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Tytuł:
Jeziora Parku Narodowego Pojezierze Smoleńskie (Rosja)
Lakes of the Smolensk Lakeland National Park (Russia)
Autorzy:
Skrzypczak, Robert
Powiązania:
https://bibliotekanauki.pl/articles/2076005.pdf
Data publikacji:
2020
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Jeziora Smoleńskie
Park Narodowy
erozja
akumulacja lodowca
aktywność wody lodowcowej
wieczna zmarzlina
kras
Smolensk Lakeland lakes
National Park
erosion
glacial accumulation
glacial water activity
permafrost
karst
Opis:
The Smolensk Lakeland National Park is situated north of Smoleńsk in the NW Russia. Its morphology is associated with the last European ice sheet: glacial erosion and accumulation, glacial water activity, locally with the so-called thermokarst process or karst in the strict sense. The post-glacial morphological depressions are filled with lake waters. The most interesting lakes are: Chistik, Mutnoye, Balshoye and Maloye Striechnoye, Glubokoye, Dolgoye, Krugloye, Pietrovskoye, Bukino, Gorodishche, Svyatec, Sapsho, Polovia, Gniloye, Rytoye, Dgo, Shchuch’ye, Baklanovskoye, Bachovskoye, Vervizhskoye, Pal’tsevskoye and Bieloye. The Smolensk Lakeland National Park is one of a few territories in Europe where the beauty of nature and landscapes dominate the long-standing human presence. Nowadays, there are a few residents, a growing number of patients, seasonal campers and tourists in the park area.
Źródło:
Przegląd Geologiczny; 2020, 68, 1; 50--53
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rzeźba strukturalna obszaru Świętokrzyskiego Parku Narodowego
Structural morphology of the area of the Świętokrzyski National Park
Autorzy:
Łajczak, Adam
Urban, Jan
Rączkowska, Zofia
Wałach, Grzegorz
Powiązania:
https://bibliotekanauki.pl/articles/2076052.pdf
Data publikacji:
2020
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
morfologia strukturalna
pasma wzgórz
gołoborza
turnie
Góry Świętokrzyskie
structural morphology
hill ranges
block fields
crags
Holy Cross Mountains
Opis:
The area of the Świętokrzyski National Park is one of the most evident examples of structural morphology in Poland. Its relief is clearly determined by bedrock lithology: the hill ranges are composed of hard quartzitic sandstones of the upper Cambrian (Łysogóry Range) and the Lower Devonian (Klonowskie Range), while the depressions, usually vast and flat-bottomed, are distributed on outcrops of soft, easily weathered and eroded Ordovician and Silurian shales, greywackes and sandstones. The parallel pattern of hill ranges and depressions, as well as a mesh-grid pattern of river valley systems and the antecedent character of river gaps, reflects fold tectonics modified by transverse faults. Such a morphology developed during the Paleogene and Neogene under hot and then warm, gradually cooling climatic conditions. In the Pleistocene, principally under the periglacial conditions, block fields (symbols of the Świętokrzyski NP) and crags (crests, table-like forms, cupolas and spurs) were formed. The shape and spatial position of most crags are related to geological structures.
Źródło:
Przegląd Geologiczny; 2020, 68, 2; 102--111
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Karkonoski Park Narodowy z otuliną jako geopark krajowy
Karkonosze National Park with its buffer zone certified as the National Geopark
Autorzy:
Knapik, R.
Migoń, P.
Powiązania:
https://bibliotekanauki.pl/articles/2074725.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
georóżnorodność
geostanowiska
edukacja geologiczna
Karkonosze
geodiversity
geosites
geoeducation
Karkonosze Mts.
Opis:
The Certificate of National Geopark for the Karkonosze National Park with its buffer zone reflects the policy of the Ministry of Environment, which aims to create a network of national geoparks in Poland. It is also a consequence of conducting by the Karkonosze National Park the project "Geosites inventory and assessment in the Karkonosze National Park and its buffer zone, including preparation of the geological map of the area", which provided solid scientific basis for the recognition of Karkonosze Mts. as national geopark. The certificate highlights the geodiversity of the Karknosze Mts., which parallels its biodiversity values and is decisive for the great attractiveness of the area among the scientists and visitors alike. Features such as mountain-top planation surfaces, glacial cirques, granite tors, and waterfalls have been invariably listed as the key elements of geoheritage of the Karkonosze Mts. Less obvious, but no less important are various mineralogical localities, exposures of granite and metamorphic rock which provide insights into the nature of igneous and rock deformation processes in the Palaeozoic era, peat bogs bearing record of palaeoenvironmental change, and remains on past mining and mineral prospecting. Geodiversity of the Karkonosze Mts. is well-documented in dozens of scientific publications, but also also consistently exposed by the Karkonosze National Park and other institutions, through wide-ranging activities of popularizing geoheritage of these mountains.
Źródło:
Przegląd Geologiczny; 2010, 58, 11; 1065-1069
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Azot mineralny w płytkich wodach podziemnych Kampinoskiego Parku Narodowego
Inorganic nitrogen in the shallow groundwater of the Kampinoski National Park
Autorzy:
Jóźwiak, K.
Powiązania:
https://bibliotekanauki.pl/articles/2075373.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
amoniak
azotyny
azotan
procesy hydrogeochemiczne
ammonia
nitrite
nitrate
hydrogeochemical processes
Opis:
The presence of mineral forms of nitrogen in the ground waters of the Kampinoski National Park (KPN) varies considerably. The research results have shown that during the nitrogen changes within the active exchange zone, nitrification processes prevail in the KPN area and the surroundings. Denitrification processes occurs as second-rate mainly to the swamp environment. The type and intensity of specific processes depends on the genesis of the environment concerned, the content of oxygen and redox conditions. The analysis of the concentration of mineral nitrogen forms can be used to asses the degree of anthropopressure in the area of the park itself and its protection zone.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/1; 791--795
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Chemizm wód źródeł w zlewni Markowego Potoku, Babiogórski Park Narodowy
Chemical properties of springwater in the Marków Potok catchment, Babiogórski National Park
Autorzy:
Malata, M.
Motyka, J.
Powiązania:
https://bibliotekanauki.pl/articles/2075256.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
chemia wody
zlewnia
sprężyny
Babiogórski Park Narodowy
water chemistry
catchment
springs
Babiogórski National Park
Opis:
The purpose of this paper is to describe the variability of the chemical characteristics of springwater in the Marków Potok catchment. Five springs were selected for research purposes. The research was performed in spring and summer 2013 and 2014. Ca was found as the most common cation, HCO3 was the most common anion and NO3 was dominated in the biogenic compounds in the analysed springwater. Comparing the period of spring and summer the highest values of most of the chemical characteristics of water occurred in the summer, the lowest in the spring. It was found that chemical properies of water springs were shaped by the diverse geological structure of the catchment area, climatic conditions, the process of dilution and the biological activity of the basin.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 912--918
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:
Identyfikacja procesów kształtujących skład chemiczny wód podziemnych poniżej torfowiska-Pożary, Kampinoski Park Narodowy
Identification of processes controlling groundwater chemistry below peatland-Pożary, Kampinos National Park
Autorzy:
Porowska, D.
Leśniak, P. M.
Powiązania:
https://bibliotekanauki.pl/articles/2074572.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
skład chemiczny wód podziemnych
hydrogeologiczno-chemiczny proces
denitryfikacja
torfowiska
groundwater chemistry
hydrogeochemical processes
denitrification
peatlands
Opis:
The aim of this study was to identify hydrogeochemical processes controlling chemical composition of groundwater of the existing peatland. The site of the study is located within the Pożary Special Protection Area of the Kampinos National Park. Lithological profilem consists mainly of varigrained sand, covered by organic matter constituting peatland. The groundwater table fluctuates between 0.6 m below and 0.3 m above ground level. Combination of high organic content of soil profile and shallow depth to the water table causes slightly reducing conditions, especially in the upper part of aquifer. There, oxidation of organic matter (and/or methane) as well as nitrate and sulphate reduction has been presumed while denitrification and/or dissimilatory nitrate reduction to ammonium (DNRA) seems to control chemistry of groundwater in deeper part of the profile. The important differences in the chemical and isotopic composition of dissolved carbon have been found in the depth profile. Carbon isotopic composition of dissolved inorganic carbon in groundwater (13CDIC) indicates that carbonate carbon is derived mostly from the decomposition of organic matter, a small contribution being derived from the dissolution of carbonate minerals. The contribution of atmospheric CO2 to chemical and isotopic composition of dissolved carbon is negligible within all parts of aquifer.
Źródło:
Przegląd Geologiczny; 2008, 56, 11; 982-990
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wpływ wybranych torfowisk na kształtowanie składu chemicznego płytkich wód podziemnych Drawieńskiego Parku Narodowego
Influence of selected peat bogs Drawa National Park on the formation of the chemical composition of shallow groundwater
Autorzy:
Ścibior, K.
Rydelek, P.
Stępień, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075246.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
hydrochemia
torfowisko
torf
Drawieński Park Narodowy
hydrochemistry
peatland
peat
Drawa National Park
Opis:
This article attempts to determine the impact of peatlands on the chemical composition and selected parameters of shallow groundwater in Drawa National Park. Three peat bogs were selected for testing: Miradz, Wydrowe Łęgi and Głodne Jeziorka. They differ from each other in terms of origins, botanical composition and properties of peat. 55 samples of organic soils (including 41 peat samples) and 17 groundwater samples were collected. The samples came from layers of peat bogs and peatlands situated directly beneath and in the immediate vicinity. During the laboratory tests are shown in the basic physicochemical parameters of the peat: ash content (AC), cation exchange capacity (CEC), pH, moisture. In addition, the data on SRT and their botanical composition marked in the course of fieldwork have been verified. Directly in the field pH, PEW and water temperatures were examined. In the groundwater samples were determined concentrations of ions HCO3, SO4, NO3, Cl, PO4, Ca, Mg, Na, K, Fe, Mn, Al, Si and other selected metals. The results showed that the peat bogs of different genesis in a different way influence the shaping of the chemical composition of shallow groundwater. Especially significant differences indicate if compared to the peat bog Miradz, Wydrowe Łęgi in opposition to Głodne Jeziorka. Groundwater from the Głodne Jeziorka and direct neighborhoods showed a much lower pH, conductivity and mineralization.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 1099--1104
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geopark Karkonosze - georóżnorodność i geoturystyka
Karkonosze Geopark - geodiversity and geotourism
Autorzy:
Knapik, R.
Migoń, P.
Szuszkiewicz, A.
Aleksandrowski, P.
Powiązania:
https://bibliotekanauki.pl/articles/2074854.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Karkonoski Park Narodowy
ochrona przyrody
geostanowiska
Karkonosze National Park
nature protection
geosites
Opis:
The Certificate of a National Geopark was awarded to the Karkonosze National Park, along with its buffer zone, in September 2010. Geodiversity of the Karkonosze Mountains, subject to the comprehensive assessment in 2008-2009, resides mainly in the variety of geological, mineralogical and geomorphological phenomena. In addition, the legacy of mining and mineral prospecting is abundant. Many of the natural phenomena make the Karkonosze Mountains an exceptional area in Poland, and are of outstanding value if considered within the European context. The value of abiotic nature of the Karkonosze is promoted through multiple activities in the field of geotourism and ecological education, including construction of an extensive network of geosites, marked tourist paths, and educational trails with information boards. Further promotion of geodiversity of the Karkonosze is carried out in cooperation with the adjacent Krkonošský narodní park on the Czech side of the mountains, aiming at an establishment of a bilateral Polish-Czech Geopark Krkonoše/Karkonosze, within the framework of the European Geopark Network.
Źródło:
Przegląd Geologiczny; 2011, 59, 4; 311-322, 360
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Skład chemiczny wód podziemnych i powierzchniowych w zlewni Świerszcza (Roztoczański Park Narodowy)
The chemical composition of groundwater and surface water in the Świerszcz catchment area (Roztocze National Park)
Autorzy:
Malata, M.
Motyka, J.
Radliński, B.
Rogala, A.
Sokołowski, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075627.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Roztoczański Park Narodowy
Świerszcz
skład chemiczny
wody podziemne
wody powierzchniowe
Roztocze National Park
chemical composition
groundwater
surface water
Opis:
The aim of the study was to evaluate the status of the aquatic environment in the Świerszcz Basin in the Roztocze National Park. Within the framework of the measuring programs (conducted in 2011-2015) we performed F2 groundwater and H1 river and indicator studies conducted in 2014-2015, chemical analyses of major cations, anions, micronutrients, and analyses ofselected physical characteristics of groundwater and surface waters. Due to the exceedances of NO3, PO4, Tl, Se, Mo and Al concentrations in the water from springs and wells during the indicator surveys, it was assessed to require purification. The high levels o NO3 and PO4 testify to the effect of anthropoprotection, while the high content of the remaining components is most probably due to natural geochemical processes.
Źródło:
Przegląd Geologiczny; 2017, 65, 11/2; 1319--1328
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Potencjał geoturystyczny wybranych obiektów Ojcowskiego Parku Narodowego i jego otuliny
Geotouristic potential of selected objects in the Ojców National Park and its protected zone area (S Poland)
Autorzy:
Dzięgiel, Maciej
Powiązania:
https://bibliotekanauki.pl/articles/20204843.pdf
Data publikacji:
2023
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
geoturystyka
Oksford górnojurajski
skalisty wapień
kras
tuf wapienny
less
geotourism
Upper Jurassic Oxfordian rocky limestone
karst
calcareous tufa
loess
Opis:
In this paper, two scenic caves, five selected karst rock forms, and five rock outcrops situated in the Ojców National Park and its protected zone area are the subject of comparative research, considered as very essential examples of geotouristic potential. Most of their karst forms differ between each other. These include Łokietek and Ciemna (Dark) cave, Kraków Gate, Rękawica and Igła Deotymy rock-cliff at Ojców, Duży Pochylec rock-cliff in Skała, and Maczuga Herkulesa rocky tower at Pieskowa Skała. Apart from them, outcrops of Quaternary calcareous tufa and rock falls at Ojców, an abrasion surface cutting Upper Jurassic limestones and covered with Cretaceous limestones and marls, Pleistocene loess at Januszowice, and the Duże Skałki (Big Rocks) former quarry of Upper Jurassic limestone at Czajowice were also studied. All of them are situated in the Silesian-Kraków Monocline. The caves, rock-cliffs and Maczuga Herkulesa rocky tower developed in the Upper Jurassic Oxfordian massive limestone. Their karst forms are diverse and picturesque. The other objects selected for research are also very interesting and important examples, displaying products of very complex geological processes. The comparative geotouristic potential evaluation of all 12 objects was made to meet tourists', educators' and investors' expectations and needs to increase their geotouristic development level. The statistical data of the annual number of visitors at the described two caves is also discussed. In general, interest in them as geotouristic abiotic nature objects has been growing regularly until today. They have become very widely known in Poland. Moreover, the Łokietek Cave, Kraków Gate rock-cliff and Maczuga Herkulesa rocky tower have become very popular worldwide.
Źródło:
Przegląd Geologiczny; 2023, 71, 3; 113-131
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Głazy narzutowe Drawieńskiego Parku Narodowego i ich znaczenie w rozwoju lokalnej geoturystyki
Erratic boulders of the Drawa National Park (NW Poland) and their role in the development of local geotourism
Autorzy:
Górska-Zabielska, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075465.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
głazy narzutowe
georóżnorodność
dziedzictwo geologiczne
geoturystyka
Drawieński Park Narodowy
erratic boulders
geodiversity
geological heritage
geotourism
Drawa National Park
Opis:
The major attraction of the Drawa National Park is its main river, the Drawa. However, the park includes also other georesources that have a large natural potential to become geovalues, received by tourists as its geoproducts. This may lead to develop geotourism, which is a tool of sustainable socio-economic development of the region. The article presents the erratic boulders, which are primarily the objects of geological heritage. Erratic material is also present in the cultural heritage of the region, e.g. in the churches, cobbled roads, hydraulic engineering constructions or as stone monuments, signposts, and forest departmental posts.
Źródło:
Przegląd Geologiczny; 2016, 64, 10; 844--847
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:
Zmiany wydajności monitorowanych źródeł w Pienińskim Parku Narodowym w latach 2003–2014 (pieniński pas skałkowy)
Variation of springs discharge in Pieniny National Park in the years 2003–2014 (Pieniny Klippen Belt)
Autorzy:
Humnicki, W.
Powiązania:
https://bibliotekanauki.pl/articles/2075386.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wydajność źródeł
Pieniński Park Narodowy
Pieniński pas skałkowy
spring discharge
Pieniny National Park
Pieniny Klippen Belt
Opis:
The paper presents the 12-years discharge variations of the three springs located within the Pieniny National Park. The background was the observations of the water table variation in the springs and seasonal measurements of the springs discharge, which made the possibility of calculation of the rating curves. Generally, the Pieniny springs are characterized by low discharge. The mean discharge of the springs studied for the period 2003–2014 was as follows: spring of the Potok pod Wysoki Dział – 1.66 dm3s‒1, spring of the Kotłowy Potok – 0.26 dm3s‒1, seasonal spring of the Kirowy Potok – 0.10 dm3s‒1. Variations of the springs discharge are different due to the fact that particular spring drain separate, and relatively small groundwater reservoir. First of all, the influence of the many-years variation in the sum of atmospheric precipitation as well as the amount of infiltrating meltwater can be observed. Observations with monthly distribution showed the characteristic shift between maximum discharge of the spring and the sum of atmospheric precipitation (about 1 month shift) as well as the thawing period (1–3 months shift). Presumably, during dry seasons the springs have mainly the thawing regime, in the normal (balanced) seasons – the thawing-precipitation regime is dominant, and during the wet season – the precipitation-thawing regime prevails. In the years 2012 and 2013 the sudden decrease of discharge of the Kotłowy Potok and Kirowy Potok springs have been observed which is in well agreement with the hydrogeological drought identified in Poland.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/1; 750--755
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ocena podatności na zagrożenia wód podziemnych metodą DRASTIC we wschodniej części Drawieńskiego Parku Narodowego
Vulnerability assessment to contamination of groundwater of the eastern part of Drawa National Park by DRASTIC method
Autorzy:
Stańczak, E.
Powiązania:
https://bibliotekanauki.pl/articles/2075223.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
DRASTIC
Ocena podatności
analiza GIS
wody gruntowe
Drawieński Park Narodowy
vulnerability assessment
GIS analysis
groundwater
Drawa National Park
Opis:
In article shown question vulnerability to contamination, natural characteristic of groundwater, for the eastern part of Drawa National Park (DNP). To vulnerability assessment used usually known range DRASTIC method. Based on input data determined pixel size of map Δx = Δy = 50 m. The DRASTIC parameters were exactly checked. One of the most important recharging infiltration (162.5 mm/year), compared with result of hydrological method. It shown similar value and this data are reliable. By means of GIS analysis calculated the DRASTIC index. Visualization superficial distribution of classes of vulnerability is shown as map of groundwater vulnerability. The results indicate that more than 90% study area is located high vulnerability class.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 1074--1079
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 22

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