla brunatnego
landslide monitoring
UAV photogrammetry
opencast lignite mine
Opis:
The article presents the results of monitoring of landslides related to opencast mining. The landslides formed on the slopes of an artificial water reservoir in the Adamów open-cast lignite mine. The photogrammetric method was used for monitoring. The study of landslide activity was performed on the basis of six photogrammetric surveys made with the DJI Phantom 4 Advanced UAV. Changes in the landslide extent and vertical displacements were determined in five measurement periods. For four periods, differential digital terrain models were made and the volume of displaced earth masses was calculated. The future extent of the landslide was determined on the basis of cracks visible in high-resolution optical photos. The research has shown that UAVs equipped with an optical camera are very useful in monitoring the stability of slopes of post-mining water reservoirs. The applied method provided detailed data on the size of displacements without compromising on safety of people involved in field surveys.
Źródło:
Przegląd Geologiczny; 2022, 70, 9; 671-681
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Badania monitoringowe wód podziemnych obszarów chronionych o różnym poziomie antropopresji
Groundwater monitoring surveys in protected areas of different anthropopressure level
Autorzy:
Krogulec, E.
Mikołajków, J.
Jóźwiak, K.
Powiązania:
https://bibliotekanauki.pl/articles/2074338.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
park narodowy
obszar chroniony
monitoring wód podziemnych
antropopresja
national park
nature reserves
groundwater monitoring
anthropopressure
Opis:
Results of supplementary hydrogeochemical analyses, conducted in the Kampinos National Park (KPN), its buffer zone and in the reserve “Bielany Forest” (“Las Bielański”) allowed revising the location of monitoring points and proposing a basic set of analyses of quality, ground-water level. This set includes measurements of physical-chemical parameters enabling to assess water quality and to define causes and consequences of groundwater chemical composition changes. Analyses of the water level monitoring results and selected hydrogeochemical indicators allows for assessment at antopopressure intensity. The survey results led to suggesting necessary range of physical-chemical tests and frequency of monitoring in affected areas under different antropopressure level.
Źródło:
Przegląd Geologiczny; 2005, 53, 6; 522--526
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zastosowanie testowych czujników pomiaru temperatury w quasi-przestrzennych (3D) sieciach pomiarowych w hydrotechnicznych budowlach ziemnych – wyniki wstępne
Application of testing temperature sensors for quasi-dimensional (3D) measurement systems used in measuring hydrotechnical earthworks–prelilinary results
Autorzy:
Borecka, A.
Sekuła, K.
Kessler, D.
Majerski, P.
Powiązania:
https://bibliotekanauki.pl/articles/2075719.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
testowy czujnik temperatury
wał przeciwpowodziowy
wyciek
monitoring termiczny
ISMOP
monitorowanie quasi-ciągłe (przestrzenne)
testing temperature sensor
levee (dike)
leakage
thermal monitoring
monitoring quasi-continuous (spatial)
Opis:
This paper presents the test point temperature sensors, designed for the ISMOP project. The point temperature sensors allow for full realization of spatial measurement by using a distributed measurement based on MESH type topology. The designed solutions described the selection and design of all elements of the sensors. It is also described how to install them at the existing levee. Applied construction and method of selection of the location of the point temperature sensors allow monitoring of levees in the quasi-spatial (3D) system, what is an alternative to termomonitoring performed by means of optical fibers.
Źródło:
Przegląd Geologiczny; 2017, 65, 10/2; 748--755
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zintegrowany system monitorowania wód podziemnych w Gdańsku i Sopocie
Integrated groundwater monitoring system in Gdańsk and Sopot
Autorzy:
Lidzbarski, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075477.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wody podziemne
monitoring wód podziemnych
system wód podziemnych
Gdańsk
groundwater
monitoring of groundwater
groundwater system of Gdańsk
Opis:
In the period 2009–2014, a groundwater monitoring system was organized in the area of Gdañsk and Sopot, integrating various types of observation networks, administrative units and respective groundwater circulation zones of the Gdañsk aquifer system. Three stages of research (diagnostic, operational, and research monitoring)resulted in a complete diagnosis of chemical and quantitative status of groundwater. The research was carried out on the basis of the existing observation network, groundwater intakes, and hydrogeological test boreholes drilled specially for this purpose. Such an approach to investigations provided many detailed data about changes in soil and water environment. Zones of past groundwater pollution were identified. The work has become the basis for activities that aimed at reducing the risks and improving the water management.
Źródło:
Przegląd Geologiczny; 2016, 64, 6; 375--381
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Historia monitoringu wód podziemnych w Państwowym Instytucie Geologicznym
History of the groundwater monitoring at the Polish Geological Institute
Autorzy:
Przytuła, Elżbieta
Mikołajczyk, Anna
Gidziński, Tomasz
Kuczyńska, Anna
Palak-Mazur, Dorota
Prażak, Jan
Woźnicka, Małgorzata
Wyszomierski, Michał
Cabalska, Jolanta
Galczak, Michał
Komorowski, Wojciech
Rojek, Anna
Powiązania:
https://bibliotekanauki.pl/articles/2075915.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
hydrogeologia
monitoring wód podziemnych
baza danych
Państwowy Instytut Geologiczny
hydrogeology
groundwater monitoring
database
Polish Geological Institute
Opis:
The Polish Geological Institute has been carrying out the tasks of the geological survey since its establishment in 1919. Hydrogeology was present from the very beginning and the groundwater monitoring became the systematic activity in the 2nd fifty years of the Institute’s life. Groundwater quantity monitoring expressed as measurements of groundwater table fluctuations was put into practice in 1972, while the groundwater quality monitoring that includes determination of chemical composition of water started in 1991. Both types of monitoring cover the entire area of Poland. Systematic hydrogeological observations and tests are one of the most important tasks carried out by hydrogeologists of the Polish Geological Institute. Results of these observations are used for many studies, analyses and forecasts carried out as part of the tasks of the hydrogeological survey, often in cooperation with universities and geological enterprises, for the needs of governmental and local administration and for reporting to the EU structures.
Źródło:
Przegląd Geologiczny; 2019, 67, 12; 982--994
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zagrożenia zbiorników wodnych wynikające z działalności człowieka na przykładzie Stawu Płaszowskiego w Krakowie
Threats to water bodies resulting from human activity : a case study of Płaszów Pond in Cracow
Autorzy:
Gawałkiewicz, R.
Powiązania:
https://bibliotekanauki.pl/articles/2075793.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
antropogeniczne zbiorniki wodne
katastrofa ekologiczna
monitoring geodezyjny
zasoby wodne
anthropogenic water bodies
ecological disaster
geodetic monitoring
water resources
Opis:
An exceptional group ofpost-mining excavations are those made as a result of the exploitation of Quaternary seams of natural aggregates. Their characteristic feature includes borrow pits, left after quarrying. They are going through the process of natural revitalization as a result of water table stabilization and the inflow of ground waters and precipitation waters, followed by the natural succession of aquatic vegetation. Plaszów Pond in Cracow-Plaszów is located close to the city centre, in its attractive region. The attractiveness of the adjacent areas can also have a negative effect on the water resources and the ecosystem. The results of geodetic monitoring of water resources show that the situation during the first three months of 2016 had symptoms of ecological disaster.
Źródło:
Przegląd Geologiczny; 2018, 66, 1; 38--47
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Możliwości zastosowania zdalnego systemu monitoringu wgłębnego i powierzchniowego osuwisk w kopalni odkrywkowej węgla brunatnego na podstawie badań wykonanych w KWB Bełchatów w ramach projektu UE RFCS Slopes
Possibilities of implementation of remote in situ and surface displacement landslide monitoring in lignite opencast mine based on the research conducted within the EU RFCS Slopes project
Autorzy:
Bednarczyk, Zbigniew
Powiązania:
https://bibliotekanauki.pl/articles/2076151.pdf
Data publikacji:
2021
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
monitoring geologiczno-inżynierski
stabilność zbocza
kopalnia odkrywkowa węgla brunatnego
geological engineering monitoring
slope stability
opencast lignite mine
Opis:
Landslides in Polish opencast lignite mines are a serious problem for the efficiency of exploitation. They can also pose a threat to adjacent areas and the environment, and in some cases even jeopardize the continuity of lignite supplies to power plants. Such phenomena are associated with a number of factors, the most important of which are the geological engineering structure, groundwater conditions, unfavourable strength parameters of clayey soils and their usually relatively steep slopes. Counteracting such a phenomena, caused by mining activity, is usually difficult because of large size of landslides and the depth of exploitation reaching in some cases over 300 m. The paper presents the first application of on-line monitoring in a Polish opencast lignite mine. Performed in the Bełchatów Mine, in situ monitoring was complemented by satellite radar interferometry (PSI), LiDAR airborne laser scanning, and terrestrial laser scanning. Research within the RFCS EU SLOPES project “Smarter Lignite Open Pit Engineering Solutions” was performed by an international consortium from six European countries. In Poland, the research was located mainly on the western slope of the Bełchatów Field. In this area, in the Polish open pit lignite mine, on-line inclinometer, and a pore pressure monitoring system were the first located at the levels of+42 : -58 m a.s.l. Geological engineering investigations included 100 m depth core drilling, index laboratory tests, IL oedometer tests, CIU, CID triaxial tests, and numerical modelling. The total amount of in situ displacement, during the period December 2016-July 2019, reached 290 mm. The largest displacements up to 250 mm were recorded: to a depth of 45 m in the direction of slope inclination, and smaller ones up to 50 mm to a depth of 72.5 m. The displacements were accompanied by a decre ase in pore pressure values by more than 200 kPa. In other parts of the mine and adjacent areas, the satellite radar interferometry detected displacements up to 60 mm/year on the outer slopes of the Szczerców dump. It also allowed identification of the landslide hazard in other areas. Data obtained from in-situ monitoring and laboratory tests on the western slope of the Bełchatów Field were included in numerical modelling using the shear strength reduction method and the limit equilibrium method. This should allow helping for better recognition and warning of the existing hazards in the investigated area.
Źródło:
Przegląd Geologiczny; 2021, 69, 12; 785--799
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 55

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