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Tytuł:
Organizacja monitoringu badawczego i jego znaczenie dla oceny stanu jednolitych części wód podziemnych i programów służących osiągnięciu celów środowiskowych
Organizing the groundwater monitoring and its significance for the assessment of groundwater body conditions and projects performed to achieve environmental objectives
Autorzy:
Prażak, J.
Woźnicka, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075426.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wody podziemne
monitoring
części wody podziemnej
groundwater
groundwater bodies
Opis:
Groundwater research monitoring, organized and carried out by the Polish Hydrogeological Survey since 2009, has been aimed at providing details on the quantitative and chemical conditions of groundwater bodies (GB) in areas of large-scale impact of mining activities and urban-industrial agglomerations. It is intended to provide information on the analysis of pressions and actual impacts on groundwater to assess the condition of groundwater bodies and to develop action programmes to achieve environmental objectives. Currently, it already operates in eight areas of mining impact, and, in the nearest future, it will cover the Basznia sulphur mining area as well as seven urban-industrial agglomerations.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 1021--1026
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zróżnicowanie mikrobiologiczne w wodach podziemnych granitu Karkonoszy
Microbiological diversity in groundwater of the Karkonosze granite
Autorzy:
Marszałek, H.
Górniak, D.
Toczek, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075768.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wody podziemne
mikroorganizmy
granit karkonoski
groundwater
microorganisms
Karkonosze granite
Opis:
The Karkonosze granite massif contains groundwater with various depths of flow systems. In the mountainous part, fresh water predominates, mainly of local flow, where as in the Jelenia Góra Basin thermal waters have been found, reaching the temperature of 97°C. In nine samples of groundwater representing different flow depths, we have described a variation in the parameters of the structure and biodiversity of prokaryotes (bacteria and archaea). The variability of prokaryotes is determined by pH, Eh, electrolytic conductivity and temperature of water.
Źródło:
Przegląd Geologiczny; 2017, 65, 11/1; 1121--1125
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wyniki pilotażowego badania zawartości substancji czynnych farmaceutyków w wodach podziemnych w próbkach wody pobranych z krajowej sieci monitoringu wód podziemnych
Results of a pilot study on the assessment of pharmaceuticals in groundwater in samples collected from the national groundwater monitoring network
Autorzy:
Kuczyńska, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075601.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wody podziemne
zanieczyszczenia wód podziemnych
farmaceutyki
groundwater
groundwater pollution
pharmaceuticals
Opis:
This article presents the results of a pilot study on the content ofpharmaceuticals and hormones in groundwater samples taken from the national groundwater monitoring network of the Polish Geological Institute - National Research Institute. Samples were collected during the surveillance monitoring of groundwater bodies in 2016 from selected 93 groundwater monitoring sites and analysedfor a total of 31 active substances. These active substances contained compounds from the following groups of drugs: natural and synthetic oestrogen hormones, cardiovascular and respiratory medications, analgesics and anti-inflammatories, antidepressants, antimicrobial drugs and anti-epileptics. The study confirmed the presence of pharmaceuticals in 63% of groundwater samples taken.
Źródło:
Przegląd Geologiczny; 2017, 65, 11/1; 1096--1103
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Polska w projekcie World Karst Aquifer Mapping Project (WOKAM)
Poland in World Karst Aquifer Mapping Project (WOKAM)
Autorzy:
Różkowski, J.
Grabala, D.
Polonius, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075436.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wody krasowe
wody podziemne
źródła krasowe
jaskinie
karst aquifers
groundwater
karst springs
caves
Opis:
The article presents World Karst Aquifer Mapping Project (WOKAM). The goal of this project, implemented in 2012– 2015, is to establish the first karst aquifer world map, presenting karst aquifers, most important water intakes, karst springs and caves. Selection criteria of the karstic objects were discussed in the paper. Database, created on their basis covering the area of Poland, includes: 17 water intakes (extracting mainly from the Triassic carbonate aquifer of Silesian – Kraków monocline), 7 springs (including 5 vaucluses from Tatra Mountains), 23 caves (located mainly in Western Tatra Mountains and in Kraków – Wieluń Upland). There is a probability of location of individual hydrogeological objects from Poland on the world karst aquifer map considering the importance of the region.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 1042--1046
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Infiltracja do wód podziemnych na podstawie pomiarów lizymetrycznych w Górach Sowich
Groundwater infiltration based on lysimeter measurements in the Sowie Mountains (SW Poland)
Autorzy:
Staśko, S.
Chodacki, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075158.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
infiltration
lysimeter method
groundwater
Sudetes
infiltracja
metody lizymetryczne
wody podziemne
Sudety
Opis:
Field research on effective infiltration has been carried out in the Sowie Mountains area in the Sudetes Mountains (SW Poland) in a lysimeter installed 0.9 m below the surface of the ground in a forest. The annual rainfall in 2011 has been measured in the range 520.9–644.8 mm for the three station, while the average precipitation of the long term observation indicate 880 mm. Air temperature was 2°C higher during experiment period from the typical to the region. During annual study (from April 2011 to May 2012) it has been measured effective infiltration volume as 78.1 mm of water in comparison total precipitation of 596.7 mm in nearest station. Groundwater recharge by infiltration is changing during the year as well as in longer period, occurs mainly in cool season (spring, autumn) and indicate impulsive nature. The highest rate was reported in the October-November period, infiltration has exceeded the 30% of the precipitation, what could be explained by the high degree of saturation of the aeration zone. The departure value recorded in the summer relates to the degree of saturation of the aeration zone and there is high rainfall of the order of 200 mm. Then at the turn of July and August there has been measured a 54 mm percolating water. However, in August and September when rainfall over 107 mm water percolation was only 0.5 mm. Recharge and water supply in summer precipitation requires an initialization precipitation value order of 30–50 mm to supplement the state of moisture contains and high transpiration of plants. Infiltrating water showed of nitrate-sulphate-bicarbonate-calcium-sodium chemical type. In the process of infiltration increase of total dissolved solids almost twice has been measured.Water are enriched in the ions+, Mg2+, K+, Ca2+, Cl–, NO3–, SO42– is observed while the reduction of the concentration of HCO3–and NH4+. Chemical water composition is quite similar to the water in the stream located close to the lisymeter point.
Źródło:
Przegląd Geologiczny; 2014, 62, 8; 414--419
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Charakterystyka występowania mikroskładników w lokalnych systemach przepływu wód podziemnych w środowisku skał węglanowych i siarczanowych Niecki Nidziańskiej
Characteristic of occurrence minor elements in the local systems of ground water in the sulphate and carbonate rocks environment Nida Basin
Autorzy:
Jóźwiak, K.
Różkowski, J.
Powiązania:
https://bibliotekanauki.pl/articles/2075423.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
mikroskładniki
wody podziemne
gips
środowisko wapienia
minor elements
groundwater
gypsum
limestones environment
Opis:
The paper presents variability of minor elements in fissured-karst waters (aquifer in gypsum and limestones rock of Neogene) and fissured waters (aquifer in marls of Upper Cretaceous) of Nida Basin in Southern Poland, which were sampled in the April 2011. Laboratory analyses of 26 minor elements in groundwaters (Ag, Al, As, B, Ba, Br, Be, Cd, Co, Cr, Cu, Hg, Li, Mn, Mo, Ni, Pb, Sb, Se, Sr, Tl, V, W, Zn, Zr and Fe), that are present in mostly in cationic form, were analysed the Acme Analytical Laboratories in Vancouver (Canada). Concentration of these components was determined with use of ICP-MS (inductively coupled plasma mass spectrometry) and ICP-AES (inductively coupled plasma atomic emission spectroscopy) using Plasma-40. The relations between the content of the analysed minor elements about very diverse of mobility in the groundwaters of local systems in the sulphate and carbonate rocks environment were discussed.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/1; 796--800
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Evolution of Polish hydrogeology
Autorzy:
Kozerski, B.
Paczyński, B.
Sadurski, A.
Skrzypczyk, L.
Powiązania:
https://bibliotekanauki.pl/articles/2066341.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
polska hydrogeologia
historia hydrogeologii
wody podziemne
Polish hydrogeology
history of hydrogeology
groundwater
Opis:
In Poland, hydrogeology as a separate scientific discipline came into being at the end of the 19th century. The first geologists were interested in springs, saline, mineralised waters of therapeutic use and dewatering of mines. Until World War I, in the early stages of hydrogeological developments, a different attitude towards groundwater problems was clearly notable in all three annexed Polish territories. The next stage of the development of Polish hydrogeology is dated to the years 1918-1939. In those times, the major focus of hydrogeological investigations was on building structures to extract artesian groundwater; mineral groundwater in the Polish spas; building municipal water intakes; and on Quaternary aquifers, widespread in Poland. Early hydrogeological handbooks were published at those times. The contemporary stage of Polish hydrogeology started in 1945, after World War II. In the early 1950s, the Department of Hydrogeology and Engineering Geology was established at the Central Board of Geology (CUG in Polish), which belonged to the Polish government as a separate ministry up to 1970. Hydrogeological companies with technology and development sections were founded in big cities. Nowadays, academic centres exist in Warsaw, Cracow, Wrocław, Gdańsk, Sosnowiec, Poznań, Kielce and Toruń. About 1400 persons with academic diplomas, 160 doctors and 22 professors of hydrogeology are active at present in the field of hydrogeology. The principal fields of Polish hydrogeology comprise the following: mine dewatering, recognition of groundwater resources and their protection, construction and exploitation of water intakes, hydrogeological cartography, mineral and thermal water resources, regional hydrogeology for physical planning, groundwater modelling and groundwater pollution, migration of pollutants and forecasting of groundwater changes. Up to the late eighties, political censorship was the main difficulty for the development of Polish hydrogeology, especially in publications related to sensitive information of groundwater occurrence and resources.
Źródło:
Przegląd Geologiczny; 2010, 58, 9/1; 730-736
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Modernizacja bazy danych GIS „Zasoby dyspozycyjne wód podziemnych” : założenia metodyczne, aktualny stan realizacji
Modernization of the GIS database of the available groundwater resources : methodological assumptions and current state of development
Autorzy:
Mordzonek, G.
Przytuła, E.
Powiązania:
https://bibliotekanauki.pl/articles/2075435.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wody podziemne
dyspozycyjne zasoby
baza danych GIS
groundwater
available resources
GIS database
Opis:
A nationwide research program, which includes hydrogeological documenting of available groundwater resources in areas previously undocumented, is being currently implemented at the Polish Geological Institute – National Research Institute at the request of the National Water Management Authority. One of the program’s tasks is modernization (update) of the GIS database maintained by the Polish Hydrogeological Survey (PHS) since 2008. The article presents the current status of work on the modernization of the database of available groundwater resources. This database will be the primary and reference material for the use of the results of information on groundwater disposable resources for the implementation of standard procedures, UE reports and other multidisciplinary studies, including preparation of the water management balance sheets and the rules of water utilization in water region and drainage basin. The Polish Geological Institute is the main executor and coordinator of this task.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 955--957
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Potencjalnie lecznicze wody radonowe Masywu Ślęży
Potentially therapeutic radon waters of Ślęża Massif
Autorzy:
Przylibski, T. A.
Fijałkowska, L.
Bielecka, A.
Powiązania:
https://bibliotekanauki.pl/articles/2074598.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
radon
222Rn
wody podziemne
wody radonowe
groundwater
radon water
medicinal water
potential therapeutic water
Opis:
The authors have conducted research on radon occurrence in the groundwater system of Ślęża Massif in the Fore-Sudetic block. The research included documenting occurrence of radon waters in the granitoids of Strzegom-Sobótka Massif, buildingNWandWslopes of Ślęża. Among several springs flowing out from the granitoids and their waste, the Klasztorne Spring is characterized by constant radon (222Rn) concentration (306 ±39 Bq/dm3), but also constant though small discharge during the year, which enables estimating the admissible volume of this spring at 0.3 m3/h. The results obtained during the research show that this water can be treated as potentially medicinal. It generates the opportunity for the nearby town of Sobótka to develop as a health resort. Confirming the presence of radon groundwater in the granitoid part of Ślęża Massif implies a great probability that such w occur in the whole area of the Strzegom-Sobótka intrusion. It opens possibilities of recognizing new resources of potential therapeutic water and entails the necessity to take suitable actions for radiological protection of people living in this area.
Źródło:
Przegląd Geologiczny; 2008, 56, 8/2; 763-771
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Oddziaływanie termiczne budynku wielkogabarytowego na wody podziemne w rejonie stacji badawczej Uniwersytetu im. Adama Mickiewicza w Poznaniu
Thermal impact of large-size building on groundwater in the area of Adam Mickiewicz University research station
Autorzy:
Okońska, M.
Oleksiewicz, M.
Marciniak, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075429.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
temperatura
wody podziemne
ciśnienie
oddziaływanie termiczne
Naramowicki Sandr
temperature
groundwater
anthropopressure
thermal impact
Opis:
During the groundwater monitoring in the area of AMU Faculty of Geographical and Geological Sciences research station, increased water temperature in observation wells located in the vicinity of the building has been reported. In the article the thermal impact degree of buildings on groundwater in the research area was determined. For this purpose, (1) the water temperature measurements in various observation wells for 2002–2015 were summarized; (2) the hydraulic conductivity values of the aquifer determined by field method in two periods of building activity were compared; (3) temperature distribution profiles in the selected observation wells were done, and (4) thermography images of the research object were made. There was also calculated the amount of heat Q emitted into the environment by building complex. The study used data from the observation well located inside the WNGiG building.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 985--991
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Czynniki określające stężenia i stosunki aktywności izotopów radu w wodach podziemnych
Factors controlling concentrations and activity ratios of radium isotopes in groundwaters
Autorzy:
Chau, N. D.
Kopeć, D.
Powiązania:
https://bibliotekanauki.pl/articles/2074778.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wody podziemne
jony
litologia
groundwater
radium isotopes
Monte-Carlo method
ion composition
lithology
Opis:
Factors controlling concentration and activity ratios of radium isotopes in groundwaters are presented. The influence of lithology, hydrological conditions and chemical composition of groundwaters on radium content is discussed. Based on simple model of adsorption/desorption processes in the rock-water system, the numerical model of evolution of radium isotopes content was developed using Monte-Carlo (MC) method. Assuming that the waters are of similar age and occur under similar conditions, one can state that concentrations of radium isotopes are the highest in Na-Cl type waters, intermediate in waters with predominant carbonate mineralization, and the lowest in sulfate-type waters. In water with predominant Na-Cl mineralization the 226Ra concentration should be higher than that of 228Ra, whereas in sulfate waters this relation is inverse.
Źródło:
Przegląd Geologiczny; 2010, 58, 6; 499-505
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Podatność naturalna i specyficzna wód podziemnych na obszarach rolniczych
Intrinsic and specific groundwater vulnerability in the agricultural areas
Autorzy:
Zabłocki, S.
Powiązania:
https://bibliotekanauki.pl/articles/2075260.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wrażliwość
wody podziemne
zagospodarowanie terenu
rolnictwo
azotany
vulnerability
groundwater
land use
agriculture
nitrates
Opis:
The main aim of the work was to evaluate intrinsic and specific vulnerability of groundwater. An assessment of intrinsic vulnerability to groundwater pollution was elaborated on the basis of the original DRASTIC method. An assessment of specific vulnerability to groundwater pollution by nitrate was elaborated by two independent methods. First method – Nitrate Vulnerability Index (NV) was an adaptation of DRASTIC method, second was based on the quotient of nitrate loads (LN) and recharge rate (R), and expected nitrate concentration (NO3exp) were computed in this method. The results were presented in the relation to four homogenous regions called hydrozones: upland, top of the upland, plain and valley. The results of the DRASTIC method indicated on higher vulnerability of the aquifer in the plain (average IPZ = 155) and lower in the upland (IPZ = 125). The results of both specific vulnerability methods confirmed high vulnerability of the aquifer in the upland unit (the nitrate concentration in the range of 10–25 mg/dm3 in 25% of the unit area; average NV = 94) and lower in the plain area (the range of 0–5 mg/dm3 in the 47% /of unit area; average NV = 81). The results present a high difference between intrinsic and specific vulnerability mainly caused by agricultural activity in the upland.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 1135--1139
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rozpoznanie udziału wód podziemnych w odpływie ze zlewni rzecznej średniej wielkości
Identification of groundwater contributions to streamflow in a medium size catchment
Autorzy:
Zięba, D.
Michalczyk, T.
Bar-Michalczyk, D.
Jaszczur, M.
Żurek, A.
Wachniew, P.
Powiązania:
https://bibliotekanauki.pl/articles/2075430.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wody podziemne
rzeki
modelowanie numeryczne
wskaźniki środowiskowe
groundwater
rivers
numerical modelling
environmental tracers
Opis:
Interactions between the groundwater and surface water affect the qualitative and quantitative status of water resources. Estimation of the fluxes and the associated loadings of contaminants exchanged between the aquifers and river reaches is an important but still not well recognized component of water resources management. Such estimates are available from the numerical models of flow and transport, however, coupling of the groundwater and surface water model domains is difficult. Calibration of the coupled models relies on the knowledge of the exchanged water fluxes, hydraulic conductivities of riverbed sediments and of other parameters. Preliminary application methods allowing for identification and quantification of the groundwater – surface water exchange is presented for the Kocinka catchment in Southern Poland.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 1161--1165
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Występowanie bakterii siarkowych a jakość wód podziemnych ujęcia Osowa
Presence of sulphur bacteria and a quality of groundwater in water intake Osowa
Autorzy:
Wargin, A.
Marchelek, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075224.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
bakterie
siarczany
jakość wód podziemnych
wody podziemne
sulphate-reducing bacteria (SRB)
groundwaters quality
groundwaters
Opis:
Microorganisms that live in groundwater should be considered not only from the sanitary-hygienic point of view but also in terms of adverse changes in groundwater chemistry in the aquifer layer and its negative influence on the installed devices. For these reasons, it is important to correct approach to the problem of bacterial contamination of groundwater. The paper presents selected results of physicochemical and bacteriological parameters of raw water and treated water (after building a water treatment plant). The aim of the study is evaluatoin of groundwater quality on water intake Osowa taking into account the presence of sulfur bacteria, as well as to determine the causes of the appearance of hydrogen sulfide smell in these waters.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 1122--1124
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Chemizm wód zlewni Kamieńczyka w Sudetach na tle badań systemów przepływu wód podziemnych
Chemical composition of groundwater of Kamieńczyk catchment area in Sudety Mts. in relation to groundwater flow systems
Autorzy:
Modelska, M.
Buczyński, S.
Staśko, S.
Powiązania:
https://bibliotekanauki.pl/articles/2075248.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
skład chemiczny
wody podziemne
strefy przepływowe
Sudety
chemical composition
groundwater
flow zones
Sudety Mts.
Opis:
The present study has shown that in small, mountainous Kamieńczyk catchment (Sudety Mts.) is possible to identify hydrodynamical conditions and chemical parameters typical for different zones of local groundwater flow systems: spring discharge, discharge variability, relationships between bicarbonate and sulphate ions, pH and silica contents. Furthermore regional flow zone was clearly chemically identified through high groundwater mineralization and strongly metamorphosed hydrogeochemical facies. This proves that studies of groundwater flow zones in mountain catchments can be effectively supported by chemical analysis of groundwater.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 950--954
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
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