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For the investigation of organic carbon fluxes reaching the seafloor, oxygen microprofiles were measured at 145 sites in different sub-regions of the Southern Ocean. At eleven sites, an in situ oxygen microprofiler was deployed for the measurement of oxygen profiles and the calculation of organic carbon fluxes. At four sites, both in situ and ex situ data were determined for high latitudes. Based on this dataset as well as on previous published data, a relationship was established for the estimation of fluxes derived by ex situ measured O2 profiles. The fluxes of labile organic matter range from 0.5 to 37.1 mgC m**2/day. The high values determined by in situ measurements were observed in the Polar Front region (water depth of more than 4290 m) and are comparable to organic matter fluxes observed for high-productivity, upwelling areas like off West Africa. The oxygen penetration depth, which reflects the long-term organic matter flux to the sediment, was correlated with assemblages of key diatom species. In the Scotia Sea (~3000 m water depth), oxygen penetration depths of less than 15 cm were observed, indicating high benthic organic carbon fluxes. In contrast, the oxic zone extends down to several decimeters in abyssal sediments of the Weddell Sea and the southeastern South Atlantic. The regional pattern of organic carbon fluxes derived from micro-sensor data suggest that episodic and seasonal sedimentation pulses are important for the carbon supply to the seafloor of the deep Southern Ocean.

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Surface samples, mostly from abyssal sediments of the South Atlantic, from parts of the equatorial Atlantic, and of the Antarctic Ocean, were investigated for clay content and clay mineral composition. Maps of relative clay mineral content were compiled, which improve previous maps by showing more details, especially at high latitudes. Large-scale relations regarding the origin and transport paths of detrital clay are revealed. High smectite concentrations are observed in abyssal regions, primarily derived from southernmost South America and from minor sources in Southwest Africa. Near submarine volcanoes of the Antarctic Ocean (South Sandwich, Bouvet Island) smectite contents exhibit distinct maxima, which is ascribed to the weathering of altered basalts and volcanic glasses. The illite distribution can be subdivided into five major zones including two maxima revealing both South African and Antarctic sources. A particularly high amount of Mg- and Fe-rich illites are observed close to East Antarctica. They are derived from biotite-bearing crystalline rocks and transported to the west by the East Antarctic Coastal Current. Chiorite and well-crystallized dioctaedral illite are typical minerals enriched within the Subantarctic and Polarfrontal-Zone but of minor importance off East Antarctica. Kaolinite dominates the clay mineral assemblage at low latitudes, where the continental source rocks (West Africa, Brazil) are mainly affected by intensive chemical weathering. Surprisingly, a slight increase of kaolinite is observed in the Enderby Basin and near the Filchner-Ronne Ice shelf. The investigated area can be subdivided into ten, large-scale clay facies zones with characteristic possible source regions and transport paths. Clay mineral assemblages of the largest part of the South Atlantic, especially of the western basins are dominated by chlorite and illite derived from the Antarctic Peninsula and southernmost South America and supported by advection within the Circumantarctic Deep Water flow. In contrast, the East Antarctic provinces are relatively small. Assemblages of the eastern basins north of 30°S are strongly influenced by African sources, controlled by weathering regimes on land and by a complex interaction of wind, river and deep ocean transport. The strong gradient in clay mineral composition at the Brazilian slope indicate a relatively low contribution of tropically derived assemblages to the western basins.

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Li-delta18O-SiO2 relationships have been examined for suites of spilitized basaltic rocks (DSDP 504B; Xigaze Ophiolite; Blanco Fracture Zone; Greater Caucasus; Rhenohercynian Fold Belt) and intra-plate evolved tholeiites (Northern Hessian Depression and Vogelsberg, W Germany; Mount Falla, Transantarctic Mountains). Relative to unaltered MORB and intra-plate primary olivine tholeiites, both the spilitic rocks and the evolved tholeiites are characterized by Li and 18O enrichment. For the spilitic rocks, Li and 18O enrichment is accompanied by a loss of SiO2 as a result of seawater hydrothermal alteration, whereas the evolved tholeiites have gained SiO2, Li and 18O from fractionation of mafic phases and assimilation of crustal rocks. On Li vs. SiO2 and delta18O vs. SiO2 diagrams, the two rock groups plot largely in distinct fields, suggesting the possibility of so distinguishing between such lithologies in the ancient rock record. Mafic granulite xenoliths from the Northern Hessian Depression have elevated Li and 18O abundances at low SiO2 contents. Even after correction for extraction of felsic components, their Li-delta18O-SiO2 signatures plot within the field of spilitic protoliths, suggesting that the lower crust in this region contains relics of spilitic rocks from a former oceanic crust.

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El componente satírico es una constante en el teatro de Federico García Lorca, en el que coexisten, en mayor o menor medida, dependiendo de la obra en cuestión, lo cómico y lo serio, ambas vertientes intrínsecas a la sátira. Dicha combinación, así como el innegable aspecto crítico, inherente a la obra lorquiana, identifican a este autor con la figura del satírico. García Lorca lleva a cabo su crítica sirviéndose del humor, que oscila entre lo puramente jocoso y el humor negro, y se manifiesta mediante el empleo de técnicas tradicionales de la sátira, con idéntico propósito al del satírico: degradar a su objeto de ataque suscitando sonrisa o repulsa. Este artículo analiza en clave de sátira Amor de don Perlimplín con Belisa en su jardín, identificando el objeto de ataque de la sátira lorquiana en esta obra y las técnicas satíricas empleadas por su autor.

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A novel processing method for the fast and economic production of hollow ceramic components has been developed by combining in situ coagulation moulding with a modified version of the technique of rotary moulding[Binner, J. G. P., Al-Dawery, I. A., Tari, G. and Yan, Y., Rotary casting technique. UK Patent application No. 0506349.0, March 2005], the latter being adapted from the polymer industry. The process was found to require a high solids content suspension, hence development work was performed in this direction though in the end a new, commercial suspension was utilised. Of the three forming routes of gel casting, direct coagulation casting and in situ coagulation moulding, the latter was found to be the most promising for the new process of rotary moulding of ceramics. Due to the low value of clay-based ceramics, a new low cost coagulant was identified and the effect of lactone concentration and temperature on setting time determined. Following substantial optimisation work, it was found that a two-speed approach to multi-axial rotation was the most successful; medium sized cream jugs could be produced in just 7 min. With respect to mould materials, the porous resin normally used for pressure casting of sanitary ware was found to be the best option, though since this is quite expensive conventional plaster-of-paris moulds were found to be a suitable material to enable companies, particularly SMEs, to become familiar with the technology whilst avoiding high costs for trials. The processed articles could be successfully fired and glazed using gas-fired kilns with no sign of any black cores. Major advantages of the process include the ability to precisely calculate the amount of ceramic slip required, eliminating either slip wastage or the need to pour used slip back into the virgin material as currently happens with slip casting. In addition, since the precursor suspension has a very high solids content, the time and energy required to dry the green product and associated moulds has been considerably reduced. © 2008 Elsevier Ltd. All rights reserved.

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O presente artigo apresenta uma pesquisa de campo sobre cultura organizacional e redes sociais que foi realizada junto a uma empresa prestadora de serviços. O objetivo foi verificar se existe a influência da cultura da organização nas características dos grupos sociais, com ênfase na centralidade. A literatura nacional e internacional evidencia que trabalhar com a centralidade significa identificar a posição em que o ator se encontra em relação às trocas e à comunicação na rede; a centralidade em uma rede traz a idéia de poder, isto é, quanto mais central é o indivíduo, mais bem posicionado ele está em relação às trocas e a comunicação. Trata-se de um estudo exploratório de natureza quantitativo; o levantamento feito através de dois questionários elaborados por Nelson(2006 e 2007), pesquisador da Illinois University. O primeiro relativo à cultura organizacional denominado Perfil de Valores Agregados (PVA), que identifica a presença e as prioridades atribuídas dentro de uma organização quanto aos temas: Trabalho “tarefa”, Relações “sociais”, Controle “poder“ e Cognição “Pensamento”. O segundo relativo às redes formadas cujo instrumento constituiu-se da apresentação de uma lista com todos os participantes da pesquisa e foi solicitado a cada membro que informasse sobre a natureza dos contatos adjacentes a cada nome. Os campos nome e cargo já foram entregues pré-preenchidos pelos pesquisadores, os campos aprovações e número de e-mails recebidos e enviados foram preenchidos por meio de estimativa do respondente e o campo dependência foi respondido respeitando-se uma escala de 1 a 6, onde 1 representava pouca e 6 muita dependência da outra pessoa. Utilizou-se uma amostra de 58 respondentes, todos funcionários próprios da empresa prestadora de serviços. Os dados foram tratados pela técnica estatística não-paramétrica Mann Whitney para os valores da cultura e para os dados das redes Sociais os índices foram apurados por meio do software Ucinet 6.0 de Borgatti, Everett, e Freeman (2002). Os resultados mostraram que os elementos centrais, ou seja, aqueles que têm o maior número de contatos na rede têm um maior alinhamento dos seus valores com os padrões da cultura organizacional e se concluiu que estes podem influenciar e participar na disseminação dos valores presentes na cultura organizacional. O que se pode perceber ao se analisar relação de nomes e funções dos colaboradores é que os quatro atores mais centrais da rede (centralidade) exercem funções gerenciais ou exercem algum tipo de liderança dentro da organização pesquisada; uma delas é Sub-gerente Operacional , duas outras são Supervisoras e a ultima é Assistente Operacional e trabalha diretamente com a Gerente Operacional. Os benefícios e a minimização de custos nas interações sociais caso a empresa utilize estes elementos centrais em programas de coaching ou mentoring, ou em outras ações de mudança, pode favorecer a retirada dos colaboradores da sua zona de conforto e ajudar a disseminar mais rapidamente a Missão, Visão e Valores Organizacionais.

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This paper presents an integer programming model for developing optimal shift schedules while allowing extensive flexibility in terms of alternate shift starting times, shift lengths, and break placement. The model combines the work of Moondra (1976) and Bechtold and Jacobs (1990) by implicitly matching meal breaks to implicitly represented shifts. Moreover, the new model extends the work of these authors to enable the scheduling of overtime and the scheduling of rest breaks. We compare the new model to Bechtold and Jacobs' model over a diverse set of 588 test problems. The new model generates optimal solutions more rapidly, solves problems with more shift alternatives, and does not generate schedules violating the operative restrictions on break timing.

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La berenjena (Solanum melongena L.) es una planta solanácea de múltiples variedades, cuyos ancestros salvajes se sitúan en Indochina y el este de África. Su cultivo fue muy temprano en zonas de China e India. Aun así, no se extendió al Occidente antiguo ni apenas se conoció, de ahí su ausencia en los textos clásicos de botánica y farmacología. Fueron los árabes quienes llevaron el cultivo de la planta por el Norte de África y Al-Andalus, de donde pasó ya a Europa. Los primeros testimonios occidentales de la berenjena aparecen en traducciones latinas de textos árabes, para incorporarse luego a la literatura farmacológica medieval y, más tarde ya, a la del Renacimiento, que empezó a tratar de ella por su posible parecido con una especie de mandrágora. Pese a que se le reconocían algunas virtudes medicinales, siempre se la tuvo bajo sospecha por ser de sabor poco agradable, indigesta y causante de algunas afecciones. Solo los botánicos de finales del Renacimiento describirían la planta y sus variedades con criterios más «científicos» y botánicos, ya sin apenas intereses farmacológicos.