Delineation of sulphide ore-zones by borehole radar tomography at Hellyer Mine, Australia

Velocity and absorption tomograms are the two most common forms of presentation of radar tomographic data. However, mining personnel, geophysicists included, are often unfamiliar with radar velocity and absorption. In this paper, general formulae are introduced, relating velocity and attenuation coefficient to conductivity and dielectric constant. The formulae are valid for lossy media as well as high-resistivity materials. The transformation of velocity and absorption to conductivity and dielectric constant is illustrated via application of the formulae to radar tomograms from the Hellyer zinc-lead-silver mine, Tasmania, Australia. The resulting conductivity and dielectric constant tomograms constructed at Hellyer demonstrated the potential of radar tomography to delineate sulphide ore zones. (C) 2001 Elsevier Science B.V. All rights reserved.

Resistively loaded helical antennas for ground-penetrating radar

Resistively loaded helical antennas, used in the normal mode and horizontally polarised, are modelled using the moment method above typical lossy ground. The distributed resistive loading was adjusted to maintain a two octave bandwidth. The centre frequency of 1 m dipoles was reduced from 250 MHz for the straight resistive wire to 50 MHz for a helix of pitch 2.5 cm and diameter 5 cm. The reduction in efficiency required to maintain the bandwidth for this helix was 12 dB. This agrees reasonably with the theory for small antennas in free space. The results were also verified by comparing measurements performed on a monopole resistively loaded helical antenna in a watertank with the numerical model used elsewhere.

An investigation of magnetic antennas for ground penetrating radar

For ground penetrating radar (GPR), smaller antennas would provide considerable practical advantages. Some of which are: portability; ease of use; and higher spatial sampling. A theoretical comparison of the fundamental limits of a small electric field antenna and a small magnetic field antenna shows that the minimum Q constraints are identical. Furthermore, it is shown that only the small magnetic loop antenna can be constructed to approach, arbitrarily closely, the fundamental minimum Q limit. This is achieved with the addition of a high permeability material which reduces energy stored in the magnetic fields. This is of special interest to some GPR applications. For example, applications requiring synthetic aperture data collection would benefit from the increased spatial sampling offered by electrically smaller antennas. Low frequency applications may also benefit, in terms of reduced antenna dimensions, by the use of electrically small antennas. Under these circumstances, a magnetic type antenna should be considered in preference to the typical electric field antenna. Numerical modeling data supports this assertion.

Sistema radar comercial

O Sistema Radar Comercial ?? uma ferramenta in??dita de intelig??ncia comercial, que permite a identifica????o de oportunidades comerciais no mercado externo, em n??vel de seis d??gitos do Sistema Harmonizado (SH6). As informa????es e an??lises oferecidas pelo Sistema cont??m elementos b??sicos para a formula????o de estrat??gias de promo????o comercial, tanto do governo como da iniciativa privada, para o direcionamento dos fluxos de investimentos voltados para a amplia????o das exporta????es brasileiras e para o balizamento dos interesses do Brasil em negocia????es internacionais. A partir de um c??digo SH, ou de uma palavra chave que identifique determinado produto, o usu??rio do Sistema pode acessar, via internet, uma gama de an??lises sobre o produto desejado, em diferentes mercados. Al??m disso, o sistema possibilita a sele????o dos ???produtos priorit??rios???, para o Brasil ou para cada Estado da Federa????o

Radar Based Collision detection developments on USV ROAZ II

This work presents the integration of obstacle detection and analysis capabilities in a coherent and advanced C&C framework allowing mixed-mode control in unmanned surface systems. The collision avoidance work has been successfully integrated in an operational autonomous surface vehicle and demonstrated in real operational conditions. We present the collision avoidance system, the ROAZ autonomous surface vehicle and the results obtained at sea tests. Limitations of current COTS radar systems are also discussed and further research directions are proposed towards the development and integration of advanced collision avoidance systems taking in account the different requirements in unmanned surface vehicles.

Gravidez após Colocação de Banda Gástrica para Tratamento da Obesidade Mórbida

Obesity is known to have a negative impact on pregnancy outcome, as it is associated with an increase in the incidence of gestational diabetes, hypertension, preeclampsia, neural tube defects, macrosomia, and late fetal death. Gastric banding is considered an appropriate intervention for morbid obesity when other weight-loss measures are unsuccessful, and this treatment has been shown to be effective in causing a sustainable weight loss. Some women will become pregnant after bariatric surgery, and the nutritional and metabolic challenges brought by gastric banding may have a profound impact on maternal health and pregnancy outcome. The authors report the case of a 27 year old pregnant woman, with a past medical history of gastric banding surgery for morbid obesity. At 18 weeks of gestation, the patient started complaining of severe nausea and vomiting, The situation deteriorated three weeks later when she rapidly developed severe desnutrition, dehydration and early signs of liver and renal failure. Migration of the gastric band was diagnosed, and laparoscopy conducted to remove it. In the day following surgery the patient complained of absent fetal movements, and an intrauterine demise was diagnosed on ultrasound. Pathological examination of the fetus and placenta failed to reveal the cause of death, but no growth restriction was documented, suggesting the occurrence of an acute event.

A Banda da Guarda Nacional Republicana e os seus fagotistas

Dissertação de Mestrado para obtenção do grau de Mestre em Artes Musiciais

Uso de imagens de radar para o cálculo da produção primária de plantas aquáticas nas várzeas da Amazônia

A área da planície de inundação da Amazônia é estimada em 300 000km² e sua produtividade primária em 1,17 x 10(14) g C yr-1. Deste total de área e produtividade, estimativas sugerem que 43% e 62%, respectivamente, são atribuídos às plantas aquáticas. Estas estimativas variam de acordo com o pulso de inundação. Por exemplo, durante o período de seca as plantas terrestres (herbáceas) geralmente ocupam áreas que apresentam plantas aquáticas na cheia. A área e a produtividade destes ecossistemas são informações essenciais para a compreensão da dinâmica biogeoquímica da Amazônia. Imagens de satélites (radar) combinadas com amostragem de campo foram utilizadas para estimar a biomassa e mapear a área de cobertura de plantas aquáticas emergentes para calcular a produção primária de plantas aquáticas na várzea do baixo Amazonas. A combinação de bandas C e L forneceu a melhor correlação (r=0,82) e um ponto de saturação de biomassa intermediário (620 gm-2) para estimar biomassa aérea. O método de segmentação e classificação por região foi utilizado para classificar combinações de bandas C e L para cada período de nível de água, e forneceu uma precisão de mapeamento maior que 95% para determinação espacial de áreas cobertas por plantas aquáticas. Combinando a distribuição espacial de plantas aquáticas, o modelo para estimativa de biomassa aérea e a porcentagem de biomassa submersa, estimou-se espacialmente uma produção primária líquida anual de 1.9x10(12) g C yr-1 (±28%) para as plantas aquáticas em uma área de 394km².

Discriminação de incrementos de desflorestamento na Amazônia com dados SAR R99B em banda L

O uso de dados de sensoriamento remoto óptico em projetos de monitoramento de extensas áreas de floresta tropical é limitado devido à intensa cobertura por nuvens. Os dados SAR (Synthetic Aperture Radar) podem ser uma alternativa interessante para detectar desflorestamento nas regiões de floresta tropical onde a cobertura por nuvens é permanente. Neste contexto, o objetivo deste trabalho é avaliar o potencial do dado SAR adquirido em banda L pelo sistema aerotransportado R99B da Força Aérea Brasileira (FAB) para discriminar incremento de desflorestamento na Amazônia. Para tanto, foram realizadas classificações MAXVER-ICM com dados SAR multipolarizados de uma área teste localizada na região Sudeste do Estado do Acre. As classificações realizadas com a combinação dos canais HH, HV e VV e com o par de polarizações HH+HV obtiveram boa concordância com o mapa produzido no projeto PRODES (k = 0,68, onde k é o índice Kappa), o qual foi adotado como dado de referência. Este resultado indica que o dado SAR multipolarizado em banda L possui bom potencial para discriminar incremento de desflorestamento na Amazônia.

Discriminação de fitofisionomias de floresta de várzea a partir do algoritmo Iterated Conditional Modes aplicado aos dados SAR/R99 (QUAD-POL/Banda L)

Utilizando-se dados do sensor aerotransportado SAR R99, adquiridos na banda L (1,28 GHz) em amplitude e com quatro polarizações (HH, VV, HV e VH), avaliou-se a distinção de fitofisionomias de floresta de várzea existentes nas Reservas de Desenvolvimento Sustentável Amanã e Mamirauá e áreas adjacentes, com a aplicação do algoritmo Iterated Conditional Modes (ICM) de classificação polarimétrica pontual/contextual. Os resultados mostraram que o uso das distribuições multivariadas em amplitude, conjuntamente com uma banda de textura, produziu classificações de qualidade superior àquelas obtidas com dados polarimétricos uni/bivariados. Esta abordagem permitiu a obtenção de um índice Kappa de 0,8963, discriminando as três classes vegetacionais de interesse, comprovando assim o potencial dos dados do SAR R99 e do algoritmo ICM no mapeamento de florestas de várzea da Amazônia.

Anàlisi genètica i molecular de les malalties Niemann-Pick tipus A/B i tipus C. Estratègies terapèutiques.

Aquest treball es basa en l’estudi de dues malalties lisosòmiques: la malaltia de Niemann-Pick A/B (NPAB) i la malaltia de Niemann-Pick tipus C (NPC). En relació a la malaltia de NPAB, s’ha realitzat l’expressió in vitro d’algunes de les mutacions de canvi d’aminoàcid trobades en pacients espanyols per tal de detectar les activitats enzimàtiques residuals. Totes les mutacions presenten una activitat molt baixa, gairebé nul•la, excepte la p.L225P i la R608del que tenen un 11% i 20% d’activitat respectivament. Els resultats obtinguts són coherents amb la severitat del fenotip que presenten els pacients. D’altra banda, s’ha caracteritzat un al•lel amb una mutació que afecta a una posició poc conservada d’un donador de splicing i que produeix la generació de trànscrits aberrants corresponents a trànscrits minoritaris de SMPD1, prèviament descrits, que no codifiquen per proteïna funcional. Respecte a malaltia de NPC, s’ha realitzat una anàlisi molecular de pacients espanyols prèviament estudiats identificant, en la majoria dels casos, la segona mutació responsable de la patologia. S’ha descrit per primer cop per aquesta malaltia una gran deleció que inclou el gen NPC1 i altres gens flanquejants i s’ha estudiat l’efecte que tenen les mutacions de splicing trobades a nivell de RNA. Per una d’aquestes mutacions, c.1554-1009G&A, s’ha assajat amb èxit una estratègia terapèutica basada en la utilització d’oligonuclèotids antisentit. D’altra banda, s’està desenvolupant un model cel•lular neuronal de la malaltia de Niemann-Pick tipus C, basat en la utilització de RNAs d’interferència, sobre el qual es podran assajar possibles estratègies terapèutiques en un futur.

Exploration of alpine orographic precipitation patterns with radar image processing and clustering techniques

A methodology of exploratory data analysis investigating the phenomenon of orographic precipitation enhancement is proposed. The precipitation observations obtained from three Swiss Doppler weather radars are analysed for the major precipitation event of August 2005 in the Alps. Image processing techniques are used to detect significant precipitation cells/pixels from radar images while filtering out spurious effects due to ground clutter. The contribution of topography to precipitation patterns is described by an extensive set of topographical descriptors computed from the digital elevation model at multiple spatial scales. Additionally, the motion vector field is derived from subsequent radar images and integrated into a set of topographic features to highlight the slopes exposed to main flows. Following the exploratory data analysis with a recent algorithm of spectral clustering, it is shown that orographic precipitation cells are generated under specific flow and topographic conditions. Repeatability of precipitation patterns in particular spatial locations is found to be linked to specific local terrain shapes, e.g. at the top of hills and on the upwind side of the mountains. This methodology and our empirical findings for the Alpine region provide a basis for building computational data-driven models of orographic enhancement and triggering of precipitation. Copyright (C) 2011 Royal Meteorological Society .

Inferring transport characteristics in a fractured rock aquifer by combining single-hole ground-penetrating radar reflection monitoring and tracer test data

Investigations of solute transport in fractured rock aquifers often rely on tracer test data acquired at a limited number of observation points. Such data do not, by themselves, allow detailed assessments of the spreading of the injected tracer plume. To better understand the transport behavior in a granitic aquifer, we combine tracer test data with single-hole ground-penetrating radar (GPR) reflection monitoring data. Five successful tracer tests were performed under various experimental conditions between two boreholes 6 m apart. For each experiment, saline tracer was injected into a previously identified packed-off transmissive fracture while repeatedly acquiring single-hole GPR reflection profiles together with electrical conductivity logs in the pumping borehole. By analyzing depth-migrated GPR difference images together with tracer breakthrough curves and associated simplified flow and transport modeling, we estimate (1) the number, the connectivity, and the geometry of fractures that contribute to tracer transport, (2) the velocity and the mass of tracer that was carried along each flow path, and (3) the effective transport parameters of the identified flow paths. We find a qualitative agreement when comparing the time evolution of GPR reflectivity strengths at strategic locations in the formation with those arising from simulated transport. The discrepancies are on the same order as those between observed and simulated breakthrough curves at the outflow locations. The rather subtle and repeatable GPR signals provide useful and complementary information to tracer test data acquired at the outflow locations and may help us to characterize transport phenomena in fractured rock aquifers.

A methodology for the classification of convective structures using meteorological radar: Application to heavy rainfall events on the Mediterranean coast of the Iberian Peninsula

During the period 1996-2000, forty-three heavy rainfall events have been detected in the Internal Basins of Catalonia (Northeastern of Spain). Most of these events caused floods and serious damage. This high number leads to the need for a methodology to classify them, on the basis of their surface rainfall distribution, their internal organization and their physical features. The aim of this paper is to show a methodology to analyze systematically the convective structures responsible of those heavy rainfall events on the basis of the information supplied by the meteorological radar. The proposed methodology is as follows. Firstly, the rainfall intensity and the surface rainfall pattern are analyzed on the basis of the raingauge data. Secondly, the convective structures at the lowest level are identified and characterized by using a 2-D algorithm, and the convective cells are identified by using a 3-D procedure that looks for the reflectivity cores in every radar volume. Thirdly, the convective cells (3-D) are associated with the 2-D structures (convective rainfall areas). This methodology has been applied to the 43 heavy rainfall events using the meteorological radar located near Barcelona and the SAIH automatic raingauge network.