4.7 Article

Avalanches, thresholds, and diffusion in mesoscale amorphous plasticity

期刊

PHYSICAL REVIEW E
卷 100, 期 4, 页码 -

出版社

AMER PHYSICAL SOC
DOI: 10.1103/PhysRevE.100.043003

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资金

  1. National Science Foundation [CMMI-1822020, PHY-1748958]
  2. Agence Nationale de la Recherche (ANR Relfi) [ANR-16-CE30-0022]
  3. Agence Nationale de la Recherche (ANR) [ANR-16-CE30-0022] Funding Source: Agence Nationale de la Recherche (ANR)

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We present results on a mesoscale model for amorphous matter in athermal, quasistatic (a-AQS), steady-state shear flow. In particular, we perform a careful analysis of the scaling with the lateral system size L of (i) statistics of individual relaxation events in terms of stress relaxation S, and individual event mean-squared displacement M, and the subsequent load increments Delta gamma, required to initiate the next event; (ii) static properties of the system encoded by x = sigma(y) - sigma, the distance of local stress values from threshold; and (iii) long-time correlations and the emergence of diffusive behavior. For the event statistics, we find that the distribution of S is similar to, but distinct from, the distribution of M. We find a strong correlation between S and M for any particular event, with S similar to M-q with q approximate to 0.65. The exponent q completely determines the scaling exponents for P(M) given those for P(S). For the distribution of local thresholds, we find P(x) is analytic at x = 0, and has a value P(x)vertical bar (x=0) = p(0) which scales with lateral system length as P-0 proportional to L-0.6. The size dependence of the average load increment appears to be asymptotically controlled by the plateau behavior of P(x) rather than by a subsequent apparent power-law behavior. Extreme value statistics arguments lead thus to a scaling relation between the exponents governing P(x) and those governing P(S). Finally, we study the long-time correlations via single-particle tracer statistics. The value of the diffusion coefficient is completely determined by and the scaling properties of P(M) (in particular from < M >) rather than directly from P(S) as one might have naively guessed. Our results (i) further define the a-AQS universality class, (ii) clarify the relation between avalanches of stress relaxation and diffusive behavior, and (iii) clarify the relation between local threshold distributions and event statistics.

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