951 resultados para hall plate
Resumo:
Recent studies in animals have shown pronounced resorption of the buccal bone plate after immediate implantation. The use of flapless surgical procedures prior to the installation of immediate implants, as well as the use of synthetic bone graft in the gaps represent viable alternatives to minimize buccal bone resorption and to favor osseointegration. The aim of this study was to evaluate the healing of the buccal bone plate following immediate implantation using the flapless approach, and to compare this process with sites in which a synthetic bone graft was or was not inserted into the gap between the implant and the buccal bone plate. Lower bicuspids from 8 dogs were bilaterally extracted without the use of flaps, and 4 implants were installed in the alveoli in each side of the mandible and were positioned 2.0 mm from the buccal bone plate (gap). Four groups were devised: 2.0-mm subcrestal implants (3.3 x 8 mm) using bone grafts (SCTG), 2.0-mm subcrestal implants without bone grafts (SCCG), equicrestal implants (3.3 x 10 mm) with bone grafts (EGG), and equicrestal implants without bone grafts (ECCG). One week following the surgical procedures, metallic prostheses were installed, and within 12 weeks the dogs were sacrificed. The blocks containing the individual implants were turned sideways, and radiographic imaging was obtained to analyze the remodeling of the buccal bone plate. In the analysis of the resulting distance between the implant shoulder and the bone crest, statistically significant differences were found in the SCTG when compared to the ECTG (P = .02) and ECCG (P = .03). For mean value comparison of the resulting linear distance between the implant surface and the buccal plate, no statistically significant difference was found among all groups (P > .05). The same result was observed in the parameter for presence or absence of tissue formation between the implant surface and buccal plate. Equicrestally placed implants, in this methodology, presented little or no loss of the buccal bone. The subcrestally positioned implants presented loss of buccal bone, even though synthetic bone graft was used. The buccal bone, however, was always coronal to the implant shoulder.
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The photoluminescence from individual quantum wells of artificially disordered weakly coupled multi-layers embedded in wide AlGaAs parabolic wells was investigated in a strong magnetic field. We show that the response of the individual wells is very different from the average response of the multi-layers studied by transport measurements and that photoluminescence represents a local probe of the quantum Hall state formed in three-dimensional electron system. The observed magnetic field induced variations of the in-layer electron density demonstrate the formation of a new phase in the quasi-three-dimensional electron system. The sudden change in the local electron density found at the Landau filling factor nu = 1 by both the magneto-transport and the magneto-photoluminescence measurements was assigned to the quantum phase transition. Copyright (C) EPLA, 2012
Resumo:
Polarized photoluminescence from weakly coupled random multiple well quasi-three-dimensional electron system is studied in the regime of the integer quantum Hall effect. Two quantum Hall ferromagnetic ground states assigned to the uncorrelated miniband quantum Hall state and to the spontaneous interwell phase coherent dimer quantum Hall state are observed. Photoluminescence associated with these states exhibits features caused by finite-size skyrmions: dramatic reduction of the electron spin polarization when the magnetic field is increased past the filling factor nu = 1. The effective skyrmion size is larger than in two-dimensional electron systems.
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Piezoresistive sensors are commonly made of a piezoresistive membrane attached to a flexible substrate, a plate. They have been widely studied and used in several applications. It has been found that the size, position and geometry of the piezoresistive membrane may affect the performance of the sensors. Based on this remark, in this work, a topology optimization methodology for the design of piezoresistive plate-based sensors, for which both the piezoresistive membrane and the flexible substrate disposition can be optimized, is evaluated. Perfect coupling conditions between the substrate and the membrane based on the `layerwise' theory for laminated plates, and a material model for the piezoresistive membrane based on the solid isotropic material with penalization model, are employed. The design goal is to obtain the configuration of material that maximizes the sensor sensitivity to external loading, as well as the stiffness of the sensor to particular loads, which depend on the case (application) studied. The proposed approach is evaluated by studying two distinct examples: the optimization of an atomic force microscope probe and a pressure sensor. The results suggest that the performance of the sensors can be improved by using the proposed approach.
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This paper is concerned with the energy decay for a class of plate equations with memory and lower order perturbation of p-Laplacian type, utt+?2u-?pu+?0tg(t-s)?u(s)ds-?ut+f(u)=0inOXR+, with simply supported boundary condition, where O is a bounded domain of RN, g?>?0 is a memory kernel that decays exponentially and f(u) is a nonlinear perturbation. This kind of problem without the memory term models elastoplastic flows.
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Polarized magnetophotoluminescence is employed to study the energies and occupancies of four lowest Landau levels in a couple quantum Hall GaAs/AlGaAs double quantum well. As a result, a magnetic field-induced redistribution of charge over the Landau levels manifesting to the continuous formation of the charge density wave and direct evidence for the symmetric-antisymmetric gap shrinkage at v = 3 are found. The observed interlayer charge exchange causes depolarization of the ferromagnetic ground state.
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We prove a uniqueness result related to the Germain–Lagrange dynamic plate differential equation. We consider the equation {∂2u∂t2+△2u=g⊗f,in ]0,+∞)×R2,u(0)=0,∂u∂t(0)=0, where uu stands for the transverse displacement, ff is a distribution compactly supported in space, and g∈Lloc1([0,+∞)) is a function of time such that g(0)≠0g(0)≠0 and there is a T0>0T0>0 such that g∈C1[0,T0[g∈C1[0,T0[. We prove that the knowledge of uu over an arbitrary open set of the plate for any interval of time ]0,T[]0,T[, 0
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Several Lamb wave modes can be coupled to a particular structure, depending on its geometry and transducer used to generate the guided waves. Each Lamb mode interacts in a particular form with different types of defects, like notches, delamination, surface defects, resulting in different information which can be used to improve damage detection and characterization. An image compounding technique that uses the information obtained from different propagation modes of Lamb waves for non-destructive testing of plate-like structures is proposed. A linear array consisting of 16 piezoelectric elements is attached to a 1 mm thickness aluminum plate, coupling the fundamental A0 and SO modes at the frequencies of 100 kHz and 360 kHz, respectively. For each mode two images are obtained from amplitude and phase information: one image using the Total Focusing Method (TFM) and one phase image obtained from the Sign Coherence Factor (SCF). Each TFM image is multiplied by the SCF image of the respective mode to improve contrast and reduce side and grating lobes effects. The high dispersive characteristic of the A0 mode is compensated for adequate defect detection. The information in the SCF images is used to select one of the TFM mode images, at each pixel, to obtain the compounded image. As a result, dead zone is reduced, resolution and contrast are improved, enhancing damage detection when compared to the use of only one mode. (C) 2013 Elsevier Ltd. All rights reserved. (AU)
Resumo:
Iberia Africa plate boundary, cross, roughly W-E, connecting the eastern Atlantic Ocean from Azores triple junction to the Continental margin of Morocco. Relative movement between the two plate change along the boundary, from transtensive near the Azores archipelago, through trascurrent movement in the middle at the Gloria Fracture Zone, to transpressive in the Gulf of Cadiz area. This study presents the results of geophysical and geological analysis on the plate boundary area offshore Gibraltar. The main topic is to clarify the geodynamic evolution of this area from Oligocene to Quaternary. Recent studies have shown that the new plate boundary is represented by a 600 km long set of aligned, dextral trascurrent faults (the SWIM lineaments) connecting the Gloria fault to the Riff orogene. The western termination of these lineaments crosscuts the Gibraltar accretionary prism and seems to reach the Moroccan continental shelf. In the past two years newly acquired bathymetric data collected in the Moroccan offshore permit to enlighten the present position of the eastern portion of the plate boundary, previously thought to be a diffuse plate boundary. The plate boundary evolution, from the onset of compression in the Oligocene to the Late Pliocene activation of trascurrent structures, is not yet well constrained. The review of available seismics lines, gravity and bathymetric data, together with the analysis of new acquired bathymetric and high resolution seismic data offshore Morocco, allows to understand how the deformation acted at lithospheric scale under the compressive regime. Lithospheric folding in the area is suggested, and a new conceptual model is proposed for the propagation of the deformation acting in the brittle crust during this process. Our results show that lithospheric folding, both in oceanic and thinned continental crust, produced large wavelength synclines bounded by short wavelength, top thrust, anticlines. Two of these anticlines are located in the Gulf of Cadiz, and are represented by the Gorringe Ridge and Coral Patch seamounts. Lithospheric folding probably interacted with the Monchique – Madeira hotspot during the 72 Ma to Recent, NNE – SSW transit. Plume related volcanism is for the first time described on top of the Coral Patch seamount, where nine volcanoes are found by means of bathymetric data. 40Ar-39Ar age of 31.4±1.98 Ma are measured from one rock sample of one of these volcanoes. Analysis on biogenic samples show how the Coral Patch act as a starved offshore seamount since the Chattian. We proposed that compression stress formed lithospheric scale structures playing as a reserved lane for the upwelling of mantle material during the hotspot transit. The interaction between lithospheric folding and the hotspot emplacement can be also responsible for the irregularly spacing, and anomalous alignments, of individual islands and seamounts belonging to the Monchique - Madeira hotspot.
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The Eifel volcanism is part of the Central European Volcanic Province (CEVP) and is located in the Rhenish Massif, close to the Rhine and Leine Grabens. The Quaternary Eifel volcanism appears to be related to a mantle plume activity. However, the causes of the Tertiary Hocheifel volcanism remain debated. We present geochronological, geochemical and isotope data to assess the geotectonic settings of the Tertiary Eifel volcanism. Based on 40Ar/39Ar dating, we were able to identify two periods in the Hocheifel activity: from 43.6 to 39.0 Ma and from 37.5 to 35.0 Ma. We also show that the pre-rifting volcanism in the northernmost Upper Rhine Graben (59 to 47 Ma) closely precede the Hocheifel volcanic activity. In addition, the volcanism propagates from south to north within the older phase of the Hocheifel activity. At the time of Hocheifel volcanism, the tectonic activity in the Hocheifel was controlled by stress field conditions identical to those of the Upper Rhine Graben. Therefore, magma generation in the Hocheifel appears to be caused by decompression due to Middle to Late Eocene extension. Our geochemical data indicate that the Hocheifel magmas were produced by partial melting of a garnet peridotite at 75-90 km depth. We also show that crustal contamination is minor although the magmas erupted through a relatively thick continental lithosphere. Sr, Nd and Pb isotopic compositions suggest that the source of the Hocheifel magmas is a mixing between depleted FOZO or HIMU-like material and enriched EM2-like material. The Tertiary Hocheifel and the Quaternary Eifel lavas appear to have a common enriched end-member. However, the other sources are likely to be distinct. In addition, the Hocheifel lavas share a depleted component with the other Tertiary CEVP lavas. Although the Tertiary Hocheifel and the Quaternary Eifel lavas appear to originate from different sources, the potential involvement of a FOZO-like component would indicate the contribution of deep mantle material. Thus, on the basis of the geochemical and isotope data, we cannot rule out the involvement of plume-type material in the Hocheifel magmas. The Ko’olau Scientific Drilling Project (KSDP) has been initiated in order to evaluate the long-term evolution of Ko’olau volcano and obtain information about the Hawaiian mantle plume. High precision Pb triple spike data, as well as Sr and Nd isotope data on KSDP lavas and Honolulu Volcanics (HVS) reveal compositional source variations during Ko’olau growth. Pb isotopic compositions indicate that, at least, three Pb end-members are present in Ko’olau lavas. Changes in the contributions of each component are recorded in the Pb, Sr and Nd isotopes stratigraphy. The radiogenic component is present, at variable proportion, in all three stages of Ko’olau growth. It shows affinities with the least radiogenic “Kea-lo8” lavas present in Mauna Kea. The first unradiogenic component was present in the main-shield stage of Ko’olau growth but its contribution decreased with time. It has EM1 type characteristics and corresponds to the “Ko’olau” component of Hawaiian mantle plume. The second unradiogenic end-member, so far only sampled by Honololu lavas, has isotopic characteristics similar to those of a depleted mantle. However, they are different from those of the recent Pacific lithosphere (EPR MORB) indicating that the HVS are not derived from MORB-related source. We suggest, instead, that the HVS result from melting of a plume material. Thus the evolution of a single Hawaiian volcano records the geochemical and isotopic changes within the Hawaiian plume.
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Questa tesi parte da un evento “minore” della storia del XIX secolo per tendere, poi, ad alcuni obiettivi particolari. L’evento è costituito da uno strano funerale postumo, quello di Piero Maroncelli, carbonaro finito alla Spielberg, graziato, poi emigrato in Francia e in America, il cui corpo viene sepolto a New York nell’estate del 1846. Quarant’anni dopo, nel 1886, i resti di Maroncelli vengono esumati e – attraverso una “trafila” particolare, di cui è protagonista la Massoneria, da una sponda all’altra dell’Atlantico – solennemente trasferiti nella città natale di Forlì, dove vengono collocati nel pantheon del cimitero monumentale, inaugurato per l’occasione. Gli eventi celebrativi che si consumano a New York e a Forlì sono molto diversi fra loro, anche se avvengono quasi in contemporanea e sotto regie politiche ispirate dal medesimo radicalismo anticlericale. E’ chiaro che Maroncelli è un simbolo e un pretesto: simbolo di un’italianità transnazionale, composta di un “corpo” in transito, fuori dello spazio nazionale, ma appartenente alla patria (quella grande e quella piccola); pretesto per acquisire e rafforzare legami politici, mercè mobilitazioni di massa in un caso fondate sul festival, sulla festa en plein air, nell’altro sui rituali del cordoglio per i “martiri” dell’indipendenza. L’opportunità di comparare questi due contesti – l’Italia, colta nella sua periferia radicale e la New York della Tammany Hall -, non sulla base di ipotesi astratte, ma nella concretezza di un “caso di studio” reale e simultaneo, consente di riflettere sulla pervasività dell’ideologia democratica nella sua accezione ottocentesca, standardizzata dalla Massoneria, e, d’altro canto, sui riti del consenso, colti nelle rispettive tipicità locali. Un gioco di similitudini e di dissomiglianze, quindi. Circa gli obiettivi particolari – al di là della ricostruzione del “caso” Maroncelli -, ho cercato di sondare alcuni temi, proponendone una ricostruzione in primo luogo storiografica. Da un lato, il tema dell’esilio e del trapianto delle esperienze di vita e di relazione al di fuori del proprio contesto d’origine. Maroncelli utilizza, come strumento di identitario e di accreditamento, il fourierismo; la generazione appena successiva alla sua, grazie alla Giovine Italia, possiede già un codice interno, autoctono, cui fare riferimento; alla metà degli anni Cinquanta, ad esso si affiancherà, con successo crescente, la lettura “diplomatica” di ascendenza sabauda. Dall’altro, ho riflettuto sull’aspetto legato ai funerali politici, al cordoglio pubblico, al trasferimento postumo dei corpi. La letteratura disponibile, al riguardo, è assai ricca, e tale da consentire una precisa classificazione del “caso” Maroncelli all’interno di una tipologia della morte laica, ben delineata nell’Italia dell’Ottocento e del primo Novecento. E poi, ancora, ho preso in esame le dinamiche “festive” e di massa, approfondendo quelle legate al mondo dell’emigrazione italiana a Mew York, così distante nel 1886 dall’élite colta di quarant’anni prima, eppure così centrale per il controllo politico della città. Dinamiche alle quali fa da contrappunto, sul versante forlivese, la visione del mondo radicale e massonico locale, dominato dalla figura di Aurelio Saffi e dal suo tentativo di plasmare un’immagine morale e patriottica della città da lasciare ai posteri. Quasi un’ossessione, per il vecchio triumviro della Repubblica romana (morirà nel 1890), che interviene sulla toponomastica, sull’edilizia cemeteriale, sui pantheon civico, sui “ricordi” patriottici. Ho utilizzato fonti secondarie e di prima mano. Anche sulle prime, quantitativamente assai significative, mi sono misurata con un lavoro di composizione e di lettura comparata prima mai tentato. La giustapposizione di chiavi di lettura apparentemente distanti, ma giustificate dalla natura proteiforme e complicata del nostro “caso”, apre, a mio giudizio, interessanti prospettive di ricerca. Circa le fonti di prima mano, ho attinto ai fondi disponibili su Maroncelli presso la Biblioteca comunale di Forlì, alle raccolte del Grande Oriente d’Italia a Roma, a periodici italoamericani assai rari, sparsi in diverse biblioteche italiane, da Milano a Roma. Mi rendo conto che la quantità dei materiali reperiti, sovente molto eterogenei, avrebbero imposto una lettura delle fonti più accurata di quella che, in questa fase della ricerca, sono riuscita a condurre. E’ vero, però, che le suggestioni già recuperabili ad un’analisi mirata al contenuto principale – le feste, la propaganda, il cordoglio – consentono la tessitura di una narrazione non forzata, nella quale il ricordo della Repubblica romana viaggia da una sponda all’altra dell’Atlantica, insieme ai resti di Maroncelli; nella quale il rituale massonico funge da facilitatore e da “mediatore culturale”; nella quale, infine, il linguaggio patriottico e la koinè democratica trans-nazionale riescono incredibilmente a produrre o a incarnare identità. Per quanto tempo? La risposta, nel caso forlivese, è relativamente facile; in quello della “colonia” italiana di New York, presto alterata nella sua connotazione demografica dalla grande emigrazione transoceanica, le cose appaiono più complesse. E, tuttavia, nel 1911, cinquantesimo dell’Unità, qualcuno, nella grande metropoli americana, si sarebbe ricordato di Maroncelli, sia pure in un contesto e con finalità del tutto diverse rispetto al 1886: segno che qualcosa, sotto traccia, era sopravvissuto.
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In dieser Arbeit wurden dünne Schichten von Heusler-Verbindungen hergestellt und auf ihre Transporteigenschaften hin untersucht.rnDer Anomale Hall-Effekt (AHE) ist dabei von besonderem Interesse. Er ist ein seit langer Zeit bekannter, jedoch noch nicht vollständig verstandener Transport-Effekt. Die meisten Veröffentlichungen theoretischer Arbeiten konzentrieren sich auf den Einfluss eines bestimmten Beitrags zum AHE. Tatsächlich gemessene experimentelle Daten können jedoch oft nicht in Einklang mit idealisierten Annahmen gebracht werden. rnDie vorliegende Arbeit diskutiert die Ergebnisse, welche aus Messungen von Materialien mit niedrigem Restwiderstand erhalten wurden. rnrnAls prototypische Materialien wurden hier hyphenation Heusler-Verbindungen untersucht. Als Material mit einer komplexen Topologie der Fermi-Fläche zeichnet sich dort der Einfluss von Defekten und der Unordnung der Kristallstruktur deutlich ab.rnrnDurch Verwendung von Filmen mit unterschiedlichem Grad der Unordnung können verschiedene Streumechanismen unterschieden werden. Für Co$_{2}$FeSi$_{0.6}$Al$_{0.4}$ and Co$_{2}$FeGa$_{0.5}$Ge$_{0.5}$ zeigt sich ein positiver AHE bei einer Unordnung vom Typ B2 und bei einer induzierten temperaturabh"angigen Streuung, wo hingegen eine Typ DO$_{3}$-Unordnung zusammen mit anderen möglichen intrinsischen Beiträgen einen negativen Effekt hervorruft.rnrnDarüber hinaus wurden die magneto-optische Kerr-Effekte (MOKE) dieser Verbindungen untersucht. Hierfür wurden Beiträge erster Ordnung als Funktion der intrinsischen und extrinsischen Parameter qualitativ analysiert. Auf den Einfluss der kristallinen Ordnung auf Beiträge zweiter Ordnung des MOKE-Signals wird ebenfalls eingegangen.rnrnDes Weiteren wurden dünne Schichten der Heusler-Verbindung Co$_{2}$MnAl auf MgO- und Si-Subs-traten (beide (100)) mit Hochfrequenz-Mag-netron-Sputtern erzeugt. Die zusammensetzung sowie die magnetischen und Transport-Eigenschaften wurden hinsichtlich unterschiedlicher Abscheidebedingungen systematisch untersucht.rnrnInsbesondere zeigt der AHE-Widerstand ein außerordentliches temperaturunabhängiges Verhalten in einem Bereich moderater Magnetfeldstärken von 0 bis 0.6,T. Hierf"ur wurde der nicht-diagonale Transport bei Temperaturen bis zu 300,$^{circ}$C analysiert. Die Daten zeigen die Eignung des Materials für Hall-Sensoren auch oberhalb der Raumtemperatur.rnrnJüngst wurde der Spin Seebeck-Effekt (SSE) entdeckt. Der Effekt aus dem Bereich der Spin-Kaloritronik erzeugt eine Spin-Spannung'' aufgrund eines Temperaturgradienten in magnetischen Materialien. Hier werden vorläufige Messungen des SSE in Ni$_{80}$Fe$_{20}$ und in Heusler-Verbindungen präsentiert.rn
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Un ambito di largo interesse nel campo dell’elettronica, è quello delle misure di corrente a larga banda, in cui la richiesta per sistemi a basso costo è aumentata sensibilmente nel corso del tempo. La causa di questo interessamento è dovuto al più frequente utilizzo di sistemi switched power ad alta frequenza, che necessitano di sensori di correnti isolati e ad alte prestazioni. L’intero lavoro prende in considerazione un sensore di nuova generazione per le misure di corrente, capace di raggiungere prestazioni oltre lo stato dell’arte. L’elaborato presentato vede, quindi, come obiettivo la creazione di un setup stabile per effettuare misure sui chip prodotti. Partendo dallo studio di fattibilità, della componentistica necessaria e dei compromessi per mantenere i costi, si giunge ad una soluzione flessibile e adatta alle misurazioni richieste. L’elaborato partirà con una introduzione sugli effetti fisici e la descrizione del componente fondamentale, passando a test funzionali effettuati su setup provvisori atti a ottenere informazioni basilari per la prosecuzione del lavoro. Infine verranno concepite e realizzate due schede a circuiti stampati per rispondere alle esigenze di progetto.