56,780 research outputs found

    Kothari, U.

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    Working together to address global problems: Royal Geographical Society (with IBG) Medals and Awards ceremony 2014

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    The Royal Geographical Society (with IBG)’s annual Medals and Awards recognise achievements in researching, communicating and teaching a wide range of geographical knowledge. The speeches and citations are a record of the ceremony of 2014 with comments by Hans Rosling and Professors Geoffrey Boulton, Susan Smith, Uma Kothari and John Dearing. The speeches encompass communicating geographical data, glaciology, environmental change, human geography and global development.<br/

    Localization and instability in sheared granular materials: role of friction and vibration

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    Shear banding and stick-slip instabilities have been long observed in sheared granular materials. Yet, their microscopic underpinnings, interdependencies and variability under different loading conditions have not been fully explored. Here, we use a non-equilibrium thermodynamics model, the Shear Transformation Zone theory, to investigate the dynamics of strain localization and its connection to stability of sliding in sheared, dry, granular materials. We consider frictional and frictionless grains as well as presence and absence of acoustic vibrations. Our results suggest that at low and intermediate strain rates, persistent shear bands develop only in the absence of vibrations. Vibrations tend to fluidize the granular network and de-localize slip at these rates. Stick-slip is only observed for frictional grains and it is confined to the shear band. At high strain rates, stick-slip disappears and the different systems exhibit similar stress-slip response. Changing the vibration intensity, duration or time of application alters the system response and may cause long-lasting rheological changes. We analyse these observations in terms of possible transitions between rate strengthening and rate weakening response facilitated by a competition between shear induced dilation and vibration induced compaction. We discuss the implications of our results on dynamic triggering, quiescence and strength evolution in gouge filled fault zones.Submission published under a 24 month embargo labeled 'U of I Access', the embargo will last until 2019-05-01The student, Konik Kothari, accepted the attached license on 2017-04-25 at 17:58.The student, Konik Kothari, submitted this Thesis for approval on 2017-04-25 at 18:10.This Thesis was approved for publication on 2017-04-26 at 18:28.DSpace SAF Submission Ingestion Package generated from Vireo submission #11071 on 2017-08-10 at 15:07:07Made available in DSpace on 2017-08-10T20:33:26Z (GMT). No. of bitstreams: 3 KOTHARI-THESIS-2017.pdf: 2654936 bytes, checksum: 03da604f37f0d94f5ba83b7593a10549 (MD5) STZ1D.py: 32665 bytes, checksum: 3365b7018559d4e468c1a72fb94323b9 (MD5) LICENSE.txt: 4210 bytes, checksum: 50c534fb605310ff3a22adc8eac2bd3b (MD5) Previous issue date: 2017-04-26Embargo set by: Colleen Fallaw for item 102842 Lift date: 2019-08-10T21:27:21Z Reason: Author requested U of Illinois access only (OA after 2yrs) in Vireo ETD systemU of I Only Restriction Lifted for Item 102842 on 2019-08-11T09:15:17Z

    A Dynamic Subfilter-scale Stress Model for Large Eddy Simulations Based on Physical Flow Scales

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    We propose a new definition of the length scale in an eddy-viscosity model for large-eddy simulations (LES). This formulation extends and generalizes a previous proposal [Piomelli, Rouhi and Geurts, Proc. ETMM10, 2014], in which the LES length scale was expressed in terms of the integral length-scale of turbulence determined by the flow characteristics and explicitly decoupled from the simulation grid; this approach was named Integral Length-Scale Approximation (ILSA). As in the original ILSA, the model coefficient was determined by the user, and required to maintain a desired contribution of the unresolved, subfilter scales (SFS) to the global transport. We propose a local formulation (local ILSA) in which the model coefficient is local in space, allowing a precise control over SFS activity as a function of location. This new formulation preserves the properties of the global model; application to channel flow and backward-facing step verifies its features and accuracy

    Large-eddy simulation of a separated flow with a sub-filter scale model based on the integral length-scale

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    A new sub-filter scale model for large-eddy simulations, which uses a length-scale proportional to the integral scale of the turbulence instead of the grid resolution to parametrize the modelled stresses, will be assessed in the prediction of the flow of a boundary-layer over a rough surface, which includes separation and reattachment

    Near Wall PIV-Measurements on the Windward Slope of a Hill

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    The turbulent flow over periodic hills was measured near to the wall, using planar Particle-Image-Velocimetry (PIV) at high spatial resolution. Our focus is on the near wall turbulence structure on the windward slope of the hill. For large-eddy simulation (LES) we suspect that, if this was not predicted accurately, it affects the prediction of the velocity profiles over the hill crest which in turn will affect the recirculation length downstream of the hill. Regarding the time averaged velocities, we were able to resolve the linear viscous region of the boundary layer. The velocity distribution and also the Reynolds stress does not comply with the law of the wall as it is valid for a turbulent boundary layer at equilibrium
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