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Статті в журналах з теми "Caustic zone"
Leftheris, B. P., and J. M. Papazian. "Use of the Shadow Optical Method of Caustics to Predict Fatigue Crack Growth in Compression." Journal of Engineering Materials and Technology 114, no. 4 (October 1, 1992): 399–405. http://dx.doi.org/10.1115/1.2904191.
Повний текст джерелаVolyar, A. V., E. G. Abramochkin, Y. E. Akimova, and M. V. Bretsko. "Reconstruction of stable states of spiral vortex beams." Computer Optics 46, no. 1 (February 2022): 5–15. http://dx.doi.org/10.18287/2412-6179-co-1032.
Повний текст джерелаLock, James A. "Near-zone transmission caustic of a hanging water drop." Applied Optics 59, no. 21 (June 10, 2020): F32. http://dx.doi.org/10.1364/ao.390328.
Повний текст джерелаSalamone, Joseph A. "Analysis of focus boom test cases using the lossy nonlinear Tricomi equation." Journal of the Acoustical Society of America 151, no. 4 (April 2022): A119. http://dx.doi.org/10.1121/10.0010838.
Повний текст джерелаYao, Jun Ping, and Sun Zhong. "Research on the Alkali Corrosion Resistance Mechanism of Ni-Cr-Cu Alloy Cast Iron." Advanced Materials Research 230-232 (May 2011): 1298–302. http://dx.doi.org/10.4028/www.scientific.net/amr.230-232.1298.
Повний текст джерелаLavenda, B. H. "Buffon's Needle on Caustics and Torus Quantization." Open Systems & Information Dynamics 10, no. 01 (March 2003): 51–64. http://dx.doi.org/10.1023/a:1022923325144.
Повний текст джерелаKantemirov, V. D., R. S. Titov, A. V. Timohin, and A. M. Jakovlev. "Improvement of methods of accounting for increased losses and dilution of minerals during production." Mining informational and analytical bulletin, no. 3-1 (March 20, 2020): 453–64. http://dx.doi.org/10.25018/0236-1493-2020-31-0-453-464.
Повний текст джерелаPettersen, Tanja. "Phase Transformation for Primary Particles in the Surface Regions of an AA1200 Alloy." Materials Science Forum 539-543 (March 2007): 311–16. http://dx.doi.org/10.4028/www.scientific.net/msf.539-543.311.
Повний текст джерелаHubral, Peter, Martin Tygel, and Jörg Schleicher. "Geometrical‐spreading and ray‐caustic decomposition of elementary seismic waves." GEOPHYSICS 60, no. 4 (July 1995): 1195–202. http://dx.doi.org/10.1190/1.1443848.
Повний текст джерелаSmit, Pieter Bart, T. T. Janssen, and T. H. C. Herbers. "TOPOGRAPHY-INDUCED FOCUSING OF RANDOM WAVES." Coastal Engineering Proceedings 1, no. 33 (December 15, 2012): 6. http://dx.doi.org/10.9753/icce.v33.waves.6.
Повний текст джерелаДисертації з теми "Caustic zone"
Wolf, Michael D. C. "Amplituden der Kernphasen im Bereich der Kaustik B und Untersuchung der Struktur der Übergangszone zum inneren Erdkern mit spektralen Amplituden der diffraktierten Phase PKP(BC)." Phd thesis, Universität Potsdam, 2002. http://opus.kobv.de/ubp/volltexte/2005/60/.
Повний текст джерелаHinsichtlich der Lage des Kaustikmaximums lassen sich die untersuchten Erdmodelle in zwei Kategorien einteilen. Eine Gruppe besteht aus den Modellen IASP91 und 1066B, deren Maxima bei 144.6 ° und 144.7 ° liegen. Zur zweiten Gruppe von Modellen zählen AK135, PREM und SP6 mit den Maxima bei 145.1 ° und 145.2 ° (SP6). Die gemessene Amplitudenkurve hat ihr Maximum bei 145 °. Alle Entfernungsangaben beziehen sich auf eine Herdtiefe von 200 km. Die Kaustikentfernung für einen Oberflächenherd ist jeweils um 0.454 ° größer als die angegeben Werte. Damit liegen die Maxima der Modelle AK135 und PREM nur 0.1 ° neben dem der gemessenen kumulierten Amplitudenkurve. Daher wird auf die Erstellung eines eigenen Modells verzichtet, da dieses eine unwesentlich verbesserte Amplitudenkurve aufweisen würde. Das Ergebnis der Untersuchung ist die Erstellung einer gemessenen kumulierten Amplituden-Entfernungskurve für die Kaustik B. Die Kurve legt die Position der Kaustik B für kurzperiodische Daten auf ± 0.15 ° fest und bestimmt damit, welche Erdmodelle für die Beschreibung der Amplituden im Entfernungsbereich der Kaustik B besonders geeignet sind. Die Erdmodelle AK135 und PREM, ergänzt durch ein einheitliches Q-Modell, geben den Verlauf der Amplituden am besten wieder. Da die Amplitudenkurven beider Modelle nahe beieinander liegen, sind sie als gleichwertig zu bezeichnen.
Im zweiten Teil der Arbeit wird die Struktur der Übergangszone in den inneren Erdkern anhand des spektralen Abklingens der Phase PKP(BC)diff am Punkt C der Laufzeitkurve untersucht. Der physikalische Prozeß der Beugung ist für die starke Abnahme der Amplituden dieser Phase verantwortlich. Die Diffraktion beeinflußt das Abklingverhalten verschiedener Frequenzanteile des seismischen Signals auf unterschiedliche Weise. Eine Deutung des Verhaltens erfordert die Berechnung von Abklingspektren. Dabei wird die Abschwächung des PKP(BC)diff Signals für acht Frequenzen zwischen 6.4 s und 1.25 Hz ermittelt und als Spektrum dargestellt. Die Form des Abklingspektrums ist charakteristisch für die Beschaffenheit der Geschwindigkeitsstruktur direkt oberhalb der Grenze zum inneren Erdkern (GIK). Die Beben, deren Kernphasen im Regionalnetz als diffraktierte Kernphasen BCdiff registriert werden, liegen in einem Entfernungsbereich jenseits von 150 °. In dieser Distanz befinden sich die Erdbebenherde der Tonga-Fidschi-Subduktionszone, deren Breitbandaufzeichnungen verwendet werden. Die Auswertung unkorrigierter Wellenformen ergibt Abklingspektren, die mit plausiblen Erdmodellen nicht in Einklang zu bringen sind. Aus diesem Grund werden die Daten einer spektralen Stationskorrektur unterzogen, die eigens zu diesem Zweck ermittelt wird. Am Beginn der Auswertung steht eine Prüfung bekannter Erdmodelle mit unterschiedlichen Geschwindigkeitsstrukturen oberhalb der GIK. Zu den untersuchten Modellen zählen PREM, IASP91, AK135Q, PREM2, SP6, OICM2 und eine Variante des PREM. Die Untersuchung ergibt, daß Modelle, die einen verringerten Gradienten oberhalb der GIK aufweisen, eine bessere Übereinstimmung mit den gemessenen Daten zeigen als Modelle ohne diese Übergangszone. Zur Verifikation dieser These wird ein Erdmodell, das keinen verringerten Gradienten oberhalb der GIK besitzt (PREM), durch eine Reihe unterschiedlicher Geschwindigkeitsverläufe in diesem Bereich ergänzt und deren synthetische Seismogramme berechnet. Das Resultat der Untersuchung sind zwei Varianten des PREM, deren Frequenzanalyse eine gute Übereinstimmung mit den Daten zeigt. Das Abklingspektrum des Erdmodells PD47, das in einer 380 km mächtigen Schicht einen negativen Gradienten besitzt, zeigt eine große Ähnlichkeit mit den gemessenen Spektren. Dennoch kann es nicht als realistisches Modell angesehen werden, da der Punkt C in einer zu großen Entfernung liegt. Darüber hinaus müßte die zu kurze Differenzlaufzeit zwischen PKP(AB) und PKP(DF) beziehungsweise PKIKP durch eine größere Änderung der Geschwindigkeitsstruktur im inneren Kern kompensiert werden. Es wird deshalb das Modell PD27a favorisiert, das diese Nachteile nicht aufweist. PD27a besitzt eine Schicht konstanter Geschwindigkeit oberhalb der GIK mit einer Mächtigkeit von 150 km. Die Art des Geschwindigkeitsverlaufs steht im Einklang mit der geodynamischen Modellvorstellung, nach der eine Anreicherung leichter Elemente oberhalb der GIK vorliegt, die als Ursache für die Konvektion im äußeren Erdkern anzusehen ist.
In this thesis the structure of the outer core is investigated with PKP core phases. The knowledge of the physical properties of the earth′s deep interior in this region is important for the understanding of geodynamical processes like the convective flow in the liquid outer core and the differential rotation of the earth′s inner core.
The first part of this thesis describes the investigation of the PKP caustic point B near 145 °. For this purpose a cumulative amplitude distance curve is determined and compared with theoretical amplitude distance curves of different standard earth models. The data are broadband seismograms of the German Regional Seismic Network (GRSN) and the Gräfenberg Array (GRF). In order to measure the absolute amplitudes of the PKP phases, a WWSSN-SP filter is applied to the seismograms. The source regions are located in the South Pacific near Vanuatu Island (4 earthquakes) and on the French atolls Mururoa and Fangataufa (4 explosions). The advantage of a standardized network of seismic stations and the usage of station and magnitude corrections is a reduction of the scatter of the amplitude data. There is even less scatter than in studies with long period amplitude data (Häge, 1981). Another reason for the reduced scattering is the use of events with an impulsive source time function. Only the low scattering of the amplitude values makes it possible to interpret the data. More scattering of the data would have prevented an interpretation. The theoretical amplitude curves are similar in the caustic B distance range. The Q depth distribution for P and S waves used for calculating the synthetic seismograms is a combination of the values of the models CIT112 and PREM. The amplitudes determined with the help of this kind of model are slightly higher than the actually measured amplitudes. However, this needs not be taken into account because the interpretation is based on the position of the caustic peak. Therefore I rejected the computation of an improved Q model.
Regarding the position of the caustic point there are two categories of earth models. The first group consists of the models IASP91 and 1066B with their maxima at 144.6 ° and 144.7 ° respectively. AK135, PREM and SP6 belong to a second group of models with caustic peaks at 145.1 ° and 145.2 ° (SP6). The measured curve has its maximum at 145 °. All distances refer to a source depth of 200 km. For a surface focus the increase in distance is 0.454 °. Therefore the peaks of the models AK135 and PREM are only 0.1 ° beside the maximum of the measured amplitude curve. The main result of this investigation is the amplitude distance curve in the vicinity of the cusp B. The curve determines the position of this point with an accuracy of ± 0.15 ° and points to earth models which would be good for modeling the amplitudes in the distance range of the PKP caustic B. The synthetic seismograms calculated for AK135 and PREM together with a standardized Q model fit the measured amplitude curve equally well.
In the second part of this study the structure of the transition zone to the earth′s inner core is investigated by using the spectral decay of the diffracted wave PKP(BC)diff at point C of the travel time curve. The physical process of diffraction is responsible for the strong reduction in amplitude of this wave. The influence of the diffraction on the seismic signal strongly depends on frequency. The interpretation of this phenomenon requires a calculation of decay spectra. In practice the attenuation of the PKP(BC)diff signal for eight frequencies between 6.4 s and 1.25 Hz are measured and visualized as a decay spectrum. The shape of a spectrum is characteristic of the velocity gradient above the inner core boundary (ICB). Those earthquakes whose core phases are recorded as diffracted core phases BCdiff lie beyond 150 °. In this distance range there are the epicenters of the Tonga-Fiji slab. The broadband waveform data of the earthquakes in this region is used in this study. Decay spectra of waveform data which are not corrected for station site effects are incompatible with standard earth models. Therefore a spectral station correction is applied, which was especially determined for this purpose. The investigation starts with a review of a number of well-known earth models like PREM, IASP91, AK135Q, PREM2, SP6, OICM2 and a version of PREM. All these models have different velocity structures at the ICB. It is shown that models with a reduced velocity gradient above the ICB agree with the data rather than models without such a transition zone. For verification purposes a model without such a reduced gradient (PREM) is completed with different kinds of gradient zones to calculate synthetic seismograms. Two variants of the PREM correspond with the measured decay constants. The decay constants of model PD47 are very close to the measured ones. This model has a 380 km thick negative gradient above the ICB. Nevertheless it is not a realistic model because point C lies in a unrealistic great distance. As a result of the low velocity zone above the inner core there is a differential travel time between the PKP(AB) and the PKP(DF) phase (also PKIKP) which is too short. This would have to be compensated by a correction of the velocities in the inner core. Thus PD27a is the most suitable model which does not have the above mentioned disadvantages. PD27a has a 150 km thick layer of constant velocity above the ICB. This kind of velocity model is compatible with geodynamical theories according to which an enrichment of light elements above the ICB is present and powers the convection in the outer earth core by its buoyancy.
Фесенко, Сергій Вікторович. "Вплив проникаючого акустичного випромінювання на поліагрегатний підвіс гіроскопа і похибки вимірювань на резонансному рівні". Doctoral thesis, Київ, 2017. https://ela.kpi.ua/handle/123456789/21511.
Повний текст джерелаConeglian, André Vinícius Lopes. "Os juntivos causais e concessivos do português brasileiro na perspectiva cognitivo-funcional: uma análise da ligação conceptual dos elementos gramaticais em uso nessa zona adverbial." Universidade Presbiteriana Mackenzie, 2015. http://tede.mackenzie.br/jspui/handle/tede/2207.
Повний текст джерелаFundação de Amparo a Pesquisa do Estado de São Paulo
In a functional perspective combined to the cognitive perspective of mental spaces, this study focuses on language use as a guidepost to the structure of human conceptual system. the main goal of this research is to verify how grammatical relations are held within the adverbial zone of causalities and, based on that, configure the mental spaces network evoked by these constructions. the specific goals of this project are verifying and analyzing: a) the conceptual connection between the categories of cause and concession; b) the linguistic elements in the construal of the connective and its mental spaces configuration; c) the usage of connectives relative to conceptual domains (content, epistemic, speech act and metalinguistic); d) the usage of tense and mood related to specific connectives and how these categories configure mental spaces; e) the order in these adverbial constructions. based on the list provided by neves (2000), it were selected three adverbial conjunctions in each domain: in the causal domain, já que, uma vez que and visto que; in the concessive domain, ainda que, mesmo que, se bem que. in this study, the corpus came from spoken and written language data available at corpus do português. the analyses considered the following points: (i) the morphosemantic nature of the causal and concessive connectives; (ii) the order of the clauses in the adverbial constructions; (iii) the tense and mood correlations in these constructions; (iv) the presence of traits of (inter)subjectivity in these constructions. these analyses converged on the main hypothesis that the connective used to express causality or concessivity particularizes the relation between adverbial and matrix clause. Regarding specific goals, it was found that: a) the conceptual connection between causality and concessivity lies in more fundamental notions of force dynamics; b) the lexical base of the connectives bears relation to categorial properties of causality and concessivity; c) the connectives show preference for conceptual domains, even though they are pragmatically ambiguous; d) the tense and mood correlations concessive and causal constructions serve to more general functions of signaling epistemic stance and mental spaces embedding; e) the order in these constructions is motived and constrained by the sematic and discursive functions of the adverbial clause. this study revealed that structural complexity in these constructions is a consequence of their semantic and pragmatic complexity with respect to their semantic-pragmatic functions in discourse and with respect to the mental spaces network configuration.
Numa perspectiva funcionalista que se combina à perspectiva cognitivista dos espaços mentais, o estudo se dirige à língua em uso como guia para estrutura do sistema conceptual humano. o objetivo geral desta pesquisa é verificar, dentro da zona adverbial de causalidade-condicionalidade-concessividade, como se manifestam no português brasileiro as relações gramaticais, e, a partir daí, configurar a contraparte da rede dos espaços mentais estabelecida nesse território. os objetivos específicos são verificar e interpretar: a) a ligação conceptual das categorias de causa e concessão; b) a materialidade linguística dos juntivos e sua pré-configuração de espaços mentais; c) o uso dos elementos juntivos nos diferentes domínio conceptuais (conteúdo, epistêmico, atos de fala e metalinguístico); d) o uso dos tempos e modos verbais específicos aos juntivos e a configuração da rede de espaços mentais por eles estabelecida; e) a ordenação dos segmentos nas construções adverbiais e a configuração da rede de espaços mentais por eles estabelecida. a partir da lista de itens juntivos apresentada em neves (2000) foram selecionados três itens juntivos de cada relação: entre os causais se analisaram já que, uma vez que e visto que; entre os concessivos, se analisaram ainda que, mesmo que e se bem que. neste estudo, foram considerados dados de língua escrita e de língua falada coletados no banco de dados do corpus do português. as análises abrangeram os pontos de investigação propostos: (i) a natureza morfossemântica dos itens juntivos causais e dos itens juntivos concessivos; (ii) a ordenação dos segmentos adverbiais em relação aos segmentos nucleares; (iii) a correlação entre tempo e modo dos verbos nessas construções adverbiais; (iv) a presença de traços de (inter)subjetividade nas construções adverbiais de causa e de concessão. o encaminhamento das análises, a partir dos objetivos traçados, convergiu na hipótese central de que o item juntivo utilizado na explicitação das relações adverbiais particulariza a relação entre o segmento nuclear e o segmento adverbial. quanto aos objetivos específicos, verificou-se que: a) a ligação conceptual entre causalidade e concessividade se explica a partir das noções do sistema cognitivo de dinâmica de forças; b) a base lexical dos itens juntivos, ligada às propriedades das categorias de causa e de concessividade; c) esses itens mostraram uma preferência por domínios específicos, ainda que os itens juntivos sejam pragmaticamente ambíguos por ocorrerem nos diversos domínios conceptuais; d) a correlação modo-temporal nas construções causais e concessivas tem as funções mais gerais de tanto marcar a postura epistêmica do falante como de marcar o encaixamento e a hierarquia dos espaços mentais ativados; e) a ordem nas construções causais e concessivas é motivada pela função semântica e pela função pragmática exercidas pelos segmentos adverbiais. O estudo revelou que a complexidade estrutural dessas construções é um reflexo de sua complexidade semântica e pragmática quanto às funções semântico-discursivas que essas construções exercem no discurso e quanto à configuração dos espaços mentais elaborados, construídos e evocados por elas.
Частини книг з теми "Caustic zone"
Webb, T. W., D. A. Meyn, and E. C. Aifantis. "Three-Dimensional Aspects of the Fracture Process Zone and Caustics." In Mechanical Behavior of Materials, 245–51. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-1968-6_28.
Повний текст джерелаXu, Zhaoyong, Runhai Yang, Jinming Zhao, Bin Wang, Yunyun Wang, Bingheng Xiong, Zhengrong Wang, Xiaoxu Lu, and Shirong Mei. "Experimental Study of the Process Zone, Nucleation Zone and Plastic Area of Earthquakes by the Shadow Optical Method of Caustics." In Earthquake Processes: Physical Modelling, Numerical Simulation and Data Analysis Part I, 1951–66. Basel: Birkhäuser Basel, 2002. http://dx.doi.org/10.1007/978-3-0348-8203-3_4.
Повний текст джерелаТези доповідей конференцій з теми "Caustic zone"
Lam, Poh-Sang, Craig S. Stripling, Donald L. Fisher, and James B. Elder. "Potential for Stress Corrosion Cracking of A537 Carbon Steel Nuclear Waste Tanks Containing Highly Caustic Solutions." In ASME 2010 Pressure Vessels and Piping Division/K-PVP Conference. ASMEDC, 2010. http://dx.doi.org/10.1115/pvp2010-25117.
Повний текст джерелаNarisetti, Raj K., Massimo Ruzzene, and Michael J. Leamy. "Wave Propagation in Two-Dimensional Nonlinear Periodic Lattices." In ASME 2009 International Design Engineering Technical Conferences and Computers and Information in Engineering Conference. ASMEDC, 2009. http://dx.doi.org/10.1115/detc2009-86279.
Повний текст джерела