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Abstract

Drought: the very word instills dread, conjuring

up images of dried-up wells, barren earth, and – perhaps worse still – empty taps and long lines to access wells. Is Poland likely to experience significant water shortages?

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Authors and Affiliations

Małgorzta Woźnicka
Agnieszka Kowalczyk
ORCID: ORCID
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Abstract

The paper presents the results of hydrogeological parameters determination carried out in the area of the Muschelkalk outcrop (Middle Triassic) near Tarnów Opolski. The studies consisted of a short pumping test in 16 piezometers and then their flooding and observation of water table recovery after the stopping of the pumping. The test allowed the values of hydraulic conductivity and specific capacity of Muschelkalk layers ranging from 8.56 · 10–8 m/s to 3.63 · 10–3 m/s and from 0.0075 to 128 m3/h/1mS, respectively, to be calculated. The wide range of values is related to the fact of studying the layers characterized by high permeability and water-bearing capacity (Karchowice Beds, Diplopora Beds and Górażdże Beds) as well as layers with low permeability (Gogolin Beds). The dense network of the research points made it possible to demonstrate the surface variability of rocks permeability and water- bearing capacity, determined mostly by the direction of outcrops of individual layers. The results of the conducted studies show that the most water-bearing zone of the area is related to the carbonate rocks of the Karchowice, Diplopora and Górażdże Beds, characterized by the highest values of hydraulic conductivity k (above 2 · 10–4 m/s) and specific capacity q (above 15 m3/h/1mS), in the belt stretching latitudinally through Kosorowice–Otmice. The studied area can be considered a Polish limestone-concrete field where several mines exploiting Muschelkalk carbonate rocks operate. The results of the conducted studies may be useful for the correct prognosis of the groundwater inflow either to already existing quarries or newly designed mines within the Major Groundwater Basins.

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Authors and Affiliations

Mirosław Wąsik
ORCID: ORCID
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Abstract

During drilling through aquifers using the rotary drilling method with drilling fluid application, the phenomenon of formation clogging in near-well zone takes place. This leads to physical changes in pore spaces in consequence of the deposition solid phase particles originating from the drilling fluid. Due to this fact, filtration velocity in the clogged zones of the aquifer formation decreases, which results in increased pressure drawdown and decreased well hydraulic efficiency. Therefore, it causes a reduction of the well total capacity. The article consists of studies connected to the development of the mud which will constitute the basis for a complex mud system intended for hydrogeological drilling in different encountered geological conditions. In the framework of laboratory research, technological parameters of six, commonly applied in oil and gas industry, polymer agents as well as new agent developed at the Drilling, Oil and Gas Faculty AGH-UST in Krakow were examined. The undertaken studies showed that the new agent, marked as CAGEx, provides the required technological parameters and can be applied as a base for drilling muds intended for hydrogeological drilling. The undertaken industrial research of the new CAGEx drilling mud carried out while drilling water intake well, confirmed the great stability of its technological parameters as well as insignificant influence on rock permeability damage in filter zone. The water intake well is characterized by high hydraulic efficiency and does not require additional activation treatment.

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Authors and Affiliations

Jan Macuda
Jakub Siemek
Sławomir Wysocki
Magdalena Gaczoł
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Abstract

The paper presents the result of hydrogeological studies of Lublin Coal Basin (LCB), particularly at Jurassic level. It is arranged in several parts: I) stratigraphy, tectonics and lithology of Jurassic system at LCB territory, 2) groundwater dynamics, 3) chemical composition of waters, 4) hyclrogeochemical stability conditions. The paper also suggests a few main directions of using the Jurassic waters in prophylaxis and therapy of many diseases. The waters, containing considerably elevated quantities of fluorine compounds come from Jurassic formation lying at the considerable depth. Coal mine joins them with saline Carboniferous waters. After pretreatment, they are discharged to the surface ancl to the river. Jurassic waters belong to the group of low mineralised waters. They contain 6-1 I mg F/dm3 fluorides. Thus they can be usefu I in prophylactics of teeth ancl paradental illnesses, particularly in risk groups. Thanks to, fluorides contained in these waters they can be used during and after treatment and to support surgical operations or rehabilitation effects.
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Authors and Affiliations

Małgorzata Ciosmak
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Abstract

The paper presents an example illustrating the problems of assessing the causes of damage that occurred to building structures located in mining and post-mining area. It is frequently necessary to determine whether probable damages came from other, non-mining causes or were caused by underground mining. This issue is particularly significant when it comes to monumental, historical objects because the cost of repairs is typically very high. The purpose of this work is to demonstrate, using the magnificent church as an example, that damage to building objects situated in mining areas does not necessarily result from mining activities. As a result, every such situation should be thoroughly evaluated to determine whether such a relationship exists. For the assessment of such a conclusion, multidirectional studies in the framework of this work were carried out: hydrogeological, mining and technical factors that cause the damage to the church building in question were analysed.
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Authors and Affiliations

Edward Cempiel
1
Piotr Strzałkowski
1
ORCID: ORCID
Roman Ścigała
1
ORCID: ORCID
Izabela Bryt-Nitarska
2
ORCID: ORCID

  1. Silesian University of Technology, 2A Akademicka Str., 44-100 Gliwice, Poland
  2. Strata Mechanics Research Institute, Polish Academy of Science, 25 Reymonta Str., 30-059 Kraków, Poland
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Abstract

Artificial water reservoirs pose impact on the natural environment. Impact of the artificial Czorsztyn Lake on groundwater and land management is assessed. The study is based on long-term observations of chemistry, groundwater levels and spring discharges during reservoir construction, filling, and 25-year-long exploitation. Land management changes caused by reservoir construction were recognized using remote sensing. Reservoir construction resulted in land management change in the study area. Built-up and forest areas gained prevalence over farmland areas. Two types of groundwater dominate: HCO3–Ca and HCO3–Ca–Mg, both before reservoir filling (68% analyses) and afterwards (95% analyses), and in control analyses from September 2020 (100% analyses). Gradual decrease in the occurrence of water types with the sulphate ion exceeding 20% mvals is documented, which points to water quality improvement trends. Moreover, changes of water saturation index values with regard to aquifer-forming mineral phases during reservoir construction and early exploitation phasei ndicate hydrochemical modifications. Decrease of groundwater level was related with transformation of the Dunajec river valley during reservoir construction and, accordingly, decrease of regional drainage base level. Groundwater level increased after reservoir filling, which points to coupled impact of the reservoir and increased precipitation recharge. Construction of the Czorsztyn Lake resulted in gradual land management transformation from farmlands into tourist-recreational areas. This change and river valley flooding by surface waters did not cause significant modifications in groundwater quantity and quality. Organization of water-sewage management related with reservoir construction resulted in noticeably improved quality trends.
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Authors and Affiliations

Włodzimierz Humnicki
1
ORCID: ORCID
Ewa Krogulec
1
Jerzy Małecki
1
ORCID: ORCID
Marzena Szostakiewicz-Hołownia
1
ORCID: ORCID
Anna Wojdalska
1
Daniel Zaszewski
1
ORCID: ORCID

  1. Faculty of Geology, University of Warsaw, Poland
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Abstract

This article shows that the most sensitive indicator of local and regional karst activity in territories of apparent karst processes is the behaviour of karst lakes. The authors propose a hydrogeological monitoring methodology for the karst pro-cess based on the phase-measuring geoelectric control method in the coastal zone of karst lakes. The geoelectric current control of hydrogeological changes in the medium at local levels uses a multi-frequency vertical electric sounding com-bined with a phase-measuring method of registering the geoelectric signal. These proven methods permit to distinguish var-iations of spatial parameters and the electric conductivity of several layers at a time. Moreover, they significantly increase the noise resistance and sensitivity of the measuring system. An adaptive algorithm function of the measuring complex for geoelectric monitoring of karst lakes’ coastal zones was developed to control the operation of facilities and data collection systems. Based on an example of a lake where karst processes are active, the key zones of hydrogeological control were identified depending on karst manifestations. The research confirmed the possibility of local and regional monitoring of the development and forecasting of destructive karst-suffosion processes based on hydrogeological regime observations of karst lakes.
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Bibliography

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Authors and Affiliations

Oleg R. Kuzichkin
1
ORCID: ORCID
Roman V. Romanov
2
ORCID: ORCID
Nikolay V. Dorofeev
2
ORCID: ORCID
Gleb S. Vasilyev
1
ORCID: ORCID
Anastasia V. Grecheneva
1
ORCID: ORCID

  1. Belgorod National Research University, 85 Pobedy St., 308015 Belgorod, Russia
  2. Vladimir State University, Vladimir, Russia
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Abstract

The use of non-centralised water supply in remote settlements is currently the only possible option. Monitoring the wa-ter quality of such supply sources is a complicated task in such areas, especially when there are active karst processes and difficult groundwater conditions. The application of deterministic analytical models of water supply under the risk of dis-turbance to groundwater dynamics is not efficient. Significant quantitative and even qualitative changes in groundwater conditions may take place between the calculated points, and the underestimation of these changes in expectation-driven computation models may result in serious geoecological issues. This research studied and justifies the use of adaptive dy-namic hydrogeological control in an area of non-centralised water supply based on the identification of key zones of geo-dynamic karst monitoring and the electrical express-monitoring of water resources. The identification of key zones is based on an integrated analysis of available groundwater information that describes changes in groundwater hydrodynamic condi-tions at the time of the karst forecast. The development of karst-suffusion processes is accompanied by more intense dy-namic changes in local areas of geologic environment compared to the general variation in intensity. Information about the occurrence of destructive groundwater processes by means of selective geodynamic monitoring may thus be obtained much earlier than with environmental geodynamics monitoring as a whole. The experimental hydrogeological control of an area of non-centralised water supply was conducted on the right bank of the Oka River in Nizhny Novgorod region, a locality with an active manifestation of karst processes. Structure and algorithms of space-time processing of hydrogeological con-trol data developed by authors have been used. The approach based on multifrequency vertical electrical sounding (MFVES) method has shown good correspondence with direct borehole observation when measuring depth of the first aq-uifer. Zones of unsafe water use have been revealed. The results demonstrated the effectiveness of the proposed method and the need for further regular observations of destructive groundwater processes by means of selective hydrogeodynamic monitoring.

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Authors and Affiliations

Oleg R. Kuzichkin
ORCID: ORCID
Roman V. Romanov
ORCID: ORCID
Nikolay V. Dorofeev
ORCID: ORCID
Anastasia V. Grecheneva
ORCID: ORCID
Gleb S. Vasilyev
ORCID: ORCID

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