scholarly journals Planar column collapse of elongated grains

2021 ◽  
Vol 249 ◽  
pp. 06006
Author(s):  
Andrea Jara ◽  
Miguel Cabrera

The granular column collapse is a benchmark configuration for the study of granular flows in dry, saturated, and submerged conditions. The collapse sequence and resultant mobility is acknowledged to be controlled by the column aspect ratio, while grain properties define the relative transition of each stage. Grain shape effects are found to modify the global shear resistance of granular media, with a strong and coupled interaction when interacting with a fluid. In this work, we present the first steps towards the study of grain shape effects in a column collapse when interacting with an ambient fluid. For this purpose, we use a planar configuration and explore the collapse of a column consisting of rod-like grains and study the initial and after collapse grain orientations. On it, the mobilized grains deposit in a preferential horizontal orientation, but further experiments are required to confirm if a nematic configuration can be achieved.

Geophysics ◽  
1984 ◽  
Vol 49 (5) ◽  
pp. 586-587 ◽  
Author(s):  
P. N. Sen

Recently there has been a considerable interest in the effect of anisotropy in the grain shape in the electrical and dielectrical properties of rocks and other inhomogeneous media (Sen 1981a, b; Sen et al, 1981; Mendelson and Cohen, 1982; and Kenyon, 1983). In this note I point out that equation (34) of Mendelson and Cohen (MC) is incorrect. The dc limit of MC equation (34) for the conductivity of rock σ, in terms of porosity ϕ and water conductivity [Formula: see text], gives [Formula: see text] or [Formula: see text] where [Formula: see text] L is the depolarization factor along the principal axis of spheroidal grain and 〈 〉 denotes an average over the distribution in L. This value of [Formula: see text] is in disagreement with the correct value of m in equation (28) of MC [equation (6) below]. [When the sign mistakes in equations MC (33)–(34) are corrected, [Formula: see text]. This agrees with equation (6) below for the case when L has a single value and averaging is redundant.] This inconsistency arises from an incorrect replacement of the inverse of an average in MC equation (33) by an average of inverses. The corrected form of MC equation (33) is [Formula: see text] where ε and [Formula: see text] are the dielectric constants of the mixture and of the matrix, respectively. The dielectric constant [Formula: see text] is complex, [Formula: see text] is real, [Formula: see text] is the permittivity of vacuum, σ the conductivity, ω the angular frequency. The last factor in the right‐hand side of the equation was replaced incorrectly by the average of the inverse, which is incorrect in general. Note that in the dc limit equation (4) above gives [Formula: see text] and, by integration, [Formula: see text] where [Formula: see text] is the dc conductivity of water, σ(0) is the dc conductivity of formation, and [Formula: see text]


1986 ◽  
Vol 34 (11) ◽  
pp. 2139-2149 ◽  
Author(s):  
S. Tiem ◽  
M. Berveiller ◽  
G.R. Canova

1978 ◽  
Vol 86 (2) ◽  
pp. 193-209 ◽  
Author(s):  
P. D. Komar ◽  
C. E. Reimers

2013 ◽  
Vol 102 (1) ◽  
pp. 71-90 ◽  
Author(s):  
T. Torskaya ◽  
V. Shabro ◽  
C. Torres-Verdín ◽  
R. Salazar-Tio ◽  
A. Revil

1980 ◽  
Vol 88 (2) ◽  
pp. 243-245 ◽  
Author(s):  
N. C. Janke

2000 ◽  
Vol 648 ◽  
Author(s):  
Tamara Radetic ◽  
Ulrich Dahmen

AbstractThin films of gold (Au) were grown on single crystal germanium (Ge) or silicon (Si) substrates using physical vapor deposition (PVD). The resulting microstructure was that of a mazed bicrystal in which two equivalent grain orientations, related to each other by a 90° rotation, are arranged in a morphology of irregularly shaped, convoluted grains. Quantitative morphological analysis showed a strong dependence of grain shape on size, with larger grains being more convoluted and smaller grains more compact. The evolution of grain size, anisotropy and shape during heating in the temperature range from 300-340 °C was studied by in-situ transmission electron microscopy (TEM).


2005 ◽  
Vol 14 (3) ◽  
pp. 293-301 ◽  
Author(s):  
N. J. Kidner ◽  
Z. J. Homrighaus ◽  
B. J. Ingram ◽  
T. O. Mason ◽  
E. J. Garboczi

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