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1

Ouédraogo, Souleymane, Augustin S. Zongo, Jean-Fidèle N’Zihou, Tizane Daho, and Antoine Béré. "Modélisation du rayonnement solaire global incident sur un plan horizontal et incliné par quatre modèles semi-empiriques sur le site de la ville de Ouagadougou." Journal de Physique de la SOAPHYS 2, no. 2 (May 12, 2021): C20A25–1—C20A25–9. http://dx.doi.org/10.46411/jpsoaphys.2020.02.25.

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Les paramètres météorologiques et radiométriques tels que le rayonnement solaire influencent fondamentalement la rentabilité et la performance des systèmes de conversion de l’énergie solaire. L’optimisation des convertisseurs d’énergie solaire dépend du modèle de rayonnement solaire utilisé. Cette étude porte sur l’estimation du rayonnement solaire incident global sur le plan horizontal et incliné sur le site de la ville de Ouagadougou. L’étude des quatre modèles de rayonnement solaire permet d’estimer le rayonnement solaire global incident sur un plan horizontal et incliné. Les différents modèles sont évalués sur une base graphique et statistique, en utilisant les indicateurs du coefficient de détermination de R^2, de l’erreur quadratique moyenne (RMSE) et le pourcentage de l'erreur absolue moyenne (MAPE). Les résultats obtenus avec les quatre modèles semi-empiriques ont été comparés avec les valeurs expérimentales instantanées mesurées sur le site de Ouagadougou. Les résultats montrent que le modèle semiempirique d’Eufrat présente la meilleure estimation du rayonnement solaire global pour le site de Ouagadougou.
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2

Chanson, Hubert. "Solutions Analytiques de l’Onde de Rupture de Barrage sur Plan Horizontal et Incliné." La Houille Blanche, no. 3 (May 2006): 76–86. http://dx.doi.org/10.1051/lhb:200603012.

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3

Hillairet, M., and D. Serre. "Chute stationnaire d'un solide dans un fluide visqueux incompressible le long d'un plan incliné." Annales de l'Institut Henri Poincare (C) Non Linear Analysis 20, no. 5 (September 2003): 779–803. http://dx.doi.org/10.1016/s0294-1449(02)00028-8.

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4

Millet, Séverine, François Rousset, Valéry Botton, and Hamda Ben Hadid. "Stabilité de l'écoulement à deux couches de films non-newtoniens sur un plan incliné." Comptes Rendus Mécanique 336, no. 3 (March 2008): 313–19. http://dx.doi.org/10.1016/j.crme.2007.10.021.

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5

Luyat, Marion, and Théophile Ohlmann. "Effet d'un contexte visuel incliné : vers une explication en termes d'inclinaison du plan médian apparent." L'année psychologique 97, no. 2 (1997): 267–92. http://dx.doi.org/10.3406/psy.1997.28953.

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6

Hillairet, M. "Chute stationnaire d’un solide dans un fluide visqueux incompressible au-dessus d’un plan incliné. Partie 2." Annales de la faculté des sciences de Toulouse Mathématiques 16, no. 4 (2007): 867–903. http://dx.doi.org/10.5802/afst.1169.

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7

Vinet, L., A. Sarcher, B. Perrouin-Verbe, F. Leboeuf, and R. Gross. "Évaluation de l’effet d’un plan incliné sur la marche des enfants avec paralysie cérébrale : quelles pistes pour la rééducation ?" Motricité Cérébrale : Réadaptation, Neurologie du Développement 38, no. 1 (March 2017): 21–33. http://dx.doi.org/10.1016/j.motcer.2017.01.002.

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8

Hattab, Mahdia, Soumia Bouziri-Adrouche, and Jean-Marie Fleureau. "Évolution de la microtexture d’une matrice kaolinitique sur chemin triaxial axisymétrique." Canadian Geotechnical Journal 47, no. 1 (January 2010): 34–48. http://dx.doi.org/10.1139/t09-098.

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L’objectif de cette recherche est de comprendre comment évolue la microtexture d’une matrice kaolinitique lorsque celle-ci est soumise à un chemin triaxial de révolution. L’approche consiste à réaliser un essai triaxial sur des éprouvettes du matériau saturé faiblement surconsolidé, puis à suivre l’évolution de la microstructure (orientation des particules et porosité) le long du chemin de chargement par des observations au microscope électronique à balayage. À l’état initial, le matériau est consolidé de façon uniaxiale, et les observations montrent une anisotropie microstructurale avec orientation privilégiée des particules suivant le plan horizontal perpendiculaire à la direction du chargement. Sur chemin isotrope, l’analyse montre une réorientation progressive des particules vers une isotropie structurale. Cette évolution se poursuit en début de chargement triaxial pour tendre ensuite vers une orientation privilégiée des particules selon un plan incliné en fin de chargement. L’évolution de la porosité est examinée à partir de mesures par porosimétrie au mercure, illustrées par des images seuillées de photos MEB. Celles-ci suggèrent l’existence d’une double porosité à l’état initial, qui semble se maintenir lors du chargement isotrope, puis évoluer vers une porosité unimodale, avec une légère diminution de la taille des pores, sur le chemin triaxial.
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9

Agunaoun, A., A. Il Idrissi, A. DaÏf, and R. Barriol. "Etude de l'évaporation en convection mixte d'un film liquide d'un mélange binaire s'écoulant sur un plan incliné soumis à un flux de chaleur constant." International Journal of Heat and Mass Transfer 41, no. 14 (July 1998): 2197–210. http://dx.doi.org/10.1016/s0017-9310(97)00319-0.

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10

Nicolini, Eric. "Nouvelles observations sur la morphologie des unités de croissance du hêtre (Fagus sylvatica L.). Symétrie des pousses, reflet de la vigueur des arbres." Canadian Journal of Botany 78, no. 1 (March 7, 2000): 77–87. http://dx.doi.org/10.1139/b99-162.

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Le hêtre a une croissance rythmique où chaque pousse annuelle est constituée d'une unité de croissance (u.c.) printanière parfois suivie, quelques semaines plus tard, d'une unité de croissance estivale. L'u.c. printanière présente une disposition foliaire alterne distique, tandis que l'u.c. estivale, selon certains auteurs, a une disposition foliaire alterne spiralée. Au terme d'observations morphologiques et histologiques de bourgeons formés à différentes périodes de l'année, il s'avère que la disposition foliaire du hêtre n'évolue pas d'un type d'u.c. à l'autre : les ébauches foliaires sont toujours disposées suivant deux droites parallèles, rapprochées sur un côté de la tige selon une disposition « plagiotrope distique ». La symétrie axiale d'une u.c. peut toutefois se modifier au cours de son allongement et évoluer d'une symétrie bilatérale vers une symétrie radiale secondaire. Cette évolution est le résultat d'une réorientation des nœuds par torsion des entre-nœuds, les plus grands déplacements d'organe foliaire étant réalisés par les u.c. les plus longues au niveau de leurs entre-nœuds les plus longs. Il est possible de rattacher degré de développement des u.c. et architecture des arbres. Les arbres les moins vigoureux (très jeunes ou situés sous couvert forestier dense) ont un axe principal plus ou moins incliné, constitué d'u.c. peu développées dont la symétrie est bilatérale; l'axe principal est plagiotrope et porte un houppier plan. En revanche, les arbres les plus vigoureux (adultes ou en situations forestières favorables) ont un axe principal vertical, constitué d'u.c. relativement longues et de symétrie radiale; l'axe principal est orthotrope et porte un houppier bien réparti tout autour de lui.Mots clés : morphologie, Fagus, vigueur, disposition foliaire, architecture.
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11

Allard, Pierre. "Variabilité des débitages laminaires au Second Mésolithique et au Néolithique ancien dans le nord de la France (VIIe et VIe millénaire BCE)." Journal of Lithic Studies 4, no. 2 (September 15, 2017): 75–103. http://dx.doi.org/10.2218/jls.v4i2.2538.

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Cet article présente un bilan des techniques de taille du Second Mésolithique et du Néolithique ancien du 7e au 6e millénaire dans le nord de la France. Cette période est caractérisée par l'apparition d'une nouvelle pratique technique qui se manifeste par la production de lames régulières associées à de nouvelles armatures de flèche de forme trapézoïdale. D’après les études menées, il semble que seuls les débitages à la percussion indirecte sont documentés dans l’ouest et le nord de l’aire considérée. Néanmoins, des analyses plus fines devront être menées pour les débitages soignés des productions de lamelles régulières et des petits nucléus présents dans les contextes de l’est de la France. Il semble désormais qu’une méthode de débitage assez commune puisse se percevoir. Elle a été parfaitement décrite sur le site des Essart à Poitiers (méthode de l’Essart A, Marchand 2009). Cette méthode d’exploitation des blocs avec des flancs orthogonaux, un plan de frappe lisse peu incliné et une surface lamellaire quadrangulaire peu cintrée apparaît comme plutôt fréquente dans les assemblages à trapèzes du Mésolithique. Malgré un concept commun, l’étude de ce « complexe » des industries à trapèzes montre une certaine variabilité du point de vue des méthodes de taille. Il semble se dégager des entités parfois bien circonscrites au sein de cet ensemble. C’est le cas du Retzien qui s’oppose nettement au Téviécien de par les procédés de préparation systématique par micro-facettage mais également par une excellente unité stylistique des types de trapèzes. Le débitage sur tranche d’éclat pour l’installation des surfaces laminaires semble pour le moment cantonné d’une zone allant du Bassin parisien à la Belgique. L’est de la France se démarque par des productions avec des talons facettés et des plans très inclinés. Il faudra donc donner du sens à ces différentes pratiques qui pour le moment sont des résultats bruts. La dimension chronologique est un élément crucial qui devra être mieux précisé. En rapport avec les résultats obtenus sur les modalités de la percussion indirecte, un meilleur cadre chronologique permettra de comprendre la synchronie ou la diachronie des variantes observées des débitages. De nouvelles découvertes et de nouvelles datations permettent de mieux préciser l’introduction de la percussion indirecte vers 6200 cal. BCE dans le Bassin parisien. Enfin, il reste encore à mieux préciser les assemblages typologiques. Nous ne disposons pas encore suffisamment de séries qui permettent de bien comprendre l’évolution des différents types de trapèzes et triangles dérivés et si certaines méthodes de débitages sont particulières à certains types d’armatures. Malgré les imprécisions des datations et la difficulté de démêler les assemblages d’armatures, on peut retenir qu’il existe probablement des moments où certains types dominent. Ce travail reste totalement à faire et il est tributaire d’une meilleure résolution chronologique et des contextes des séries du Second Mésolithique
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12

HU, JUN, BING-HONG ZHOU, YI-HONG HANG, QIU-SHENG LIU, and SHU-DAO ZHANG. "Linear spatio-temporal instability analysis of ice growth under a falling water film." Journal of Fluid Mechanics 649 (April 13, 2010): 453–66. http://dx.doi.org/10.1017/s002211201000025x.

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A linear spatio-temporal stability analysis is conducted for the ice growth under a falling water film along an inclined ice plane. The full system of linear stability equations is solved by using the Chebyshev collocation method. By plotting the boundary curve between the linear absolute and convective instabilities (AI/CI) of the ice mode in the parameter plane of the Reynolds number and incline angle, it is found that the linear absolute instability exists and occurs above a minimum Reynolds number and below a maximum inclined angle. Furthermore, by plotting the critical Reynolds number curves with respect to the inclined angle for the downstream and upstream branches, the convectively unstable region is determined and divided into three parts, one of which has both downstream and upstream convectively unstable wavepackets and the other two have only downstream or upstream convectively unstable wavepacket. Finally, the effect of the Stefan number and the thickness of the ice layer on the AI/CI boundary curve is investigated.
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13

Redmann, Erica, Alina Sheikh, Areej Alqahtani, Mica McCarty-Glenn, Shazrah Syed, Rita S. Mehta, and Andrea B. Ward. "Terrestrial Locomotion in American Eels (Anguilla rostrata): How Substrate and Incline Affect Movement Patterns." Integrative and Comparative Biology 60, no. 1 (May 20, 2020): 180–89. http://dx.doi.org/10.1093/icb/icaa016.

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Synopsis Fishes overcome a variety of challenges in order to invade the terrestrial environment. Terrestrial invasions by fish occur over a variety of environmental contexts. In order to advance their bodies on land, fishes capable of terrestrial excursions tend to use one of three different types of locomotor modes: axial-based, appendage-based, or axial-appendage-based. Elongate species with reduced appendages, such as the American eel, Anguilla rostrata, rely on axial based locomotion in water and on land. When eels move from water to land as part of their complex life cycle, they inevitably encounter a variety of substrates and must traverse variable degrees of incline. The aim of this study was to determine the effect of substrate and incline on the terrestrial locomotion of the American eel. In order to do this, eels were filmed from a dorsal view on three substrates and four inclines: sand, loose pebbles, and fixed (glued) pebbles at 0°, 5°, 10°, and 15°. We digitized 20 evenly spaced points along the body to examine the following characteristics of locomotion: velocity, distance ratio (DR), and wave parameters such as wave amplitude, frequency, and length and assessed whether substrate, incline, or body position affected these parameters. DR, our metric of movement efficiency, was highest on the flat sand condition and lowest on 15° pebble conditions. Efficiency also varied across the body. Velocity followed a similar pattern being highest on sand at 0° and lowest at the steepest inclines. Wave amplitude generally increased toward the tail but was similar across substrates and inclines. Wave frequency was relatively consistent across the body on both pebble substrates, but on sand, frequency was higher toward the head but decreased toward the tail. Wavelengths on sand were the longest at 0° near the head and shorter wavelengths were observed on steeper inclines. Both pebble substrates elicited lower wavelengths that were more similar across the body. Overall, A. rostrata were more effective in navigating compliant substrates but struggled at steeper inclines. Our findings provide insight into locomotor challenges that American eels may encounter as they move from and between bodies of water.
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14

Maheshwari, Vidhi, Maria Carlone, Frank R. Fronczek, and Luigi G. Marzilli. "Ligand and coordination-plane distortions in platinum(II) complexes of isomers of dimethyl-2,2′-bipyridine." Acta Crystallographica Section B Structural Science 63, no. 4 (July 17, 2007): 603–11. http://dx.doi.org/10.1107/s0108768107027024.

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Pseudo-square-planar platinum(II) complexes containing 4,4′ (4,4′-Me2bipy), 5,5′ (5,5′-Me2bipy) and 6,6′ (6,6′-Me2bipy) isomers of dimethyl-2,2′-bipyridine (Me2bipy) were synthesized and structurally characterized to assess the effects of methyl-group position on structure. The Pt—N distances in (Me2bipy)PtCl2 complexes fall in the typical range [2.017 (3)–2.032 (3) Å]. Only minor distortions such as 2.4 and 5.5° twisting of the two pyridyl rings in (4,4′-Me2bipy)PtCl2 (I) and (5,5′-Me2bipy)PtCl2 (II), respectively, occur. However, (6,6′-Me2bipy)PtCl2 (III) is highly distorted: the two pyridyl rings in (III) have a large bowing angle (θB) of 19.2°. The presence of distortions in (III), but not in (I) and (II), is attributed to repulsions between the 6,6′-methyl groups and the cis chloro ligands. [(4,4′-Me2bipy)2Pt](BF4)2 (IV) undergoes a bow-incline deformation having a large θB value (24.2°), and the ligands are inclined relative to the coordination plane by 18.80 (13)°. Complex (IV) joins a small list of distorted bis-bipyridine complexes; this finding can be attributed to the unfavorable repulsions between the 6,6′ hydrogen substituents of opposing ligands. Some of these complexes exhibit canting rather than bow-incline distortion, a trend suggesting that subtle solid-state effects determine the nature of the distortion.
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15

Subramanian, Priya, Oliver Brausch, Karen E. Daniels, Eberhard Bodenschatz, Tobias M. Schneider, and Werner Pesch. "Spatio-temporal patterns in inclined layer convection." Journal of Fluid Mechanics 794 (April 6, 2016): 719–45. http://dx.doi.org/10.1017/jfm.2016.186.

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This paper reports on a theoretical analysis of the rich variety of spatio-temporal patterns observed recently in inclined layer convection at medium Prandtl number when varying the inclination angle ${\it\gamma}$ and the Rayleigh number $R$. The present numerical investigation of the inclined layer convection system is based on the standard Oberbeck–Boussinesq equations. The patterns are shown to originate from a complicated competition of buoyancy driven and shear-flow driven pattern forming mechanisms. The former are expressed as longitudinal convection rolls with their axes oriented parallel to the incline, the latter as perpendicular transverse rolls. Along with conventional methods to study roll patterns and their stability, we employ direct numerical simulations in large spatial domains, comparable with the experimental ones. As a result, we determine the phase diagram of the characteristic complex 3-D convection patterns above onset of convection in the ${\it\gamma}{-}R$ plane, and find that it compares very well with the experiments. In particular we demonstrate that interactions of specific Fourier modes, characterized by a resonant interaction of their wavevectors in the layer plane, are key to understanding the pattern morphologies.
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16

Falsaperla, Paolo, Andrea Giacobbe, and Giuseppe Mulone. "Stability of the Plane Bingham–Poiseuille Flow in an Inclined Channel." Fluids 5, no. 3 (August 27, 2020): 141. http://dx.doi.org/10.3390/fluids5030141.

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We study the stability of laminar Bingham–Poiseuille flows in a sheet of fluid (open channel) down an incline with constant slope angle β∈(0,π/2). This problem has geophysical applications to the evolution of landslides. In this article, we apply to this problem recent results of Falsaperla et al. for laminar Couette and Poiseuille flows of Newtonian fluids in inclined channels. The stability of the basic motion of the generalised Navier–Stokes system for a Bingham fluid in a horizontal channel against linear perturbations has been studied. In this article, we study the flows of a Bingham fluid when the channel is oblique and we prove a stabilizing effect of the Bingham parameter B. We also study the stability of the linear system with an energy method (Lyapunov functions) and prove that the streamwise perturbations are always stable, while the spanwise perturbations are energy-stable if the Reynolds number Re is less than the critical Reynolds number Rc obtained solving a generalised Orr equation of a maximum variational problem.
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17

Sato, Saori, Hideto Hiraide, Masato Yoshida, and Hiroyuki Yamamoto. "Changes in xylem tissue and laccase transcript abundance associated with posture recovery in Chamaecyparis obtusa saplings growing on an incline." Functional Plant Biology 40, no. 6 (2013): 637. http://dx.doi.org/10.1071/fp12313.

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Lignin is a major component of plant cell walls and is synthesised through oxidative polymerisation of monolignols. The transcription level of laccase, an enzyme implicated in monolignol polymerisation, is higher in the tissue forming compression wood than in normal wood. Compression wood, which is a special xylem tissue that develops to reorient inclined stems, also has a higher lignin content than normal wood. In the present study, Chamaecyparis obtusa Endl. saplings were grown on an incline and the following variables were tracked for 10 weeks: posture recovery of the saplings; development of xylem tissue on the lower side of inclined stems; and the transcription level of laccase. The posture of saplings approached vertical after 8 weeks, the development of compression wood reached a peak around 6 weeks and laccase transcription was the highest after 4 weeks. These results suggest a sequence of righting mechanisms. Inclination stimulates an increase in the abundance of laccase transcript and this increase encourages the formation of compression wood. The accumulation of compression wood then causes the stem to bend upward.
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18

Kannas, Theodoros M., Eleftherios Kellis, and Ioannis G. Amiridis. "Biomechanical Differences Between Incline and Plane Hopping." Journal of Strength and Conditioning Research 25, no. 12 (December 2011): 3334–41. http://dx.doi.org/10.1519/jsc.0b013e31821764e4.

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19

Cross, Rod. "Motion of an inclined cylinder on an inclined plane." European Journal of Physics 36, no. 5 (June 26, 2015): 055011. http://dx.doi.org/10.1088/0143-0807/36/5/055011.

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20

Alyea, Hubert N. "Tilted TOPS: Inclined plane projection." Journal of Chemical Education 66, no. 9 (September 1989): 765. http://dx.doi.org/10.1021/ed066p765.

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21

Venable, D. D., A. P. Batra, and T. Hubsch. "Modifying the inclined-plane experiment." Physics Teacher 39, no. 4 (April 2001): 215–17. http://dx.doi.org/10.1119/1.1367787.

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22

Woods, David R., and S. P. Lin. "Instability of a liquid film flow over a vibrating inclined plane." Journal of Fluid Mechanics 294 (July 10, 1995): 391–407. http://dx.doi.org/10.1017/s0022112095002941.

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The problem of the onset of instability in a liquid layer flowing down a vibrating inclined plane is formulated. For the solution of the problem, the Fourier components of the disturbance are expanded in Chebychev polynomials with time-dependent coefficients. The reduced system of ordinary differential equations is analysed with the aid of Floquet theory. The interaction of the long gravity waves, the relatively short shear waves and the parametrically resonated Faraday waves occurring in the film flow is studied. Numerical results show that the long gravity waves can be significantly suppressed, but cannot be completely eliminated by use of the externally imposed oscillation on the incline. At small angles of inclination, the short shear waves may be exploited to enhance the Faraday waves. For a given set of relevant flow parameters, there exists a critical amplitude of the plane vibration below which the Faraday wave cannot be generated. At a given amplitude above this critical one, there also exists a cutoff wavenumber above which the Faraday wave cannot be excited. In general the critical amplitude increases, but the cutoff wavenumber decreases, with increasing viscosity. The cutoff wavenumber also decreases with increasing surface tension. The application of the theory to a novel method of film atomization is discussed.
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23

Lomask, Laurie. "Leer a Vallejo desde Valle-Inclán." Archivo Vallejo 1, no. 1 (November 29, 2018): 11. http://dx.doi.org/10.34092/av.v1i1.19.

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Este trabajo explorará las conexiones entre César Vallejo y Ramón María del Valle-Inclán (1866-1936), novelista, dramaturgo y poeta español. Ya se ha notado que Vallejo se inspiró en uno de los versos de Valle-Inclán para el título de su novela, Fabla salvaje (1923). Sin embargo, la conexión entre estos dos escritores es aún más profunda. Basándose en el uso del esperpento, expuesto en la obra de teatro Luces de bohemia (publicada por primera vez en 1920, y en versión definitiva en 1924), se hará una comparación con los textos teatrales de Vallejo, en particular con su obra Entre las dos orillas corre el río (comenzada en 1930 bajo el título Moscú contra Moscú) y varias colecciones de tratados sobre el valor y la función del teatro. En los dos autores el esperpento, efectivamente, representa la dificultad de evolucionar entre generaciones, de transicionar entre el pasado y el futuro. Mientras en Valle-Inclán los personajes sufren físicamente para superar el plano ético, en Vallejo vemos que lo físico y lo ético no se separan, sino que profundizan la complejidad del existir en el tiempo. Tanto en el arte como en la política, el progreso se ve limitado por las condiciones físicas que inscriben y demarcan toda experiencia humana. ABSTRACTThis paper explores the connections between Cesar Vallejo and Ramon Maria del Valle-Inclan (1866-1936), Spanish novelist, playwright and poet. So far, we have seen that Vallejo was inspired by one of the verses of Valle-Inclan for the title of his novel, Fabla salvaje (‘Wild Fabla’, 1923); however, the connection between these two writers is even deeper. Based on the use of the esperpento ‘grotesque’, exposed in the work of Luces de bohemia (‘Lights of bohemia’) first published in 1920 and in final version in 1924, there will be a comparison with the theatrical texts of Vallejo, in particular with his work Entre las dos orillas corre el río (‘Between the Two Shores Run the River’), started in 1931, and several collections of treaties of theater’s value and function. Both authors represent esperpento, as a difficulty of evolving between generations, of transition between the past and the future. While in Valle-Inclan’s characters suffer physically to overcome the ethical plane, in Vallejo, the physical and ethical planes are not separated, but that deepens the complexity of existing in the time. Progress is limited by the physical conditions that register and draw all human experience in art and politics. Keywords: grotesque, distortion, physical body, theater, Valle-Inclan.
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Sattar, MH. "A Case report of Class II Division 2 Malocclusion in Adult women treated by Fixed appliance with CIA and removable anchor plate incorporated bite plane: Biomechanical Considerations." Bangladesh Journal of Orthodontics and Dentofacial Orthopedics 1, no. 2 (July 31, 2013): 18–24. http://dx.doi.org/10.3329/bjodfo.v1i2.15987.

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This article describes our treatment of Class II, division 2 adult patients requiring premolar extractions. Division 2 cases are often characterized by severe deep bites, lingually inclined upper central and lower incisors, and labially flared maxillary lateral incisors. This patients also tend to exhibit problems with the upper and lower occlusal planes, such as deep curves of Spee, High lip line, marked labiomental depression. Because of the deep bite and supra eruption of the maxillary incisors, the gingival margins of the maxillary anterior teeth are malaligned, and the lingually inclined mandibular incisors have excessively high gingival margins ( Fig. 1 ). The treatment protocol for this patients includes extraction of premolars both upper and lower in right side to relieve crowding, with simultaneous correction of the deep bite by intrusion of the upper and/or lower incisors. Intrusion mechanics are performed with a bite opening bend on a preformed nickel titanium arch wire. Space closure is accomplished with power chain and guard behind the extracted site in anchor plate. Extraction of upper premolar and lower 1st molar (tooth no 36) in left side was done earlier. A 21 years old women with Cl-II Div-II malocclusion type B came to Dental Centre, Dhaka, with chief complaint of an unhappy smile. Retroclined 4 Incisors, Deep bite, Crowding, deficient lower facial height, Gummy smile and a moderately convex hard- and soft-tissue profile because of a retrusive mandible with over jet of 1.5mm and over bite of 6 mm was observed. The mechanics plan should be individualized based on the specific treatment goals. Camouflage Treatment was done with the help of an anchor plate incorporated anterior incline plane. Intrusion mechanics are performed with preformed nickel titanium Connecticut Intrusion Arch (CIA) and anchor plate incorporated bite plane. Treatment was successfully completed with extractions of both pre-molars in right side and left lower 1st molar (Tooth no 36) and upper 1st premolar(Tooth no 24) already extracted ( Fig. 2 A) before starting of orthodontic treatment. Treatment of 20 months which improves incisor inclination, Deep bite correction; eliminate crowding, normal smile line and improvement of gummy smile. With the above mentioned protocol normal inclination of both upper-lower incisor, normal over jet and over bite were also achieved. DOI: http://dx.doi.org/10.3329/bjodfo.v1i2.15987 Ban J Orthod & Dentofac Orthop, April 2011; Vol-1, No.2, 18-24
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25

Bartkiewicz, Przemysław, and Mariusz Łęcki. "Warsaw Stock Exchange – the inclined plane." Zeszyty Naukowe Uniwersytetu Szczecińskiego Finanse, Rynki Finansowe, Ubezpieczenia 2015, no. 74/1 (April 30, 2015): 11–22. http://dx.doi.org/10.18276/frfu.2015.74/1-01.

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26

Man, Yin, and Wei Feng Zheng. "Load Conversion on Inclined Plane Foundation." Applied Mechanics and Materials 744-746 (March 2015): 514–17. http://dx.doi.org/10.4028/www.scientific.net/amm.744-746.514.

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According to the mechanics characteristics of inclined plane foundations in transmission line project, rotary theories of spatial coordinate system were used. Load conversion method on inclined plane foundation is analyzed and obtained to get normal section bearing capacity of the column. Meanwhile, the derivation steps and calculation formulas are shown.
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27

Thiele, Uwe, Kai Neuffer, Michael Bestehorn, Yves Pomeau, and Manuel G. Velarde. "Sliding drops on an inclined plane." Colloids and Surfaces A: Physicochemical and Engineering Aspects 206, no. 1-3 (July 2002): 87–104. http://dx.doi.org/10.1016/s0927-7757(02)00082-1.

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28

Wehrbein, William M. "Frictional forces on an inclined plane." American Journal of Physics 60, no. 1 (January 1992): 57–58. http://dx.doi.org/10.1119/1.17043.

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29

Stautberg Greenwood, Margaret. "Inclined plane on a frictionless surface." Physics Teacher 28, no. 2 (February 1990): 110. http://dx.doi.org/10.1119/1.2342957.

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30

Mertens, Keith, Vakhtang Putkaradze, and Peter Vorobieff. "Braiding patterns on an inclined plane." Nature 430, no. 6996 (July 2004): 165. http://dx.doi.org/10.1038/430165a.

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31

Furman, Robert, and Brook Niemiec. "Variation in Acrylic Inclined Plane Application." Journal of Veterinary Dentistry 30, no. 3 (September 2013): 161–66. http://dx.doi.org/10.1177/089875641303000305.

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32

Cutrale, Francesco, and Enrico Gratton. "Inclined Single Plane Illumination Microscopy (ISPIM)." Biophysical Journal 102, no. 3 (January 2012): 192a. http://dx.doi.org/10.1016/j.bpj.2011.11.1048.

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33

Erwansyah, Eka, Muhammad Wira Sakti, and Nasyrah Hidayati. "Inclined bite plane: indications and application." Makassar Dental Journal 9, no. 3 (November 28, 2020): 240–42. http://dx.doi.org/10.35856/mdj.v9i3.364.

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Background: The prevalence of malocclusion in Indonesia is about 80% of the population and is a fairly common dental and oral health problem so that treatment of malocclusion from an early age is very important and needed. One of malocclusion treatment for preventing malocclusion is the use of removable orthodontic devices in the form of inclined bite plane. Con-clusion: Inclined bite plane can be made on the orthodontic plate of maxilla and mandible. In the maxilla inclined bite plane can function as a functional appliance in treatment of Class II malocclusion division 1, as a retention device after treatment using twin blocks and in the mandible serves to correct anterior crossbite.
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34

Hewitt, Maria E., Annette Bamundo, Rebecca Day, and Catherine Harvey. "Perspectives on Post-Treatment Cancer Care: Qualitative Research With Survivors, Nurses, and Physicians." Journal of Clinical Oncology 25, no. 16 (June 1, 2007): 2270–73. http://dx.doi.org/10.1200/jco.2006.10.0826.

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Purpose Cancer survivors have many medical and psychosocial needs that are unaddressed in the post-treatment period. Qualitative research was carried out to assess how a survivorship care plan created by oncologists could improve the quality of survivorship care. Participants and Methods Focus groups and interviews conducted with cancer survivors, nurses, primary care physicians, and oncologists provide insights into post-treatment follow-up practices and the acceptability and feasibility of providing survivors and referring physicians with a cancer survivorship care plan. Results Cancer survivors reported satisfaction with post-treatment medical care, but felt that their psychosocial needs were not met. Survivors expressed enthusiastic support for receipt of a follow-up care plan. Primary care physicians viewed themselves as playing an important role during the post-treatment period and indicated that a written care plan for follow-up would help them improve their survivorship practices. Nurses recognized the need to improve the care of cancer survivors and suggested that they could play an active role in creating and implementing cancer survivorship plans. Physicians providing oncology care acknowledged the value of survivorship care plans, but were not inclined to complete them because such plans would not reduce other reporting and communication requirements and would be burdensome to complete given their busy schedules. Conclusion Survivorship care planning is viewed favorably by consumers, nurses, and physicians, however there are several barriers to its adoption. Barriers may be overcome with: electronic medical records, changes in reporting requirements of insurers, advocacy on the part of patients, and incorporation of care planning in education and training programs.
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35

Vitvitskyi, Yaroslav. "INFLUENCE OF THE RELIEF ON THE EROSION DEGRADATION CHERNOZEMS OF THE PRYDNISTERSKA UPLAND." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS, no. 11(01) (January 13, 2021): 280–93. http://dx.doi.org/10.30970/gpc.2020.1.3213.

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This publication deals with the erosive degradation of chernozem soils in the context of the the Prydnisterska Upland relief. The structure of the soil coverage of the studied area is represented by two subzonal subtypes of chernozem soils. Precisely: typical and podzolic, with a total area of 4 060 km2 (62% of the territory). The major part of these are flat interfluve: flat interfluve, wavy interfluves dissected by beam and valley forms, high fragmentary terrace complexes with insignificant horizontal dismemberment. The background surfaces of the intensity of erosion chernozem soils degradation are slopes of different steepness, exposure and morphometry. With the help of the geoinformational program ArcGIS, the distribution of slopes with the corresponding parameters of steepness and total area is determined. Inclined slopes with the steepness of 1–3° (1 700 km2) are dominant. The area with a steepness of 5° or less is approximately 87% of the total area of chernozem soils. However are of slightly inclined relief with only mere erosion occurant. The steep surfaces expositional distribution indicates the predominance of the southern, southwestern exposure slopes of an average length of 500–1 500 m. The results of the field morphological studies show that in the 5–6° – incline surfaces of inflection areas chernozem podzolic and strongly washed away. The degree of typical chernozem soils erosion is mostly associated with transversely convex and slightly convex slopes. In accordance with the degree of erosion, slightly washed typical chernozem soils formed on the same slopes of 2–3°, medium washed on 3–5°, strongly washed 8° incline. However, on the oblique slopes with an incline of 3–5° of complex shapes, typical chernozem soils the entire humus line is washed away. Particularly critical degree of chernozem soils erosion is observed within the complex slopes of river meanders and beam girder systems. In addition to the listed morphometric parameters of slope surfaces, the development of erosion degradation is influenced by the local unreasonable placement of linear boundaries. Thus, roads laid perpendicularly to river valleys and watersheds or along the plane of individual slopes form artificial bases of erosion, accelerating degradation processes. The formation of natural quarries leads to the active development of linear erosion of regressive nature. Key words: podzolic chernozem; typical chernozem; Prydnisterska Upland; GIS-analysis; erosive degradation; slope morphology; relief.
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36

de Ryck, Alain, and Olivier Louisnard. "Depth and minimal slope for surface flows of cohesive granular materials on inclined channels." Journal of Fluid Mechanics 727 (June 19, 2013): 191–235. http://dx.doi.org/10.1017/jfm.2013.246.

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AbstractWe present analytical predictions of the depth and onset slope of the steady surface flow of a cohesive granular material in an inclined channel. The rheology of Jop, Forterre & Pouliquen (Nature, vol. 441, 2006, pp. 727–730) is used, assuming co-axiality between the stress and strain-rate tensors, and a coefficient of friction dependent on the strain rate through the dimensionless inertial number $I$. This rheological law is augmented by a constant stress representing cohesion. Our analysis does not rely on a precise $\mu (I)$ functional, but only on its asymptotic power law in the limit of vanishing strain rates. Assuming a unidirectional flow, the Navier–Stokes equations can be solved explicitly to yield parametric equations of the iso-velocity lines in the plane perpendicular to the flow. Two types of channel walls are considered: rough and smooth, depicting walls whose friction coefficient is respectively larger or smaller than that of the flowing material. The steady flow starts above a critical onset angle and consists of a sheared zone confined between a surface plug flow and a deep dead zone. The details of the flow are discussed, depending on dimensionless parameters relating the static friction coefficient, cohesion strength of the material, incline angle, wall friction, and channel width. The depths of the flow at the centre of the channel and at the walls are calculated by a force balance on the flowing material. The critical angle for the onset of the flow is also calculated, and is found to be strongly dependent on the channel width, in agreement with experimental results on heap stability and in rotating drums. Our results predict the important conclusion that a cohesive material always starts to flow for an incline angle lower than 90° between smooth walls, whereas in a narrow enough channel with rough walls, it may not flow, even if the channel is inclined vertically.
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37

Vöth, Stefan. "Inclined Rope Reeving Systems." E3S Web of Conferences 278 (2021): 01010. http://dx.doi.org/10.1051/e3sconf/202127801010.

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Main part of crane systems in general and hoisting systems especially are rope-reeving systems. They are used to reduce the loading on the rope itself and on the following parts in the hoist drive. In order to transfer the performance required the reduced loading has to be compensated by higher speeds. General standard are reeving systems with just vertical rope orientation. They have advantages, as they are not difficult to plan, to build and to operate. On the other hand, they comprise disadvantages as well. One main disadvantage of vertical rope orientation is the tendency to load sway.
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38

Jia, Ying, Hua Yang, Ping Li, Jiangyan Xiong, and Bo Chen. "Cone beam computed tomography analysis in 3D position of maxillary denture." Open Medicine 12, no. 1 (October 28, 2017): 340–46. http://dx.doi.org/10.1515/med-2017-0049.

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AbstractThe dynamic correlation between teeth and denture morphology as well as the morphological positions needs to be explored.Methodology63 adult patients with skeletal class III malocclusions that met the inclusion criteria were enrolled and imaged with Cone Beam Computed Tomography (CBCT), and Digital Imaging and Communications in Medicine (DICOM) data were collected. The torque angle and axial inclination were measured and analyzed for the corona, root, and entire body of every tooth on the maxilla.ResultsThere is a statistically significant difference between the coronal axial inclination/coronal torque angle for the skeletal class III malocclusion cases and Andrew’s six keys of occlusion. On the sagittal plane of the maxillary denture (except that the secondary molar is inclined medial-distally), the remaining teeth are inclined towards the labia with slightly larger angles compared to the normal occlusion. In the coronal direction, the maxillary anterior teeth tend to have a corona that inclines medial-distally, whereas the posterior teeth have a buccal inclination compared to the normal occlusion.ConclusionSagittal and transversal compensations prevail in maxillary dentures; for the camouflaged treatment design for skeletal class III, there is limited scope of sagittal and transversal movements on the maxillary denture.
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39

Cheng, Hsin Yu, and Yung Chou Kao. "Five-Axis NC Program Conversion for Inclined Plane Machining." Applied Mechanics and Materials 479-480 (December 2013): 333–37. http://dx.doi.org/10.4028/www.scientific.net/amm.479-480.333.

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Machining processes on an inclined plane include mostly hole making, profiling, and pocketing. It comprises of 80% - 90% cutting process in five-axis machining and is therefore very important in multi-axis machining work. However, five-axis machining processes are normally difficult to introduce and to use because five-axis CAD/CAM and post-processor are normally demanded to generate five-axis NC program even though it is for the 2D contour machining on a plane with inclined angle. Therefore, this paper studies the inclined plane machining methods and extends traditional three-axis milling machining processes and methods so as to directly convert 2-1/2 and three-axis NC program into five-axis machining program to ease the application of five-axis machining processes. This study integrates the developed three-axis NC program interpreter, inclined plane coordinates transformation, and post-processor to simply the inclined plane NC programming. Two-dimensional NC program on a plane can be converted into five-axis NC program on the inclined-plane by the proposed methodology. Case study has been utilized to verify the utilization and correctness of the proposed methodology
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40

Thakur, Ruchi, AnandL Shigli, and Gagan Thakur. "An uncommon indication of lower inclined plane." Journal of Dental Research and Scientific Development 1, no. 1 (2014): 24. http://dx.doi.org/10.4103/2348-3407.126137.

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41

Benyettou, M., S. Chouraqui ., and A. Bouadi . "Drop Behavior on an Inclined Solid Plane." Journal of Applied Sciences 5, no. 9 (August 15, 2005): 1690–91. http://dx.doi.org/10.3923/jas.2005.1690.1691.

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42

BALMFORTH, N. J., R. V. CRASTER, and R. SASSI. "Shallow viscoplastic flow on an inclined plane." Journal of Fluid Mechanics 470 (October 31, 2002): 1–29. http://dx.doi.org/10.1017/s0022112002001660.

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Evolving viscoplastic flows upon slopes are an important idealization of many flows in a variety of geophysical situations where yield stress is thought to play a role. For such models, asymptotic expansions suitable for slowly moving shallow fluid layers (lubrication theory) reduce the governing equations to a simpler problem in terms of the fluid thickness. We consider the version of the theory for fluids described by the Herschel–Bulkley constitutive law, and provide a variety of solutions to the reduced equation, both numerical and analytical. For extruded inclined domes, we derive the characteristic temporal behaviour of measures of the dome's dimensions.
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43

Abdulahad, Joseph. "Flow of Soap Films on Inclined Plane." AL-Rafidain Journal of Computer Sciences and Mathematics 7, no. 2 (December 1, 2010): 67–78. http://dx.doi.org/10.33899/csmj.2010.163886.

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44

Greenslade, Thomas B. "Rolling Soup Cans Down an Inclined Plane." Physics Teacher 58, no. 6 (September 2020): 387. http://dx.doi.org/10.1119/10.0001832.

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45

Lee, Joseph H. W., and Valiant W. L. Cheung. "Inclined Plane Buoyant Jet in Stratified Fluid." Journal of Hydraulic Engineering 112, no. 7 (July 1986): 580–89. http://dx.doi.org/10.1061/(asce)0733-9429(1986)112:7(580).

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46

McCall, Richard P. "Variations on the Frictionless Inclined Plane Problem." Physics Teacher 42, no. 4 (April 2004): 212–14. http://dx.doi.org/10.1119/1.1696588.

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47

KITA, Yoshihiro, and Takayuki HAYASHIBE. "Study of Roller Burnishing on inclined plane." Proceedings of Conference of Kansai Branch 2003.78 (2003): _5–17_—_5–18_. http://dx.doi.org/10.1299/jsmekansai.2003.78._5-17_.

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48

Sonar, Prasad, Ishan Sharma, and Jayant Singh. "Granular flow down a flexible inclined plane." EPJ Web of Conferences 140 (2017): 03074. http://dx.doi.org/10.1051/epjconf/201714003074.

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49

Aghamohammadi, Cina, and Amir Aghamohammadi. "Slipping and rolling on an inclined plane." European Journal of Physics 32, no. 4 (June 10, 2011): 1049–57. http://dx.doi.org/10.1088/0143-0807/32/4/017.

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50

Gómez, R. W., J. J. Hernández-Gómez, and V. Marquina. "A jumping cylinder on an inclined plane." European Journal of Physics 33, no. 5 (July 25, 2012): 1359–65. http://dx.doi.org/10.1088/0143-0807/33/5/1359.

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