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  • 1
    ISSN: 1573-4803
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Abstract A study was undertaken to obtain more accurate structural information on poly(p-phenylene sulfide) (PPS) through Rietveld analysis. A few samples of PPS crystallized in a relatively wide range of physical conditions were selected with the aim of eventually identifying the occurrence of structural modifications induced by the various crystallization procedures. According to the results, the structural modifications are relatively small and essentially confined to variations of the C–S–C angle, for which values within the range 102°–105° were found close to those proposed by Garbarczyk. In particular, the strong influence of the amorphous phase in determining the crystallographic cell dimension was investigated.
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  • 2
    ISSN: 1862-0760
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract LixCoO2 samples with different nominal load x were prepared submitting HT-LiCoO2 membrane electrodes to electrochemical polarisation, followed by aging in open circuit conditions. Care was taken to obtain samples for both positive and negative overcharge beyond the canonical regime (0.6≤x≤1) of the LixCoO2 electrode. For 11 samples in the range 0.37≤x≤1.43, Rietveld refinements of X-ray diffraction data were performed, with Li at 3a, Co at 3b and O at 6c in the space group R-3m as starting model. In the range 0.37≤x≤1, results show a continuous variation of theac unit cell and structural parameters such as the lithium site occupancy and the Li-O and Co-O interatomic distances. For samples in the range 1≤x≤1.43, Li2CO3 was detected as an impurity which might be due to decomposition of the electrolyte, and, if the negative overcharge was high enough, an abnormally high electron density at the 3a site indicates some Li→Co substitution. Results from Co-K edge X-ray absorption spectroscopy for the samples with x=0.37, 0.89, 1 and 1.43 show a clear shift of the absorption maximum with the oxidation state of Co and support the conclusions from Rietveld refinement. GNXAS refinement of EXAFS spectra for the samples with x=0.37 and 1 suggest that cation disordering may occur also for deep lithium deintercalation (positive overcharge), a fact which was not detectable from diffraction data.
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  • 3
    Publication Date: 2015-04-02
    Description: Inhalation of erionite has been proven to be the cause of the extended epidemic of malignant mesothelioma occurring in Central Anatolia, Turkey, and of cases of lung diseases in the U.S.A. Its carcinogenicity is three orders of magnitude greater than that of regulated asbestos. Here we report the results of the investigation of the structural and crystal chemical modifications occurring in erionite leached with artificial lysosomal fluid (ALF) and Gamble’s solution. ALF leaching produces a migration of Na + ions from Ca1 to Ca2 extraframework cationic site, without the occurrence of any significant modification of the chemical composition of the fibers. In contrast, leaching with Gamble’s solution induces a complex ionic-exchange process resulting in a temporary partial replacement of Na + by Ca 2+ , coming from the fluid, which is fixed at a third Ca3 cationic site. Subsequently, the exchange process reverses. In fact, Ca 2+ is removed from Ca3 and Na + migrates back to Ca1, the structure being indistinguishable from the starting, unleached material. Such processes seem to be accompanied by a progressive amorphization of fibers. Present data could provide valuable background for a more detailed comprehension of the morphostructural/biological activity relationships inducing pathogenicity.
    Print ISSN: 0003-004X
    Electronic ISSN: 1945-3027
    Topics: Geosciences
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  • 4
    Publication Date: 2015-04-29
    Description: The present work analyses the thermal behaviour of alum-(K), KAl(SO 4 ) 2 ·12H 2 O, by in situ laboratory high-temperature powder X-ray diffraction data from 303 K to melting, which starts at 355 K and is completed, due to kinetics, at 359 K. The calculated a 0 linear thermal expansion coefficient is of 14.68(11) x 10 –6 K –1 within the investigated thermal range. The k disorder parameter, describing the extension of the orientational disorder of the sulfate group, has been found to decrease from ~0.70 to ~0.65 just before melting. It has been demonstrated that the occurrence of the disorder implies the coexistence of K + ions in both six- and seven-fold coordination. This is necessary for assigning a reasonable bond-valence sum of 0.81 valence units (vu) to the ‘average’ K + ion a instead of 0.66 vu, which is obtained in the case of six-fold coordination alone. We can describe the temperature dependence of k from 93–355 K by means of the empirical equation k = 0.798(12) + 2.5(11) x 10 –4 T – 1.9(2) x 10 –6 T 2 , which includes reference low-temperature data. Bond-valence analysis has shown that, on cooling, an increase of the k disorder parameter and shortening of the K–O2 bond distance act together to maintain constancy in the bond-valence sum at the K site, stabilizing the structure. Therefore, the need for keeping the ‘average’ K + ion at a reasonable bond-valence sum appears to be the driving force for the ordering process involving the sulfate group.
    Print ISSN: 0026-461X
    Electronic ISSN: 1471-8022
    Topics: Geosciences
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  • 5
    Publication Date: 2014-02-20
    Description: Cinnabar use on painting is historically documented from ancient times, together with its tendency to darken. The most accepted mechanism for this kind of deterioration considers cinnabar (α-HgS) transformation into its polymorph metacinnabar, β-HgS, but recent studies have cast doubt on this hypothesis. On this background, an in situ high-temperature X-ray powder diffraction study of the thermal behaviour of cinnabar has been carried out. Data, measured in transmission geometry on a non-hermetically sealed capillary, indicate that the α-HgS (trigonal)-〉β-HgS (cubic) phase transition occurs at 673 K and is completed at 698 K due to kinetics reasons. The thermal expansion of cinnabar is fairly isotropic, the a -parameter being slightly softer against heating. A fast cooling of metacinnabar at room temperature ( T ) produced a mixture of both polymorphs. The analysis of the kinetics of the β-HgS-〉α-HgS transformation at room- T shows a low rate of conversion, but not low enough to be consistent with a persistence of metacinnabar for a time span of 2000 years as hypothesized in reference data for Pompeian frescoes.
    Print ISSN: 0935-1221
    Electronic ISSN: 1617-4011
    Topics: Geosciences
    Published by Schweizerbart
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  • 6
    Publication Date: 2016-05-17
    Description: The quantitative chemical composition of a sample of erionite-Na from Rome, Oregon (USA) was retrieved by SEM-EDX standardless analysis. The analysed fibres have a diameter commonly smaller than 3 μm, i.e . those more easily inhalable, therefore representing a typical case encountered during environmental investigations. The claimed dependence of the toxicity and biological activity of the fibres to their crystal chemical features renders the reliable chemical characterization of paramount importance. To reduce the errors induced by particle size/morphology effects, an empirical procedure was adopted. In particular, correction factors were calculated for each oxide as a function of the particle diameter using shards of zeolites and feldspathoids of known bulk composition. Those correction factors have to be considered as sample specific. Experimental conditions were optimised in order to minimize the effect of alkali metal migration. Results indicate that particle effects cause on the oxide concentrations a relative underestimation of Al 2 O 3 and K 2 O by up to ca . 10 %, whereas Na 2 O is overestimated by up to ca . 15 %. Moreover, the SiO 2 concentration is independent from dimension even in the case of very small particles. Finally, comparison between electron-microprobe and SEM-EDX bulk analyses of crystals pointed out a relative underestimation of Na, K, (of ca. 10–15 %) and Ca (of ca . 5 %) for the SEM data, in good agreement with reference structural investigations.
    Print ISSN: 0935-1221
    Electronic ISSN: 1617-4011
    Topics: Geosciences
    Published by Schweizerbart
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  • 7
    Publication Date: 2016-05-17
    Description: The thermal behaviour of otavite, CdCO 3 , has been investigated from 303 K up to decomposition, which starts at 603 K and is completed, due to kinetics, at 648 K. The dependence of the cell parameters on temperature is peculiar as the a parameter slightly increases up to 453 K and subsequently contracts. Microstrain 0 follows the same behaviour. The possible occurrence of orientational disorder of the CO 3 group has been observed near the decomposition temperature T d . However, the partial superposition of Bragg reflections of otavite and its decomposition product, CdO, coupled to fast kinetics, lead to less accurate structural parameters near T d , requiring confirmation of such result.
    Print ISSN: 0935-1221
    Electronic ISSN: 1617-4011
    Topics: Geosciences
    Published by Schweizerbart
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  • 8
    Publication Date: 2013-11-19
    Description: A detailed morphological, crystal-chemical, and structural characterization of erionite from the type locality of Durkee, Oregon, has been carried out by combining field emission scanning electron microscopy (FESEM) and laboratory parallel-beam transmission X-ray powder diffraction (XRPD). According to the crystal-chemical formula (Na 5.38 K 1.99 Mg 0.24 )[Al 7.66 Si 28.34 O 72.09 ]·29.83H 2 O, the sample has been classified as erionite-Na. The Rietveld refinement has indicated that the extraframework cations are located at three Ca1, Ca2, and Ca3 sites, the first one containing all available Mg. Moreover, the absence of the additional K2 site found in both dehydrated erionite and erionite-K has been demonstrated for this erionite sample. Furthermore, our results revealed the absence of Fe and Ca although previous investigations have reported the presence of a variable content of both these elements in erionite samples from Durkee. This is relevant information because it is well known from amphibole asbestos that Fe 2+ has been claimed to be one of the causes of carcinogenesis by participating in Fenton chemistry and producing free radicals.
    Print ISSN: 0003-004X
    Electronic ISSN: 1945-3027
    Topics: Geosciences
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  • 9
    Publication Date: 2012-08-01
    Description: An in situ high-temperature X-ray powder diffraction study of the thermal behavior of realgar (α-As 4 S 4 ) has been carried out. Data, measured in transmission geometry on a non-hermetically sealed capillary, indicate that the realgar -〉 β-As 4 S 4 phase transition starts at 558 K and is completed at 573 K due to kinetics. Melting starts at 578 K and is completed at 588 K. Thermal expansion of realgar is significant and fairly isotropic. In fact, the a -and b -parameters expand almost at the same rate, whereas the c -parameter is slightly softer against heating. Moreover, the β-angle contracts as temperature is raised. The geometry of the As 4 S 4 molecule is largely independent from heating. The lengthening of a few As-S and As-As contacts above or near the sum of the As,S van der Waals radii represents the driving force of the phase transition. In addition, the thermal behavior of arsenolite As 2 O 3 and non-stoichiometric As 8 S 8+x crystals produced from As 4 S 4 melt recrystallization has been investigated. Two members located along the β-As 4 S 4 -alacranite (As 8 S 9 ) series joint were identified at RT: a term close to the β-As 4 S 4 end-member (As 8 S 8+x : x = ca. 0.1) and one term of approximate As 8 S 8.3 composition. The thermal expansion of β-As 4 S 4 is significantly anisotropic following the α b 〉 α a 〉 α c relationship. This is clearly the result of the different packing scheme of the As 4 S 4 cages in β-As 4 S 4 with respect to realgar. The dependence of cell parameters and volume of As 8 S 8.3 is more complicated. In fact, a strong discontinuity on the dependence of cell parameters and volume is observed in the 403–443 K thermal range, i.e., that at which As 8 S 8.3 converts partly to realgar. A significant volume expansion is observed as a result of a change of composition to As 8 S 8.7 .
    Print ISSN: 0003-004X
    Electronic ISSN: 1945-3027
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  • 10
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    Mineralogical Society of Great Britain and Ireland
    Publication Date: 2013-10-26
    Description: A sample of levyne-Na from Dunseverick, Antrim, Northern Ireland, UK, has been characterized from the crystal chemical and structural point of view. Its mean crystal chemical formula, calculated on the basis of 54(Si+Al), is Na 7.72 Ca 4.62 K 1.31 Sr 0.08 Mg 0.02 (Al 19.55 Si 34.45 O 107.50 )·50.5H 2 O. Levyne-Na is associated with erionite-Na whose chemical formula is Na 6.08 Ca 0.85 K 2.55 Mg 0.16 (Al 10.41 Si 25.59 O 72.13 )·30.6H 2 O, calculated on the basis of 36(Si+Al). Their compositions are consistent with those of levyne/erionite inter/overgrowth reported in the literature. The structural analysis, carried out by the Rietveld method on laboratory parallel-beam X-ray powder diffraction data, is in good agreement with the chemical composition representing a significant improvement with respect to the available data so far. Extra-Framework (EF) cations are allocated at four sites, Ca1, Na3, K4 and Na5 with partial occupancy. Water molecules are distributed among five sites. Possible coexistence schemes of cations, forced by the avoidance of short contacts are proposed and validated by bond valence analysis.
    Print ISSN: 0026-461X
    Electronic ISSN: 1471-8022
    Topics: Geosciences
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