985 resultados para Fine Arts


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This work is focused on the study of the fine speckle contrast present in planar view observations of matched and mismatched InGaAs layers grown by molecular beam epitaxy on InP substrates. Our results provide experimental evidence of the evolution of this fine structure with the mismatch, layer thickness, and growth temperature. The correlation of the influence of all these parameters on the appearance of the contrast modulation points to the development of the fine structure during the growth. Moreover, as growth proceeds, this structure shows a dynamic behavior which depends on the intrinsic layer substrate stress.

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Ancien possesseur : Labrouste, Henri (1801-1875)

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Ancien possesseur : Labrouste, Henri (1801-1875)

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Comprend : [ Planche dépliante entre pp. 64-65. ] Elévation des faces des murs du Salon de l'Académie [royale des Arts de peinture et de sculpture. XVIIIè siècle.] [ Cote : BNF C 107129. ] ; [ Planche dépliante entre pp.104-105. ] Plan et élévation de la salle où se tiennent ordinairement les Assemblés. [ Académie royale des Arts de peinture et de sculpture. XVIIIè siècle.] [ Cote : BNF C 107130. ] ; [ Planche dépliante entre pp.164-166. ] Plan et élévation de la troisième salle de l'Académie [royale des Arts de peinture et de sculpture] où sont les vases de Medicis. [XVIIIè siècle.] [ Cote : BNF C 106592. ] ; [ Planche dépliante entre pp.208-209. ] Plan de la salle séparée des autres. [ Une salle de l'Académie royale des Arts de peinture et de sculpture. XVIIIè siècle.] [ Cote : BNF C 107131. ] ; [ Planche dépliante entre pp. 246-247. ] Plan du vestibule par où on entre dans le salon [de l'Académie royale des Arts de peinture et de sculpture. XVIIIè siècle.] [ Cote : BNF C 107132. ] ; [ Planche dépliante entre pp.256-257. ] Plan de l'Ecole du modèle [ à l'Académie royale des Arts de peinture et de sculpture. XVIIIè siècle.] [ Cote : BNF C 107133. ]

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Comprend : [ Planche 1. Croissance de la vigne. Différents modes de culture et différents stades de croissance. XVIIIè siècle.] Dessiné par Durival, gravé par Collin fils. [ Cote : BNF C 147091. ] ; [ Planche 2. Croissance de la vigne. Manière de la faire correctement pousser. XVIIIè siècle.] [ Cote : BNF C 147092. ] ; [ Planche 3. Croissance de la vigne. Différents stades. XVIIIè siècle.] Dessiné par Durival, gravé par Collin. [ Cote : BNF C 147093. ]

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Iowa Citizen Aide - Ombudsman Office received a complaint on February 22, 2010, concerning the manner in which the mayor and several city council members for the City of Monticello (City) attempted to remove the city administrator from his position. It was alleged that the mayor and at least one council member went to the homes of other council members and sought their signatures on a letter of offer requesting the city administrator to resign or face a vote to terminate his employment. We were asked to investigate whether this action complied with Iowa’s Open Meetings Law.

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Knowledge of the reflectivity of the sediment-covered seabed is of significant importance to marine seismic data acquisition and interpretation as it governs the generation of reverberations in the water layer. In this context pertinent, but largely unresolved, questions concern the importance of the typically very prominent vertical seismic velocity gradients as well as the potential presence and magnitude of anisotropy in soft surficial seabed sediments. To address these issues, we explore the seismic properties of granulometric end-member-type clastic sedimentary seabed models consisting of sand, silt, and clay as well as scale-invariant stochastic layer sequences of these components characterized by realistic vertical gradients of the P- and S-wave velocities. Using effective media theory, we then assess the nature and magnitude of seismic anisotropy associated with these models. Our results indicate that anisotropy is rather benign for P-waves, and that the S-wave velocities in the axial directions differ only slightly. Because of the very high P- to S-wave velocity ratios in the vicinity of the seabed our models nevertheless suggest that S-wave triplications may occur at very small incidence angles. To numerically evaluate the P-wave reflection coefficient of our seabed models, we apply a frequency-slowness technique to the corresponding synthetic seismic wavefields. Comparison with analytical plane-wave reflection coefficients calculated for corresponding isotropic elastic half-space models shows that the differences tend to be most pronounced in the vicinity of the elastic equivalent of the critical angle as well as in the post-critical range. We also find that the presence of intrinsic anisotropy in the clay component of our layered models tends to dramatically reduce the overall magnitude of the P-wave reflection coefficient as well as its variation with incidence angle.