807 resultados para Sliding friction


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Studio della caratterizzazione micromeccanica di provini in alluminio 6082 T6 saldati con la tecnica della rotary friction welding, tecnica innovativa nell’ambito delle tecnologie di giunzione solida, che sfrutta il principio della saldatura per attrito. Dopo un'introduzione teorica sulle principali tematiche affrontate e sui principali sistemi di misura usati, verranno effettuate micrografie dei giunti e prove di microdurezza sugli stessi. Si termina riportando i grafici delle microdurezze trovate, in modo da poter confrontare i risultati ottenuti con le caratteristiche del materiale base. Da questi si osserva che: nonostante la qualità accettabile dei giunti, le elevate temperature raggiunte durante la saldatura hanno alterato il trattamento termico del materiale base, che da T6 assume caratteristiche più simili a un T4. In altre parole il materiale saldato presenta caratteristiche micromeccaniche inferiori a quelle nominalmente assegnabili al materiale base.

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Il presente lavoro di tesi si pone come obiettivo la caratterizzazione microstrutturale di una serie di giunti realizzati tramite un innovativo processo di saldatura allo stato solido denominato Rotary Friction Welding. In tale ricerca si descrive il percorso seguito per arrivare a tale caratterizzazione partendo da una discussione delle principali tecniche di saldatura, in particolare quelle per attrito, per passare poi ad un’analisi dettagliata della fase di creazione dei giunti saldati e della successiva fase dedicata alla verifica microstrutturale. I risultati ottenuti, ci forniranno indici di confronto sulla qualità del materiale, sui processi tecnologici, sui trattamenti e su alcune fondamentali proprietà meccaniche

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Nel seguente elaborato si propone lo sviluppo di un modello agli elementi finiti (FEM) del processo di friction welding del quale, attraverso i dati rilevati da prove sperimentali di validazione termica, vengono valutati i parametri ottimali di simulazione. Ai risultati così ottenuti vengono applicati anche algoritmi per la valutazione della microstruttura e della qualità della saldatura, sviluppati originariamente per l'analisi dell'estrusione: in entrambi i casi a seguito del confronto con le analisi metallografiche dei provini è stato possibile validare ulteriormente il modello creato.

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The Scilla rock avalanche occurred on 6 February 1783 along the coast of the Calabria region (southern Italy), close to the Messina Strait. It was triggered by a mainshock of the Terremoto delle Calabrie seismic sequence, and it induced a tsunami wave responsible for more than 1500 casualties along the neighboring Marina Grande beach. The main goal of this work is the application of semi-analtycal and numerical models to simulate this event. The first one is a MATLAB code expressly created for this work that solves the equations of motion for sliding particles on a two-dimensional surface through a fourth-order Runge-Kutta method. The second one is a code developed by the Tsunami Research Team of the Department of Physics and Astronomy (DIFA) of the Bologna University that describes a slide as a chain of blocks able to interact while sliding down over a slope and adopts a Lagrangian point of view. A wide description of landslide phenomena and in particular of landslides induced by earthquakes and with tsunamigenic potential is proposed in the first part of the work. Subsequently, the physical and mathematical background is presented; in particular, a detailed study on derivatives discratization is provided. Later on, a description of the dynamics of a point-mass sliding on a surface is proposed together with several applications of numerical and analytical models over ideal topographies. In the last part, the dynamics of points sliding on a surface and interacting with each other is proposed. Similarly, different application on an ideal topography are shown. Finally, the applications on the 1783 Scilla event are shown and discussed.

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The main objective of this project is to experimentally demonstrate geometrical nonlinear phenomena due to large displacements during resonant vibration of composite materials and to explain the problem associated with fatigue prediction at resonant conditions. Three different composite blades to be tested were designed and manufactured, being their difference in the composite layup (i.e. unidirectional, cross-ply, and angle-ply layups). Manual envelope bagging technique is explained as applied to the actual manufacturing of the components; problems encountered and their solutions are detailed. Forced response tests of the first flexural, first torsional, and second flexural modes were performed by means of a uniquely contactless excitation system which induced vibration by using a pulsed airflow. Vibration intensity was acquired by means of Polytec LDV system. The first flexural mode is found to be completely linear irrespective of the vibration amplitude. The first torsional mode exhibits a general nonlinear softening behaviour which is interestingly coupled with a hardening behaviour for the unidirectional layup. The second flexural mode has a hardening nonlinear behaviour for either the unidirectional and angle-ply blade, whereas it is slightly softening for the cross-ply layup. By using the same equipment as that used for forced response analyses, free decay tests were performed at different airflow intensities. Discrete Fourier Trasform over the entire decay and Sliding DFT were computed so as to visualise the presence of nonlinear superharmonics in the decay signal and when they were damped out from the vibration over the decay time. Linear modes exhibit an exponential decay, while nonlinearities are associated with a dry-friction damping phenomenon which tends to increase with increasing amplitude. Damping ratio is derived from logarithmic decrement for the exponential branch of the decay.

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Costruzione di un modello numerico base per la simulazione del processo Rotary Friction Welding.

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High resolution friction force maps of the benzylammonium terminated crystalline surface of a layer compound are presented. The lateral force map acquired with an atomic force microscope, reveals a significant contrast between different molecular orientations yielding molecular rows which differ from their neighboring ones. The single crystals are formed by stacks of copper oxalate sheets sandwiched between stereoregular organic cations, resulting in highly organized surface structures. Single molecular defects are observed at small loads. The experimental results are compared with numerical calculations which indicate a transition from an unperturbed state at small loads to a distorted state at higher loads. (C) 2011 American Institute of Physics.

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Los sistemas de brackets de baja fricción reducen la fricción en comparación con los convencionales. La fricción se define como la fuerza resistencia entre dos objetos en movimiento que entran en contacto. Junto con la fijación (binding) y la muesca (notching), la fricción es responsable de la resistencia de deslizamiento que se observa en ortodoncia en las etapas de alineado, nivelado y cierre de espacios. Se ha establecido que la alta fricción puede impedir que se alcancen los niveles fuerza óptima para los tejidos de soporte. Los estudios de laboratorio revelan que la fricción es menor en los sistemas de brackets de baja fricción y en los que han sido diseñados de forma correcta, la fijación es más importante en cuanto a la resistencia de deslizamiento. Los estudios clínicos apoyan la idea de que la resistencia de deslizamiento es la misma en brackets de baja fricción y en los convencionales. Además, aseguran que la fricción tiene poca influencia en el ambiente clínico. Una revisión sistemática de estudios clínicos supervisados concluye que existe poca evidencia confiable que apoye el uso de los sistemas fijos de brackets de baja fricción sobre los aparatos convencionales o viceversa. A la luz de la evidencia existente, la reducción en la fricción producida por sistemas de brackets de baja fricción no muestra ventaja clínica.

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Permeability measured on three samples in a triaxial cell under effective confining pressure from 0.2 to 2.5 MPa ranges from 10**-18 to 10**-19 m**2. Overall, results indicate that permeability decreases with effective confining pressure up to 1.5 MPa; however, measurements at low effective pressure are too dispersed to yield a precise general relationship between permeability and pressure. When the effective pressure is increased from 1.5 to 2.5 MPa, permeability is roughly constant (~1-4 x 10**-19 m**2). Samples deformed in the triaxial cell developed slickenlined fractures, and permeability measurements were performed before and after failure. A permeability increase is observed when the sample fails under low effective confining pressure (0.2 MPa), but not under effective pressure corresponding to the overburden stress. Under isotropic stress conditions, permeability decrease related to fracture closure occurs at a relatively high effective pressure of ~1.5 MPa. Coefficients of friction on the fractures formed in the triaxial cell are ~0.4.

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Slowslip forms part of the spectrum of fault behaviour between stable creep and destructive earthquakes. Slow slip occurs near the boundaries of large earthquake rupture zones and may sometimes trigger fast earthquakes. It is thought to occur in faults comprised of rocks that strengthen under fast slip rates, preventing rupture as a normal earthquake, or on faults that have elevated pore-fluid pressures. However, the processes that control slow rupture and the relationship between slow and normal earthquakes are enigmatic. Here we use laboratory experiments to simulate faulting in natural rock samples taken from shallow parts of the Nankai subduction zone, Japan, where very low-frequency earthquakes - a form of slow slip - have been observed.We find that the fault rocks exhibit decreasing strength over millimetre-scale slip distances rather than weakening due to increasing velocity. However, the sizes of the slip nucleation patches in our laboratory simulations are similar to those expected for the very lowfrequency earthquakes observed in Nankai. We therefore suggest that this type of fault-weakening behaviour may generate slow earthquakes. Owing to the similarity between the expected behaviour of slow earthquakes based on our data, and that of normal earthquakes during nucleation, we suggest that some types of slow slip may represent prematurely arrested earthquakes.