[Pinguicula alpina]

R. Anheisser

[Pinguicula vulgaris]

R. Anheisser

Pollen record and age determiation of sediments from the Labaz Lake area

Pollen records from perennially frozen sequences provide vegetation and climate reconstruction for the last 48,000 14C years in the central part of Taymyr Peninsula. Open larch forest with Alnus fruticosa and Betula nana grew during the Kargin (Middle Weichselian) Interstade, ca. 48,000-25,000 14C yr B.P. The climate was generally warmer and wetter than today. Open steppe-like communities with Artemisia, Poaceae, Asteraceae, and herb tundralike communities with dwarf Betula and Salix dominated during the Sartan (Late Weichselian) Stade, ca. 24,000-10,300 14C yr B.P. The statistical information method used for climate reconstruction shows that the coldest climate was ca. 20,000-17,000 14C yr B.P. A warming (Allerød Interstade?) with mean July temperature ca. 1.5°C warmer than today occurred ca. 12,000 14C yr B.P. The following cooling with temperatures about 3°-4°C cooler than present and precipitation about 100 mm lower corresponds well with the Younger Dryas Stade. Tundra-steppe vegetation changed to Betula nana-Alnus fruticosa shrub tundra ca. 10,000 14C yr B.P. Larch appeared in the area ca. 9400 14C yr B.P. and disappeared after 2900 14C yr B.P. Cooling events ca. 10,500, 9600, and 8200 14C yr B.P. characterized the first half of the Holocene. A significant warming occurred ca. 8500 14C yr B.P., but the Holocene temperature maximum was at about 6000-4500 14C yr B.P. The vegetation cover approximated modern conditions ca. 2800 14C yr B.P. Late Holocene warming events occurred at ca. 3500, 2000, and 1000 14C yr B.P. A cooling (Little Ice Age?) took place between 500 and 200 14C yr ago.

Age determination and sedimentology on profile Lz1021

A 9.14 m long sediment sequence was recovered from Lake Fryxell, Taylor Valley, southern Victoria Land, Antarctica, and investigated for its chronology and sedimentological, mineralogical, and biogeochemical changes. The basal part of the sequence is dominated by coarse clastic matter, i.e., mainly sand. The sediment composition suggests that a lake existed in Fryxell basin during the Middle Weichselian by ca. 48,000 cal. year BP. After a short period of lake-level lowstand ca. 43,000 cal. year BP, lower Taylor Valley became occupied by the proglacial Lake Washburn, which was at least partly supplied by meltwater and sediments from the Ross Ice Sheet that was advanced to the mouth of Taylor Valley. Evaporation of Lake Washburn to lower levels started during the Last Glacial Maximum at ca. 22,000 cal. year BP, long before the Ross Ice Sheet retreated significantly. Lake-level lowering was discontinuous with a series of high and low stands. From ca. 4000 cal. year BP environmental conditions were similar to those of today and lower Fryxell basin was occupied by a small lake. This lake evaporated to a saline or hypersaline pond between ca. 2500 and 1000 cal. year BP and refilled subsequently.

Average structure of an An (sub 48) plagioclase from the Hogarth Ranges

The average structure (CI) of a volcanic plagioclase megacryst with composition Ano, from the Hogarth Ranges, Australia, has been determined using three-dimensional, singlecrystal neutron and X-ray diffraction data. Least squaresr efinements, incorporating anisotropic thermal motion of all atoms and an extinction correction, resulted in weighted R factors (based on intensities) of 0.076 and 0.056, respectively, for the neutron and X-ray data. Very weak e reflections could be detected in long-exposure X-ray and electron diffraction photographs of this crystal, but the refined average structure is believed to be unaffected by the presence of such a weak superstructure. The ratio of the scattering power of Na to that of Ca is different for X ray and neutron radiation, and this radiation-dependence of scattering power has been used to determine the distribution of Na and Ca over a split-atom M site (two sites designated M' and M") in this Ano, plagioclase. Relative peak-height ratios M'/M", revealed in difference Fourier sections calculated from neutron and X-ray data, formed the basis for the cation-distribution analysis. As neutron and X-ray data sets were directly compared in this analysis, it was important that systematic bias between refined neutron and X-ray positional parameters could be demonstrated to be absent. In summary, with an M-site model constrained only by the electron-microprobedetermined bulk composition of the crystal, the following values were obtained for the M-site occupanciesN: ar, : 0.29(7),N ar. : 0.23(7),C ar, : 0.15(4),a nd Car" : 0.33(4). These results indicate that restrictive assumptions about M sites, on which previous plagioclase refinements have been based, are not applicable to this Ano, and possibly not to the entire compositional range. T-site ordering determined by (T-O) bond-length variation-t,o : 0.51(l), trm = t2o = t2m = 0.32(l)-is weak, as might be expectedf rom the volcanic origin of this megacryst.

Precipitation of rutile and anatase (Tio12) fine powders and their conversion to MTiO3 (M = Ba, Sr, Ca) by the hydrothermal method

Fine powders of TiO2 (rutile) with high degree of crystallinity are formed from aqueous titanium oxychloride solution under hydrothermal conditions at 160–230°C and 15–100 kg/cm2 for 1–2 hours. The anatase phase is produced from the same medium when sulfate ion impurity is present, with Image . Both these fine powders are converted to BaTiO3, SrTiO3 or CaTiO3 when suspended in Ba(OH)2 or Sr(OH)2 solution or in an aqueous slurry of carbonate-free CaO with Image , at 180–280°C and 12–65 kg/cm2 for 4–8 hours. The resulting fine powders contain monocrystallites of the perovskite phase with 0.1–1.5 μm particle size.

Phase relations in the system Ca-Ta-O and thermodynamics of calcium tantalates in relation to calciothermic reduction of Ta2O5

Phase equilibria of the system Ca-Ta-O is established by equilibrating eleven samples at 1200 K for prolonged periods and phase identification in quenched samples by optical and scanning electron microscopy, energy dispersive spectroscopy and X-ray diffraction. Four ternary oxides are identified: CaTa4O11, CaTa2O6, Ca2Ta2O7 and Ca4Ta2O9. Isothermal section of the phase diagram is composed using the results. Thermodynamic properties of the ternary oxides are measured in the temperature range from 975 to 1275 K employing solid-state galvanic cells incorporating single crystal CaF2 as the solid electrolyte. The cells essentially measure the chemical potentials of CaO in two-phase fields (Ta2O5 + CaTa4O11), (CaTa4O11 + CaTa2O6), (CaTa2O6 + Ca2Ta2O7), and (Ca2Ta2O7 + Ca4Ta2O9) of the pseudo-binary system CaO-Ta2O5. The standard Gibbs energies of formation of the four ternary oxides from their component binary oxides Ta2O5 and CaO are given by: Delta G(f)((ox))(o) (CaTa4O11) (+/- 482)/J mol(-1) = -58644+21.497 (T/K) Delta G(f)((ox))(o) (CaTa2O6) (+/- 618)/J mol(-1) = -55122+21.893 (T/K) Delta G(f)((ox))(o) (Ca2Ta2O7) (+/- 729)/J mol(-1) = -82562+31.843 (T/K) Delta G(f)((ox))(o) (Ca4Ta2O9) (+/- 955)/J mol(-1) = -126598+48.859 (T/K) The Gibbs energy of formation of the four ternary compounds obtained in this study differs significantly from that reported in the literature. The thermodynamic data and phase diagram are used for understanding the mechanism and kinetics of calciothermic and electrochemical reduction of Ta2O5 to metal. (C) 2014 Elsevier B.V. All rights reserved.

Epidemiologia das infecções causadas por Staphylococcus aureus resistente a meticilina com perfil comunitário (CA-MRSA) em pacientes atendidos em um hospital terciário no Rio de Janeiro

O Staphylococcus aureus resistente a meticilina (MRSA) foi inicialmente descrito como um patógeno associado a infecções relacionadas à assistência em saúde; porém, um clone de MRSA, o CA-MRSA emergiu na comunidade e está atualmente incrementando nos hospitais. O objetivo desta tese foi descrever aspectos relacionados com a epidemiologia das infecções por cepas CA-MRSA no Hospital Universitário Pedro Ernesto da Universidade do Estado do Rio de Janeiro (HUPE/UERJ), avaliando especificamente fatores de risco relacionado com as infecções por CA-MRSA. Usando informações das bases de dados do laboratório de microbiologia, da farmácia e da Comissão para Controle da Infecção Hospitalar do HUPE/UERJ foi realizado um estudo retrospectivo de infecções/colonizações por cepas de S. aureus (fevereiro 2005 a Julho 2011). Foi realizado um estudo caso e controle, utilizando como casos os pacientes com infecções por cepas CA-MRSA. Na avaliação da susceptibilidade aos antimicrobianos usados em infecções graves por MRSA (vancomicina, teicoplanina, daptomicina e linezolida), foram determinadas as concentrações inibitórias mínimas (CIM) das amostras por diferentes metodologias (testes de difusão em agar, microdiluição em caldo e E-test). Nas analises das tendências temporais da apresentação dos subtipos de MRSA, usando um critério fenotípico para classificação das cepas MRSA, foi observada uma diminuição do número de cepas de MRSA multirresistente (HA-MRSA) (p<0.05). Também foi observada uma tendência ao aumento de cepas não-multirresistentes (CA-MRSA), mas sem alcançar a significância estatística (p = 0.06) igual que os S. aureus sensíveis a meticilina (MSSA) (p = 0.48). Não houve associação entre o subtipo de MRSA e a mortalidade devida à infecção por cepas MRSA. Uma idade acima de 70 anos (OR: 2.46, IC95%: 0.99 - 6.11), a presença de pneumonia adquirida no hospital (OR: 4.94, IC95%: 1.65 -14.8), a doença pulmonar obstrutiva crônica (OR: 6.09, IC95% 1.16 31.98) e a leucemia (OR: 8.2, IC95%: 1.25 54.7) foram fatores de risco associadas à mortalidade nas infecções por cepas de S. aureus. Usando curvas de Kaplan-Meier, foi observada uma tendência ao aumento da mortalidade em infecções causadas por MSSA na primeira semana, porém sem alcançar significância estatística (p = 0.07). Não foram observadas amostras MRSA com susceptibilidade intermediaria a vancomicina, linezolida, daptomicina ou teicoplanina. A dinâmica das infecções por S. aureus no HUPE/UERJ mudou durante o período de estudo, com menor número de episódios infecciosos causados por cepas de MRSA multirresistentes. Existe uma tendência ao aumento das cepas não-multirresistentes de MRSA entanto que a taxa de infecções por MSSA permaneceu estável no período do estudo. O perfil de resistência dos estafilococos não teve associação com a mortalidade

Computer simulation for effect of Pr(III) on Ca(II) speciation in human interstitial fluid

A multiphase model of metal ion speciation in human interstitial fluid was constructed and the effect of Pr(III) on Ca(II) speciation was studied. Results show that free Ca2+, [Ca(HCO3)], and [Ca(Lac)] are the main species of Ca(II). Because of the competition of Pr(III) for ligands with Ca(II), the percentages of free Ca2+, [Ca(Lac)], and [Ca(His)(Thr)H-3] increase gradually and the percentages of CaHPO4(aq) and [Ca(Cit)(His)H-2] decrease gradually with the increase in the total concentration of Pr(III). However, the percentages of [Ca(HCO3)] and CaCO3(aq) first increase and then begin to decrease when the total concentration of Pr(III) exceeds 6.070 x 10(-4) M.

层流恒界面池中CA-12萃取钇的质量传递动力学

用层流恒界面池研究了CA-12萃取钇的动力学。测定了搅拌速度、酸度、萃取剂浓度、温度对萃取速率的影响。测得CA-12萃取钇的活化能为48.96kJ/mol,此过程属于化学反应控制。当CA-12中加入少量的P507时,其活化能降至23.19kJ/mol。萃取过程由化学反应控制转变为扩散和化学反应混合控制。