Death has a touch of class: society and space in Brookwood Cemetery, 1853-1903

Changes in the cultures and spaces of death during the Victorian era reveal the shifting conceptualisations and mobilisations of class in this period. Using the example of Brookwood Necropolis, established 1852 in response to the contemporary burial reform debate, the paper explores tensions within the sanitary reform movement, 1853–1903. Whilst reformist ideology grounded the cemetery's practices in a discourse of inclusion, one of the consequences of reform was to reinforce class distinctions. Combined with commercial imperatives and the modern impulse towards separation of living and dead, this aspect of reform enacted a counter-discourse of alienation. The presence of these conflicting strands in the spaces and practices of the Necropolis and their changes during the time period reflect wider urban trends.

Magnetotelluric deep soundings, gravity and geoid in the south Sao Francisco craton: Geophysical indicators of cratonic lithosphere rejuvenation and crustal underplating

In the south Sao Francisco craton a circular and 8-m amplitude geoid anomaly coincides with the outcropping terrain of an Archean-Paleoproterozoic basement. Broadband magnetotelluric (MT) data inversions of two radial profiles within the positive geoid and Bouguer gravity anomaly yield geo-electrical crustal sections, whereby the lower crust is locally more conductive (10 to 100 Omega m) in spatial coincidence with a denser lower crust modeled by the gravity data. This anomalous lower crust may have resulted from magmatic underplating, associated with Mesoarchean and Proterozoic episodes of tholeiitic dike intrusion. Long-period MT soundings reveal a low electrical resistivity mantle (20 to 200 Omega m) from depths beyond 120 km. Forward geoid modeling, using the scope of the low electrical resistivity region within the mantle as a constraint, entails a density increase (40 to 50 kg/m(3)) possibly due to Fe enrichment of mantle minerals. However, this factor alone does not explain the observed resistivity. A supplemented presence of small amounts of percolated carbonatite melting (similar to 0.005 vol.%), dissolved water and enhanced oxygen fugacity within the peridotitic mantle are viable agents that could explain the less resistive upper mantle. We propose that metasomatic processes confined in the sub-continental lithospheric mantle foster the conditions for a low degree melting with variable CO(2), H(2)O and Fe content. Even though the precise age of this metasomatism is unknown it might be older than the Early Cretaceous based on the evidence that a high-degree of melting in a lithospheric mantle impregnated with carbonatites originated the tholeiitic dike intrusions dispersed from the southeastern border of the Sao Francisco craton, during the onset of the lithosphere extension and break-up of the western Gondwana. The proxies are the NE Parana and Espinhaco (130 Ma, Ar/Ar ages) tholeiitic dikes, which contain (similar to 3%) carbonatites in their composition. The occurrence of a positive geoid anomaly (+ 10 m) and pre-tholeiites (age > 138 Ma), carbonatites and kimberlites along the west African continental margin (Angola and Namibia) reinforces the presumed age of the Sao Francisco-Congo craton rejuvenation to be prior to its fragmentation in the Lower Cretaceous. (C) 2010 Elsevier B.V. All rights reserved.

Evaluation of trace element levels in muscles, liver and gonad of fish species from Sao Francisco River of the Parana Brazilian state by using SR-TXRF technique

This study is focused on the analysis of an accumulation of inorganic elements in muscles, liver and gonad of seven fish species from Sao Francisco River located in the Parana state of Brazil. Concentrations of the elements were determined using the SR-TXRF technique. In the muscles of fish species, negative length dependent relationships were observed for chromium and zinc ion absorption. The obtained results showed that accumulated Cr ions values are above the limits defined in the Brazilian legislative norm on food. (C) 2010 Elsevier Ltd All rights reserved.

Tectonic fabric revealed by AARM of the proterozoic mafic dike swarm in the Salvador city (Bahia state): Sao Francisco Craton, NE Brazil

Magnetic fabric and rock magnetism studies were performed on 25 unmetamorphosed mafic dikes of the Meso-Late Proterozoic (similar to 1.02 Ga) dike swarm from Salvador (Bahia State, NE Brazil). This area lies in the north-eastern part of the Sao Francisco Craton, which was dominantly formed/reworked during the Transamazonian orogeny (2.14-1.94 Ga). The dikes crop out along the beaches and in quarries around Salvador city, and cut across both amphibolite dikes and granulites. Their widths range from a few centimeters up to 30 m with an average of similar to 4 m, and show two main trends N 140-190 and N 100-120 with vertical dips. Magnetic fabrics were determined using both anisotropy of low-field magnetic susceptibility (AMS) and anisotropy of anhysteretic remanent magnetization (AARM). The magnetic mineralogy was investigated by many experiments including remanent magnetization measurements at variable low temperatures (10-300 K), Mossbauer spectroscopy, high temperature magnetization curves (25-700 degrees C) and scanning electron microscopy (SEM). The rock magnetism study suggests pseudo-single-domain magnetite grains carrying the bulk magnetic susceptibility and AARM fabrics. The magnetite grains found in these dikes are large and we discard the presence of single-domain grains. Its composition is close to stoichiometric with low Ti substitution, and its Verwey transition occurs around 120 K. The main AMS fabric recognized in the swarm is so-called normal, in which the K(max)-K(int) plane is parallel to the dike plane and the magnetic foliation pole K(min)) is perpendicular to it. This fabric is interpreted as due to magma flow, and analysis of the K m inclination permitted to infer that approximately 80% of the dikes were fed by horizontal or sub-horizontal flows (K(max) < 30 degrees). This interpretation is supported by structural field evidence found in five dikes. In addition, based on the plunge of K(max), two mantle sources could be inferred; one of them which fed about 80% of the swarm would be located in the southern part of the region, and the other underlied the Valeria quarry. However, for all dikes the AARM tensors are not coaxial with AMS fabrics and show a magnetic lineation (AARM(max)) oriented to N30-60E, suggesting that magnetite grains were rotated clockwise from dike plane. The orientation of AARM lineation is similar to the orientation of a system of faults in which the Salvador normal fault is the most important. These faults were formed during Cretaceous rifting in the Reconcavo-Tucano-jatoba assemblage that corresponds to an aborted intra-continental rift formed during the opening of the South Atlantic. Therefore, the AARM fabric found for the Salvador dikes is probably tectonic in origin and suggests that the dike swarm was affected by the important tectonic event responsible for the break-up of the Gondwanaland. (C) 2008 Elsevier B.V. All rights reserved.

Neoproterozoic glacial dynamics revealed by provenance of diamictites of the Bebedouro Formation, Sao Francisco Craton, Central Eastern Brazil

One of the main questions on Neoproterozoic geology regards the extent and dynamics of the glacial systems that are recorded in all continents. We present evidence for short transport distances and localized sediment sources for the Bebedouro Formation, which records Neoproterozoic glaciomarine sedimentation in the central-eastern Sao Francisco Craton (SFC), Brazil. New data are presented on clast composition, based on point counting in thin section and SHRIMP dating of pebbles and detrital zircon. Cluster analysis of clast compositional data revealed a pronounced spatial variability of clast composition on diamictite indicating the presence of individual glaciers or ice streams feeding the basin. Detrital zircon ages reveal distinct populations of Archean and Palaeoproterozoic age. The youngest detrital zircon dated at 874 +/- 9 Ma constrains the maximum depositional age of these diamictites. We interpret the provenance of the glacial diamictites to be restricted to sources inside the SFC, suggesting deposition in an environment similar to ice streams from modern, high latitude glaciers.

Rhyacian (2.23-2.20 Ga) juvenile accretion in the southern Sao Francisco craton, Brazil: Geochemical and isotopic evidence from the Serrinha magmatic suite, Mineiro belt

The Serrinha magmatic suite (Mineiro belt) crops out in the southern edge of the Sao Francisco craton, comprising the Brito quartz-diorite, Brumado de Cima and Brumado de Baixo granodiorites, granophyres and felsic sub-volcanic and volcanic rocks, part of which intruded into the Nazareno greenstone belt. The suite rocks have petrographic features that are consistent with magma supercooling due to the low water content combined with volatile loss, leading to crystallization of quartz and alkaline feldspar at the rims of plagioclase phenocrysts (granophyric intergrowth). The investigated rocks are sub-alkaline, calc-alkaline and show low content in rare earth elements. The U-Pb zircon crystallization ages for the Brumado de Cima granodiorite [2227 +/- 22 (23) Ma] and a coeval granophyre [2211 +/- 22 (23) Ma], coupled with available single-zircon Pb evaporation ages for the Brito and Brumado de Baixo plutons, are significantly older than the ""Minas orogeny"" (ca. 2100-2050 Ga) of Quadrilatero Ferrifero area, eastward from the Serrinha suite. Our data establish an early Rhyacian event tectonically linked with the evolution of the Mineiro belt. The bulk Nd isotopic signature [low negative to positive epsilon(Nd(t)) values] of the Serrinha samples are consistent with the important role of Paleoproterozoic mantle components in the magma genesis. The integrated geologic, geochemical and isotopic information suggests that Paleoproterozoic evolution of the Mineiro belt initiated in a passive continental margin basin with deposition of the Minas Supergroup at ca. 2500 Ma. This stage was succeeded by outboard rupture of the oceanic lithosphere with development and coalescence of progressively younger magmatic arcs during Rhyacian time. One of the earliest arcs formed the Serrinha suite. The tectonic collage of the Serrinha and Ritapolis (2190-2120 Ma) arcs produced the NE-SW Lenheiro shear zone, resulting in mylonitization and recrystallization of both the granitoid intrusions and host rocks. As a matter of fact juxtaposition of distinct magmatic units in age and origin took place along the Lenheiros structure in this sector of the Mineiro belt. (C) 2009 Elsevier Ltd. All rights reserved.

Kolerahanteringen i Falun år 1834 & 1853 : En studie av sundhetsnämndens agerande

Syftet med uppsatsen är att undersöka vilka åtgärder som Falu stad, genom sundhetsnämnden, vidtog när farsoten kolera spreds i Sverige år 1834 respektive år 1853 samt om dessa åtgärder skiljer sig över tid. Frågeställningarna som används är: Vilka förebyggande åtgärder mot kolera vidtog staden genom sundhetsnämnden år 1834 och år 1853? Hur agerade läkarna i Falun mot kolerahotet? Skiljer sig Falu sundhetsnämnds åtgärder i jämförelse med andra städers sundhetsnämnder? Skiljer sig sundhetsnämndens åtgärder mellan åren 1834 och 1853? Materialet som används består av sundhetsnämndens mötesprotokoll från åren 1834 och år 1853, kolerakungörelser från de båda tidpunkterna, stadsläkare- och gruvläkarapporter samt utdrag från Tidning för Falu län och stad. Resultatet visar, att Falun vid båda tillfällena spärrades av genom att vaktstationer upprättades vid vägarna och vid stadens gräns. En karantänsstation upprättades vid stadens hälsobrunn för att ta om hand personer som inte vistats på kolerafri ort de 10 senaste dagarna. Staden delades in i tio distrikt som bemannades med en distriktschef samt några uppsyningsmän, som kontrollerade att staden hölls ren och att invånarna var rena. Stadens läkare var väldigt aktiva under sundhetsnämndens möten år 1834 och gav flera förslag på vad som behövdes göras medan de år 1853 intog en mer passiv roll. Åtgärderna i Stockholm år 1834 är snarlika de åtgärder som genomfördes i Falun samma år, huvudstaden delades också in i distrikt och det tillsattes även distriktschefer och uppsyningsmän. En annan likhet är att både Falun och Stockholm beställde färdiga likkistor för att ha i beredskap. Såväl sundhetsnämnderna i Karlskrona, Ystad och Arboga liksom Falun år 1853 vidtog i stort sett samma åtgärder som gjordes redan år 1834 t ex spärrningsåtgärder, karantänsskydd, införandet av kolerasjukhus och extra insatser för de mest utsatta i samhället.

En okänd svensk folkrörelse : Svenska Skolornas Fredsförenings fredsarbete 1922-1929

Den här undersökningen ämnar kartlägga Svenska Skolornas Fredsförenings (SSF) fredarbete under 1920-talet, en ansats som inte tidigare gjorts på detta sätt. Medlemmarna i denna före­ning arbetade outtröttligt för en fredligare värld, där fredsfostran av unga sågs som den bästa metoden för att få till stånd en internationell varaktig fred. Syftet med undersökningen är att, genom en kvalitativ innehållsanalys av delar av SSFs bevarade tryckta skrifter, beskriva SSFs principer och pedagogiska metoder samt utröna varför de ansåg fredsfostran riktad mot skolan som viktig. Resultaten visar att SSF hade ambitionen att genom internationellt samarbete på­verka barnen i en sådan riktning att de aldrig skulle kunna ta till vapen för att lösa konflikter. Istället skulle barn lära sig att tänka kritiskt, vara självständiga och få en förståelse för andra folks kulturer. Genom att respektera och leva efter kristna, jämlika och demokratiska ideal, menade SSF att krig skulle gå att förhindra.  

Recuperação com base em Checkpointing : uma abordagem orientada a objetos

Independentemente do modelo de programação adotado, no projeto e implementação de aplicações de alta disponibilidade, faz-se necessário usar procedimentos de tolerância a falhas. Dentre as atividades que trazem consigo interesse de pesquisa na área de Tolerância a Falhas, estão os mecanismos de recuperação em um sistema computacional. Do ponto de vista prático, estes mecanismos buscam manter próximo do mínimo o tempo total de execução de aplicações computacionais de longa duração, ao mesmo tempo em que as preparam para não sofrerem perdas significativas de desempenho, em caso de falhas. Paralelamente à evolução dos sistemas computacionais, foi possível observar também a evolução das linguagens de programação, principalmente as que utilizam o paradigma orientado a objetos. O advento da área de tolerância a falhas na orientação a objetos resultou em novos problemas na atividade de recuperação quanto aos mecanismos de salvamento de estados e retomada da execução, principalmente no que se refere às dificuldades de gerenciamento e controle sobre a alocação de objetos. Entretanto, observa-se que a complexidade de implementação dos mecanismos de recuperação, por parte dos programadores, exige deles conhecimentos mais especializados para o salvamento dos estados da aplicação e para a retomada da execução. Portanto, a simplificação do trabalho do programador, através do uso de uma biblioteca de checkpointing que implemente os mecanismos de salvamento de estados e recuperação é o ponto focal deste trabalho. Diante do contexto exposto, nesta dissertação, são definidas e implementadas as classes de uma biblioteca que provê mecanismos de checkpointing e recuperação. Esta biblioteca, denominada de Libcjp, visa aprimorar o processo de recuperação de aplicações orientadas a objetos escritas na linguagem de programação Java. Esta linguagem foi escolhida para implementação devido à presença dos recursos de persistência e serialização. Para a concepção do trabalho, são considerados ambos os cenários no paradigma orientado a objetos: objetos centralizados e distribuídos. São utilizados os recursos da API de serialização Java e a tecnologia Java RMI para objetos distribuídos. Conclui-se o trabalho com a ilustração de casos de uso através de diversos exemplos desenvolvidos a partir de seus algoritmos originais inicialmente, e incrementados posteriormente com os mecanismos de checkpointing e recuperação. Os componentes desenvolvidos foram testados quanto ao cumprimento dos seus requisitos funcionais. Adicionalmente, foi realizada uma análise preliminar sobre a influência das ações de checkpointing nas características de desempenho das aplicações.

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Nível de satisfação dos pais do ensino fundamental da sociedade caritativa e literária de São Francisco de Assis-ZN (SCALIFRA-ZN), no Estado do Rio Grande do Sul

A satisfação do cliente tem se colocado como prioridade de investigação para acadêmicos e praticantes de marketing nas últimas décadas. Isto se deve à difusão do conceito de marketing, e o consequente aumento do interesse pela retenção dos clientes. As escolas de ensino fundamental no Estado do Rio Grande do Sul passam pelo mesmo fenômeno, devido ao crescimento do número de concorrentes e da intensidade competitiva. Este trabalho, realizado no início de 2001, objetiva mensurar e analisar a satisfação dos clientes de quatro escolas de ensino fundamental da SCALIFRA-ZN no Estado do Rio Grande do Sul, indicando, como conclusão, pontos de melhoria a serem seguidos pelas mesmas.