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Wyszukujesz frazę "Borkiewicz, O." wg kryterium: Autor


Wyświetlanie 1-3 z 3
Tytuł:
Synchrotron microanalytical methods in the study of trace and minor elements in apatite
Autorzy:
Rakovan, J.
Luo, Y.
Borkiewicz, O.
Powiązania:
https://bibliotekanauki.pl/articles/2086554.pdf
Data publikacji:
2008
Wydawca:
Polskie Towarzystwo Mineralogiczne
Tematy:
synchrotron
microanalysis
XRF
EXAFS
XANES
apatite
Opis:
Synchrotron X-ray facilities have the capability for numerous microanalytical methods with spatial resolutions in the micron to submicron range and sensitivities as low as ppm to ppb. These capabilities are the result of a high X-ray brilliance (many orders of magnitude greater than standard tube and rotating anode sources); a continuous, or white, spectrum through the hard X-ray region; high degrees of X-ray columniation and polarization; and new developments in X-ray focusing methods. The high photon flux and pulsed nature of the source also allow for rapid data collection and high temporal resolution in certain experiments. Of particular interest to geoscientists are X-ray fluorescence microprobes which allow for numerous analytical techniques including X-ray fluorescence (XRF) analysis of trace element concentrations and distributions; X-ray absorption spectroscopy (XAS) for chemical speciation, structural and oxidation state information; X-ray diffraction (XRD) for phase identification; and fluorescence microtomography (CMT) for mapping the internal structure of porous or composite materials as well as elemental distributions (Newville et al. 1999; Sutton et al. 2002; Sutton et al. 2004). We have employed several synchrotron based microanalytical methods including XRF, microEXAFS (Extended X-ray Absorption Fine Structure), microXANES (X-ray Absorption Near Edge Structure) and CMT for the study of minor and trace elements in apatite (and other minerals). We have also been conducting time resolved X-ray diffraction to study nucleation of and phase transformations among precursor phases in the formation of apatite from solution at earth surface conditions. Summaries of these studies are given to exemplify the capabilities of synchrotron microanalytical techniques.
Źródło:
Mineralogia; 2008, 39, 1/2; 31--40
1899-8291
1899-8526
Pojawia się w:
Mineralogia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Immobilizacja Pb(II) przez krystalizację piromorfitu na galenie w obecności nawozów fosforanowych
Immobilization of Pb(II) by crystallization of pyromorphite on galena in the presence of phosphate fertilizers
Autorzy:
Manecki, M.
Bajda, T.
Wegner, M.
Borkiewicz, O.
Powiązania:
https://bibliotekanauki.pl/articles/183579.pdf
Data publikacji:
2009
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
rekultywacja
neutralizacja skażeń Pb
zanieczyszczenie gleb
reclamation
neutralization of contamination with Pb
soil pollution
Opis:
In the presence of PO/4/3- and Cl/- ions, dissolution of galena PbS is accompanied with crystallization of pyromorphite Pb5(PO4)3Cl. This results in reduction of Pb(II) concentration which is more effective at pH 4 and 5 than at pH 2 and 3. When commercial fertilizers (Azofoska and Superfosfat) are used, the mechanism of Pb immobilization is identical. Azofoska is more effective and lowers the concentration of Pb below 0.05 mg/dm3.
Źródło:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2009, 35, 2/1; 263-269
0138-0974
Pojawia się w:
Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The philipsbornite–segnitite solid-solution series from Rędziny, eastern metamorphic cover of the Karkonosze granite (SW Poland)
Autorzy:
Gołębiowska, B.
Włodek, A.
Pieczka, A.
Borkiewicz, O.
Polak, M.
Powiązania:
https://bibliotekanauki.pl/articles/191534.pdf
Data publikacji:
2016
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
arsenates
oxidation zone
philipsbornite
segnitite
carminite
chemical composition
Rędziny
Opis:
Supergene minerals of the philipsbornite–segnitite series, PbAl3(AsO4)(AsO3OH)(OH)6–PbFe3+3(AsO4) (AsO3OH)(OH)6, accompanied by carminite, PbFe3+2(AsO4)2(OH)2, were found in relics of hydrothermal quartz– chlorite–arsenopyrite veins, associated with subordinate polymetallic ores disseminated in contact zones of a dolomitic marble deposit at Rędziny, Western Sudetes, Poland, and recognized by means of electron microprobe and X-ray and electron-back-scattered diffraction (XRD and EBSD). Philipsbornite and segnitite, as the two minerals of the series, exhibit highly variable compositions, especially in terms of the range of Fe3+ Al3+ substitution at the G site, with a distinct gap between the values of 0.52 and 0.89 for the Fe/(Al+Fe) ratio; substitutions at the D and T sites are less important. In this respect, the minerals are almost identical with philipsbornite and segnitite, known from other localities. The gap might be a consequence of the limited miscibility of the end-members, but also might be attributed to crystallization under the changing and distinctly differing activities of Al3+ and Fe3+. The unit-cell parameters of philipsbornite, a = 7.1245(13) Ο, c = 17.0967(45) Ο, make the mineral comparable with philipsbornites from other occurrences. The EBSD analysis confirmed the rhombohedral structure of both minerals and the space group symmetry R-3m. The minerals crystallized in the sequence: philipsbornite -> segnitite -> carminite, which reflects (i) decreasing acidity in the oxidation zone, due to the leaching of sulphate ions and interaction of the solutions with a nearby dolomite lens, and (ii) varying activities of Al3+, Fe3+ and Pb2+ cations, mobilized by the solutions through interaction with the silicate host containing disseminated arsenopyrite and subordinate sulphides, up to complete Pb2+ depletion.
Źródło:
Annales Societatis Geologorum Poloniae; 2016, 86, 1; 73-83
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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