32 research outputs found
The effects of a counter-current interstitial flow on a discharging hourglass
This work experimentally investigates the effects of an interstitial fluid on the discharge of granular material within an hourglass. The experiments include observations of the flow patterns, measurements of the discharge rates, and pressure variations for a range of different fluid viscosities, particle densities and diameters, and hourglass geometries. The results are classified into three regimes: (i) granular flows with negligible interstitial fluid effects; (ii) flows affected by the presence of the interstitial fluid; and (iii) a no-flow region in which particles arch across the orifice and do not discharge. Within the fluid-affected region, the flows were visually classified as lubricated and air-coupled flows, oscillatory flows, channeling flows in which the flow preferentially rises along the sidewalls, and fluidized flows in which the upward flow suspends the particles. The discharge rates depends on the Archimedes number, the ratio of the effective hopper diameter to the particle diameter, and hourglass geometry. The hopper-discharge experiments, as well as experiments found in the literature, demonstrate that the presence of the interstitial fluid is important when the nondimensional ratio (N) of the single-particle terminal velocity to the hopper discharge velocity is less than 10. Flow ceased in all experiments in which the particle diameter was greater than 25% of the effective hopper diameter regardless of the interstitial fluid
Origin of stabilization of macrotwin boundaries in martensites
The origin of stabilization of complex microstructures along macrotwin
boundaries in martensites is explained by comparing two models based on
Ginzburg-Landau theory. The first model incorporates a geometrically nonlinear
strain tensor to ensure that the Landau energy is invariant under rigid body
rotations, while the second model uses a linearized strain tensor under the
assumption that deformations and rotations are small. We show that the
approximation in the second model does not always hold for martensites and that
the experimental observations along macrotwin boundaries can only be reproduced
by the geometrically nonlinear (exact) theory
On the modified nonlinear Schr\"odinger equation in the semiclassical limit: supersonic, subsonic, and transsonic behavior
The purpose of this paper is to present a comparison between the modified
nonlinear Schr\"odinger (MNLS) equation and the focusing and defocusing
variants of the (unmodified) nonlinear Schr\"odinger (NLS) equation in the
semiclassical limit. We describe aspects of the limiting dynamics and discuss
how the nature of the dynamics is evident theoretically through
inverse-scattering and noncommutative steepest descent methods. The main
message is that, depending on initial data, the MNLS equation can behave either
like the defocusing NLS equation, like the focusing NLS equation (in both cases
the analogy is asymptotically accurate in the semiclassical limit when the NLS
equation is posed with appropriately modified initial data), or like an
interesting mixture of the two. In the latter case, we identify a feature of
the dynamics analogous to a sonic line in gas dynamics, a free boundary
separating subsonic flow from supersonic flow.Comment: 30 pages, 2 figures. Submitted to Acta Mathematica Scientia (special
issue in honor of Peter Lax's 85th birthday
Silo Music and Silo Quake: Granular Flow Induced Vibration
Acceleration and sound measurements during granular discharge from silos are
used to show that silo music is a sound resonance produced by silo quake. The
latter is produced by stick-slip friction between the wall and the granular
material in tall narrow silos. For the discharge rates studied, the occurrence
and frequency of flow pulsations are determined primarily by the surface
properties of the granular material and the silo wall. The measurements show
that the pulsating motion of the granular material drives the oscillatory
motion of the silo and the occurrence of silo quake does not require a resonant
interaction between the silo and the granular material.Comment: 16 pages, submitted to Powder Technolog
Solving the Klein-Gordon equation using Fourier spectral methods: A benchmark test for computer performance
The cubic Klein-Gordon equation is a simple but non-trivial partial
differential equation whose numerical solution has the main building blocks
required for the solution of many other partial differential equations. In this
study, the library 2DECOMP&FFT is used in a Fourier spectral scheme to solve
the Klein-Gordon equation and strong scaling of the code is examined on
thirteen different machines for a problem size of 512^3. The results are useful
in assessing likely performance of other parallel fast Fourier transform based
programs for solving partial differential equations. The problem is chosen to
be large enough to solve on a workstation, yet also of interest to solve
quickly on a supercomputer, in particular for parametric studies. Unlike other
high performance computing benchmarks, for this problem size, the time to
solution will not be improved by simply building a bigger supercomputer.Comment: 10 page