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Tytuł:
Protecting Wieliczka Salt Mine against water hazard on the example of the Mina traverse
Autorzy:
Gonet, A.
Stryczek, S.
Powiązania:
https://bibliotekanauki.pl/articles/299177.pdf
Data publikacji:
2017
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
salt mine
water hazard
Wieliczka
Opis:
Water surrounding every salt mine creates catastrophic hazard for that place. One of such cases is uncontrollable flooding of the Wapno Salt Mine, near Innowrocław (see article Kortas G. and Maj A., Przegląd Solny, 10, 2014). The causes of catastrophic water fluxes to the Mina traverse located in level IV at a depth of 170 m b.s. in the historical Wieliczka Salt Mine is presented in this paper. The complex geological build of the immediate neighborhood of the Mina traverse was described, paying attention to the evidently disadvantageous hydrogeological conditions in the northern part of the salt dome. The most important actions aimed at limiting the water hazard in Wieliczka Salt Mine concentrated on managing and so liquidating the disastrous flux of water and solids to the Mina traverse, which started in 1992. A unique solution was proposed to solve this problem, i.e. an internal safety pillar was construed with the use of dedicated unique technologies.
Źródło:
AGH Drilling, Oil, Gas; 2017, 34, 1; 219-229
2299-4157
2300-7052
Pojawia się w:
AGH Drilling, Oil, Gas
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Method used for safety pillar reconstruction on the example of the Dunajewski gallery in the “Wieliczka” Salt Mine
Autorzy:
Gonet, A.
Stryczek, S.
Powiązania:
https://bibliotekanauki.pl/articles/299030.pdf
Data publikacji:
2018
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
pillar reconstruction
Wieliczka Salt Mine
Opis:
Preserving such unique objects as the “Wieliczka” Salt Mine for the future generations is an obvious obligation. Water is the biggest threat to this object and many similar ones. At the last stage or even in the course of mine exploitation salt mines are flooded as this is the simplest method of their liquidation applied worldwide. However this method cannot be used in the “Wieliczka” Salt Mine , which was put on the UNESCO World Cultural and Natural Heritage list in 1978. Geological and hydrogeological conditions in the Dunajewski gallery are presented in this paper. The Dunajewski gallery is localized directly east of the Mina gallery, where a catastrophic water flux was observed in 1992, threatening the mine with flooding and with considerable damage on the surface. Authors describe the pipeline injection method which was used in that situation. This was a fast and economic method thanks to which the Dunajewski gallery and the adjoining leaching gallery could be efficiently and tightly filled. Specialist recipes for sealing slurry had to be worked out. The slurry was prepared in an injection column elevated in the neighborhood of the Kościuszko shaft and then transported with special pipelines through the Kościuszko shaft and some workings to the Dunajewski gallery. In this way the off-side safety pillar in the area of the Dunajewski gallery was reconstructed.
Źródło:
AGH Drilling, Oil, Gas; 2018, 35, 1; 49-56
2299-4157
2300-7052
Pojawia się w:
AGH Drilling, Oil, Gas
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ground uplift after the closure of water leaks in the Mina drift of the Wieliczka Salt Mine
Wypiętrzenia terenu po zamknięciu wycieku w poprzeczni Mina w Kopalni Soli Wieliczka
Autorzy:
Maj, A.
Kortas, G.
Ulmaniec, P.
Powiązania:
https://bibliotekanauki.pl/articles/184710.pdf
Data publikacji:
2012
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
kopalnia soli Wieliczka
niecka osiadań
wypiętrzenia terenu
Wieliczka Salt Mine
subsidence trough
ground uplift
Opis:
After putting the water leaks in the Wieliczka Salt Mine under control, upon construction of dams in 2007, the ground subsidence stopped. Presently, however, ground uplifts are observed on land surface. This paper presents geological, mining, and hydro-geological conditions occurring in the leak areas. Using the examples of previous subsidence, the authors have demonstrated the shaping of ground uplifts observed in levelling surveying by precise measurement methods. With a correction relating to the subsidence caused by working convergence that also occur in ground displacements, it was found that the maximum ground uplifts reached 63 mm, with the continuing trends in the years to come. It was established that the causes of uplifting included increase of pressure in suffosion caverns and the displacement effect, with irrigation of dried and drained formations during the flow of water into the salt mine.
Po opanowanym wdarciu wód do Kopalni Soli Wieliczka przez zamknięcie wycieku w 2007 r. ustały obniżenia powierzchni i obecnie wykształcają się wypiętrzenia. W pracy przedstawiono warunki geologiczno-górnicze i hydrogeologiczne w strefie wycieku i na tle poprzednich obniżeń pokazano kształtowanie się wypiętrzeń terenu, obserwowane w pomiarach geodezyjnych niwelacją precyzyjną. Biorąc pod uwagę poprawkę na uczestniczące w przemieszczeniach terenu osiadania spowodowane wpływami kopalni, stwierdzono, że maksymalne wypiętrzenia osiągnęły 63 mm, a teren w następnych latach może się nadal wypiętrzać. Wskazano, że przyczyną wypiętrzeń jest zwiększenie ciśnienia w kawernach sufozyjnych oraz efekt wypornościowy i nawadnianie osuszonych i zdrenowanych utworów w trakcie spływu wód do kopalni.
Źródło:
Geology, Geophysics and Environment; 2012, 38, 1; 9-22
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The complex hydrogeology of the unique Wieliczka salt mine
Autorzy:
Brudnik, K.
Czop, M.
Motyka, J.
d'Obyrn, K.
Rogoż, M.
Witczak, S.
Powiązania:
https://bibliotekanauki.pl/articles/2066345.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
sól kamienna
hydrogeologia
kopalnia soli Wieliczka
rock salt
hydrogeology
water catastrophes
Wieliczka Salt Mine
Opis:
The saltmine in Wieliczka is a mining plant which is unique on the worldwide scale, which has been developing since the Middle Ages until the present times. The high geological complexity of bedrock in the vicinity of the mine, which is associated with the Carpathians orogeny, determines the high level of complexity of local hydrogeological conditions. At present, about 260 l/min of water discharges into the mine, which is considered very high as for a salt mine. 86% of that amount comes from three major inflows, i.e. WVII-16 (from Fornalska II chamber), WVI-32 (from Z-32 chamber) and WVI-6 (from Z-28 chamber). These seepages cause threats to the mine, not only due to their large volumes but also due to high quantities of salt that is leaching from the rock mass. The most troubled area in the Wieliczka salt mine, from the hydrogeological viewpoint, is the northern border, where salt deposits are in contact with strongly dislocated sandstones via a gypsum-clay layer. These sandstone deposits comprise not very productive aquifers that, to some degree, are isolated from one another.
Źródło:
Przegląd Geologiczny; 2010, 58, 9/1; 787-796
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Innovative technology of tight liquidation of workings on the example of the Wieliczka Salt Mine
Autorzy:
Gonet, Andrzej
Stryczek, Stanisław Antoni
Powiązania:
https://bibliotekanauki.pl/articles/1853908.pdf
Data publikacji:
2021
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
kopalnia soli
bezpieczeństwo kopalni
Kopalnia Soli Wieliczka
salt mine
water hazard
safety pillar
Mine Wieliczka
Opis:
The authors of the paper describe the way in which the longitudinal working Gussmann was mined in level V and the longitudinal working Kosocice in level VI, which in both cases resulted in a water flux from behind the northern boundary of the salt deposit. Only after concrete dams were seated on both levels, the brine flux was stopped leaving a direct contact of the dams with the pressurized water around the mine. For the sake of controlling water beyond the dams, steel pipelines were conducted through both dams and equipped with gauges before the dams. Their use in a saline environment, the developing corrosion increased the possibility that the tightness of the pipelines would be damaged. For this reason a decision was made to protect the mine by making a tight reconstruction of the safety pillar in both levels along the longitudinal working for about 600 m from the dams eastwards. For this purpose the pipeline injection method was applied. As the volume of voids to be tightly filled equaled to about 3800 m3, the task had to be divided into stages. Because of considerable distances of the liquidated workings from the closest shaft, the sealing slurries were prepared in a special injection center on the surface from where they were transported to the destination with a pumping pipeline through the Kościuszko shaft. The most important aspect of liquidating the end parts of the longitudinal working was to properly select the sealing slurries in view of their best cooperation with the rock mass, and such parameters as tightness, durability and cost. At the end stage of works, both longitudinal workings were equipped with dams, which were sealed up with the hole injection method. The innovative technology was implemented in the Wieliczka Salt Mine to reconstruct the safety pillar in levels VI and V in the most westward workings, the mine was shortened by about 600 m, the length of the ventilation system was reduced, systematic observations and pressure read-outs in dams 3 and 4 were systematically eliminated in dams 3 and 4. In this way the costs were lowered and safety of the mine improved.
Źródło:
Archives of Mining Sciences; 2021, 66, 1; 3-12
0860-7001
Pojawia się w:
Archives of Mining Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Selected hydrochemical ratios of waters from inflows at level VI in "Wieliczka" Salt Mine
Autorzy:
Obyrn, K. d'
Postawa, A.
Powiązania:
https://bibliotekanauki.pl/articles/184638.pdf
Data publikacji:
2013
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
mining hydrogeology
hydrochemical ratios
"Wieliczka" Salt Mine
Opis:
Relationships between major ions, such as Cl- , SO4 2- and Na+ and some microelements, may serve as good indicators of genesis and chemical transformations occurring during groundwater flow. The chemical composition of water from inflows at the level VI of "Wieliczka" Salt Mine is formed mainly by the dissolution of different types of salts caused by waters circulating in complicated systems of semipermeable rocks and fractured sandstones. This complicated geological structure is additionally disturbed by seven centuries of mining activity. Individual inflows are recharged by different flow systems, thus water/rock contact times are different. The authors analysed basic hydrochemical ratios: sodium/chlorides (rNa+rCl-), sulphides/chlorides (rSO42- • 100/rCl-) and chlorides/iodides (Cl-/I-). The obtained results proved that hydrochemical ratios may serve as a supporting tool for better assessment of water threats in the western part of "Wieliczka" Salt Mine.
Stosunki zawartości jonów głównych i niektórych mikroskładników w wodzie, zwane wskaźnikami hydrochemicznymi, mogą być pomocne w analizie genezy wód podziemnych i interpretacji zmian, jakim wody ulegały w czasie krążenia w górotworze. Skład chemiczny wycieków na poziomie VI Kopalni Soli „Wieliczka" kształtuje się w efekcie rozpuszczania różnych typów soli przez wody krążące w skomplikowanym systemie półprzepuszczalnych skał typu mułowce i spękanych, pokruszonych piaskowców. Dodatkowo sytuację komplikują efekty, trwającej tu od siedmiu stuleci, działalności górniczej. Analizie poddane zostały podstawowe wskaźniki hydrochemiczne: sodowo-chlorkowy rNa+/rCl-, siarczanowy rSO42- • 100/rCl- oraz chlorkowo-jodkowy Cl-/l-. Wyniki badań posłużyły jako narzędzia wspomagające ocenę zagrożeń wodnych w zachodnim rejonie kopalni.
Źródło:
Geology, Geophysics and Environment; 2013, 39, 3; 163-174
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Assessment of the qualitative and quantitative stability of “Wieliczka” Salt Mine (Poland) brines and of their possible use for medicinal purposes
Autorzy:
d'Obyrn, K.
Postawa, A.
Powiązania:
https://bibliotekanauki.pl/articles/2060046.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Wieliczka Salt Mine
brines
balneotheraphy
liquid treatments
Opis:
Water inflow to a salt mine usually poses a threat to the mine and sometimes even to its existence. On the other hand the healing properties of salt have been known since Antiquity and brines extracted from the mines have been used in the treatment of various diseases. The “Wieliczka” Salt Mine in southern Poland has been conducting organized rehabilitation and therapeutic activities for respiratory tract diseases for almost 200 years. This paper presents preliminary results of a study focused on pre-selection of out-of-deposit water inflows into the mine workings which show the lowest variability in yield and in chemical composition, and which can potentially be used in the health resort operated by the mine. The results indicate that brines from the WVII-16 leak are the only ones which can be taken into account when considering the use of Wieliczka brines for medicinal purposes for baths, rinses, irrigation, and at lower mineralisation levels, in liquid treatments
Źródło:
Geological Quarterly; 2014, 58, 3; 459--464
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Colourful speleothems in the Wieliczka Salt Mine
Autorzy:
Sawłowicz, Z.
Przybyło, J.
Boroń, K.
Powiązania:
https://bibliotekanauki.pl/articles/2060052.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
halite
speleothem
Wieliczka mine
iron minerals
colours
Opis:
Secondary halite deposits in the Wieliczka Salt Mine are represented by various forms of speleothems. Some of them, e.g. stalactites, cauliflowers or crusts, reveal various hues, yellow to red to brown. These hues are related to iron compounds, but the forms, occurrence and composition of these compounds has not previously been studied. To explain the origin of their colours a detailed study of samples collected in the mine, including brines and water soluble extracts and produced experimentally in the laboratory, has been undertaken using SEM, XRD and AAS. The colourful speleothems are compared, using SEM-EDS, with the forms and composition of rusting metal artefacts, where several iron oxide minerals have been identified. We suggest that coloured halite is generally pure halite of which the surface was covered by a ferric minerals suspension in the brine. Colours of the speleothems stem from the various colours of iron minerals whereas their intensity is related probably to the type of fluid that coated the crystals, a continuous film or finely dispersed micron-size mineral aggregates.
Źródło:
Geological Quarterly; 2014, 58, 3; 449--458
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New data on celestine-rich salts in the Wieliczka salt deposits
Autorzy:
Nowińska, J.
Powiązania:
https://bibliotekanauki.pl/articles/184740.pdf
Data publikacji:
2017
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
rock salt
Badenian
Wieliczka
strontium
celestine
geochemistry
Opis:
Pale brownish celestine-rich salt rocks were found near the Franciuszek Müller gallery, in the chambers of the 3rd level in the Wieliczka Salt Mine. The complex of rock salts subjected to exploration occurred within a large seam approximately 15 m thick. Detailed research revealed that the salt has the form of a block incorporated within the gray salts body and being similar to other blocks of green salts, well known in the upper part of the deposit. A characteristic petrographical feature of the pale brown rock salt owed to the presence of celestine (SrSO 4 ). That strontium mineral was re-examined, using X-ray powder data, and scanning microscope observations, with EDS analysis. The investigated rock salts exhibited a mineral association of halite (main component), anhydrite, celestine, calcite, gypsum, clay materials, iron compounds and a small amount of bitumen. Interrigenous sediments and the insoluble part of salt occurred higher content of strontium that in halite. Celestine crystals were observed in two forms: elongated platy crystals, forming fan-shaped aggregates and granular aggregates, strongly associated with anhydrite. On carbonate and sulphate strontium usually appearing as needle shaped aggregates of celestine. No barium minerals were observed. The development and paragenesis of celestine suggested a post-sedimentary origin of these rocks that ought to be connected with diagenetic processes. An important observation that confirmed that thesis was the transformation of fine crystalline anhydrite into platy crystals, recrystallization and primary accumulation of strontium, as a result of evaporation processes.
Źródło:
Geology, Geophysics and Environment; 2017, 43, 1; 57-68
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Salt tectonics in front of the Outer Carpathian thrust wedge in the Wieliczka area (S Poland) and its exposure in the underground salt mine
Autorzy:
Burliga, S.
Krzywiec, P.
Dąbroś, K.
Przybyło, J.
Włodarczyk, E.
Źróbek, M.
Słotwiński, M.
Powiązania:
https://bibliotekanauki.pl/articles/184289.pdf
Data publikacji:
2018
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
Carpathian Foredeep
Miocene
salt tectonics
Wieliczka salt deposit
Opis:
Salt deposits in the Wieliczka area (Wieliczka Salt Deposit – WSD) in southern Poland comprise salt-rich strata belonging to an evaporite succession that originated in the Carpathian Foredeep basin in the Middle Miocene Badenian (Serravallian) times, ca 13.81–13.45 Ma. Although they have been mined since the 13th century and decades of investigations provided abundant data on their origin and structure, some aspects of their geological evolution are still not fully understood. This study presents current concepts on the lithostratigraphy and tectonics of the WSD. The salt-bearing facies developed near to the southern basin margin, delineated by the Carpathian orogenic front. Such a location triggered the redeposition of sediments and gravity-driven deformation followed by tectonic deformation related to the forelandward advancement of the Carpathian thrusts. As a result, the WSD consists of folds and slices composed of two main salt members: (1) the stratified salt member, with intercalating salt, sulphates and siliciclastics, and (2) the boulder salt member, built of clays with large, isolated blocks of salt. The stratified member contains abundant meso-scale tectonic structures recording the soft-sediment deformation and deformation related to the northward tectonic push exerted by the advancing Carpathian thrust wedge. The boulder member originated due to the syntectonic erosion of evaporites along the basin margins and their redeposition during progressive northward migration of the Carpathian front. Recent interpretations of seismic data imply that the WSD constitutes the core of a triangle zone developed at the contact of the Carpathian orogenic wedge with the backthrust-displaced foredeep sedimentary fill. Meso-scale examples of sedimentary and tectonic structures in the salt-bearing succession exposed in the underground Wieliczka Salt Mine are described and their formation modes discussed.
Źródło:
Geology, Geophysics and Environment; 2018, 44, 1; 71-90
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Bromide concentration in mine waters from the Wieliczka salt mine as an indicator of their origin and migration of flow paths in the salt deposit
Autorzy:
Winid, B.
Witczak, S.
Powiązania:
https://bibliotekanauki.pl/articles/191608.pdf
Data publikacji:
2004
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
brine
mine waters
bromine
Wieliczka Salt Mine
South Poland
Opis:
The subject of this study is the chemistry of waters contained in the salt deposit of Wieliczka. The bromide content determined in relation to the chloride one, using the evaporation curve or the Cl/Br ratio, point to dissolution of chloride minerals as the main process in the origin of mine waters. Because of a number of processes involved in the circulation of waters within the deposit, the Br content in mine water depends on three factors: concentration of salts associated with leaching of the deposit, Br content in the salt, and dissolution - evaporation cycles on the water migration paths. The diagram Br vs. Cl or vs. density is used to explain these factors.
Źródło:
Annales Societatis Geologorum Poloniae; 2004, 74, No 3; 277-283
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wielician (Middle Badenian) foraminifers from the stratotype area : Wieliczka Salt Mine, Poland (Paratethys, Middle Miocene)
Autorzy:
Gonera, M.
Wiewiórka, J.
d'Obyrn, K.
Bukowski, K.
Powiązania:
https://bibliotekanauki.pl/articles/2060050.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Middle Miocene
foraminifera
Wieliczka Salt Mine
Middle Badenian
Wielician
Opis:
The most abundant benthic foraminifers recorded in the Wielician salt-enclosed xenoliths are: Bulimina spp., Uvigerina spp., Valvulineria complanata, and Cibicides pseudoungerianus. The predominant taxon in the planktonic assemblage is Globigerina bulloides with a median 98.9% in biozone IIC and 89.1% in the later IID. The IIC assemblage differs from the IID one in both taxon composi tion and abundance. The most pronounced differences are those revealed by Valvulineria complanata counts, number of benfhic taxa and the plankfonic/benthic (P/B) rafio. Pseudotriplasia minuta (one of the Wielician index taxa) occurs only in the IID biozone, present in 16 among 28 samples. There is a noticeable difference in sur- face sculpture morphology pattern in the predominant Bulimina and Uvigerina taxa in the IIC versus the IID biozones. There are smooth (Bulimina elongata) and weakly striate (Uvigerina semiornata plexus) forms in the IIC biozone, foll owed by heavily costate (Bulimina striata) and spinose-pustu l ate (Uvigerina orbignyana plexus) forms in the IID. Globigerina druryi and G. decoraperta- the CPN 8 planktonic index taxa - had not been found in the material studied. Globigerinita uvula is un- usually common in the samples studied. The samples analysed display an abundance of Globigerina bulloides typical of the sub-evaporite Wielician. Hence the studied Wielician stratotype area supports the thesis of the Globigerina bulloides Acme as the valid name designation for the substage.
Źródło:
Geological Quarterly; 2014, 58, 3; 427--438
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Assumptions for the proposed method of monitoring deformations in wooden grating casings in the conditions of Wieliczka Salt Mine
Autorzy:
Szpak, M.
Powiązania:
https://bibliotekanauki.pl/articles/89069.pdf
Data publikacji:
2015
Wydawca:
Politechnika Wrocławska. Wydział Geoinżynierii, Górnictwa i Geologii. Instytut Górnictwa
Tematy:
mining casing
historic excavations
wooden constructions
Wieliczka Salt Mine
Opis:
This article describes a measuring method used for monitoring deformations in wooden grating mining casings. It is intended, in particular, to determine the degree of deflection of load-bearing elements in relation to their original position. It was prepared especially to supplement the technical evaluation of wooden supporting casings in historic mines, underground sections of tourist routes, tunnels etc. The primary reason for the development of this problem were the designs prepared in recent years for large-scale grating constructions at Wieliczka Salt Mine and those for their reconstructions (strengthenings). The article describes the assumptions for the method proposed as well as the measurement system prepared. At Wieliczka Salt Mine two chambers with grating casings were selected and these were equipped with measuring devices. This paper presents the characteristics of these structures, the distribution of the devices installed and the course of the measuring process.
Źródło:
Mining Science; 2015, 22, Special Issue 2; 161-170
2300-9586
2353-5423
Pojawia się w:
Mining Science
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Causes and consequences of water flux on the example of transverse heading Mina in the Salt Mine "Wieliczka"
Przyczyny i skutki dopływu wody na przykładzie poprzeczni Mina w Kopalni Soli „Wieliczka”
Autorzy:
Gonet, A.
Stryczek, S.
Brudnik, K.
Powiązania:
https://bibliotekanauki.pl/articles/220284.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
zagrożenie wodne
Wieliczka
kopalnia soli
salt mine
water hazard
Opis:
The causes of disastrous water flux in the historical Salt Mine “Wieliczka“ have been presented on the example of transverse heading Mina at the IV level at a depth of 175 m bsl. The complex geological setting of direct environment of the transverse heading Mina has been described paying attention to unfavorable hydrogeological conditions in the northern part of the salt deposit. The main activities oriented to limiting the water hazard in the Salt Mine “Wieliczka“ and the reconstruction of inner safety pillar, which had been seriously damaged by mining activities, have been analyzed. A selection of objects inside the mine, saved from flooding thanks to protection works has been visualized in photos.
Na przykładzie zabytkowej Kopalni Soli „Wieliczka” przedstawiono co doprowadziło do katastrofalnego dopływu wody do poprzeczni Mina położonej na IV poziomie na głębokości 175 m ppt. Opisano złożoną budowę geologiczną bezpośredniego otoczenia poprzeczni Mina zwracając uwagę na wyjątkowo niekorzystne warunki hydrogeologiczne panujące od północnej strony złoża soli. Podano główne kierunki działań dla ograniczenia zagrożenia wodnego Kopalni Soli „Wieliczka” mające na celu odbudowę wewnętrznego filara bezpieczeństwa, który został poważnie uszkodzony wcześniejszymi robotami górniczymi. Pokazano wybrane obiekty znajdujące się wewnątrz kopalni, które dzięki pracom zabezpieczającym udało się uratować od zatopienia.
Źródło:
Archives of Mining Sciences; 2012, 57, 2; 323-334
0860-7001
Pojawia się w:
Archives of Mining Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Application of laser scanners to determine the shape of mine excavations for safety assessment, using the example of the cross-cut mina in the salt mine Wieliczka
Autorzy:
Lipecki, T.
Jaśkowski, W.
Powiązania:
https://bibliotekanauki.pl/articles/225491.pdf
Data publikacji:
2009
Wydawca:
Politechnika Warszawska. Wydział Geodezji i Kartografii
Tematy:
Wieliczka
kopalnia soli
skanowanie laserowe
salt mine
laser scanning
Źródło:
Reports on Geodesy; 2009, z. 2/87; 239-250
0867-3179
Pojawia się w:
Reports on Geodesy
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 22

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