Informacja

Drogi użytkowniku, aplikacja do prawidłowego działania wymaga obsługi JavaScript. Proszę włącz obsługę JavaScript w Twojej przeglądarce.

English (EN)·Polski (PL)·Yкраїнський (UK)
Przejdź do strony domowej biblioteki Centralna Biblioteka Wojskowa Link otwiera się w nowym oknie Logo biblioteki Prolib Integro - strona głównaCentralna Biblioteka Wojskowa

Wyszukujesz frazę "ore bearing" wg kryterium: Temat

  Lista filtrów
Wyrównaj
Wyświetlanie 1-15 z 26
Tytuł:
Factors Affecting Ballability of Mixture Iron Ore Concentrates and Iron Oxide Bearing Wastes in Metallurgical Processing
Autorzy:
Udo, M. O.
Esezobor, D. E.
Apeh, F. I
Afolalu, A. S.
Powiązania:
https://bibliotekanauki.pl/articles/123037.pdf
Data publikacji:
2018
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
ballabilty
bearing wastes
iron ore concentrates
Opis:
Iron oxide bearing wastes (IOBS) are produced at every part of processing stage of sinter, molten iron and steel production. They are hard to handle and in many cases are stockpiled only to be a source of environmental pollution. However, they can be balled into pellets. Pellets characterized by good ballability values are transportable and recyclable as they can withstand stress without disintegrating back to dust. Yet, ballability is affected by certain factors like the grain sizes of the materials, the moisture and binder contents of the ball mix, wettability of the balled materials and the processing perimeters of the granulator. The objective of this research work is to investigate the factors affecting ballability of mixture of iron ore concentrates and iron oxide bearing wastes in metallurgical processing. The parameters under consideration were: grain size of materials, the moisture contents, speed of balling disc, IOBS and bentonite (binder) contents of the balled mix. The investigation was carried out by balling different volume fractions of mix containing iron oxide concentrate and IOBS using a balling disc and testing the resulting balls for green compressive strength using an universal testing machine. It was found that the ballability of the mixture of iron ore concentrate and IOBS increases as grain sizes of the materials reduce but increases as the moisture contents and IOBS content increase up to an optimum value of moisture content in the mix before it starts to reduce. The ballability also increases along with the speed of the granulator (balling disc) within the limit of this work. An increase in ballability with a slight raise in bentonite content in the mix was observed as well.
Źródło:
Journal of Ecological Engineering; 2018, 19, 3; 235-242
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Praktyczne aspekty oszacowania ilościowego składu mineralnego miedzionośnych skał osadowych na podstawie procedury obliczeń analogicznej do normy CIPW
Practical aspects of estimating the quantitative mineral composition of copper-bearing sedimentary rocks based on a calculation procedure analogical to the CIPW norm
Autorzy:
Nowak, I.
Powiązania:
https://bibliotekanauki.pl/articles/2061667.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
ilościowy skład mineralny
minerały kruszcowe
norma CIPW
margiel miedzionośny
łupek miedzionośny
quantitative mineral composition
ore minerals
CIPW norm
copper-bearing marl
Kupferschiefer
Opis:
W pracy przedstawiono możliwość oszacowania zawartości minerałów kruszcowych na podstawie analiz chemicznych próbek miedzionośnych skał osadowych z synklinorium północnosudeckiego i z monokliny przedsudeckiej, stosując obliczenia w sposób analogiczny do procedury CIPW. Dane mineralogiczne uzyskano za pomocą mikroskopu optycznego i mikrosondy elektronowej (EPMA). Ilościowy skład minerałów płonnych określono metodą XRD, a kruszców metodą komputerowej analizy obrazu mikroskopowego (CAMI). Zdefiniowano rzeczywisty zespół minerałów płonnych i kruszcowych, ich skład chemiczny, określono proporcje kruszców miedzi oraz wybrano pierwiastki będące głównymi składnikami zidentyfikowanych minerałów. Zgodnie z danymi mineralogicznymi i chemicznymi opracowano procedurę obliczeń analogicznie do normy CIPW. Zespół minerałów kruszcowych określony na podstawie obliczeń stosunków wagowych jest zgodny z obserwacjami mikroskopowymi skał miedzionośnych. Uzyskane tą metodą zawartości kruszców są zbliżone lub nieco wyższe w próbkach nisko zmineralizowanych i nieco niższe w próbkach bogato okruszcowanych w porównaniu do wyników metody CAMI. Różnice te mogą być spowodowane odmiennymi sposobami uśredniania próbek (sproszkowana, uśredniona skała i preparat mikroskopowy). Obliczone proporcje udziału kruszców są zgodne z proporcjami uzyskanymi metodą CAMI. Wykonane obliczenia ilościowego składu minerałów kruszcowych za pomocą procedury kalkulacyjnej podobnej do CIPW mogą być zastosowane do wstępnego oszacowania ilościowej zawartości kruszców w rudach podczas geologicznych prac poszukiwawczo-rozpoznawczych, wymagają one jednak przetestowania innych wariantów rozdzielania pierwiastków pomiędzy zestaw minerałów.
The paper presents a possibility of estimating the content of ore minerals based on chemical analyses of copper-bearing sedimentary rock samples from the North-Sudetic Synclinorium and from the Fore-Sudetic Monocline using a calculation procedure similar to the CIPW norm. The mineralogical data was obtained by means of an optical microscope and an electron microprobe (EPMA). The quantitative composition of gangue minerals was determined using the XRD method, and of the ores by the computer microscopic image analysis (CAMI). The actual set of gangue and ore minerals, their chemical composition, and proportions of copper ores were determined in the samples. Elements that are the main components of identified minerals were selected. The calculation procedure has been developed in accordance with the mineralogical and chemical data. The set of ore minerals determined based on the calculation of the weight ratios is consistent with the microscopic observations of copper-bearing rocks. The obtained ore contents are similar or slightly higher in poorly mineralized samples and slightly lower in highly mineralized samples in comparison to the results of the CAMI method. These differences may be due to different methods of averaging samples (powdered, averaged rock samples, and a thin section). The calculated ore proportions are consistent with those obtained by the CAMI method. The study calculations of the quantitative ore mineral composition using the calculation procedure analogical to the CIPW norm can be used to a preliminary approximation of the quantity of ores in geological prospection and exploration studies, but they require testing of more variants of the element partition between the set of minerals.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2018, 472; 155--170
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Parametry geotechniczne częstochowskich iłów rudonośnych z rejonu Konopisk (SW obrzeżenie Częstochowy)
Geotechnical properties of siderite-rich clays from Konopiska municipality (SW margin of Częstochowa)
Autorzy:
Dudko-Pawłowska, I.
Kowalska, M.
Gawlik, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075725.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
glina kruszona
Konopiska
właściwości geologiczno-inżynierskie
ore-bearing clay
geological-engineering properties
Opis:
In the vicinity of the Konopiska municipality (SW margin of Częstochowa) ore-bearing clays have been deposited. These formations, only locally covered by younger sediments, constitute direct foundation subsoil, so their geotechnical parameters may conditionate founding possibility of various structures. The paper presents results of a series of experiments (conducted accordingly to PN-B-04481: 1988) dedicated to estimation of the geological-engineering properties of these clays in terms of the possibility of their use as a founding ground or a material to build earth structures. It has been learned that the tested soils contain high amounts of clayey fraction, occur in semi-solid state and show relatively high shear-strength parameters. Their natural water content is close to the optimum one (18-20%), at which a clear peak of the dry density (about 1.7 Mg/m3) is noted. Low colloidal activity proves that they are prone to expansion. All these properties indicate that they can constitute a competent subsoil for typical structures of the first or second geotechnical category, unless obviously the ultimate and serviceability limit states are checked and satisfied for the particular geotechnical case.
Źródło:
Przegląd Geologiczny; 2017, 65, 10/2; 848--855
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmienność mineralizacji kruszcowej w rejonie północno-zachodniego przedłużenia złoża Lubin–Sieroszowice
Variability of ore mineralization in the north-west-trending extensionof the Lubin–Sieroszowice deposit
Autorzy:
Oszczepalski, S.
Chmielewski, A.
Speczik, S.
Powiązania:
https://bibliotekanauki.pl/articles/2061710.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
cechsztyńska seria miedzionośna
łupek miedzionośny
mineralizacja kruszcowa
Rote Faule
rejon Kożuchów-Grochowice
Zechstein Copper-bearing Series
Kupferschiefer
ore mineralization
Rote Fäule
Kożuchów-Grochowice area
Opis:
Państwowy Instytut Geologiczny – PIB prowadzi poszukiwania stratyfikowanych złóż rud miedzi w obrębie spągowych utworów cechsztynu od połowy lat 50. XX w., kiedy odkryto złoże Lubin–Sieroszowice. Do 1991 r. zrealizował szereg programów wiertniczych, natomiast w okresie późniejszym prowadził badania próbek skał z rdzeni pozyskiwanych w trakcie poszukiwań złóż węglowodorów przez przemysł naftowy. W rezultacie tych prac poszukiwawczo-badawczych w północno-zachodnim otoczeniu złoża Lubin–Sieroszowice wyznaczono obszary perspektywiczne. Obszary te są usytuowane pomiędzy udokumentowanym złożem Bytom Odrzański i wschodnią granicą zielonogórskiego obszaru, w którym znajdują się utwory wtórnie utlenione. W rejonie Kożuchowa, dolne partie cechsztyńskiej serii miedzionośnej zawierają jedynie siarczkową mineralizację reliktową z towarzyszącymi tlenkami żelaza, a utwory o cechach redukcyjnych z siarczkami metali występują w górnych partiach wapienia cechsztyńskiego lub w spągu anhydrytu dolnego. W rejonie Grochowic, w którym jest obecna strefa redukcyjna, w najbliższym sąsiedztwie obszaru z utworami wtórnie utlenionymi występuje bogata mineralizacja miedziowo-srebrowa reprezentowana przez siarczki typu Cu-S (chalkozyn, digenit, kowelin), przechodząca w kierunku wschodnim w mineralizację zdominowaną siarczkami systemu Cu-Fe-S (bornit, chalkopiryt) ze znacznym udziałem galeny i sfalerytu. Przestrzenna zmienność mineralizacji siarczkowej względem utworów utlenionych wskazuje, że złoże Bytom Odrzański przedłuża się w kierunku północno-zachodnim, kontynuując się w formie pasa miedzionośnego wzdłuż wschodniej granicy obszaru ze skałami utlenionymi. Prowadzona obecnie eksploracja wiertnicza w obrębie przewidywanego pasa miedzionośnego stwarza przesłanki do możliwości udokumentowania i zagospodarowania głębokich złóż rud miedzi.
The Polish Geological Institute – NRI has conducted investigations of the Kupferschiefer series since 1957, when the giant sediment-hosted stratiform Cu-Ag ore deposit was discovered in the central part of the Fore-Sudetic Monocline. Until 1991, a number of drilling programs were completed by PGI-NRI and later research has been focusing mainly on cooperation with oil and gas industry and their core material. Over the last few years, thanks to systematic examination of the drill holes located in the north-western extension, many prospective areas have been recognized and delineated. These prospects are located between Lubin-Sieroszowice deposit and the eastern part of the Zielona Góra oxidized field. In the Kożuchów area, the lower part of Zechstein copper-bearing series contain only relict sulphide mineralization accompanied by iron oxides while reduced rocks with metal sulphides occur in the uppermost part of Zechstein Limestone or at the base of Lower Anhydrite. Grochowice area, where reduced facies prevail in copper-bearing series, is characterized by the predomination of rich Cu-Ag mineralization proximaly to oxidized area. The western part of studied area is dominated by Cu-S type sulphides (chalcocite, digenite, covellite) whereas the eastern part is represented by Cu-Fe-S type minerals (bornite, chalcopyrite) with high galena and sphalerite concentrations. The spatial variability of sulphide mineralization with respect to the oxidized rocks indicates that Bytom Odrzański deposit extends in the north-west direction, continuing in the form of a copper belt along the eastern border of the oxidized area. An extensive deep exploration drilling program is implemented to verify the resource potential within predicted copper belt.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2017, 468; 109--141
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A dinosaur track assemblage from the Upper Hettangian (Lower Jurassic) marginal-marine deposits of Zapniów, Holy Cross Mountains, Poland
Autorzy:
Niedźwiedzki, G.
Pieńkowski, G.
Powiązania:
https://bibliotekanauki.pl/articles/2060538.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
dinosaur tracks
Przysucha Ore-bearing Formation
Upper Hettangian
Lower Jurassic
Holy Cross Mountains
Polska
Opis:
Upper Hettangian (Lower Jurassic) marginal-marine Przysucha Ore-bearing Formation exposed at Zapniów mine and clay-pit (northwestern part of the Holy Cross Mountains area, central Poland) revealed an interesting assemblage of dinosaur tracks. Although mostly yielding poorly preserved and isolated tracks probably left in shallow water conditions, the site nevertheless indicates a diversity of early saurischian (theropods and sauropodomorphs) and ornithischian (thyreophorans) dinosaur trackmakers. This new assemblage is partly consistent with the Lower-Middle Hettangian ichnorecord from the same region. The tracks are preserved in sediments of a barrier-foreshore origin within a barrier/lagoonal depositional system, belonging to the highstand systems tract, located below a marked erosional surface (sequence boundary), which is associated with a substantial fall in sea level at the end of Hettangian times. Here we described all previously and newly collected or observed in the field dinosaur tracks from both surface and underground exposures at Zapniów. Four ichnospecies: Grallator isp., Anchisauripus isp., cf. Tetrasauropus isp., and cf. Anomoepus isp. were identified. The theropod and ornithischian tracks show distinct similarities to those described from the richest in this region and most famous Gliniany Las dinosaur track assemblage, in age approximately coeval to Zapniów. Two sizes of theropod tracks (small and medium) indicate the presence of two different size classes or species of predators in this area. The described cf. Tetrasauropus isp. from Zapniów is the first unquestioned evidence of basal sauropodomorphs in the Upper Hettangian of the Holy Cross Mountains and first record of this ichnotaxa in the Lower Jurassic of Poland. Additionally, two theropod trackways (Anchisauripus isp.) show evidence for trotting. The new finds suggest similarities between marginal-marine environments (delta-plain and foreshore-barrier/lagoon lithofacies) association of dinosaurs containing low-browsing thyreophorans accompanied by small or juvenile sauropodomorphs and small to medium sized theropods. Presence of the ornithischian footprints suggests their prominent role as a major component in Middle-Upper Hettangian dinosaur faunas in marginal-marine environments dominating in the region.
Źródło:
Geological Quarterly; 2016, 60, 4; 840--856
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Operating conditions of slide bearings of mills used in KGHM Polska Miedź S.A.
Warunki pracy łożysk ślizgowych młynów użytkowanych w KGHM Polska Miedź S.A.
Autorzy:
Olszewski, A.
Łubiński, J. I.
Pawlos, W.
Kuźba, B.
Powiązania:
https://bibliotekanauki.pl/articles/190871.pdf
Data publikacji:
2016
Wydawca:
Stowarzyszenie Inżynierów i Techników Mechaników Polskich
Tematy:
hydrodynamic bearing
copper ore processing
ball mill
computer simulation
łożyska hydrodynamiczne
młyny kulowe
mielenie
symulacja komputerowa
Opis:
The paper contains the results from a technical analysis of the conditions of the operation of hydrodynamic bearings supporting the drums of ore processing mills at KGHM Polska Miedź S.A. A theoretical analysis was performed on the grounds of onsite examination and measurements of principal dimensions of the bearings of interest. The computer simulation covered the characteristics of the oil film in the bearings as a function of bearing clearance, load, lubricant viscosity, and journal tilting in relation to two planes (horizontal and vertical). The results of the analysis indicate that the bearings currently operate close to maximum capacity and that there is a significant deflection of the Bering journals under the applied joint load of the drum’s own weight and the process load of grinders and slurry. The current extent of tilting can cause oil film breakage at the bearing’s edge. The result of calculations amended by bearings’ examination and measurements allowed the formulations of conclusions regarding the current state of the bearings and evaluated load conditions. Guidelines were established for later developments in the capacity and reliability of the bearings.
W artykule przedstawiono analizę warunków pracy łożysk hydrodynamicznych młynów rudy zainstalowanych w KGHM Polska Miedź S.A. Analiza teoretyczna została poprzedzona wizją lokalną oraz wykonaniem stosownych pomiarów geometrii czopów i łożysk. Symulacja komputerowa charakterystyk filmu olejowego łożysk obejmowała zbadanie wpływu wartości luzu łożyskowego, obciążenia, lepkości oleju smarującego oraz ukosowania czopa w dwóch płaszczyznach (poziomej i pionowej). Analiza wskazuje, że zainstalowane łożyska pracują na granicy swojej nośności, a ugięcie osi czopów spowodowane ugięciem walczaka pod działaniem ciężaru własnego i nadawy wywołuje znaczne ukosowanie czopa w panwi mogące prowadzić do przerywania filmu olejowego na krawędziach zewnętrznych. Przeprowadzone obliczenie uzupełnione o oględziny pomiary łożysk wykonane w KGHM Polska Miedź S.A. pozwoliły na sformułowanie wniosków odnośnie do stanu istniejących łożysk, ich obciążenia oraz możliwości zwiększenia nośności i niezawodności.
Źródło:
Tribologia; 2016, 268, 4; 177-189
0208-7774
Pojawia się w:
Tribologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Storm-influenced deposition and cyclicity in a shallow-marine mudstone succession - example from the Middle Jurassic ore-bearing clays of the Polish Jura (southern Poland)
Autorzy:
Leonowicz, P. M.
Powiązania:
https://bibliotekanauki.pl/articles/2060303.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
bioturbated mudstones
storm deposits
transgressive-regressive cycles
Ore-Bearing Częstochowa Clay Formation
Silesian-Cracow region
Opis:
Sedimentological analysis of bioturbated mudstones from the Middle Jurassic ore-bearing Częstochowa Clay Formation has revealed common relics of sedimentary structures, such as thin silt/sand laminae, bedding-plane accumulations of shell debris, small and medium silt-sand lenses, as well as silt-, sand- and shell-debris-rich levels, accompanied by erosion surfaces and minor scours. These features document periodical high-energy conditions of mud deposition, including storm stirring, event sedimentation and the activity of storm-generated bottom currents, which were responsible for seafloor erosion and sediment supply from shallower parts of the basin. The sea bottom was prevalently below the storm wave base, but it rose above it during exceptionally strong storms and in the Early Bathonian zigzag chron when the basin experienced considerable shallowing. The shallowest and highest energy conditions occurred in the late macrescens subchron, when the bottom was close to, or above the fair-weather wave base. The estimated depth of the sea did not exceed several tens of metres, but in some periods it could be even less than 20 m. Based on the vertical variation of the sand, silt and clay contents, seven transgressive-regressive cycles have been distinguished in the approximately 75-m thick succession spanning the Upper Bajocian - Upper Bathonian. Cycles TR1, TR2+3, TR5 and TR6+7 correlate with those distinguished in the coeval succession from central Poland, although the stratigraphic position of cycle boundaries is slightly shifted. These cycles record relative sea-level changes that affected the entire Polish Basin. Regressions R2 and R6 were smaller-scale-events, generated in response to a local tectonic activity and autocyclic shoreline progradation.
Źródło:
Geological Quarterly; 2015, 59, 2; 325--344
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sedimentology of the “ore-bearing dolomite” of the Kraków-Silesia region (Middle Triassic, southern Poland)
Autorzy:
Matysik, M.
Powiązania:
https://bibliotekanauki.pl/articles/191964.pdf
Data publikacji:
2014
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
ore-bearing dolomite
epigenetic dolomitization
lead-zinc mineralization
facies pattern
peritidal and subtidal facies
Middle Triassic
muschelkalk
Upper Silesia
Polska
Opis:
The depositional history and facies heterogeneity of the epigenetically dolomitized Middle Triassic carbonates of southern Poland are poorly recognized, and existing concepts of fluid circulation entirely overlook the primary lithology as a factor controlling fluid flow. This study reconstructs the consecutive phases of Kraków-Silesia Sub-basin history in the Anisian and highlights their influence on the development of the so-called “ore-bearing dolomite”. Extensive fieldwork and microfacies analyses were carried out in order to decipher the original depositional fabric of the ore-bearing dolomites. As a rule, epigenetic dolomitization affected a horizon of porous strata, 35 m thick and resting directly on impermeable, wavy-nodular clay-rich calcilutites of the Gogolin Formation, which represent the interval of deepest and fully marine (offshore) sedimentation. The sedimentary succession of the porous strata is bipartite. The lower part (Olkusz Beds) is composed of Balanoglossites and Thalassinoides micritic firmgrounds and peloidal packstones-grainstones, representing shoreface-foreshore facies assemblages, whereas the upper part (Diplopora Beds) consists of dolocretes, rhizolites, cryptalgal laminites, peloidal packstones-grainstones and bioturbated fine-grained dolostones, formed in a system of tidal flats and lagoons. These two parts are separated by a subaerial disconformity, which marks a sequence boundary. During emersion, the underlying deposits were subjected to meteoric diagenesis, which led to the development of moldic porosity. This combination of depositional history and diagenetic alteration determined the routes of initial migration of dolomitizing solutions on the one hand, and the location of cavern formation on the other. Owing to progressive dissolution, small caverns were changed into large karstic forms, in which the ore minerals precipitated ultimately. These findings emphasize the importance of sedimentological analysis to the understanding of the evolution of the Kraków-Silesia ore province.
Źródło:
Annales Societatis Geologorum Poloniae; 2014, 84, 2; 81-112
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sources of radon and its measurement techniques in underground uranium mines – an overview
Autorzy:
Sahu, P.
Panigrahi, D. C.
Mishra, D. P.
Powiązania:
https://bibliotekanauki.pl/articles/92136.pdf
Data publikacji:
2014
Wydawca:
Główny Instytut Górnictwa
Tematy:
underground uranium mine
radon exhalation
uranium-bearing ore
backfill tailings
mine water
accumulation technique
podziemna kopalnia uranu
ekshalacja radonu
rudy uranu
wody kopalniane
technika akumulacji
Opis:
Purpose This study aims to identify the potential sources of radon exhalation and its measurement in underground uranium mines to control the radiation levels within safe limits and protect miners from radiation hazards. Methods An extensive literature review on radon exhalation in underground uranium mines from various sources such as uranium ore, backfill tailings and mine water has been carried out. The influence of different important factors, viz. ore grade, porosity, grain size and moisture content on radon exhalation has been discussed in depth. Different methods for the measurement of radon exhalation from various sources in mines have also been presented in this paper. Results The review of literature revealed that the radon exhalation rate in porous uranium bearing rocks is less affected by the ore grade than in non-porous rocks. The exhalation of radon from backfill tailings is quantitatively more significant than from the uranium ore itself due to higher bulk porosity and enhanced surface area. Thus, porosity is the dominant factor that affects the rate of radon exhalation from rock surfaces into mine openings. Practical implications The knowledge of the sources of radon and quantitative estimation of radon from various sources will be very much useful in the planning and designing of ventilation systems in underground uranium mines. The accurate measurement of radon exhalation in underground uranium mines can be made by choosing the optimum size of accumulation chamber and a suitable radon build-up period in the chamber. Originality/ value The study portrays the important sources of radon and its measurement techniques in underground uranium mines based on an extensive literature review. The methods of measurement of radon exhalation from the ore body and backfill tailings in underground uranium mines, used by the authors of this paper, comparatively give more accurate results than previously used methods. Furthermore, the methods are more effective in terms of portability, cost and time for measuring the average radon exhalation across a large.
Źródło:
Journal of Sustainable Mining; 2014, 13, 3; 11-18
2300-1364
2300-3960
Pojawia się w:
Journal of Sustainable Mining
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The significance of mudstone fabric combined with palaeoecological evidence in determining sedimentary processes - an example from Middle Jurassic of southern Poland
Autorzy:
Leonowicz, P. M.
Powiązania:
https://bibliotekanauki.pl/articles/2059717.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
black mudstones
parallel lamination
storm deposits
ichnofabric
bottom oxygenation
Ore-Bearing Częstochowa Clay Formation
Opis:
Analysis of the fabric of laminated black mudstones of the Ore-Bearing Częstochowa Clay Formation (Bathonian, southern Poland) is used for reconstruction of sedimentary processes and conditions. Small-scale sedimentary features indicate that ore-bearing clays were deposited below storm-wave base in a shallow epicontinental sea, but structures reflecting quiet settling from suspension are not common. Most of recognized lamina types record the activity of bottom currents generated by storms. The benthic faunal association indicates that suboxic conditions prevailed on the seafloor, restricting infaunal activity to cryptobioturbation. Recurrent short-lived reoxygenetion events, linked probably to storms, resulted in the development of dysoxic conditions, recorded by a more diverse trace fossil association (consisting of Chondrites, Trichichnus, pyritized burrows, Palaeophycus and Protovirgularia) and colonization of the seafloor by epifaunal bivalves (Bositra). Truly anoxic conditions might have been briefly established, leading to mass mortality of Bositra.
Źródło:
Geological Quarterly; 2013, 57, 2; 243--260
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
An introduction to the palaeoenvironmental reconstruction of the Bathonian (Middle Jurassic) ore-bearing clays at Gnaszyn, Kraków-Silesia Homocline, Poland
Autorzy:
Gedl, P.
Kaim, A.
Powiązania:
https://bibliotekanauki.pl/articles/138596.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
baton
iły rudonośne
jura środkowa
monoklina śląsko-krakowska
osady
Polska
Bathonian ore-bearing clays
Dark deposits
Kraków-Silesia Homocline
Middle Jurassic
Polska
Opis:
This paper provides introductory data for multidisciplinary studies on palaeoenvironmental reconstructions of the Bathonian (Middle Jurassic) ore-bearing clays exposed at Gnaszyn, southern Poland. These dark-coloured fine-clastic deposits have been studied for micropalaeontology, sedimentology and geochemistry (published in separate papers within this volume). Brief outlines of the Middle Jurassic palaeogeography of the Polish epicontinental basin and the geology of the Kraków-Silesia Homocline are given. A description of the ore-bearing clays succession exposed in the clay-pit at Gnaszyn is provided, including locations of the sections studied, their ammonite biostratigraphy, brief lithology and macrofossil distribution. The sample positions collected for micropalaeontological and geochemical studies are specified.
Źródło:
Acta Geologica Polonica; 2012, 62, 3; 267-280
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Faunal dynamics of bivalves and scaphopods in the Bathonian (Middle Jurassic) ore-bearing clays at Gnaszyn, Kraków-Silesia Homocline, Poland
Autorzy:
Kaim, A.
Sztajner, P.
Powiązania:
https://bibliotekanauki.pl/articles/138633.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
baton
Gnaszyn
iły rudonośne
jura
łódkonogi
małże
paleoekologia
Polska
ślimaki
Bathonian
bivalves
gastropods
Jurassic
ore-bearing clays
palaeoecology
Polska
Scaphopods
Opis:
The environment at the Gnaszyn section - as deduced from bivalve and scaphopod dynamics - was controlled by the substrate consistency and possibly oxygen deficiency near the sediment-water interface and/or oxygen content fluctuations. The middle part of the section dominated by nuculoid and corbulid bivalves and Laevidentalium-type scaphopods probably reflects a soupy substrate and possibly oxygen deficiency in the sediment. Slightly coarser and better-oxygenated silts in the upper and lower parts of the section offered a less soupy substrate consistency, allowing the development of communities dominated by astartids, byssate bivalves, and Dentalium- and Plagioglypta-type scaphopods.
Źródło:
Acta Geologica Polonica; 2012, 62, 3; 381-395
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Faunal dynamics of gastropods in the Bathonian (Middle Jurassic) ore-bearing clays at Gnaszyn, Kraków-Silesia Homocline, Poland
Autorzy:
Kaim, A.
Powiązania:
https://bibliotekanauki.pl/articles/138635.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
baton
Gnaszyn
iły rudonośne
jura
paleoekologia
Polska
ślimaki
Bathonian
gastropods
Jurassic
ore-bearing clays
palaeoecology
Polska
Opis:
The succession of gastropods in the Gnaszyn section is quite monotonous and shows significant changes only in the proximity of concretion layers, at least partially because of diagenetic reasons. Otherwise, the section is dominated by gastropods (cylidrobullinids, bullinids, and mathildids) most of which preyed probably on sedentary organisms (polychaetes and/or coelenterates) that possibly flourished on the sea bottom at that time. The other groups of gastropods are represented by larval or juvenile shells. Their presence shows that the environmental conditions that were probably unfavourable for gastropods living directly on the sea bottom most likely because of a soupy substrate consistency, possible oxygen deficiency near the sediment-water interface and/or oxygen content fluctuations. Adult and/or subadult individuals of these gastropods occur only in the higher part of the section, reflecting a time when these conditions improved. A new heterostrophic gastropod species, Promathildia gedli, is described.
Źródło:
Acta Geologica Polonica; 2012, 62, 3; 367-380
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Organic-walled dinoflagellate cysts from the Bathonian ore-bearing clays at Gnaszyn, Kraków-Silesia Homocline, Poland - a palaeoenvironmental approach
Autorzy:
Gedl, P.
Powiązania:
https://bibliotekanauki.pl/articles/138764.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
baton
dinocysty
iły rudonośne
jura środkowa
monoklina śląsko-krakowska
paleośrodowisko
Polska
Bathonian
dinoflagellate cysts
Kraków-Silesia Homocline
Middle Jurassic
ore-bearing clays
palaeoenvironment
Polska
Opis:
A succession of Middle-Upper Bathonian (Subcontractus.Retrocostatum zones) ore-bearing clays exposed at Gnaszyn has been investigated for the presence of dinoflagellate cysts. The assemblages are dominated by Ctenidodinium. However, analysis of diversity shows some subtle differences throughout the succession, possibly related to the palaeoenvironmental conditions in the photic zone. Impoverished assemblages, dominated by Ctenidodinium, occur mainly in monotonous muddy intervals. More diverse assemblages, albeit also dominated by Ctenidodinium, occur in intervals which contain siderite concretion levels. The taxonomic composition of the former assemblage seems to reflect slightly restricted conditions in the photic zone, possibly related to a minor reduction in salinity and/or increase in nutrient availability. More diverse dinoflagellate cyst assemblages reflect periods of less intense terrigenous influx and relatively higher, possibly normal, salinity. These changes were possibly caused by variable intensity of freshwater influx into the basin, controlled by sea-level fluctuations. Sea-level changes may be related to migrations of Tethyan water masses, which were probably partly responsible for the composition of the dinoflagellate cyst assemblages.
Źródło:
Acta Geologica Polonica; 2012, 62, 3; 439-461
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Palaeoenvironmental interpretation of echinoderm assemblages from Bathonian ore-bearing clays at Gnaszyn (Kraków-Silesia Homocline, Poland)
Autorzy:
Boczarowski, A.
Powiązania:
https://bibliotekanauki.pl/articles/138733.pdf
Data publikacji:
2012
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
baton
iły rudonośne
jura środkowa
paleośrodowisko
Polska
szkarłupnie
Bathonian
echinoderms
Middle Jurassic
ore-bearing clays
palaeoenvironment
Polska
Opis:
This paper presents the results of an investigation into the variability of echinoderm assemblages from Bathonian ore-bearing clays from Gnaszyn. Remains of Crinoidea, Asteroidea, Ophiuroidea, Echinoidea, and Holothuroidea have been studied from 38 rock samples. The most common echinoderms represented are the crinoids Balanocrinus berchteni and Chariocrinus andreae and a few species of the holothurian genera Priscopedatus, Calclamna, Staurocaudina, Eocaudina, Achistrum, Theelia and Hemisphaeranthos. The echinoderms from Gnaszyn show various life strategies: benthic or epibenthic forms, sessile sestonophages (Crinoidea), motile macrophages (Asteroidea) and detritivores (Asteroidea, Ophiuroidea, Echinoidea), infaunal and epifaunal detritus feeders, sediment feeders or rake-feeders (Holothuroidea). Their presence suggests well oxygenated and presumably relatively cold bottom marine waters. The parts of the Gnaszyn section around concretion horizons and characterized by the ubiquitous occurrence of the holothurian Theelia and echinoids were deposited during phases of optimal living conditions with sufficient influx of plant detritus and good oxygenation of the sea bottom. These parts commonly host echinoderm associations dominated by crinoid remains, which occasionally are still articulated (or disarticulated but remaining intact) - this points to a quiet environment with normal oxygenation of the bottom waters but anaerobic/dysaerobic conditions in the sediment.
Źródło:
Acta Geologica Polonica; 2012, 62, 3; 351-366
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 26

Ta witryna wykorzystuje pliki cookies do przechowywania informacji na Twoim komputerze. Pliki cookies stosujemy w celu świadczenia usług na najwyższym poziomie, w tym w sposób dostosowany do indywidualnych potrzeb. Korzystanie z witryny bez zmiany ustawień dotyczących cookies oznacza, że będą one zamieszczane w Twoim komputerze. W każdym momencie możesz dokonać zmiany ustawień dotyczących cookies