(Table 3) Run conditions and phase relations and proportions during cooling rate experiments on ODP Interval 163-989B-10R-7,55-59

Equilibrium melting and controlled cooling experiments were undertaken to constrain the crystallization and cooling histories of tholeiitic basalts recovered by the Ocean Drilling Program drilling of Site 989 on the Southeast Greenland continental margin. Isothermal experiments conducted at 1 atm. and at the fayalite-magnetite-quartz buffer using lava sample Section 163-989B-10R-7 yielded the equilibrium appearance sequence with decreasing temperature: olivine at 1184 ± 2ºC; plagioclase at 1177ºC ± 5ºC; augite at 1167 ± 5ºC; and pigeonite at 1113 ± 12ºC. In controlled cooling experiments using the same starting composition and cooling rates between 10ºC/hr and 2000ºC/hr, we find a significant temperature delay in the crystallization of olivine, plagioclase, and augite (relative to the equilibrium appearance temperature); pigeonite does not form under any dynamic crystallization conditions. Olivine exhibits the largest suppression in appearance temperature (e.g., 30º for 10ºC/hr and >190º at 100ºC/hr), while plagioclase shows the smallest (~10ºC at 10ºC/hr; 30ºC at 100ºC/hr, and ~80ºC at 1000ºC/hr). These results are in marked contrast to those obtained on lunar basalts, which generally show a large suppression of plagioclase crystallization and modest suppression of olivine crystallization with an increased cooling rate. The results we report agree well with the petrography of lavas recovered from Site 989. Furthermore, the textural analysis of run products, representing a large range of cooling rates and quench temperatures (1150ºC to 1000ºC), provide a framework for evaluating cooling conditions necessary for glass formation, rates of plagioclase growth, and kinetic factors governing plagioclase growth morphology. Specifically, we use these insights to interpret the textural and mineralogical features of the unusual compound flow recovered at Site 989. We concluded from the analysis that this flow most likely records multiple breakouts from a distal tube at an abrupt break in slope, possibly a fault scarp, resulting in the formation of a lava fan delta. This interpretation implies that normal faulting of the oldest lava sequences (lower and, possibly, middle series) preceded eruption of Site 989 lavas.

Geochemistry, isotopic ratios and mineral composition of samples from ODP Leg 163 sites

Thirty-five samples from the drill core of the three Leg 163 sites (Sites 988, 989, and 990) off the southeast coast of Greenland were analyzed for 27 major, minor, and trace elements by X-ray fluorescence (XRF) and for 25 trace elements, including 14 rare-earth elements (REEs), by an inductively coupled plasma source mass spectrometer (ICP/MS). Sr- and Nd-isotope data are reported for seven samples and oxygen-isotope data are reported for 19 plagioclase separates. In addition, a reconnaissance survey of the composition of the main mineral phases, plagioclase, pyroxene, and oxides was determined on an electron microprobe to provide the basic information required for petrogenetic modeling. Olivine pseudomorphs are present in many of the samples, but in no case was an olivine grain found that was fresh enough to give a reliable analysis. The chemical and isotopic data recorded here were determined to provide a comparison with the larger data sets acquired by the Edinburgh, Copenhagen, and Leicester laboratories from both Legs 152 and 163 drill cores. This will permit a detailed comparison of the North Atlantic flood basalt province as a whole with the better known Columbia River, Deccan, and Karoo continental flood basalt provinces, for which substantial chemical data sets are already available at Washington State University.

Geochemistry and isotopic ratios of basalts from ODP Leg 163 sites

Voluminous, subaerial magmatism resulted in the formation of extensive seaward-dipping reflector sequences (SDRS) along the Paleogene Southeast Greenland rifted margin. Drilling during Leg 163 recovered basalts from the SDRS at 66ºN (Site 988) and 63ºN (Sites 989 and 990). The basalt from Site 988 is light rare-earth-element (REE) enriched (La(n)/Yb(n) = 3.4), with epsilon-Nd(t=60) = 5.3, 87Sr/86Sr = 0.7034, and 206Pb/204Pb = 17.98. It is similar to tholeiites recovered from the Irminger Basin during Leg 49 and to light-REE-enriched tholeiites from Iceland. Drilling at Site 989, the innermost of the sites on the 63ºN transect, was proposed to extend recovery of the earliest part of the SDRS initiated during Leg 152. These basalts are, however, younger than those from Site 917 and are compositionally similar to basalts from the more seaward Sites 990 and 915. Many of the basalts from Sites 989 and 990 show evidence of contamination by continental crust (e.g., epsilon-Nd(t=60) extends down to -3.7, 206Pb/204Pb extends down to 15.1). We suggest that the contaminant is a mixture of Archean granulite and amphibolite and that the most contaminated basalts have assimilated ~5% of crust. Uncontaminated basalts are isotopically similar to basalts from Site 918, on the main body of the SDRS, and are light-REE depleted. Consistent with previous models of the development of this margin, we show that at the time of formation of the basalts from Sites 989 and 990 (1) melting was at relatively shallow levels in a fully-fledged rift zone; (2) fragments of continental crust were present in the lithosphere above the zones of melt generation; and (3) the sublithospheric mantle was dominated by a depleted Icelandic plume component.

Oxygen potentials and phase equilibria in the system Ca-Co-O and thermodynamic properties of Ca3Co2O6 and Ca3Co4O9.163

Oxygen potentials established by the equilibrium between three condensed phases, CaOss+CoOss+ Ca3Co2O6 and CoOss+Ca3Co2O6+Ca3CO3.93+O-alpha(9.36-delta), are measured as a function of temperature using solid-state electrochemical cells incorporating yttria-stabilized zirconia as the electrolyte and pure oxygen as the reference electrode. Cation non-stoichiometry and oxygen non-stoichiometry in Ca3Co3.93+alpha O9.36-delta are determined using different techniques under defined conditions. Decomposition temperatures and thermodynamic properties of Ca3Co2O6 and Ca3Co4O9.163 are calculated from the results. The standard entropy and enthalpy of formation of Ca3Co2O6 at 298.15 K are evaluated. Using thermodynamic data from this study and auxiliary information from the literature, phase diagram for the ternary system Ca-Co-O is computed. Isothermal sections at representative temperatures are displayed to demonstrate the evolution of phase relations with temperature. (C) 2014 Elsevier Inc. All rights reserved.

Sapientia, 1987, Vol. XLII, nº 163 (número completo)

Contenido: Dios en la filosofía / Octavio N. Derisi -- Trascendencia y trascendentalidad / Octavio N. Derisi -- El hombre en el mundo desde una perspectiva aristotélica / Silvana Filippi -- El evolucionismo materialista y la doctrina hilemórfica / Jorge Martínez Barrera -- Notas y comentarios -- Bibliografía

Dados estatísticos : eleições federais, estaduais, realizadas no Brasil em 1962 e em confronto com anteriores. Referendum 6.163

Apresenta dados estatísticos e quadros sinópticos das eleiçõs federais e estaduais no Brasil em 1962.

Final Supplemental Environmental Document Pacific herring commercial fishing regulations (Sections 163, 163.1, and 164, Title 14, California Code of Regulations)

(PDF contains 63 pages.)

Quantitative data on the feeding of Cyclops strenuus Fischer and Cyclops viridis Jurine. [Translation from: Trudy saratov.Otd.vses.nauchno-issled.Inst.ozer.rech.ryb.Khoz. 1, 163-176, 1951.]

Cyclopids, exactly in the same way as daphnids, significant component in the nutrition of plankton-f and the young of the majority of fishes. It is established that the food spectrum of cyclopids is extremely broad: daphnids, planarians, Copepodite stages of copepods (cannibalism), rotifers, protists, bacteria, phytoplankton and so on. It is clear that the problem of studying these or other components of feeding in the general food spectrum can be definitely resolved only after obtaining exact quantitative data on the feeding of cyclopids. This article attempts to fill the gap in the study of the quantitative side of the feeding of cyclopias; in it is investigated the size of the 24-hour ration of cyclopids feeding on protists, the dependence of the ration on some factors of the external medium, and the difference of 24-hour consumption per unit weight of tody with two species of cyclopids (Cyclops strenuus and Cyclops viridis).

Some aspects of the ecology of the limnoplankton, with special reference to the phytoplankton. [Translation from: Svensk Botanisk Tidskrift 13(2) 129-163, 1919.]

This paper tries to develop more generally some fundamental bases for the ecological study of freshwater plankton. A special attention is given to the phytoplankton associations which can be separated out and made into groups according to their dependence upon changing environments. Plankton formations in different types of water bodies (ponds, lakes and rivers) are studied.

Tropical forest history of the Ecuadorian Andes over the last 34,000 years: preliminary results from pollen and oxygen isotope analyses of Trident 163-13 from the eastern equatorial Pacific [abstract]

EXTRACT (SEE PDF FOR FULL ABSTRACT): Pollen from the upper 2.75 m of a core taken 200 km west of the Golfo de Guayaquil, Ecuador (Trident 163-13, 3° S, 84° W, 3,000 m water depth) documents changes in Andean vegetation and climate of the Cordillera Occidental for ~17,000 years before and after the last glacial maximum.

Estudo ambiental do eixo viário da Amazônia (Rodovia BR-163): aptidão agrícola para soja e pecuária.

O trabalho divulga os resultados do estudo agroambiental realizado nos espaços amazônicos, no médio Tapajós, tendo como centro a rodovia BR-163, diagnosticada quanto à sua natureza e potencialidades. O GEIPOT solicitou ao Núcleo, um estudo sobre a aptidão agrícola das terras para a cultura de soja e pecuária, com a finalidade de elaborar um planejamento racional e eficiente do uso das terras, dando enfoque à demanda por transporte originada no setor agrícola, minimizando os impactos causados ao meio ambiente.

C 163 INST-D 2013. 344 Modelos de Trajes típicos del folclor colombiano (Boyacá, Santander y Pacífico)

17 fotografías, dieciséis en tono de grises.

Variáveis preditoras do desenvolvimento das dimensões das competências relacionais na preservação da intimidade do utente

Introdução: A compreensão do papel da intimidade no cuidar é uma questão essencial para o estabelecimento das competências relacionais no processo de cuidar o utente, visto que este se centra no desenvolvimento de relações interpessoais. Na formação dos estudantes de Enfermagem, visa-se o desenvolvimento de competências, assentes na compreensão da dimensão ética dos cuidados de forma a “promover o desenvolvimento ético, com respeito pela autonomia das pessoas, pressupõe prudência, reflexão crítica, consciência de cidadania e de responsabilidade” (Bettencourt, 2008: 61). Sendo assim, o modelo de formação em enfermagem deve assentar num processo reflexivo que proporcione aos estudantes a aquisição de posturas e condutas que lhe permitam a aquisição de competências profissionais. Objetivo: Compreender quais as variáveis que são preditoras do desenvolvimento das dimensões das competências relacionais na preservação da intimidade do utente. Metodologia: Estudo descritivo – correlacional de abordagem quantitativa. A população acessível, foram os estudantes da licenciatura em enfermagem de uma Escola Superior de Enfermagem integrada numa Universidade (A) e de uma Escola Superior de Saúde integrada num Instituto Politécnico (B). A amostra foi constituída por todos os estudantes de enfermagem das referidas escolas a partir do ano em que iniciam o primeiro ensino clínico. Os instrumentos de recolha de dados foram um questionário de caracterização dos estudantes e do contexto clínico e um Inventário de Competências Relacionais de Ajuda (ICRA). Os dados foram analisados com recurso ao Software IBM® SPSS® Statistic (Statistical Package for Social Sciences) de onde se fez uma análise dedutiva. Resultados: As variáveis independentes que melhor predizem a variável dependente (Competências relacionais) são a Escola seguida do ano e do acompanhamento em ensino clínico. Após a utilização dos métodos de seleção de preditores (seleção de Forward, seleção Backward e seleção Stepwise) as nossas variáveis independentes preditoras são o ano, a escola e o tipo de acompanhamento em EC, as restantes foram excluídas (sexo, idade, estado civil e habilitações literárias). Conclusões: As variáveis preditoras evidenciam a sua importância no desenvolvimento das competências relacionais dos estudantes de enfermagem, interferindo nos seus comportamentos enquanto estudantes e futuros enfermeiros. São variáveis que de uma ou de outra forma vão influenciar como é que cada estudante se vai comportar perante as situações de cuidado, onde se salientam nomeadamente o sexo e o ano do curso, variáveis que são intrínsecas a cada estudante, enquanto a Escola e o tipo de acompanhamento em EC são extrínsecas aos estudantes. Estas últimas são, portanto, as que consideramos que poderão ser alteradas em cada escola para que os estudantes adquiram e desenvolvam este domínio das competências de forma mais harmoniosa com o cuidar em enfermagem. Referencia Bibliográficas Almeida, M.J.F. (2004), A intimidade da «pessoa doente» em contexto hospitalar: valores e fundamentos éticos, Dissertação de mestrado, Porto: Faculdade de Medicina da Universidade do Porto. Acedido em 14/08/2012, disponível em: http://hdl.handle.net/10216/9667 Bettencourt, M. (2008), «Tomada de posição sobre a segurança do cliente», Revista da Ordem dos Enfermeiros, Nº 29, maio, Lisboa: Ordem dos enfermeiros, pp. 57-62. Melo, R.C.; Parreira, P.M. (2009), «Predictors of the development of relational skills: Study with students of nursing», in The 1st International Nursing Research Conference of World Academy of Nursing Science, Japão: Kobe International Exhibition Hall, pp. 90. Acedido em 17/08/2012, disponível em: http://wans.umin.ne.jp/confe/wans_1st.pdf