Autor: Zuber, A. - Prolib Integro

Skocz do pozycji: 1.

Tytuł:: On the origin of chloride waters in the Polish Flysch Carpathians
Autorzy:: Zuber, A.
Chowaniec, J.
Borowiec, M.
Tematy:: chloride waters
ultrafiltration
diagenetic waters
oil-field waters
catagenesis
flysch Carpathians; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2062987.pdf Link otwiera się w nowym oknie
Opis:: Chloride waters in the Polish Flysch Carpathians are remnants of marine sedimentation water which was chemically and isotopically changed due to ultrafiltration and the release of dehydration water (diagenetic water) during the burial diagenesis of clay minerals. In the western part of the study area, the diagenetic end-member is characterized by δ18O and δ2H values of about +6.5 and –30.0‰, respectively, and Cl– content in the range of 3.8 and 13.8 g/dm3. In some fault areas, such waters migrate to the surface and mix with local meteoric waters as indicated by mixing lines in δ18O–δ2H and δ18O–Cl– graphs. In several wells of the eastern part, waters containing a significant proportion of marine water occur. However, in majority of deep wells, mixtures of diagenetic and meteoric waters of Quaternary and pre-Quaternary climates are present, as deduced from δ18O–Cl– linear relations. In most cases, they do not exhibit linear relations also expected in δ18O–δ2H graphs due to the shifts of δ2H to heavier isotopic values supposedly caused by involvement of water in the generation of hydrocarbons.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Groundwater ages and altitudes of recharge areas in the Polish Tatra Mts. as determined from 3H, d18O and d2H data
Autorzy:: Zuber, A.
Małecki, J.
Duliński, M.
Tematy:: Tatra Mts.
groundwater
environmental isotopes
tritium ages; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2060203.pdf Link otwiera się w nowym oknie
Opis:: Large and medium karstic springs in the Polish Tatra Mts. occasion ally sampled during low flows exhibited little scatter of stable isotope composition and distinct differences between particular sampling sites. For extreme stable isotope values of four springs, the recharge altitudes were estimated by making use of topographic and geological maps. The altitude effect found in that way served for determining the recharge altitudes of other sampled sites. The altitude-effect gradients found in that way are -0.21‰/100 m and-1.45‰/100 m for delta exp.18 O and delta exp. 2 H, respectively. In general, large karstic springs (exsurgents) have the highest recharge altitudes whereas medium spring and deep wells are characterized by much lower altitudes. Tritium data interpreted with the aid of lumped parameter models yielded mean ages of ca. 3 years for low flows in large karstic springs, ca. 10 years for medium springs, and 50 to 100 years for deep wells, all with very wide age distributions. For four deep wells, the regional hydraulic conductivity estimated from tritium ages (0.8 ´ 10-6 m/s) is about 20 times lower than the geometric mean found from pumping tests (17 ´ -10–6 m/s) suggesting the existence of obstacles to regional flow.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: Pochodzenie i wiek wody mineralnej w Dobrowodzie k. Buska Zdroju
Origin and age of mineral water at Dobrowoda near the Busko Spa
Autorzy:: Chowaniec, J.
Najman, J.
Olszewska, B.
Zuber, A.
Tematy:: zapadlisko przedkarpackie
woda mineralna
skład izotopowy
gazy szlachetne
interglacjał
pre Pleistocen
baden
transgresja
Carpathian Foredeep
mineral water
stable isotopes
noble gases
water age
interglacial
pre-Pleistocene
Badenian transgression; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2074688.pdf Link otwiera się w nowym oknie
Opis:: In Dobrowoda village which is situated within the central area of the Polish Carpathian Foredeep, saline sulphur water has been found in a deep depression filled with Badenian sands. Environmental tracer data indicate similar interglacial age as that of shallow mineral waters occuring in Cretaceous marls in the nearby Busko Spa. Primary sulphates and secondary sulphides in all mineral waters of this region originated mainly from the dissolution of Badenian gypsum strata whereas the salinity is supposed to be the remnant of chloride salts of the same age which were completely washed out by meteoric waters during the long infiltration period after the regression of the Miocene sea. The hypothetical recharge area(s) are to the west of the study area, which means that chemical Badenian sediments occupied much larger area than the present extent of the sulphate series.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Cervical spine MRI findings in patients with mucopolysaccharidosis type II
Autorzy:: Kieć-Wilk, Beata
Tylki-Szymańska, Anna
Żuber, A.
Jurecka, A.
Jurkiewicz, E.
Dostawca treści:: Repozytorium Uniwersytetu Jagiellońskiego

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Skocz do pozycji: 5.

Tytuł:: Znaczniki środowiskowe w wodach termalnych niecki podhalańskiej
Environmental tracers in thermal waters of Podhale Basin
Autorzy:: Chowaniec, J.
Duliński, M.
Mochalski, P.
Najman, J.
Śliwka, J.
Zuber, A.
Tematy:: niecka popdhalańska
wody termalne
wiek wody
gazy szlachetne
Podhale basin
thermal waters
water age
noble gases; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2074700.pdf Link otwiera się w nowym oknie
Opis:: Tritium and stable isotope data delta exp.18 O and delta exp.2H) for wells near the recharge area of the thermal system of the Podhale Basin indicate the presence of modern waters recharged at the lowest altitudes of the outcrops of water bearing formations. In turn, delta exp.18O and delta exp.2H values obtained for deep part of the basin may be interpreted as either the result of a high altitude recharge or a cold climate. Helium contents are in general unusually high but can not be interpreted quantitatively at the present stage of the study. The noble gas temperatures (NGT) values obtained from Ne and Ar data disagree with temperatures deduced from the known dependence of air temperature on altitude and altitudes of recharge areas found from the stable isotope data. High concentrations ofHe (ca. 10-4 cm3STP/g), and low NGT deduced from Ne and Ar concentrations suggest the presence of pre-Holocene water in the northeastern part of the basin, which means slow movement of water. Stable isotope and exp.14C data indicate the presence of much younger Holocene waters in the western part of the basin.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 6.

Tytuł:: Mineral and thermal waters of Poland
Autorzy:: Ciężkowski, W.
Chowaniec, J.
Górecki, W.
Krawiec, A.
Rajchel, L.
Zuber, A.
Tematy:: Polska
wody lecznicze
wody mineralne
uzdrowiska
Polska
therapeutic waters
mineral waters
thermal waters
health resorts; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2066349.pdf Link otwiera się w nowym oknie
Opis:: Definitions, history, resources, origin, and use of mineral and thermal waters in Poland are discussed. Mineral and some thermal waters have been used on the present territory of Poland for therapeutic purposes probably since the Roman times and according to documents since medieval ages. Nowadays, different types of mineral and thermal waters are exploited in a number of Spas for therapeutic purposes, whereas in some other areas thermal waters are exploited for recreation and heating purposes. Their occurrences, origin, chemical types, legal aspects of exploitation, potential vulnerability and bottling are presented.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 7.

Tytuł:: Water ages in thermal system of the Podhale Basin (Inner Carpathians, southern Poland)
Autorzy:: Chowaniec, J.
Duliński, M.
Mochalski, P.
Najman, J.
Śliwka, I.
Zuber, A.
Tematy:: thermal waters
environmental tracers
water age
Podhale basin
Inner Carpathians; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2062981.pdf Link otwiera się w nowym oknie
Opis:: Karstified carbonates which outcrop in the Tatras, Inner Carpathians, southern Poland, and dip to the north under the flysch sediments of the Podhale Basin, represent the largest known renewable reservoir of thermal waters in the country, with temperatures up to about 80°C. Measurements of He excess, Ne and Ar unexpectedly revealed the existence of glacial age waters in the northeastern part of the basin, and late Holocene age waters in other parts. The noble gas data are shown to be in accordance with newly interpreted earlier long-term records of 3H, δ18O and δ2H in waters of the karstic springs, and with available determinations of 3H, δ18O, δ2H, 14C and δ13C in cold and thermal well waters.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 8.

Tytuł:: Typy chemiczne szczaw w Karpatach fliszowych a wiek wody
Chemical facies of CO2-rich waters in the Flysch Carpathians versus water age
Autorzy:: Chowaniec, J.
Ciężkowski, W.
Duliński, M.
Józefko, I.
Porwisz, B.
Zuber, A.
Tematy:: szczawy zwykłe
izotopy trwałe
tryt
wiek wody
hydrochemia
CO2-rich waters
stable isotopes
tritium
water age
hydrochemistry; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2063169.pdf Link otwiera się w nowym oknie
Opis:: Wykazano, że skład chemiczny i mineralizacja zwykłych szczaw w zachodniej części polskich Karpat fliszowych silnie zależą od wieku wody. Wody współczesne są zazwyczaj typu HCO3-Ca z mineralizacją poniżej 3 g/dm3, a wody wieku glacjalnego reprezentują różne typy ze zwiększonym udziałem jonów Mg2+ Mg2+ i Na+ lub Na+ i Mg2+, o mineralizacji znacznie przekraczającej 3 g/dm3. Zaobserwowane zależności mogą być przydatne dla lepszej identyfikacji wieku wód oraz procesów mieszania się wód o bardzo zróżnicowanym wieku.
Chemical composition and total dissolved solids (TDS) of CO2-rich waters in the western part of the Polish Carpathians depend strongly on the age of water. Modern waters are of the HCO3-Ca type with TDS usually below 3 g/l, whereas glacial age waters are of different types with increased contents of Mg2+, Mg2+ and Na+, or Na+and Mg2+, with TDS content significantly above 3 g/l. The relationships observed may serve for a better identification of ages and mixing patterns between waters of significantly different ages.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 9.

Tytuł:: Hydrodynamic modelling, environmental tracers and hydrochemistry of a confined sandy aquifer (Kędzierzyn-Głubczyce Subtrough, SW Poland)
Autorzy:: Witczak, S.
Szklarczyk, T.
Kmiecik, E.
Szczepańska, J.
Zuber, A.
Różański, K.
Duliński, M.
Tematy:: confined aquifers
hydrodynamic modelling
environmental tracers
hydrochemistry
water quality; Pokaż więcej
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:: https://bibliotekanauki.pl/articles/2059481.pdf Link otwiera się w nowym oknie
Opis:: Sarmatian sands and bur ied Pleis to cene val leys of the Kedzierzyn-Głubczyce Subtrough represent one of the main aquifers in southern Poland ( MGWB-332 - Major Ground Water Basin). This aquifer is intensively exploited, supplying tap water for the human population and for industry in the whole area; but, being confined, it has no influence on the ground water ecosystems. Two Ground Water Bodies (GWB-128 and GWB-129), introduced by administrative decisions according to EUDirectives, approximately cover the area of MGWB-332. The present study is related to the eastern part, the Sarmatian and buriedval eys sands of MGWB-332, i.e. to the most im - portant part of the multiaquifer GWB-129 which in profile consists of Holocene and Pleistocene sands, confined Sarmatian and Pleistocene buried valley sands, and Badenian sands. The presence and influence of deeper permeable formations is not addressed. The Sarmatian and Badenian aquifers are recharged and drained mainly by vertical seepages. Hydrodynamic modelling of the whole Kędzierzyn-Głubczyce Subthrough and tracer data indicate modern ages at the out crops of the Sarmatian under the Pleistocene deposits and mid to early Holocene ages close to the Odra River valley. Waters are of the HCO3-Ca type, changing at the centre of the Sarmatian to the SO4-Ca type due to the contribution of ascending sulphate water from the Badenian strata, whereas water in the buried Quaternary valley is of the HCO3-Na type, which means no significant contribution of ascending waters. Polluted modern waters occur only at the north west ern boundary in the area of the hydrogeological window. The quality of waters and their hydrochemistry result from water-rock in teractions and seepage exchanges with overlying and underlying aquifers belonging to the same GWB. Natural distributions of most major, minor and trace constituents are very wide, exemplifying difficulties in defining the quality of water in aunique way for the whole aquifer and particularly for the investigated multi-aquifer GWB.
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 10.

Tytuł:: Nucleation and Crystal Growth of Cu on Ir Tips Under Ultra-High Vacuum and in the Presence of Oxygen
Autorzy:: Zuber, S. M.
Ciszewski, A.
Tematy:: 61.16.Fk
81.15.Ef
68.35.Bs; Pokaż więcej
Wydawca:: Polska Akademia Nauk. Instytut Fizyki PAN
Powiązania:: https://bibliotekanauki.pl/articles/2013288.pdf Link otwiera się w nowym oknie
Opis:: Results concerning the morphology of Cu adsorption layers deposited from vapor under ultrahigh vacuum on Ir tip and the influence of oxygen on this morphology are reported. The method employed was field electron emission microscopy. It was found that the presence of oxygen decreases the copper wettability of iridium. Preadsorption of oxygen on the Ir surface is followed by an increase in cohesion interaction between atoms of the Cu deposited onto the tip at room temperature. Coadsorption of Cu and O on the Ir tip surface at liquid nitrogen temperature, when followed by gradually heating the adlayer, results in crystallization of the deposit in the temperature range from 430 K to about 700 K. Some evidence indicates the formation of Cu$\text{}_{2}$O with a high degree of crystallinity under these conditions. Cu and O coadsorption on the Ir surface at a temperature higher than 1090 K leads to selective accumulation of Cu on the {111} faces and to formation of epitaxial crystals which are oriented to the substrate in the same manner as the Cu crystals grown at ultra-high vacuum from Cu flux containing no oxygen. Oxygen incorporated into the Cu beam interact preferentially with {011} and {001} Ir faces, where it can produce oxide layers.
Dostawca treści:: Biblioteka Nauki

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