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Badania hydrogeologiczne w drugim 50-leciu istnienia Państwowego Instytu Geologicznego na tle ich starszej historii

Sadurski A., Skrzypczyk L.

Przegląd Geologiczny

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2018

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Vol. 66, nr 10

604--614

EN

The Polish Geological Institute (PGI) was established in 1919 according to the act of the Polish Parliament. Four departments made up the structure of PGI at that time, and one of them was Department of Hydrology. The first head of this Department was Prof. Dr. Romuald Rosłoński, also the professor of the Lwów Technical University. He is recognized as a founder of the Polish hydrogeological school. The term hydrogeology was used in the Polish literature 120 years ago, but has slowly been implemented in science as a separate research field. In the period of time between the First and Second World War the PGI team of hydrogeologists dealt with groundwater resources and water supply, hydrogeological cartography, groundwater geochemistry and hydraulic properties of rocks hosting aquifers and aquitards, and water balances of drainage basins. Hydrogeology at that time was closely connected with regional geology, tectonics and petrology on the one hand and with mining activity and civil engineering on the other hand. After the World War II in 1949, the Section of Hydrogeology was established as a part of the Geological Institute. In 1953 this was renamed the Department of Hydrogeology, with the authorization for scientific activity. The scope of this activity encompassed regional hydrogeological recognition, cartography, hydrogeology of ore deposits and mining, geophysical logging in hydrogeology and drilling diagnosis. Mathematical modeling of groundwater flow started in this Department with the physical, analog simulation in the late 60s. of the 20th century. Results of the regional investigation of groundwater occurrences and geochemistry were presented in many hydrogeological maps prepared under the guidance of Professor C. Kolago. Groundwater resources were estimated both in the regions and the whole country by the team led by Professor B. Paczyński as a head and an editor. The brines, mineralized and thermal groundwaters were identified by this Department in close cooperation with branches of the PGI under direction of B. Paczyński, Z. Płochniewski and J. Dowgiałło from the Polish Academy of Sciences. The alteration and rise of the hydrogeological studies in the PGI took place at the beginning of 2000 due to the twin projects resulted from Poland’s accession to the European Union. There was little time for the EU directives implementation, especially for Water framework directive (FWD) and integrated water resources management to be introduced in practice. To meet these needs, the state hydrogeological survey (SHS) was organized in the PGI. This survey has been established according to Water Law Act from July 18 of 2001. The SHS imposed new duties resulting from the EU Groundwater Directive (2006/118/EU) on the protection of groundwater against pollution and deterioration (Official Journal UE, L 372 from 27.12.2006). There are legal, organizational and research tasks within the monitoring network and water management planning projects, which projects that belong to duties of the SHS. The main tasks of this survey include: groundwater monitoring organization and control and quality and geochemistry control of groundwater resources within groundwater bodies, gathering of hydrogeological data in data banks, analysis of current data and forecast elaboration, documentation of groundwater resources, publication of maps, guidebooks etc. This is the current activity of the hydrogeological team of the Polish Geological Institute.

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Zalecenia dotyczące prowadzenia badań na potrzeby projektów budowli wodno-melioracyjnych

Borys M., Jędryka E.

Gospodarka Wodna

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2014

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Nr 7

250--260

PL

W artykule podano podstawowe informacje dotyczące wykonywania niezbędnych badań na potrzeby opracowania projektów różnych typów budowli hydrotechnicznych zaliczanych do urządzeń melioracji wodnych podstawowych. Omówiono szczegółowo zakresy badań geotechnicznych, hydrogeologicznych i hydraulicznych, a także ogólny zakres badań związanych z ochroną środowiska. Podano ogólne zalecenia dotyczące zakresu i metodyki prowadzenia badań dla wybranych typów budowli, tj. małych zbiorników wodnych, budowli i urządzeń funkcjonalnie związanych ze zbiornikami i ciekami wodnymi, kanałów, wałów przeciwpowodziowych oraz złóż materiału gruntowego niezbędnego do budowy nasypów ziemnych.

EN

The article presents the basic information on realisation of analyses necessary for the purposes of design of different hydraulic engineering facilities classified as the basic land reclamation facilities. It discusses the detailed scope of geotechnical,hydrogeological and hydraulic research, as well as general scope of analyses related to the environmental protection. The article presents general recommendations concerning the scope and methodology of realisation of analyses for selected types of constructions, i.e. small reservoirs, facilities and equipment related to reservoirs and watercourses, canals, embankments and soil deposits necessary for construction of soil banks.

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Ocena pracy i zasięgu oddziaływania „dużego” ujęcia wód podziemnych po 40 latach użytkowania

Węgrzyn A., Woźniak M., Grzebulska B., Nowakowski C., Sobolewska A., Sopel Ł.

Biuletyn Państwowego Instytutu Geologicznego

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2013

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nr 456 Hydrogeologia z. 14/2

627--632

PL

W artykule przedstawiono wyniki kompleksowych badań hydrogeologicznych w celu oceny sprawności 40-letnich studni, poprawności wyznaczonych w latach 70. XX w. wielkości zasobów eksploatacyjnych „dużego” ujęcia i zasięgu jego oddziaływania. Badania hydrogeologiczne objęły prace terenowe, kartograficzne, pompowania pomiarowe oraz badania modelowe. Prace terenowe przeprowadzono w trakcie normalnej pracy Zakładu, co wiązało się z szeregiem uciążliwości wynikających z ograniczeń poboru wody dla celów technologicznych. W rezultacie przeprowadzonych badań stwierdzono, iż stan techniczny większości badanych studni, w wyniku 40-letniej eksploatacji, uległ znacznej poprawie, na co wskazuje wyraźny wzrost wydatku jednostkowego nawet o 4,5 raza. Według próbnych pompowań i badań modelowych ujęcie może pracować na poziomie zatwierdzonych zasobów (również pozwoleń wodnoprawnych), jednakże obszar zasilania i oddziaływania jest niemal 2–3 razy większy w stosunku do obszaru oszacowanego metodami analitycznymi zaprezentowanymi w dokumentacji hydrogeologicznej wykonanej w latach 70 ubiegłego wieku.

EN

The paper presents the results of comprehensive hydrogeological studies to evaluate the efficiency of 40-years old wells, correctness of the amount of exploitable groundwater resources of a “large” intake, predicted in the 1970s, and to assess the range of its influence zone. Hydrogeological studies included field work, mapping, test pumping and modelling. Field work was carried out during the normal operation of the Department, which was associated with a number of nuisances resulting from water intake limits for technological purposes. The research found that the technical condition of most wells after 40 years of operation has greatly improved, as indicated by a marked increase in the specific well’s discharge as much as 4.5 times. According to test pumping and modelling studies, the intake can still work at the level of approved groundwater resources (including water-legal permits), however the recharge area and influence zone are almost 2–3 times greater compared to the area estimated by analytical methods presented in the hydrogeological documentation compiled in the 1970s.

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Geological conditions of groundwater occurrence in the Pieniny Klippen Belt (West Carpathians, Poland)

Humnicki W.

Studia Geologica Polonica

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2009

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Vol. 132

39-69

EN

The paper presents selected results of hydrogeological research carried out in the Pieniny National Park and adjacent areas during the period of 1995-2004. The objectives of the studies were to explore the geological environment and conditions of groundwater occurrence, its circulation and drainage system, as well as the physico-chemical properties of groundwaters. An important part of the research were rock fissuring measurements in natural outcrops which made it possible to determine the fissures spatial orientation, the fissuring parameters, and the fissure permeability coefficient. Investigations of rock matrix hydrogeological parameters in selected lithostratigraphic complexes of the Pieniny Klippen Belt were also carried out. Groundwater occurrence conditions in alluvial and weathering cover deposits are characterized as well.