New source-material for the socio-economic history of the Hindus of Goa

The Mhamai brothers were the suppliers of daily commodities / stationery to the viceroys / governors of Goa. Since late 18th century their agency house worked in partnership with several other trading houses all over the west coast of India. They also served as brokers for the French East India company in Goa during the critical period of anglo-french wars. The Mhamais were also revenue farmers, particularly customs and tobacco tax farming. I had the privilege of taking their family archives to the Xavier Centre of Historical Research in 1979 and making the history of the family known worldwide.

Avaliação de material educativo: adequação de quatro volantes sobre alimentação da criança de 0 a 12 meses de idade

Foi feita, através do Serviço de Educação de Saúde Pública da Secretaria de Estado da Saúde de São Paulo (Brasil), avaliação do tipo pré-teste de material instrucional - quatro volantes sobre alimentação da criança de 0 a 12 meses de idade, utilizados no programa de Assistência à Criança da referida Secretaria, com o objetivo de fornecer subsídios para reformulação deste material. O estudo foi realizado em 18 Centros de Saúde da Região Leste da Grande São Paulo, com uma amostra de 50 mães entrevistadas, clientes das Unidades Sanitárias e 48 funcionários. Investigou-se a compreensão das mães e dos funcionários em relação ao conteúdo do material instrucional e a percepção da viabilidade das práticas recomendadas nos volantes. Os resultados mostraram que em relação a 3 volantes a maioria das mensagens foi interpretada corretamente, sendo que para as mães a "boa compreensão" variou de 80,0% a 96,0% e para o pessoal auxiliar de 90,9% a 100,0%. Quanto à percepção da impossibilidade de se por em prática as orientações - avaliada através de interpretação de caráter projetivo - foi maior entre os funcionários (80,0% e mais) do que entre as mães (em torno de 50%). Identificaram-se algumas barreiras de comunicação e obtiveram-se sugestões que contribuiram para reformulação e melhoria dos materiais.

Educação em saúde para alunos de primeiro grau: avaliação de material para ensino e profilaxia da esquistossomose

Considerando a importância da informação sobre a esquistossomose para alunos de 7 a 15 anos, faixa etária apontada como de alta prevalência em regiões endêmicas e cujos hábitos colaboram para a disseminação da doença, foi elaborado um material de ensino baseado em um texto de conotação literária, o qual foi aplicado em escolas de região considerada foco isolado da doença no Município do Rio de Janeiro (Brasil). Desenvolveu-se uma metodologia de uso do material a ser empregada pelos professores, que resultou eficaz em promover aprendizagem de conceitos e cuidados básicos em relação à esquistossomose. Propõe-se o uso deste processo para outras doenças parasitárias a serem testadas em áreas caracteristicamente endêmicas.

Influência da longevidade da solução de Verhoeff na intensidade/especificidade das fibras elásticas, em material biológico de origem suína

As fibras elásticas são responsáveis pela elasticidade e flexibilidade dos tecidos. A técnica de Verhoeff é o método mais utilizado para demonstrar a presença destas fibras, corando-as de preto. A solução de Verhoeff é exclusivamente utilizada de um modo extemporâneo, no entanto, pela revisão da literatura verificou-se que a mesma poderia ter uma maior durabilidade. O presente estudo tem como principal objectivo determinar a longevidade da solução de Verhoeff. Utilizou-se material biológico de origem suína,fixado em formol neutro tamponado a 10% e incluído em parafina. Foi avaliado um total de 33 lâminas segundo critérios de intensidade e especificidade. Os resultados obtidos provam que o tempo tem influência sobre a referida solução, levando à perda de intensidade de coloração, não se tendo registado alterações significativas a nível de especificidade. Concluiu-se que a solução de Verhoeff pode não ser uma solução descartável, encontrando-se em perfeitas condições de utilização até às 48h de repouso.

Active and passive behaviors of soft tissues: Pelvic floor muscles

: A new active-contraction visco-elastic numerical model of the pelvic floor (skeletal) muscle is presented. Our model includes all elements that represent the muscle constitutive behavior, contraction and relaxation. In contrast with the previous models, the activation function can be null. The complete equations are shown and exactly linearized. Small verification and validation tests are performed and the pelvis is modeled using the data from the intra-abdominal pressure tests

Avaliação da exposição de crianças a material particulado em suspensão

Este trabalho teve como principal objectivo caracterizar a exposição de crianças a partículas atmosféricas e aos elementos químicos que as constituem. Pretendeu-se também determinar as fontes e processos que afectam os níveis e composição das partículas em suspensão no ar ambiente e no interior de salas de aula de escolas do 1º ciclo localizadas no centro de Lisboa. Os efeitos das partículas atmosféricas na saúde humana manifestam-se sobretudo ao nível do aparelho respiratório, dependendo da sua composição química, e principalmente da sua dimensão. As partículas inaláveis (PM10) podem depositar-se nas unidades funcionais do sistema respiratório. O PM2,5 podem atingir os alvéolos pulmonares e penetrar no sistema circulatório. As crianças são um dos principais grupos de risco, visto que os seus órgãos e tecidos ainda estão em desenvolvimento, ficando mais susceptíveis à exposição de partículas. A recolha de material particulado foi realizada no ar ambiente recorrendo a um colector PARTISOL e no interior e exterior das escolas usando amostradores GENT. A concentração total de partículas em suspensão foi determinada por gravimetria. A caracterização química da matéria particulada foi efectuada por Análise por Activação com Neutrões (INAA) para a determinação da concentração dos elementos e por Cromatografia Iónica para a quantificação de iões solúveis em água. Em 2007, a concentração média anual de PM2,5 no Centro de Lisboa foi de 18µg/m3. Através da Análise de Componentes Principais e Regressão Multilinear verificou-se que a massa das partículas da fracção fina resulta essencialmente da produção de aerossóis secundários (35%) de uma fonte de cálcio (28%) e da emissão de poluentes por veículos motorizados (23%). No interior das escolas verificou-se que as concentrações de partículas são mais elevadas comparativamente com o ambiente exterior, principalmente no PM2,5-10 (74µg/m3). A ressuspensão de partículas causada pelas actividades desempenhadas no interior das salas e a suspensão de poeiras do solo transportada pelas crianças, são as principais causas apontadas. O Ca é o elemento maioritário no interior das escolas. Os resultados obtidos neste trabalho não excederam os limites estabelecidos pela Legislação Portuguesa.

Evaluation and additional recommendations for preparing a whole blood control material

OBJECTIVE: The assessment of an easy to prepare and low cost control material for Hematology, available for manual and automated methods. MATERIAL AND METHOD: Aliquots of stabilized whole blood were prepared by partial fixation with aldehydes; the stability at different temperatures (4. 20 and 37 °C) during periods of up to 8-9 weeks and aliquot variability with both methods were controlled. RESULTS: Aliquot variability with automated methods at day 1, expressed as CV% (coefficient of variation) was: white blood cells (WBC) 2.7, red blood cells (RBC) 0.7, hemoglobin (Hb) 0.6, hematocrit (Hct) 0.7, mean cell volume (MCV) 0.3, mean cell hemoglobin (MCH) 0.6, mean cell hemoglobin concentration (MCHC) 0.7, and platelets (PLT) 4.6. The CV (coefficient of variation) percentages obtained with manual methods in one of the batches were: WBC 23, Hct 2.8, Hb 4.5, MCHC 5.9, PLT 41. Samples stored at 4ºC and 20ºC showed good stability, only a very low initial hemolysis being observed, whereas those stored at 37ºC deteriobed a rapidly (metahemoglobin formation, aggregation of WBC and platelets, as well as alteration of erythrocyte indexes). CONCLUSIONS: It was confirmed that, as long as there is no exposure to high temperatures during distribution, this material is stable, allowing assessment, both esternal and internal, for control purposes, with acceptable reproductivity, both for manual and auttomatic methods.

Preliminary results of a study of magnetic properties in the Foum-Zguid dyke (Morocco)

This work focuses on the study of flow and propagation of magma using rock magnetic analyses along sections across the thick Jurassic dyke of Foum-Zguid (Southern Morocco). Thermomagnetic data show that Ti-poor titanomagnetite is the main magnetic carrier. Petrographic analysis shows that the main Ti phase (ilmenite) occurs either as lamellae within spinel (center of the dyke) or as isolated grains (dyke margin). Bulk magnetic properties display distinct behavior according to the distance to the dyke margin; grain size of the main magnetic carrier decreases towards the center of the dyke, while the natural remanent magnetization and the bulk magnetic susceptibility increase. Only the magnetic susceptibility ellipsoid close to the dyke margin corresponds to that usually found in thin dykes, with the magnetic foliation sub parallel to dyke margins. Maximum principal axis is in most cases either parallel or perpendicular to the intersection between the planes of magnetic foliation and dyke wall. Moreover, when this axis is perpendicular to the intersection it is associated with a more oblate magnetic susceptibility ellipsoid shape, indicating the presence of complex magnetic fabrics. The studied magnetic properties show that, in this 100 m wide thick dyke, flow structures related with dyke propagation are only preserved close to the quickly cooled dyke margins.

Study of the Saldanha Massif (MAR, 36 degrees 34 ' N): Constrains from rock magnetic and geophysical data

We present a study of the magnetic properties of a group of basalt samples from the Saldanha Massif (Mid-Atlantic Ridge - MAR - 36degrees 33' 54" N, 33degrees 26' W), and we set out to interpret these properties in the tectono-magmatic framework of this sector of the MAR. Most samples have low magnetic anisotropy and magnetic minerals of single domain grain size, typical of rapid cooling. The thermomagnetic study mostly shows two different susceptibility peaks. The high temperature peak is related to mineralogical alteration due to heating. The low temperature peak shows a distinction between three different stages of low temperature oxidation: the presence of titanomagnetite, titanomagnetite and titanomaghemite, and exclusively of titanomaghemite. Based on established empirical relationships between Curie temperature and degree of oxidation, the latter is tentatively deduced for all samples. Finally, swath bathymetry and sidescan sonar data combined with dive observations show that the Saldanha Massif is located over an exposed section of upper mantle rocks interpreted to be the result of detachment tectonics. Basalt samples inside the detachment zone often have higher than expected oxidation rates; this effect can be explained by the higher permeability caused by the detachment fault activity.

Thick dyke emplacement and internal flow: A structural and magnetic fabric study of the deep-seated dolerite dyke of Foum Zguid (southern Morocco)

Knowledge on forced magma injection and magma flow in dykes is crucial for the understanding of how magmas migrate through the crust to the Earth's surface. Because many questions still persist, we used the long, thick, and deep-seated Foum Zguid dyke (Morocco) to investigate dyke emplacement and internal flow by means of magnetic methods, structural analysis, petrography, and scanning electron microscopy. We also investigated how the host rocks accommodated the intrusion. Regarding internal flow: 1. Important variations of the rock magnetic properties and magnetic fabric occur with distance from dyke wall; 2. anisotropy of anhysteretic remanent magnetization reveals that anisotropy of magnetic susceptibility (AMS) results mainly from the superposition of subfabrics with distinct coercivities and that the imbrication between magnetic foliation and dyke plane is more reliable to deduce flow than the orientation of the AMS maximum principal axis; and 3. a dominant upward flow near the margins can be inferred. The magnetic fabric closest to the dyke wall likely records magma flow best due to fast cooling, whereas in the core the magnetic properties have been affected by high-temperature exsolution and metasomatic effects due to slow cooling. Regarding dyke emplacement, this study shows that the thick forceful intrusion induced deformation by homogeneous flattening and/or folding of the host sedimentary strata. Dewatering related to heat, as recorded by thick quartz veins bordering the dyke in some localities, may have also helped accommodating dyke intrusion. The spatial arrangement of quartz veins and their geometrical relationship with the dyke indicate a preintrusive to synintrusive sinistral component of strike slip.

Variation of magnetic properties in sedimentary rocks hosting the Foum Zguid dyke (southern Morocco): Combined effects of re-crystallization and Fe-metasomatism

The effects of dyke intrusion on the magnetic properties of host sedimentary rocks are still poorly understood. Therefore, we have evaluated bulk magnetic parameters of standard palaeomagnetic samples collected along several sections across the sediments hosting the Foum Zguid dyke in southern Morocco. The study has been completed with the evaluation of the magnetic fabric after laboratory application of sequential heating experiments. The present study shows that: (1) close to Fourn Zguid dykes, the variations of the bulk magnetic parameters and of the magnetic fabric is strongly related with re-crystallization and Fe-metasomatism intensity. (2) The thermal experiments on AMS of samples collected farther from the dyke and, thus, less affected by heating during dyke emplacement, indicate that 300-400 degrees C is the minimum experimental temperature necessary to trigger appreciable transformations of the pre-existing magnetic fabrics. For temperatures higher than ca. 580 degrees C, the magnetic fabric transformations are fully realized, with complete transposition of the initial fabric to a fabric similar to that of samples collected close to the dyke. Therefore, measured variations of the magnetic fabric can be used to evaluate re-crystallization temperatures experienced by the host sedimentary rock during dyke emplacement. The distinct magnetic behaviour observed along the cross-sections strongly suggests that samples collected farther from the dyke margins did not experience thermal episodes with temperatures higher than 300 degrees C after dyke emplacement. (3) AMS data shows a gradual variation of the magnetic fabric with distance from the dyke margin, from sub-horizontal K-3 away from the dyke to vertical K3 close to the dyke. Experimental heating shows that heat alone can be responsible for this strong variation. Therefore, such orientation changes should not be unequivocally interpreted as the result of a stress field (resulting from the emplacement of the dyke, for instance). (4) Magnetic studies prove to be a very sensitive tool to assess rock magnetic transformations, thermally and chemically induced by dyke intrusion in hosting sediments.

Cr2O3 thin films grown at room temperature by low pressure laser chemical vapour deposition

Chromia (Cr2O3) has been extensively explored for the purpose of developing widespread industrial applications, owing to the convergence of a variety of mechanical, physical and chemical properties in one single oxide material. Various methods have been used for large area synthesis of Cr2O3 films. However, for selective area growth and growth on thermally sensitive materials, laser-assisted chemical vapour deposition (LCVD) can be applied advantageously. Here we report on the growth of single layers of pure Cr2O3 onto sapphire substrates at room temperature by low pressure photolytic LCVD, using UV laser radiation and Cr(CO)(6) as chromium precursor. The feasibility of the LCVD technique to access selective area deposition of chromia thin films is demonstrated. Best results were obtained for a laser fluence of 120 mJ cm(-2) and a partial pressure ratio of O-2 to Cr(CO)(6) of 1.0. Samples grown with these experimental parameters are polycrystalline and their microstructure is characterised by a high density of particles whose size follows a lognormal distribution. Deposition rates of 0.1 nm s(-1) and mean particle sizes of 1.85 mu m were measured for these films. (C) 2011 Elsevier B.V. All rights reserved.

Comparing a current-carrying circular wire with polygons of equal perimeter: Magnetic field versus magnetic flux

We compare the magnetic field at the centre and the self-magnetic flux through a current-carrying circular loop, with those obtained for current-carrying polygons with the same perimeter. As the magnetic field diverges at the position of the wires, we compare the self-fluxes utilizing several regularization procedures. The calculation is best performed utilizing the vector potential, thus highlighting its usefulness in practical applications. Our analysis answers some of the intuition challenges students face when they encounter a related simple textbook example. These results can be applied directly to the determination of mutual inductances in a variety of situations.