51 research outputs found
Spatial scaling in fracture propagation in dilute systems
The geometry of fracture patterns in a dilute elastic network is explored
using molecular dynamics simulation. The network in two dimensions is subjected
to a uniform strain which drives the fracture to develop by the growth and
coalescence of the vacancy clusters in the network. For strong dilution, it has
been shown earlier that there exists a characteristic time at which a
dynamical transition occurs with a power law divergence (with the exponent )
of the average cluster size. Close to , the growth of the clusters is
scale-invariant in time and satisfies a dynamical scaling law. This paper shows
that the cluster growth near also exhibits spatial scaling in addition to
the temporal scaling. As fracture develops with time, the connectivity length
of the clusters increses and diverges at as , with . As a result of the scale-invariant
growth, the vacancy clusters attain a fractal structure at with an
effective dimensionality . These values are independent
(within the limit of statistical error) of the concentration (provided it is
sufficiently high) with which the network is diluted to begin with. Moreover,
the values are very different from the corresponding values in qualitatively
similar phenomena suggesting a different universality class of the problem. The
values of and supports the scaling relation with the
value of obtained before.Comment: A single ps file (6 figures included), 12 pages, to appear in Physica
Self-Similar Law of Energy Release before Materials Fracture
A general law of energy release is derived for stressed heterogeneous
materials, being valid from the starting moment of loading till the moment of
materials fracture. This law is obtained by employing the extrapolation
technique of the self-similar approximation theory. Experiments are
accomplished measuring the energy release for industrial composite samples. The
derived analytical law is confronted with these experimental data as well as
with the known experimental data for other materials.Comment: Latex, 15 pages, no figure
New model for surface fracture induced by dynamical stress
We introduce a model where an isotropic, dynamically-imposed stress induces
fracture in a thin film. Using molecular dynamics simulations, we study how the
integrated fragment distribution function depends on the rate of change and
magnitude of the imposed stress, as well as on temperature. A mean-field
argument shows that the system becomes unstable for a critical value of the
stress. We find a striking invariance of the distribution of fragments for
fixed ratio of temperature and rate of change of the stress; the interval over
which this invariance holds is determined by the force fluctuations at the
critical value of the stress.Comment: Revtex, 4 pages, 4 figures available upon reques
Slider-Block Friction Model for Landslides: Application to Vaiont and La Clapiere Landslides
Accelerating displacements preceding some catastrophic landslides have been
found empirically to follow a time-to-failure power law, corresponding to a
finite-time singularity of the velocity [{\it Voight},
1988]. Here, we provide a physical basis for this phenomenological law based on
a slider-block model using a state and velocity dependent friction law
established in the laboratory and used to model earthquake friction. This
physical model accounts for and generalizes Voight's observation: depending on
the ratio of two parameters of the rate and state friction law and on the
initial frictional state of the sliding surfaces characterized by a reduced
parameter , four possible regimes are found. Two regimes can account for
an acceleration of the displacement. We use the slider-block friction model to
analyze quantitatively the displacement and velocity data preceding two
landslides, Vaiont and La Clapi\`ere. The Vaiont landslide was the catastrophic
culmination of an accelerated slope velocity. La Clapi\`ere landslide was
characterized by a peak of slope acceleration that followed decades of ongoing
accelerating displacements, succeeded by a restabilizing phase. Our inversion
of the slider-block model on these data sets shows good fits and suggest to
classify the Vaiont (respectively La Clapi\`ere) landslide as belonging to the
velocity weakening unstable (respectively strengthening stable) sliding regime.Comment: shortened by focusing of the frictional model, Latex document with
AGU style file of 14 pages + 11 figures (1 jpeg photo of figure 6 given
separately) + 1 tabl
Oscillatory Finite-Time Singularities in Finance, Population and Rupture
We present a simple two-dimensional dynamical system where two nonlinear
terms, exerting respectively positive feedback and reversal, compete to create
a singularity in finite time decorated by accelerating oscillations. The power
law singularity results from the increasing growth rate. The oscillations
result from the restoring mechanism. As a function of the order of the
nonlinearity of the growth rate and of the restoring term, a rich variety of
behavior is documented analytically and numerically. The dynamical behavior is
traced back fundamentally to the self-similar spiral structure of trajectories
in phase space unfolding around an unstable spiral point at the origin. The
interplay between the restoring mechanism and the nonlinear growth rate leads
to approximately log-periodic oscillations with remarkable scaling properties.
Three domains of applications are discussed: (1) the stock market with a
competition between nonlinear trend-followers and nonlinear value investors;
(2) the world human population with a competition between a
population-dependent growth rate and a nonlinear dependence on a finite
carrying capacity; (3) the failure of a material subjected to a time-varying
stress with a competition between positive geometrical feedback on the damage
variable and nonlinear healing.Comment: Latex document of 59 pages including 20 eps figure
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