Student mathematical notebook of William Tudor, 1795

Notebook containing the handwritten mathematical exercises of William Tudor, kept in 1795 while he was an undergraduate at Harvard College. The volume contains rules, definitions, problems, drawings, and tables on geometry, trigonometry, surveying, calculating distances, sailing, and dialing. Some of the exercises are illustrated with hand-drawn diagrams. The Menusration of Heights and Distances section contains color drawings of buildings and trees, and some have been altered with notes in different hands and with humorous additions. For instance, a drawing of a tower was drawn into a figure titled “Egyptian Mummy.” Some of the images are identified: “A rude sketch of the Middlesex canal,” Genl Warren’s monument on Bunker Hill,” “Noddles Island,” “the fields of Elysium,” and the “Roxbury Canal.” The annotations and additional drawings are unattributed.

Drusen do disco óptico e tilted disc

Trabalho Final do Curso de Mestrado Integrado em Medicina, Faculdade de Medicina, Universidade de Lisboa, 2014

Queratocone : impacto psico-social da doença na vida do doente

Trabalho Final do Curso de Mestrado Integrado em Medicina, Faculdade de Medicina, Universidade de Lisboa, 2014

Baixa visual em crianças do ensino fundamental do município do Recife

Enquadramento: O acesso à saúde ocular em escolares dirige primariamente a prevenção de problemas visuais que dificultem o aprendizado, impossibilitando o desenvolvimento das atividades intelectuais e sociais. Os projetos de promoção da saúde oftalmológica são, para a grande maioria dos alunos, a primeira e rara oportunidade de avaliar a visão. Objetivos: Identificar os tipos de déficit visuais mais comuns nas crianças da região metropolitana do Recife; Identificar as queixas mais frequentes relacionadas a baixa de visão; Realizar campanha preventiva para identificação dos déficits, tendo como referência a Guarnição de Aeronáutica de Recife (GAR). Métodos: Estudo descritivo, transversal, intervencionista e quantitativo. A pesquisa ocorreu nos anos de 2013 e 2014, em uma população de 1500 crianças residentes na cidade de Recife, estado de Pernambuco, Brasil, com idades variando entre 7 e 9 anos, onde obtivemos uma amostra de 490 inscrições para participação no programa. Resultados: No primeiro período, atingimos 98,5% de objetividade, aumentando para 99,3% no segundo período. Os estudantes realizaram as consultas maioritariamente pela manhã (58,7%), em escola particular (81,6%) e na sua maioria (57,1%), eram do sexo feminino. A presença de queixas atingiu 78,6% e os sinais e sintomas mais referidos foram: cefaleia (20,8%), prurido ocular (17,6%) e dificuldade de enxergar o quadro (16,8%). Foram identificados e corrigidos 53 casos de erros de refração sendo o astigmatismo (4,74%), o mais diagnosticado, 7 casos de estrabismo e tratados 12 de conjuntivite. Conclusões: Em 2013, 15,1% e em 2014, 14,2% das crianças apresentaram baixa acuidade visual. Astigmatismo e miopia representam 10% dos problemas mais comuns seguidos de hipermetropia e conjuntivite. 84% do total de nossa amostra refere dificuldade de visualização no quadro negro, 68% manifestam cefaleias, 85% dor ocular, 75,5% vermelhidão ocular e 80,3% prurido ocular. Resumindo, os distúrbios visuais são comuns nas crianças, justificando programas de saúde preventiva nas unidades de saúde da FAB. Palavras-chave: Acuidade visual; Criança; Preventiva.

(Table 2) Estimated basement temperatures at DSDP Hole 69-504B

The achievement of deep penetration (562 m) of seafloor basalts at Hole 504B, near the Costa Rica Rift (1°13.63'N, 83°43.81'W), on DSDP Legs 69 and 70 presented a rare opportunity to examine the structure of young (6 m.y.) oceanic crust. In addition to the recovery of samples for laboratory studies, an extensive suite of downhole logs and experiments was carried out at this site, for two main purposes: (1) to allow reliable deductions about the nature of the entire section of penetrated crust, because recovery of samples was far from complete (-25%); (2) to probe the physical state of rock around the drilled hole on a scale of tens of meters to kilometers. Information on the latter large-scale phenomena at Hole 504B were provided mainly by the oblique seismic experiment, utilizing a bore-hole seismometer (Stephen 1983), and by the large-scale-electrical- resistivity experiment described below.

Chemical and mineral compositions of sediments from ODP Site 127-797

In order to reconstruct past variations in the aeolian dust (Kosa) contribution to the Japan Sea, and to establish a direct link between terrestrial and marine climatic records, we have applied statistical procedures to distinguish and quantify detrital subcomponents within the detrital fraction of the late Quaternary hemipelagic sediments in the Japan Sea. Q-mode factor analysis with varimax and oblique rotation of the factors followed by multiple-regression analysis between mineral composition and factor loadings was conducted using six ''detrital'' elements. Four detrital subcomponents were defined, which are attributed to Kosa derived from ''typical'' loess, Kosa from ''weathered'' loess, and fine and coarse arc-derived detritus, respectively, based on comparisons with the chemical and mineral compositions of probable source materials. Using these detrital subcomponents, the variation in Kosa fraction was reconstructed for the last 200 ky. The results reveal millennial-scale as well as glacial-interglacial scale variations in Kosa contribution. Especially, millennial-scale variability of Kosa contribution suggests the presence of high frequency variation in summer monsoon precipitation in the central to east Asia during the last 200 ky.

Clay mineralogy of ODP Site 131-808 sediments

Drill core recovered at Ocean Drilling Program Site 808 (Leg 131) proves that the wedge of trench sediment within the central region of the Nankai Trough comprises approximately 600 m of hemipelagic mud, sandy turbidites, and silty turbidites. The stratigraphic succession thickens and coarsens upward, with hemipelagic muds and volcanic-ash layers of the Shikoku Basin overlain by silty and sandy trench-wedge deposits. Past investigations of clay mineralogy and sand petrography within this region have led to the hypothesis that most of the detritus in the Nankai Trough was derived from the Izu-Honshu collision zone and transported southwestward via axial turbidity currents. Shipboard analyses of paleocurrent indicators, on the other hand, show that most of the ripple cross-laminae within silty turbidites of the outer marginal trench-wedge facies are inclined to the north and northwest; thus, many of the turbidity currents reflected off the seaward slope of the trench rather than moving straight down the trench axis. Shore-based analyses of detrital clay minerals demonstrate that the hemipelagic muds and matrix materials within sandy and silty turbidites are all enriched in illite; chlorite is the second-most abundant clay mineral, followed by smectite. In general, the relative mineral percentages change relatively little as a function of depth, and the hemipelagic clay-mineral population is virtually identical to the turbidite-matrix population. Comparisons between different size fractions (<2 µm and 2-6 µm) show modest amounts of mineral partitioning, with chlorite content increasing in the coarser fraction and smectite increasing in the finer fraction. Values of illite crystallinity index are consistent with conditions of advanced anchimetamorphism and epimetamorphism within the source region. Of the three mica polytypes detected, the 2M1 variety dominates over the 1M and 1Md polytypes; these data are consistent with values of illite crystallinity. Measurements of mica bo lattice spacing show that the detrital illite particles were eroded from a zone of intermediate-pressure metamorphism. Collectively, these data provide an excellent match with the lithologic and metamorphic character of the Izu-Honshu collision zone. Data from Leg 131, therefore, confirm the earlier interpretations of detrital provenance. The regional pattern of sediment dispersal is dominated by a combination of southwest-directed axial turbidity currents, radial expansion of the axial flows, oblique movement of suspended clouds onto and beyond the seaward slope of the Nankai Trough, and flow reflection back toward the trench axis.

Subcompact vehicle energy absorbing column evaluation and improvement. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

Vehicular crash test of a continuous concrete median barrier without a footing. Final report.

Federal Highway Administration, Washington, D.C.

Small car driver inflatable restraint system evaluation. Volume III: investigation of potential crash survivability of a current production subcompact vehicle equipped with an advanced driver restraint system. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

Small car driver inflatable restraint system evaluation. Volume IV - evolving a low mount passenger air cushion restraint system (ACRS) for the Vega subcompact vehicle. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

Final report of a 1990 Chevrolet Caprice into a 50% left offset barrier in support of CRASH3 damage algorithm reformulation. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

Results of a 30 degree angled barrier crash test on the Calspan RSV conducted in England.

National Highway Traffic Safety Administration, Washington, D.C.

RSV test monitoring and data publication - Renault R20TS-to-Calspan RSV 75 degree right side impact at Renault. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

RSV test monitoring and data publication - Renault R20TS-to-Calspan RSV 75 degree left side impact at Peugeot. Final report.

National Highway Traffic Safety Administration, Washington, D.C.