235 resultados para APT:n faktorit
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Trata da explicação da teoria do APT, abarcando o estudo de suas fontes de referência, pressupostos, modelo matemático, testes empíricos e estudos de aplicação prática de suas medidas de risco. Ressalta os aportes da teoria ao estudo do risco de preços da Teoria Financeira, descrevendo os trabalhos que identificaram vantagens do APT em relação ao CAPM, relativas ao conteúdo econômico de sua equação de equilíbrio e compravaçãu empírica. Inclue um levantamento das críticas realizadas à teoria, destacando os argumentos de resposta fornecidos pelos defensores do APT. Também explica a: metccoloçias de estimativa e teste do modelo, ilustrando a forma em que são mensurados os fatores econórnicc, de risco de preços
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This article evaluates the long-term clinical performance of porcelain laminate veneers bonded to teeth prepared with the use of an additive mock-up and aesthetic pre-evaluative temporary (APT) technique over a 12-year period. Sixty-six patients were restored with 580 porcelain laminate veneers. The technique, used for diagnosis, esthetic design, tooth preparation, and provisional restoration fabrication, was based on the APT protocol. The influence of several factors on the durability of veneers was analyzed according to pre- and postoperative parameters. With utilization of the APT restoration, over 80% of tooth preparations were confined to the dental enamel. Over 12 years, 42 laminate veneers failed, but when the preparations were limited to the enamel, the failure rate resulting from debonding and microleakage decreased to 0%. Porcelain laminate veneers presented a successful clinical performance in terms of marginal adaptation, discoloration, gingival recession, secondary caries, postoperative sensitivity, and satisfaction with restoration shade at the end of 12 years. The APT technique facilitated diagnosis, communication, and preparation, providing predictability for the restorative treatment. Limiting the preparation depth to the enamel surface significantly increases the performance of porcelain laminate veneers. (Int J Periodontics Restorative Dent 2012;32:625-635.)
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To develop two new models of expedited partner therapy for the UK, and evaluate them for feasibility, acceptability and preliminary outcome estimates to inform the design of a randomised controlled trial (RCT).
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The control part of the execution of a constraint logic program can be conceptually shown as a search-tree, where nodes correspond to calis, and whose branches represent conjunctions and disjunctions. This tree represents the search space traversed by the program, and has also a direct relationship with the amount of work performed by the program. The nodes of the tree can be used to display information regarding the state and origin of instantiation of the variables involved in each cali. This depiction can also be used for the enumeration process. These are the features implemented in APT, a tool which runs constraint logic programs while depicting a (modified) search-tree, keeping at the same time information about the state of the variables at every moment in the execution. This information can be used to replay the execution at will, both forwards and backwards in time. These views can be abstracted when the size of the execution requires it. The search-tree view is used as a framework onto which constraint-level visualizations (such as those presented in the following chapter) can be attached.
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The choice value and the testing process against the vigilance parameter, characteristic of ART Neural Network, are merged. Only, a single unique test is required to determine if a committed category node can represent the current input or not. Advantages of APT over ART are: 1-Avoid testing every committed category node before deciding to train a committed category node or a new node must be committed, 2-The vigilance parameter is fixed during training, and 3-The choice value parameter is eliminated.
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So gut sich im nördlichen Harzvorland die Sandstein- Fazies des Hilssandsteins als morphologisch herausragende Schichtrippe kartieren ließ, so problematisch ist bis heute ihre genaue stratigraphische Position geblieben. Die von STROMBECK (1856, Tab.S.493) aufgestellten Schichtgruppen Hilssandstein und Minimuston verwendete noch STOLLEY (1937, S.1,54) in stratigraphischem Sinn, obgleich es sich um Fazieseinheiten handelt, deren Grenzen durchaus schräg zu den biostratigraphischen Zonen verlaufen können. Beispiele für die Richtigkeit dieses Prinzips lieferten die Beobachtungen am Flammenmergel des Hils und der Sackmulde (JORDAN & SCHMIDT 1968): Die Bildungszeit der Flammenmergel-Fazies beginnt nach neuer Zonengliederung (COLLIGNON 1965) nicht zugleich mit dem Ober-Alb, sindern erst im unteren Ober-Alb und reicht bis zum Cenoman, kann aber auch schon im Ober-Alb beendet sein. Ein ähnliches Verhalten wurde daher auch von der Quarzsandstein-Fazies des Hilssandsteins im Raum Salzgitter-Goslar vermutet. Seltene Vorkommen von Acanthohoplites milletianus D'ORB. in den Steinbrüchen von Ostlutter und in der Sandgrube bei Goslar waren für BODE & SCHROEDER (1912 - 1926) bei ihrer geologischen Kartenaufnahme der Beweis für Unter-Gault (= Unter-Alb) -Alter des Sandsteins. Bei der Auswertung der Bohrungen im Gebiet von Hornburg grenzte SEITZ (1943, S.355,398) die Quarzsandstein Fazies mit dem Gaultkonglomerat nach unten gegen tonige Apt-Serien ab und stellte die obere Faziesgrenze des Hilssandsteins gegen Minimuston nach einem Leymeriellen Fund etwa in die Mitte des oberen Unter-Albs. Weiter östlich durchgeführte mikropaläontologische Beobach- tungsn in der Unterkreide am Kleinen Fallstein (BACH 1965) bestätigten, daß hier die Quarzsandschüttung bereits im Unter-Alb beendet war. Im Westen des Untersuchungsgebietes soll die Quarzsandschüttung im Hils nach BRINKMANN (1937, S.15) im Ober-Apt, örtlich sogar im Ober-Hauterive (FRATSCHNER 1950, S.31) begonnen und nach einem Hoplites-Fund (BRINKMANN 1937, S.15) bis ins oberste Mittel-Alb angedauert haben. Den Hilssandstein der Sackmulde stell- tein JORDAN & SCHMIDT (1968, S.428) ins Unter-Alb, vermuteten aber dessen Sedimentationsbeginn im Ober-Apt. Im Untersuchungsgebiet dieser Arbeit wurde das Unter- Alb-Alter des Hilssandsteins von DEWIEL (1951, S.39) unter anderem in der Finkeikuhle (bei Salzgitter-Bad) angezweifeit: Seines Erachtens ist dort die gesamte, ungefähr 50 m mächtige, tonig-sandige Folge mit Sandsteinbänken in ihrem oberen Teil dem Ober-Apt zuzuordnen. Er unterstrich damit WEIGELTs (1923, S.44/45) Auffassung von einer zumindest partiellen Zugehörigkeit des Sandsteins zum hohen Neokom. Abgesehen von der guten Übereinstimmung in der Datierung der Hilssandstein-Region des Kleinen Fallsteins nach Makro- wie Mikrofauna, gaben die zum Teil widersprüchlichen Altersangaben für dieselbe Schichtregion in den anderen Gebieten Südniedersachsens Anlaß zur Skepsis. Das hiesige Institut machte es sich daher zur Aufgabe, die stratigraphische Stellung des Hilssandsteins zunächst im Hils (SEILER 1973) und im Raum Salzgitter-Goslar erneut zu untersuchen. Die hier bearbeiteten Aufschlüsse (Abb.l) (Bl. Ringelheim, Salzgitter, Lutter a.B., Goslar) liegen im wesentlichen im Ausstrich der Unterkreide an den Flanken der Innerste-Mulde (gelegentlich auch Ringelheimer Mulde genannt). Bekanntlich entstand diese asymmetrische, mit Kreide-Sedimenten gefüllte Mulde durch halokinetisch modifizierte junge (?subherzynische) tektonische Bewegungen (s. KÖLBEL 1944). An ihrer Westflanke und in der Harzrandzone westlich Goslar bildet der Hilssandstein eine Schichtrippe und überlagert transgressiv Trias- und Jura-Schichten. - An seiner Basis treten örtlich (z.B. SO Ortshausen, SW Neuwallmoden) geringmächtige Brauneisenstein-Phosphorit- Lagen auf, deren Zugehörigkeit zum Neokom- oder Gaultkonglomerat bisher nicht sicher war. An der östlichen Muldenflanke ist der Hilssandstein in Tagesaufschlüssen aus zwei Gebieten bekannt: a) im Kreuzungsbereich der rheinisch streichenden Ringel- heimer Störungszone (KÖLBEL 1944, S.82) mit dem eggisch bis steil-herzynisch streichenden Salzgitterer Sattel in der Umgebung von Gitter und Grube "Finkeikuhle", b) am Südende des Salzgitterer Sattels. - Hier, wie auch am Südteil der östlichen Sattelflanke bei Groß-Döhren und Weddingen (Aufschluß 5: "Morgenstern"), liegt der Hilssandstein samt Gaultkonglomerat transgressiv auf den erzführenden Serien der tieferen Unterkreide.
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Bogotá (Colombia) : Universidad de la Salle. Facultad de Ciencias Económicas y Sociales. Programa de Finanzas y Comercio Internacional
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Universidade Estadual de Campinas . Faculdade de Educação Física
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Universidade Estadual de Campinas . Faculdade de Educação Física
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Universidade Estadual de Campinas. Faculdade de Educação Física
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Universidade Estadual de Campinas . Faculdade de Educação Física
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Universidade Estadual de Campinas . Faculdade de Educação Física
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The analysis of interviews with open-ended questions is a common practice amongst researchers in the field of Management. The difficulty therein is to convert the linguistic data into categories or quantitative values for subsequent statistical treatment. Proposals made to this end generally entail counting lexical occurrences which, since they are founded on previously established meanings, fail to include semantic associations made by interviews. This article aims to present an analysis tool comprising a set of techniques apt to generate linguistic units that can be statistically described, compared, modeled and inferred: the Quantitative Propositional Analysis (QPA), Its main difference from other such methods lies in the choice of a proposition - and not the lexical unit - as analysis unit. We present the application of this method through a study about the international expansion of retail firms.
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The brief interaction of precipitation with a forest canopy can create a high spatial variability of both throughfall and solute deposition. We hypothesized that (i) the variability in natural forest systems is high but depends on system-inherent stability, (ii) the spatial variability of solute deposition shows seasonal dynamics depending on the increase in rainfall frequency, and (iii) spatial patterns persist only in the short-term. The study area in the north-western Brazilian state of Rondonia is subject to a climate with a distinct wet and dry season. We collected rain and throughfall on an event basis during the early wet season (n = 14) and peak of the wet season (n = 14) and analyzed the samples for pH and concentrations of NH4+, Na+, K+, Ca2+ Mg2+,, Cl-, NO3-, SO42- and DOC. The coefficient 3 4 cient of variation for throughfall based on both sampling intervals was 29%, which is at the lower end of values reported from other tropical forest sites, but which is higher than in most temperate forests. Coefficients of variation of solute deposition ranged from 29% to 52%. This heterogeneity of solute deposition is neither particularly high nor particularly tow compared with a range of tropical and temperate forest ecosystems. We observed an increase in solute deposition variability with the progressing wet season, which was explained by a negative correlation between heterogeneity of solute deposition and antecedent dry period. The temporal stability of throughfall. patterns was Low during the early wet season, but gained in stability as the wet season progressed. We suggest that rapid plant growth at the beginning of the rainy season is responsible for the lower stability, whereas less vegetative activity during the later rainy season might favor the higher persistence of ""hot"" and ""cold"" spots of throughfall. quantities. The relatively high stability of throughfall patterns during later stages of the wet season may influence processes at the forest floor and in the soil. Solute deposition patterns showed less clear trends but all patterns displayed a short-term stability only. The weak stability of those patterns is apt to impede the formation of solute deposition -induced biochemical microhabitats in the soil. (C) 2008 Elsevier B.V. All rights reserved.