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Tytuł:
Concentration of 222Rn in groundwaters flowing through different crystalline rocks: and example from îlŕ?a Massif (Poland)
Stężenia 222Rn w wodach podziemnych przepływających przez różne skały krystaliczne: przykład z Masywu Ślęży (Polska)
Autorzy:
Przylibski, T.
Powiązania:
https://bibliotekanauki.pl/articles/340196.pdf
Data publikacji:
2004
Wydawca:
Główny Instytut Górnictwa
Tematy:
masyw Ślęży
skażenie radonem
skażenie promieniotwórcze wody
Ślęża Massif
radon contamination
water radioactive contamination
Źródło:
Prace Naukowe GIG. Górnictwo i Środowisko / Główny Instytut Górnictwa; 2004, 1; 55-56
1643-7608
Pojawia się w:
Prace Naukowe GIG. Górnictwo i Środowisko / Główny Instytut Górnictwa
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Bulk chemical composition of Sołtmany chondrite
Autorzy:
Przylibski, T. A.
Łuszczek, K.
Powiązania:
https://bibliotekanauki.pl/articles/411498.pdf
Data publikacji:
2012
Wydawca:
Polskie Towarzystwo Meteorytowe
Tematy:
meteorite
ordinary chondrite
L-chondrite
bulk composition
meteorite fall
observed fall
Opis:
The authors examined the bulk chemical composition of the Sołtmany chondrite which fell on April 30th, 2011 in Northern Poland. Based on the analysis of 47 elements, it was concluded that Sołtmany is representative of L-type of ordinary chondrites. However, compared to the average values observed in other L-type ordinary chondrites, Sołtmany displays higher content of Ni, P, Cd, Pb, and As. The Ni and P content closely resembles typical values for H-type ordinary chondrites. Furthermore, Sołtmany displays other distinct properties including very low Zn content and lower contents of Mo and Zr than the average values found in other L-type ordinary chondrites. Consistent with other L-type ordinary chondrites, the absolute content of REE in Sołtmany is higher than that of CI-type carbonaceous chondrites while the REE trend lines for both Sołtmany and CI-chondrites are similar. Due to similar times of year of when both falls took place and the proximity of their strewn fields, the chemical composition of Sołtmany was compared with that of Jesenice, an L6 ordinary chondrite which fell on April 9th, 2009 in Europe. The analysis led to a conclusion that Sołtmany and Jesenice are not launch-paired. Nevertheless, even though they do not represent fragments of the same meteoroid, their origin on a common parent body (an asteroid – planetesimal) cannot be conclusively ruled out on the sole basis of their bulk chemical composition.
Źródło:
Meteorites; 2012, 2, No. 1-2; 31-37
2299-0313
2299-1220
Pojawia się w:
Meteorites
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wyniki badań mineralogicznych i petrologicznych nowych okazów meteorytu Pułtusk w 150 rocznicę spadku
Results of mineralogical and petrological research of new samples on the Pułtusk meteorite at the 150th anniversary of the fall
Autorzy:
Przylibski, T. A.
Łuszczek, K.
Powiązania:
https://bibliotekanauki.pl/articles/2075816.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Pułtusk
meteoryt
chondryt
zwyczajny chondryt
chondryt H5
meteorite
chondrite
ordinary chondrite
H5 chondrite
Opis:
One of the largest observed stone meteorite shower in the history of mankind on Earth took place on Thursday evening on January 30, 1868, about seven o’clock near Pułtusk in Poland. Despite the 150th anniversary of the fall of chondrite officially classified as Pułtusk H5 with a shock stage S3 there is still little published data on the chemical composition of minerals of this chondrite as well as its petrological characteristics in the literature. The authors carried out mineralogical and petrological research that will help a little to fill this gap in knowledge about the Pułtusk chondrite. Meteorite specimens found by Piotr Kuś in 2015 and investigated by the authors are undoubtedly part of the Pułtusk fall of January 30, 1868. They can be classified as ordinary chondrite H5, S2,W2. The authors stated that the studied rock is characterized by a varied shock level -from S1 to S2/3, as well as it contains chondrules of the chromite-plagioclase unequilibrated rock. In the composition of the examined fragment of Pułtusk chondrite, the authors identified silicates: olivine, diopside, bronzite and clinohyperstene, and oligoclase, oxides: chromite (and spinel), sulfides: troilite, FeNi alloy mineral phases: kamacite and taenite, as well as phosphates: merrilite and apatite. The chemical composition of olivine crystals as well as low- and high-Ca pyroxenes crystals and plagioclase crystals (about the composition of oligoclase) confirms that the examined specimen comes from the Pułtusk fall and it is a rock that should be classified as a petrographic type H5.
Źródło:
Przegląd Geologiczny; 2018, 66, 6; 368--378
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The occurrence of 226Ra and 228Ra in groundwaters of the Polish Sudety Mountains
Autorzy:
Przylibski, T.
Dorda, J.
Kozłowska, B.
Powiązania:
https://bibliotekanauki.pl/articles/147165.pdf
Data publikacji:
2002
Wydawca:
Instytut Chemii i Techniki Jądrowej
Tematy:
groundwaters
radium
radium waters
Sudety Mountains
Opis:
The paper presents preliminary measurement results of the concentrations of 226Ra and 228Ra isotopes in the groundwaters of the Polish part of the Sudety Mountains. The analysis of sampling results for water from 55 intakes showed that the average concentrations amount to 0.144 Bq/dm3 for 226Ra and 0.083 Bq/dm3 for 228Ra, while the extreme values reach 0.007 and 0.92 Bq/dm3 for 226Ra, and 0.004 and 0.4 Bq/dm3 for 228Ra. The activity ratio 228Ra/226Ra in the examined groundwaters ranges between 0.099 and 2.059. The result of the conducted research implies that the highest concentrations of 226Ra and 228Ra occur in the waters with the highest general mineralization (the highest values of total dissolved solids (TDS)).
Źródło:
Nukleonika; 2002, 47, 2; 59-64
0029-5922
1508-5791
Pojawia się w:
Nukleonika
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Selected processes in acidulous waters from Swieradów Zdrój in the light of the results of chemical analyses over the last thirty years
Wybrane procesy w szczawach Świeradowa Zdroju w wietle wyników analiz chemicznych z ostatnich trzydziestu lat - 100
Autorzy:
Przylibski, T. A.
Kozlowski, J.
Kabat, T.
Powiązania:
https://bibliotekanauki.pl/articles/191294.pdf
Data publikacji:
1998
Wydawca:
Polskie Towarzystwo Geologiczne
Opis:
In this paper the variability of chemical composition of Swieradów Zdrój acidulous waters for over thirty years is presented. Attempts were made at the interpretation of some noticeable effects occuring in these waters. Irregular fluctuations of free carbon dioxide content in acidulous waters (waters contained more than 1000 mg/dm3 of free CO2) and the lack of a general trend in its changes, as well as slow and constant decrease of total dissolved solids (TDS) in shallow intakes should be underlined. TDS changes in time are the result of various stages of deep circulation waters mixing with slightly mineralized shallow waters. To a certain extent, these changes may depend on the chemical composition changes of deep circulation acidulous waters. Correlation of the TDS changes in time with the variability of some ions concentration (mainly HCO3-, Ca2+, rarely Mg2+, K+) testifies to the origins of these ions from dissolution of rocks by acidulous waters of deep circulation. The origin of other ions should be connected with shallow circulation waters and with deep circulation acidulous waters as well. The lack of correlation between free carbon dioxide contents and concentration of hydrogen carbonate ion as well as lack of correlation between pH and CO2 and HCO3- concentration has not been explained yet and requires further research.
W pracy przedstawiono zmienność składu chemicznego szczaw Świeradowa Zdroju na przestrzeni ostatnich trzydziestu kilku lat. Podjęto także próbę interpretacji niektórych z zaobserwowanych zjawisk zachodzących w tych wodach. Na szczególne podkreślenie zasługuje stwierdzenie nieregularnych wahań zawartości wolnego dwutlenku węgla w szczawach oraz brak generalnego trendu jej zmian, a także powolny, stały spadek mineralizacji ogólnej w płytkich ujęciach. Korelacja zmian mineralizacji ogólnej (TDS) w czasie ze zmiennością stężeń niektórych jonów świadczy o pochodzeniu tych jonów z rozpuszczania skał przez szczawy głębokiego krążenia. Brak korelacji pomiędzy zawartością wolnego dwutlenku węgla a stężeniem jonu wodorowęglanowego nie został wyjaśniony i wymaga dalszych badań.
Źródło:
Annales Societatis Geologorum Poloniae; 1998, 68, 1; 95-103
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zawartość minerałów FeNi w chondrytach H jako wskaźnik zasobności pozaziemskich skał rudonośnych w wybrane metale
Concentration of FeNi minerals in H chondrites as an indicator of extraterrestrial ore-bearing rocks wealth in selected metals
Autorzy:
Blutstein, K.
Przylibski, T. A.
Łuszczek, K.
Powiązania:
https://bibliotekanauki.pl/articles/2075845.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
meteoryty
zwykłe chondryty
stop FeNi
pozaziemskie zasoby metali
chondryt H
asteroida 6 Hebe
meteorite
ordinary chondrite
H chondrite
FeNi alloy
extraterrestrial metal resources
H chondriteparent body
6 Hebe asteroid
Opis:
Extraterrestrial resources should be the basic sources of materials for the development of humankind civilization in space as well as they could replace the Earth’s resources when they would be exhausted. They can be obtained from the planets, their moons or asteroids, primarily NEOs but also from the asteroid belt. This article presents the results of petrographic research on the content of FeNi minerals whose may be a source of iron and nickel, in H type ordinary chondrites: Pułtusk, Cher- gach, Tamdakht, Gao-Guenie andNWA 4555, which parent body is probably the 6Hebe. The results confirm that the volumetric abundance of FeNi minerals in H type chondrites is ca. 8%. Moreover, this study shows the reliability of the reflected-light optical microscopy for determination of ore mineral concentrations in extraterrestrial rocks with weathering grade W0. Taking into account the homogenous spatial distribution of metallic grains (proved by author’s microscopic observations) and knowing the amount of FeNi minerals in rocks with Hchondrite composition, the amount of potential FeNi resources on Hparent bodies can be calculated. It was estimated that the iron resources from Hebe’s FeNi minerals would cover 1.3 million years of terrestrial mining production whereas nickel resources would last for approx. 100 milion years. A small NEO asteroid like (143624) 2003 HM16 (2 km in diameter) has resources comparable with 15 months of mining iron production and over 100 years of nickel production at present rate.
Źródło:
Przegląd Geologiczny; 2018, 66, 12; 776--784
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Potencjalnie lecznicze wody radonowe Masywu Ślęży
Potentially therapeutic radon waters of Ślęża Massif
Autorzy:
Przylibski, T. A.
Fijałkowska, L.
Bielecka, A.
Powiązania:
https://bibliotekanauki.pl/articles/2074598.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
radon
222Rn
wody podziemne
wody radonowe
groundwater
radon water
medicinal water
potential therapeutic water
Opis:
The authors have conducted research on radon occurrence in the groundwater system of Ślęża Massif in the Fore-Sudetic block. The research included documenting occurrence of radon waters in the granitoids of Strzegom-Sobótka Massif, buildingNWandWslopes of Ślęża. Among several springs flowing out from the granitoids and their waste, the Klasztorne Spring is characterized by constant radon (222Rn) concentration (306 ±39 Bq/dm3), but also constant though small discharge during the year, which enables estimating the admissible volume of this spring at 0.3 m3/h. The results obtained during the research show that this water can be treated as potentially medicinal. It generates the opportunity for the nearby town of Sobótka to develop as a health resort. Confirming the presence of radon groundwater in the granitoid part of Ślęża Massif implies a great probability that such w occur in the whole area of the Strzegom-Sobótka intrusion. It opens possibilities of recognizing new resources of potential therapeutic water and entails the necessity to take suitable actions for radiological protection of people living in this area.
Źródło:
Przegląd Geologiczny; 2008, 56, 8/2; 763-771
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Thermophysical properties of the Sołtmany meteorite
Autorzy:
Szurgot, M.
Wach, R. A.
Przylibski, T.A.
Powiązania:
https://bibliotekanauki.pl/articles/411496.pdf
Data publikacji:
2012
Wydawca:
Polskie Towarzystwo Meteorytowe
Tematy:
chondrite
differential scanning calorimetry (DSC)
specific heat capacity
thermal capacity
thermal diffusivity
thermal conductivity
Opis:
Bulk density, porosity and thermophysical properties of the Sołtmany meteorite have been determined. The mean bulk density of the meteorite is 3.475‧103kg/m3, mean bulk density of the crust is 4.3‧103 kg/m3, grain density 3.71‧103 kg/m3, and porosity 6.4 ±} 0.4%. Mean specific heat capacity determined by DSC in temperature range between 223 and 823 K increases from 595 to 1046 J/(kg‧K), and is equal to 728 J/(kg‧K) at room temperature. Specific heat capacity of various samples is in the range 705–769 J/(kg‧K) at room temperature. Thermal capacity of Sołtmany chondrite is equal to 2.53‧106 J/(m3‧K), thermal diffusivity (1.5–1.8)‧10-6 m2/s, and thermal conductivity 3.9–4.5 W‧m–-1‧K-1at room temperature. Differential scanning calorimetry revealed two reversible phase transitions in the Sołtmany’s troilite: α/β transition at 423 K, and β/γ transition at 596.6 K.
Źródło:
Meteorites; 2012, 2, No. 1-2; 53-65
2299-0313
2299-1220
Pojawia się w:
Meteorites
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Primitive enstatite achondrites
Autorzy:
Pilski, A. S.
Przylibski, T. A.
Łuszczek, K.
Powiązania:
https://bibliotekanauki.pl/articles/411494.pdf
Data publikacji:
2011
Wydawca:
Polskie Towarzystwo Meteorytowe
Tematy:
Acapulcoite
lodranite
winonaite
brachinite
ureilite
metachondrite
primitive achondrite
enstatite chondrite
primitive enstatite achondrite
Opis:
Conclusions drawn from the breadth of analytical data on primitive achondrites and enstatite chondrites paired with results of research performed by the authors have led the authors to propose the establishing of a new group of meteorites: primitive enstatite achondrites. The group is defined as the residual remaining after the partial melting of their protolith, which, in the case of primitive enstatite achondrites, is the parent body of enstatite chondrites. In this article are characterized textural features and characteristics of their mineral, chemical, and isotopic composition. The most important of these defining features are the presence of relic chondrules and/or triple junctions of crystal faces, as well as characteristic atomic and molar ratios of main elements: Si, Al, Fe, Mg, Mn and Ca, and particularly the molar ratios Fe/Mn and Fe/Mg. Another important characteristic is the isotopic composition of entrained noble gases, especially ratios of the heaviest of the isotopes and oxygen isotopes, whose values should be close to that typical for enstatite chondrites. It seems likely that the first meteorite to be classified as primitive enstatite achondrite will be the Zakłodzie enstatite achondrite.
Źródło:
Meteorites; 2011, 0, 0; 9-21
2299-0313
2299-1220
Pojawia się w:
Meteorites
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Comparative analysis of the Baszkówka and Mt. Tazerzait chondrites: genetic conclusions based on astrophysical data and the mineralogical and petrological data
Autorzy:
Pilski, A. S.
Przylibski, T. A.
Zagożdżon, P. P.
Powiązania:
https://bibliotekanauki.pl/articles/2059300.pdf
Data publikacji:
2001
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
meteorites
chondrites
solar system
asteroids
asteroid-collisions
Opis:
The L5 chondrites Baszkówka and Mt. Tazerzait are characterised. Their astronomical, mineralogical and petrological characteristics confirm that these meteorites are similar. They could be derived from the same parent body, though from the different depths below its surface. A third meteorite - the Tjerebon - might have arisen from the same swarm of meteoroids. The parent body to these meteorites in the asteroid belt can not be established at present. The porosity, of these chondrites suggests that they formed close to the surface of their parent asteroid. The process of formation of the parent rock of the Baszkówka chondrite is similar in some respects to sedimentation of a weakly compacted terrestrial sandstone. Thus, a two-stage geological history may be envisaged: firstly formation of the component minerals and mineral aggregates of this meteorite. Then, later in a different environment, the accretion of fragments of this parent material, together with a small amount of matrix, into a strongly porous sedimentary rock.
Źródło:
Geological Quarterly; 2001, 45, 3; 331-342
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Skład gazów rozpuszczonych w wodzie termalnej eksploatowanej odwiertem KT-1 w Karpnikach na obszarze granitu karkonoskiego w Sudetach
Composition of gas dissolved in thermal water extracted from borehole BKT-1 at Karpniki (Karkonosze granite area, Sudetes)
Autorzy:
Przylibski, T. A.
Żak, S.
Kowalska, A.
Domin, E.
Powiązania:
https://bibliotekanauki.pl/articles/2075848.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
skład gazu
gaz szlachetny
azot
hel
argon
radon
gas composition
noble gas
nitrogen
helium
Opis:
The detailed research of a gas mixture released from the thermal water, which is extracted from borehole KT-1 at Karpniki, showed the predominance of nitrogen (98.08% by volume) with subordinate Ar (1.52%) and He (0.32%) and trace amounts of CO2 (0.07%) and CH4 (0.01%). The 222Rn radionuclide is also dissolved in this water, showing an activity concentration of 245 Bq/dm3 at the outflow and 256 Bq/dm3 in the aquifer. A small value of the gas exponent (0.014), and also a value of the δ coefficient close to 1 (0.93) were calculated based on the dissolved Ar and N2 content in the water examined, as well as on concentrations of argon and nitrogen in water, assuming that atmospheric air is present above the water surface with a contemporary composition and under normal pressure. The data obtained indicate that these gases and additionally CO2 and CH4 are of atmospheric origin. These gases were either dissolved in rainwater, which infiltrated deep into the Karkonosze granite massif, orformed within the organic layer covering this exposed intrusion. This is evidenced by concentrations of these gases that can be comparable to their atmospheric equivalents. Helium is a radiogenic gas formed as a result of nuclear transformation of isotopes assigned to natural radioactive series. The radiogenic and also radioactive gas is represented by the 222Rn radioisotope which is released from reservoir rocks, in an amount of 5% of the atom poolforming in the reservoir rock, into thermal water that subsequently reaches borehole KT-1 from a distance of 34 m at most. The thermal paleoinfiltration water has been heated up as a result of the conduction, and the source of heat is the temperature of the rocks resulting from an average geothermal gradient of 2.96°C per 100 m. The results of the authors’research indicate that there are no traces of inflow of hotfluids (especially water) from the deeper layers of the crust or from the mantle. If the examined thermal water is considered as paleoinfiltration water, its static resources may be limited, non-renewable.
Źródło:
Przegląd Geologiczny; 2018, 66, 8; 483--494
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Uranium, radium and radon isotopes in selected brines of Poland
Autorzy:
Kozłowska, B.
Walencik, A.
Przylibski, T. A.
Dorda, J.
Zipper, W.
Powiązania:
https://bibliotekanauki.pl/articles/148912.pdf
Data publikacji:
2010
Wydawca:
Instytut Chemii i Techniki Jądrowej
Tematy:
uranium
radium
radon
brines
Opis:
Natural radioactive isotopes were studied in nine different types of brines from four locations in Poland. Investigated brines are exploited from various geological structures composed of the rocks of different chemical and mineral composition as well as different age and depth. All investigated brines are used in balneotherapy (i.e. baths, inhalations, showers). The main goal of this study was to obtain some basic knowledge on the activity range of natural elements such as uranium, radium and radon in different brine types in Poland and their variability depending on their location in certain geological structures. Activities of 234,238U, 226,228Ra and 222Rn isotopes were measured with the use of two nuclear spectrometry techniques: liquid scintillation and alpha spectrometry. The activity concentrations of 222Rn vary from below 1 to 76.1 plus or minus 3.7 Bq/l, for the 226Ra isotope from 0.19 plus or minus 0.01 to 85.5 plus or minus 0.4 Bq/l and for 228Ra from below 0.03 to 2.17 plus or minus 0.09 Bq/l. For uranium isotopes, the concentrations are in the range from below 0.5 to 5.1 plus or minus 0.4 mBq/l for 238U and from 1.6 plus or minus 0.4 to 45.6 plus or minus 2.0 mBq/l for 234U. The obtained results indicate high radium activity concentrations corresponding to high mineralization of waters.
Źródło:
Nukleonika; 2010, 55, 4; 519-522
0029-5922
1508-5791
Pojawia się w:
Nukleonika
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Polish national intercomparisons of measurement methods of 222Rn concentration in waters
Krajowe pomiary interkalibracyjne stężenia 222 Rn w próbkach wód
Autorzy:
Przylibski, T.
Mamont-Cieśla, K.
Stawarz, O.
Kłos, B.
Dorda, J.
Powiązania:
https://bibliotekanauki.pl/articles/340341.pdf
Data publikacji:
2004
Wydawca:
Główny Instytut Górnictwa
Tematy:
intercomparison measurement
radon contamination
radiological protection in Poland
Radon Centre
Źródło:
Prace Naukowe GIG. Górnictwo i Środowisko / Główny Instytut Górnictwa; 2004, 1; 71-73
1643-7608
Pojawia się w:
Prace Naukowe GIG. Górnictwo i Środowisko / Główny Instytut Górnictwa
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wody lecznicze regionu sudeckiego : wybrane problemy
Mineral waters of the Sudetic region (SW Poland) : selected problems
Autorzy:
Ciężkowski, W.
Kiełczawa, B.
Liber-Makowska, E.
Przylibski, T.
Żak, S.
Powiązania:
https://bibliotekanauki.pl/articles/2075535.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
wody mineralne
wody lecznicze
wody termalne
wody radonowe
mieszanie wód
region sudecki
mineral waters
medicinal waters
thermal waters
radon waters
mixing of waters
Sudetic region
Opis:
Mineralized waters used for medical treatment are common in the Sudetes. Due to reservoir rock types and the depth of groundwater circulation, two main types of groundwater deposits are distinguished. These are fissure deposits, the most often present in granites and gneisses, andfissure-porous deposits present first of all in sandstones. The main types of mineralized groundwater are CO2-rich waters, containing up to 99.5% of CO2 as the primary gas component, thermal waters characterized by the temperatures up to 87°C, which classifies these waters as the warmest in Poland, as well as radon waters, containing the highest activity concentrations of 222Rn, reaching above 2,000 Bq/dm3. All these groundwater types are infiltration waters. Discharge rates of the intakes in the Sudetes changes with time, which is influenced by changes in atmospheric parameters. The time of reaction is similar for all the intakes in the same hydrogeological structure. The process of mixing between the highly-mineralized, deep-circulation groundwater component and the shallow-circulation, low-mineralized component is intensely studied. Another problem is the presence of CO2 in the amount exceeding its solubility in the water. Juvenile CO2 flows from the deep crust through tectonic discontinuities, where it dissolves in groundwater, forming CO2-oversaturated waters, as well as itforms gas anomalies in soil air. CO2 concentrations may reach in soils more than 60 vol.%, and the flux of this gas reaches even 66 g/m2/d. Radon dissolves in groundwater in the zone of its out flow, where reservoir rocks are densely cracked, weathered, and cut by tectonic faults. The hydrogeochemical background of 222Rn in groundwater of the Sudetes is between 4 and 306 Bq/dm3.
Źródło:
Przegląd Geologiczny; 2016, 64, 9; 671--682
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Natural radioactivity of groundwater from the Przerzeczyn-Zdrój Spa
Autorzy:
Walencik, A.
Kozłowska, B.
Przylibski, T. A.
Dorda, J.
Zipper, W.
Powiązania:
https://bibliotekanauki.pl/articles/148493.pdf
Data publikacji:
2010
Wydawca:
Instytut Chemii i Techniki Jądrowej
Tematy:
radon
radium
uranium
groundwater
medicinal water
Opis:
The present authors performed investigations of natural radioactivity in groundwater from the Przerzeczyn- -Zdrój Spa. Some of the waters are regarded as medical and are used for balneological purposes. Samples from seven groundwater intakes were collected 5 times over a period of 8 years (1999–2007). In order to obtain necessary data, two different nuclear spectrometry techniques were applied: α spectrometry and liquid scintillation spectrometry. The activity concentrations of 222Rn varied in the range from 15±2 Bq/l to 154±22 Bq/l. The results of activity concentrations of 226,228Ra varied from below 10 mBq/l to 30±1.5 mBq/l and from below 30 mBq/l to 60±4 mBq/l, respectively. Activity concentration lower than minimum detectable activity (MDA) was obtained for 3 samples for 226Ra and 4 for 228Ra determinations out of 7 investigated samples. The uranium content in the studied samples was determined once and the value ranged from 4.5±0.6 mBq/l to 13.6±1.2 mBq/l for 238U and from 17.1±0.9 mBq/l to 52.2±2.8 mBq/l for 234U. All obtained values for uranium isotopes showed activity concentrations above MDA. The activity ratios 234U/238U, 222Rn/226Ra and 226Ra/238U and the correlations between different isotopes concentrations were evaluated.
Źródło:
Nukleonika; 2010, 55, 2; 169-175
0029-5922
1508-5791
Pojawia się w:
Nukleonika
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 17

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