Localization in underground tunnels

Positioning technologies are becoming ubiquitous and are being used more and more frequently for supporting a large variety of applica- tions. For outdoor applications, global navigation satellite systems (GNSSs), such as the global positioning system (GPS), are the most common and popular choice because of their wide coverage. GPS is also augmented with network-based systems that exploit existing wireless and mobile networks for providing positioning functions where GPS is not available or to save energy in battery-powered devices. Indoors, GNSSs are not a viable solution, but many applications require very accurate, fast, and exible positioning, tracking, and navigation functions. These and other requirements have stim- ulated research activities, in both industry and academia, where a variety of fundamental principles, techniques, and sensors are being integrated to provide positioning functions to many applications. The large majority of positioning technologies is for indoor environments, and most of the existing commercial products have been developed for use in of ce buildings, airports, shopping malls, factory plants, and similar spaces. There are, however, other spaces where positioning, tracking, and navigation systems play a central role in safety and in rescue operations, as well as in supporting speci c activities or for scienti c research activities in other elds. Among those spaces are underground tunnels, mines, and even underwater wells and caves. This chapter describes the research efforts over the past few years that have been put into the development of positioning systems for underground tun- nels, with particular emphasis in the case of the Large Hadron Collider (LHC) at CERN (the European Organization for Nuclear Research), where localiza- tion aims at enabling more automatic and unmanned radiation surveys. Examples of positioning and localization systems that have been devel- oped in the past few years for underground facilities are presented in the fol- lowing section, together with a brief characterization of those spaces’ special conditions and the requirements of some of the most common applications. Section 5.2 provides a short overview of some of the most representative research efforts that are currently being carried out by many research teams around the world. In addition, some of the fundamental principles and tech- niques are identi ed, such as the use of leaky coaxial cables, as used at the LHC. In Section 5.3, we introduce the speci c environment of the LHC and de ne the positioning requirements for the envisaged application. This is followed by a detailed description of our approach and the results that have been achieved so far. Some last comments and remarks are presented in a nal section.

A new empirical system for rock slope stability analysis in exploitation stage

An empirical system was developed to obtain a quality index for rock slopes in road infrastructures, named Slope Quality Index (SQI), and it was applied to a set of real slopes.The SQI is supported in nine factors affecting slope stability that contemplate the evaluation of different parameters. Consequently, each factor is classified by the degree of importance and influence by assigned weights. These weights were established through a statistical analysis of replies to a survey that was distributed to several experienced professionals in the field. The proposed SQI varies between1 and 5, corresponding to slopes in very good and very bad condition state, respectively. Besides the advantage linked to a quantitative and qualitative evaluation of slopes, theSQI also allows identifying the most critical factors on the slope stability, which is a fundamental issue for an efficient management of the slope network in the road infrastructure, namely in the planning of conservation and maintenance operations.

Efeito da dissipação térmica nas juntas de soldagem de componentes through hole

Dissertação de mestrado integrado em Engenharia de Materiais

Lactacidemia: métodos de dosagem do ácido lático

A critical study of three methods for the determination of lactic acid (EDWARDS, MENDEL & GOLDSCHEIDER, MILLER & MUNTZ) is presented and some modifications are proposed. It was shown t hat more accurate results could be obtained with Edward's technic when an Iena glass filter is connected with the absorption tube. Before the dropping of the permanganate solution it is necessary to pass a current of air through the reaction flask to avoid the oxidation of the non-lactic acid substances which interfere with the reaction. The absorption tube must be maintained at 18°C during the destillation and the titration of the bisulphite binding aldehyde at 4°C. When the sample contains more than 5 mg it is useful to work with greater quantities of the bisulphite. More permanganate is consumed when the lactic acid concentration is higher. The sensivity of the method permits the titration of 0.04 mg to 5 mg of lactic acid in the sample. The calculated error of the method gave 0.018 % and the normal values for blood determined in 20 human cases averaged 10.30 mg per 100 ml (Table VI). MENDEL and GOLDSCHEIDER'S method was modified in the following details: Somogyis deproteinization was performed instead metaphosphoric acid as in the original method; to avoid the evaporation of the acetic aldehyde during the heating time with sulfuric acid a special glass stopped tube is proposed (Fig. 2). The reaction with sulfuric acid and veratrol is performed in an ice bath. Blood proteins precipitants were tried and Somogyi's lattest tecnic showed better results (Table V). Colorimetric readings were done in the PULFRICH photometer using filter S 53 and a 10 mm cup. The method is accurate within an error of 0.23 % and samples of 5 to 70 microg. could be easily determined. Normal values for human blood averaged 10.78 mg per 100 ml. More accurate results were obtained with the technic of MILLER & MUNTZ. Slight modifications were introduced: deproteinization with copper sulfate and sodium tungstate; satured p-hydroxydiphenyl solution according to KOENEMANN which is stable for 5 months when stored in the ice-box. Using the PULFRICH step-photometer the error is 0.17% with samples varying from 0.1 to 10 microg. of lactic acid. The filter employed was S 57 with the 5 mm cup. The method was adapted to 0.1 ml of blood. Normal values for human blood gave an average of 10.58 mg per 100 ml.

Emprêgo do teste químico para o estudo da eliminação das gonadotropinas durante o ciclo menstrual

A chemical test previously described for the diagnosis of pregnancy was applied to the study of the excretion of gonadotropin in the urine during menstrual cycle. The chemical test is based on the selective adsorption by kaolim of the reducing substances biologically related to urinary gonadotropin. The active substance when acidified to pH 4.0 is adsorbed by the kolin and eluated with O.1N sodium hydroxide. The alkaline solution is treated by Somogyi's copper reagent and the excess not reduced is titrated by 0.005 N sodium thiosulfate. Gonadotropin is quantitatively addorbed by kaolin at pH 4.0 and eluated by alkaline solution as previously demonstrated by the A. (1). In the present paper the complete menstrual cycle was studied daily. It was observed that normally there are two distinct maxima of excretion. This study is based on 11 normal cycles (24-30 days) and 34 abnormal ones. Normal cycles showed a intramenstrual estrogens elimination from 200 to 260 mice units determinated by the Allen - Doisy full estrus smear test. The abnormal cycles belonging also to normal women showed much less estrogen excretion (14 to 25 mice units) Table II). In those cases with decreased estrogen excretion no fall in the curve after 14 th. day was observed. The A. suggest that the peaks of gonadotropin excretion is not related to the oculation but possibly due, the first one, to the follicle stimulating hormone and the second to the luteinizing hormone of hormone stimulating of the inerstitial tissue.

Avaluació de la tècnica de fitoextracció per a la reducció de concentracions de metalls pesants en sòls contaminats per la indústria minera

L’explotació minera, especialment la mineria metàl•lica, ha estat sempre associada ariscos de contaminació ambiental de sòls, aigües i vegetació, originats per l’activitatextractiva, les operacions de concentració dels minerals i pels emplaçaments de residusminers sense una gestió adequada. En molts casos els residus miners s’abocavendirectament a rius i rierols o s’acumulaven en piles pròximes a centres habitats iactivitats agrícoles. Concretament s’estudia els cas de les mines d’Osor. Donada la possible presència de quantitats elevades de metalls pesants en aquests sòlses decideix avaluar una tècnica de remediació de sòls lleugera com la fitoextracció. Lafitoextracció es basa en l’ús de plantes bioacumuladores que absorbeixen metalls delsòl. Aquesta tècnica permet una descontaminació del sòl no agressiva i de baix cost peròrequereix un tractament de llarga durada

Role of fibronectin in the adhesion of Acinetobacter baumannii to host cells.

Adhesion to host cells is an initial and important step in Acinetobacter baumannii pathogenesis. However, there is relatively little information on the mechanisms by which A. baumannii binds to and interacts with host cells. Adherence to extracellular matrix proteins, such as fibronectin, affords pathogens with a mechanism to invade epithelial cells. Here, we found that A. baumannii adheres more avidly to immobilized fibronectin than to control protein. Free fibronectin used as a competitor resulted in dose-dependent decreased binding of A. baumannii to fibronectin. Three outer membrane preparations (OMPs) were identified as fibronectin binding proteins (FBPs): OMPA, TonB-dependent copper receptor, and 34 kDa OMP. Moreover, we demonstrated that fibronectin inhibition and neutralization by specific antibody prevented significantly the adhesion of A. baumannii to human lung epithelial cells (A549 cells). Similarly, A. baumannii OMPA neutralization by specific antibody decreased significantly the adhesion of A. baumannii to A549 cells. These data indicate that FBPs are key adhesins that mediate binding of A. baumannii to human lung epithelial cells through interaction with fibronectin on the surface of these host cells.

La cascarilla cerámica y su uso innovador

The ceramic shell is a material mainly used for making foundry molds. This research demonstrates that ceramic shell can be used for making sculptures with exceptional definition in its finish. The research has identified a number of advantages of the material to meet the challenges of an artist during the making of a sculpture. The research has been developed in six stages: In the first stage data were collected from the chaff as the process material. This was the starting point for research. In the second stage, we have set the appropriate composition of the slurry, both in percentage and type of binder, and firing curve. To this end, we evaluated the application characteristics, thickness, drying, mechanical strength, the reduction coefficient and porosity. In the third stage it was observed that the husk is suitable for all types of materials acting as support. It was also found that the slurry can be used with various sculptural processes: modeling, molding using silicone or plaster mold, shuttering, with internal metal frame, and so on. In addition, we have established methods to repair and modify the husk by hand and power tools. In the fourth stage we have found ways to modify the surface of the husk with other minerals that affect the structure: introduction of filing of copper, bronze and iron in the slurry ceramics, different staining procedure in hot or cold, by enamel slip, and so on. In the fifth stage sculptures were made using the methods established in the previous stages, to verify this hypothesis. The sixth stage, which is annexed, contains a new method to process the ceramic shell as a mold in casting that emerged from the proven methods in the investigation.

SwissBioisostere: a database of molecular replacements for ligand design.

The SwissBioisostere database (http://www.swissbioisostere.ch) contains information on molecular replacements and their performance in biochemical assays. It is meant to provide researchers in drug discovery projects with ideas for bioisosteric modifications of their current lead molecule, as well as to give interested scientists access to the details on particular molecular replacements. As of August 2012, the database contains 21 293 355 datapoints corresponding to 5 586 462 unique replacements that have been measured in 35 039 assays against 1948 molecular targets representing 30 target classes. The accessible data were created through detection of matched molecular pairs and mining bioactivity data in the ChEMBL database. The SwissBioisostere database is hosted by the Swiss Institute of Bioinformatics and available via a web-based interface.

New palaeontological investigations in the Jurassic of western Thailand

The paleontological investigations of the Jurassic of Western Thailand, districts of Mae Sot (Tak-Mae Sot highway, Padaeng Tak and Ban Mae Kut Luang Zinc mines) and Umphang (Klo Tho), provide age constraints for the Late Indosinian orogeny, the Paleotethys closure and the timing of the marine Jurassic inundation of Sundaland. The basal conglomerate of the Jurassic is derived from the pelagic Triassic Mae Sariang substratum. Stratigraphy, microfacies and paleontology of the Jurassic marine strata focus especially on ammonites, bivalves, large benthic foraminifera and algae. Among ammonites, the Tethyan Catulloceras perisphinctoides Gemmellaro marks the Upper Toarcian (Aalensis Zone) along the Tak-Mae Sot highway and Riccardiceras longalvum (Vacek). Malladaites pertinax (Vacek), Abbasites sp. and Vacekia sp. indicate Middle Aalenian to lowermost Bajocian in the Padaeng Mine (SE of Mae Sot) and Klo-Tho (Umphang). Vacekia sp., Spinammatoceras schindewolfi Linares and Sandoval and Malladaites vaceki Linares and Sandoval indicate Middle Aalenian to lowermost Upper Aalenian at Ban Mae Kut Luang (NE of Mae Sot). Among foraminifers, the large benthic foraminifer Timidonella sarda Bassoullet, Chabrier and Fourcade in the Western Tethys is indicative for Aalenian-Bajocian times, as characterized in the section at the Tak-Padaeng Zinc mine and the Klo-Tho Formation near Umphang. The endemic foraminifer Gutnicella kaempferi characterizes the Pu Khloe Khi Formation near Umphang. Among bivalves, shallow marine, dominantly endemic fauna includes Parvamussium donaiense (Mansuy) and Bositra ornate (Quenstedt), from the Toarcian to the Early Bajocian. A consideration of the faunal affinity shows that the fauna is partly endemic with Northern Tethyan (Eurasian) affinity. Crown Copyright (C) 2010 Published by Elsevier B.V. on behalf of International Association for Gondwana Research. All rights reserved.

Novas Pragas Agrícolas na Ilha de São Nicolau - Cabo Verde - Tuta absoluta (Meyrick) (Lep - Gelechiidae) e Bactrocera invadens (Drew, Tsuruta & White) (Dipt - Tephritidae)

Em algumas das ilhas do Arquipélago de Cabo Verde entraram, nos últimos dois anos, espécies invasoras que constituem pragas de culturas agrícolas e que têm apresentado elevada repercussão económica. Entre elas contam-se a traça do tomateiro, Tuta absoluta (Meyrick) (Lepidoptera: Gelechidae) e Bactrocera invadens (Drew, Tsuruta & White) (Diptera: Tephritidae). Com o objectivo de avaliar a presença destas pragas na ilha de São Nicolau, foram instaladas armadilhas com atractivos em quatro zonas com bananeiras (Ribeira Prata, Fajã, Maiama e Campo de Preguiça) para a monitorização da mosca da fruta. Foram também instaladas ensaios em seis parcelas de tomateiro para a comparação de estratégias de protecção contra T. absoluta, armadilha com feromona sexual para captura em massa em conjunto com Bacillus thuringiensis e tratamento com deltametrina. Das quatro zonas monitorizadas, B. invadens só foi encontrada no Vale da Fajã. No que diz respeito a T. absoluta, fez-se a comparação entre a população presente em três estratos do tomateiro e não se encontraram diferenças significativas. As estratégias de protecção contra T. absoluta também não diferiram significativamente no que se refere ao número de minas nas folhas e frutos furados. Nesidiocoris tenuis foi identificado como inimigo natural de T. absoluta presente na ilha.

Trazas de metales en agua, sedimento y organismos bentónicos en bancos naturales de las Regiones Tacna y Moquegua

En septiembre del 2009 se evaluó el contenido de trazas de metales en los bancos naturales de Meca-Lozas (Tacna), Tancona y Punta Coles (Moquegua), en un ámbito donde la temperatura fue inferior al patrón estacional y en presencia de Aguas Costeras Frías en toda la columna de agua. Las trazas de cobre, plomo y cadmio contenidos en agua de los tres bancos naturales, no superaron los Estándares de Calidad Ambiental para Conservación del Ambiente Acuático (Grupo 4). Las trazas de cobre, plomo, cadmio y cinc para sedimentos, no superó al Probable Nivel de Efecto estipulado en la Tabla de Protección Costera de los EE UU, a excepción del cobre que superó el estándar en una estación (136,99 μg/g) de Meca-Las Lozas. Sólo las concentraciones traza de cobre en los tres bancos naturales y en los cuerpos eviscerados de caracol negro (Thaisella chocolata), lapa (Fissurella sp.), chanque (Concholepas concholepas) y choro (Aulacomya atra) superaron el límite máximo permisible internacional estipulado por la FAO, siendo la mayor concentración de 1782,27 μg/g en la especie Fissurella sp. muestreada en Meca-Lozas, por lo que se concluye que las especies que bioacumulan más trazas de cobre son Fissurella sp., Thaisella chocolata, Concholepas concholepas y Aulacomya atra.

Origin of a restraining bend in an evolving strike-slip system: The Cenozoic As Pontes basin (NW Spain)

The As Pontes basin (12 km2), NW Iberian Peninsula, is bounded by a double restraining bend of a dextral strike-slip fault, which is related to the western onshore end of the Pyrenean belt. Surface and subsurface data obtained from intensive coal exploration and mining in the basin since the 1960s together with additional structural and stratigraphic sequence analysis allowed us to determine the geometric relationships between tectonic structures and stratigraphic markers. The small size of the basin and the large amount of quality data make the As Pontes basin a unique natural laboratory for improving our understanding of the origin and evolution of restraining bends. The double restraining bend is the end stage of the structural evolution of a compressive underlapping stepover, where the basin was formed. During the first stage (stepover stage), which began ca. 30 Ma ago (latest Rupelian) and lasted 3.4 My, two small isolated basins bounded by thrusts and normal faults were formed. For 1.3 My, the strike-slip faults, which defined the stepover, grew towards each other until joining and forming the double restraining bend, which bounds one large As Pontes basin (transition stage). The history of the basin was controlled by the activity of the double restraining bend for a further 3.4 My (restraining bend stage) and ended in mid-Aquitanian times (ca. 22 Ma).

Rheotaxial growth of CuInSe2 thin films

CuInSe2 thin films were deposited onto glass and liquid¿indium¿coated glass substrates by coevaporation of copper, indium, and selenium. The morphology, composition, and crystalline properties have been studied in relation to the deposition process parameters. The deposition rate and the grain size are higher in films grown on liquid indium than on glass and depend on the indium film thickness. Films grown on indium do not show the same crystalline phases of films grown on glass, and in order to obtain films free of spurious phases the Cu fluxes must be increased.

Origin of a restraining bend in an evolving strike-slip system: The Cenozoic As Pontes basin (NW Spain)

The As Pontes basin (12 km2), NW Iberian Peninsula, is bounded by a double restraining bend of a dextral strike-slip fault, which is related to the western onshore end of the Pyrenean belt. Surface and subsurface data obtained from intensive coal exploration and mining in the basin since the 1960s together with additional structural and stratigraphic sequence analysis allowed us to determine the geometric relationships between tectonic structures and stratigraphic markers. The small size of the basin and the large amount of quality data make the As Pontes basin a unique natural laboratory for improving our understanding of the origin and evolution of restraining bends. The double restraining bend is the end stage of the structural evolution of a compressive underlapping stepover, where the basin was formed. During the first stage (stepover stage), which began ca. 30 Ma ago (latest Rupelian) and lasted 3.4 My, two small isolated basins bounded by thrusts and normal faults were formed. For 1.3 My, the strike-slip faults, which defined the stepover, grew towards each other until joining and forming the double restraining bend, which bounds one large As Pontes basin (transition stage). The history of the basin was controlled by the activity of the double restraining bend for a further 3.4 My (restraining bend stage) and ended in mid-Aquitanian times (ca. 22 Ma).