995 resultados para Marcus, Emma
Resumo:
After a rockfall event, a usual post event survey includes qualitative volume estimation, trajectory mapping and determination of departing zones. However, quantitative measurements are not usually made. Additional relevant quantitative information could be useful in determining the spatial occurrence of rockfall events and help us in quantifying their size. Seismic measurements could be suitable for detection purposes since they are non invasive methods and are relatively inexpensive. Moreover, seismic techniques could provide important information on rockfall size and location of impacts. On 14 February 2007 the Avalanche Group of the University of Barcelona obtained the seismic data generated by an artificially triggered rockfall event at the Montserrat massif (near Barcelona, Spain) carried out in order to purge a slope. Two 3 component seismic stations were deployed in the area about 200 m from the explosion point that triggered the rockfall. Seismic signals and video images were simultaneously obtained. The initial volume of the rockfall was estimated to be 75 m3 by laser scanner data analysis. After the explosion, dozens of boulders ranging from 10¿4 to 5 m3 in volume impacted on the ground at different locations. The blocks fell down onto a terrace, 120 m below the release zone. The impact generated a small continuous mass movement composed of a mixture of rocks, sand and dust that ran down the slope and impacted on the road 60 m below. Time, time-frequency evolution and particle motion analysis of the seismic records and seismic energy estimation were performed. The results are as follows: 1 ¿ A rockfall event generates seismic signals with specific characteristics in the time domain; 2 ¿ the seismic signals generated by the mass movement show a time-frequency evolution different from that of other seismogenic sources (e.g. earthquakes, explosions or a single rock impact). This feature could be used for detection purposes; 3 ¿ particle motion plot analysis shows that the procedure to locate the rock impact using two stations is feasible; 4 ¿ The feasibility and validity of seismic methods for the detection of rockfall events, their localization and size determination are comfirmed.
Resumo:
The paper analyses and compares infrasonic and seismic data from snow avalanches monitored at the Vallée de la Sionne test site in Switzerland from 2009 to 2010. Using a combination of seismic and infrasound sensors, it is possible not only to detect a snow avalanche but also to distinguish between the different flow regimes and to analyse duration, average speed (for sections of the avalanche path) and avalanche size. Different sensitiveness of the seismic and infrasound sensors to the avalanche regimes is shown. Furthermore, the high amplitudes observed in the infrasound signal for one avalanche were modelled assuming that the suspension layer of the avalanche acts as a moving turbulent sound source. Our results show reproducibility for similar avalanches on the same avalanche path.
Resumo:
The Powell Basin is a small oceanic basin located at the NE end of the Antarctic Peninsula developed during the Early Miocene and mostly surrounded by the continental crusts of the South Orkney Microcontinent, South Scotia Ridge and Antarctic Peninsula margins. Gravity data from the SCAN 97 cruise obtained with the R/V Hespérides and data from the Global Gravity Grid and Sea Floor Topography (GGSFT) database (Sandwell and Smith, 1997) are used to determine the 3D geometry of the crustal-mantle interface (CMI) by numerical inversion methods. Water layer contribution and sedimentary effects were eliminated from the Free Air anomaly to obtain the total anomaly. Sedimentary effects were obtained from the analysis of existing and new SCAN 97 multichannel seismic profiles (MCS). The regional anomaly was obtained after spectral and filtering processes. The smooth 3D geometry of the crustal mantle interface obtained after inversion of the regional anomaly shows an increase in the thickness of the crust towards the continental margins and a NW-SE oriented axis of symmetry coinciding with the position of an older oceanic spreading axis. This interface shows a moderate uplift towards the western part and depicts two main uplifts to the northern and eastern sectors.
Resumo:
BACKGROUND: Due to the distinct cultural and language differences that exist in Switzerland, there is little information on the dietary intake among the general Swiss population. Adequately assessing dietary intake is thus paramount if nutritional epidemiological studies are to be conducted. OBJECTIVE: To assess the reproducibility and validity of a food-frequency questionnaire (FFQ) developed for French-speaking Swiss adults. DESIGN: A total of 23 men and 17 women (43.1+/-2.0 years) filled out one FFQ and completed one 24-hour dietary recall at baseline and 1 month afterward. RESULTS: Crude Pearson's correlation coefficients between the first and the second FFQ ranged from 0.58 to 0.90, intraclass correlation coefficient (ICC) ranged between 0.53 and 0.92. Lin's concordance coefficients ranged between 0.55 and 0.87. Over 80% of participants were classified in the same or adjacent tertile using each FFQ. Macronutrient intakes estimated by both FFQs were significantly higher than those estimated from the 24-hour recall for protein and water, while no significant differences were found for energy, carbohydrate, fats (five groups), and alcohol. De-attenuated Pearson's correlation coefficients between the 24-hour recall and the first FFQ ranged between 0.31 and 0.49, while for the second FFQ the values ranged between 0.38 and 0.59. Over 40 and 95% of participants fell into the same or the adjacent energy and nutrient tertiles, respectively, using the FFQs and the 24-hour recall. CONCLUSIONS: This FFQ shows good reproducibility and can be used determining macronutrient intake in a French-speaking Swiss population in an epidemiological setting.
Resumo:
Mineralógicamente se distinguen tres grupos de arenales: costa de Poniente, costa de Levante e isla Grossa. Las playas de la costa de Poniente se caracterizan por la presencia constante de dolomita, hornblenda y por los minerales opacos. Costa de Levante es ms rica en especies mineralógicas que la costa de Poniente, dominando la dolomita, los piroxenos y la turmalina; y en la isla Grossa predominan los piroxenos, especialmente la enstatita. La proporción de carbonatos es muy elevada en todas las muestras, 20-50 %. Domina en las playas de la costa de Poniente la arena de grano grueso, y en las playas de Levante e isla de Poarena fina. Los cantos son abundantes en las playas de Poniente y estn presentes en las de Levante. Cabo de Palos parece actuar de barrera, separando dos provincias petrogenticas.
Resumo:
O objetivo deste trabalho foi selecionar clones de seringueira (Hevea spp.) promissores para a região do planalto do Estado de São Paulo. De uma população de 70 clones, de polinização controlada, integrantes do experimento de avaliação em pequena escala, foram avaliados 16 da série IAC 300. O experimento foi instalado na Estação Experimental de Pindorama, no espaçamento de 7 x 3 m, em delineamento de blocos casualizados, com três repetições, tendo os clones RRIM 600 e GT 1 como testemunhas. Quanto à produção de borracha seca, destacaram-se oito e dez clones superiores ao RRIM 600 e GT 1, respectivamente. Todos os clones avaliados apresentaram-se vigorosos em relação ao perímetro do caule na abertura do painel. Sete deles mostraram alta resistência; sete, resistência moderada, e dois, suscetíveis à antracnose do painel. Sugere-se sua avaliação em experimentos de grande escala, para avaliar, além da produção, os demais caracteres secundários, em diferentes ambientes, para futuras recomendações em larga escala para o Estado de São Paulo.
Resumo:
Increasing anthropogenic pressures urge enhanced knowledge and understanding of the current state of marine biodiversity. This baseline information is pivotal to explore present trends, detect future modifications and propose adequate management actions for marine ecosystems. Coralligenous outcrops are a highly diverse and structurally complex deep-water habitat faced with major threats in the Mediterranean Sea. Despite its ecological, aesthetic and economic value, coralligenous biodiversity patterns are still poorly understood. There is currently no single sampling method that has been demonstrated to be sufficiently representative to ensure adequate community assessment and monitoring in this habitat. Therefore, we propose a rapid non-destructive protocol for biodiversity assessment and monitoring of coralligenous outcrops providing good estimates of its structure and species composition, based on photographic sampling and the determination of presence/absence of macrobenthic species. We used an extensive photographic survey, covering several spatial scales (100s of m to 100s of km) within the NW Mediterranean and including 2 different coralligenous assemblages: Paramuricea clavata (PCA) and Corallium rubrum assemblage (CRA). This approach allowed us to determine the minimal sampling area for each assemblage (5000 cm² for PCA and 2500 cm²for CRA). In addition, we conclude that 3 replicates provide an optimal sampling effort in order to maximize the species number and to assess the main biodiversity patterns of studied assemblages in variability studies requiring replicates. We contend that the proposed sampling approach provides a valuable tool for management and conservation planning, monitoring and research programs focused on coralligenous outcrops, potentially also applicable in other benthic ecosystems
Resumo:
The text of Lucifer Calaritanus' Moriundurn esse shows numerous quotations borrowed from other christian writers, specially Luctance, the anonymous De laude martyrii and Cyprian. The author adapts and orderly inserts those texts in his writing without indicating its source. Some passages borrowed from Cicero's Catil. IV 18 and 20 allow to increase the scarse number of secular quotations indicated in this writing and ut same time they prove that here Lucifer also follows the orderly method of quotation auulied to the christian writers.
Resumo:
Two reminiscences from the Cicero's speeches against Catiline in the letters of St Jerome and St Augustine.
Ciència catalana a Madrid: el discurs de Jesús M. Bellido Golferichs a la Biblioteca Nacional (1927)
Resumo:
We analyze Dr. Bellido"s discourse at the Spanish National Library in Madrid (1927) in the framework of what has been called Medical Catalanism. Further development of this case study will provide a better understanding of Catalan as a scientific language, the importance of the role played by Catalan publishing industry and the cultural and political relationship between Madrid and Barcelona.