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9 March 2015

Weakest-Link Scaling and Extreme Events in Finite-Sized Systems

,
and
1
School of Mineral Resources Engineering, Technical University of Crete, Chania 73100, Greece
2
Department of Applied Science and Technology, Politecnico di Torino, Corso Duca degli Abruzzi 24,10129 Torino, Italy
*
Author to whom correspondence should be addressed.
This article belongs to the Special Issue Entropic Aspects in Statistical Physics of Complex Systems

Abstract

Weakest-link scaling is used in the reliability analysis of complex systems. It is characterized by the extensivity of the hazard function instead of the entropy. The Weibull distribution is the archetypical example of weakest-link scaling, and it describes variables such as the fracture strength of brittle materials, maximal annual rainfall, wind speed and earthquake return times. We investigate two new distributions that exhibit weakest-link scaling, i.e., a Weibull generalization known as the κ-Weibull and a modified gamma probability function that we propose herein. We show that in contrast with the Weibull and the modified gamma, the hazard function of the κ-Weibull is non-extensive, which is a signature of inter-dependence between the links. We also investigate the impact of heterogeneous links, modeled by means of a stochastic Weibull scale parameter, on the observed probability distribution.

1. Introduction

In statistical mechanics, the velocities of non-interacting particles are viewed as random variables that follow the Maxwell–Boltzmann distribution. Quantities of interest are often macroscopic (system) properties, such as the energy or the entropy, that involve averages over many particles. Evaluating these properties involves calculating averages over suitable probability distributions. Randomness is also a factor in the analysis of macroscopic variables. Environmental time series, energy and mineral reserves and earthquakes are just a few examples of phenomena that exhibit stochastic fluctuations. In addition, the lifetimes (times to failure) of various natural and engineered materials and devices are also random variables. In contrast with statistical mechanics, there is a strong interest not only in average quantities, but also in the extreme values of such distributions [1]. The classical extreme value theory studies the probability distributions of extreme events [2,3]. The Fisher–Tippet–Gnedenko theorem shows that the distribution of suitably-scaled transformations of the maxima or minima of a collection of independent and identically distributed (i.i.d.) variables follows the generalized extreme value (GEV) distributions, which include the Gumbel, Weibull and Fréchet distributions. The type of GEV obtained depends on the tail behavior of the probability distribution for the i.i.d. random variables. Extensions that involve stochastic scalings have been recently proposed in [4].
We investigate systems that obey the weakest-link scaling (WLS) principle. In the WLS framework, the system response (e.g., material strength) is controlled by the weakest link (unit), which implies a marked deviation from statistical independence. The Weibull model [3] is the archetypical probability distribution for WLS systems and is widely used in reliability modeling [5]. It finds application as a model of the fracture strength of brittle and quasi-brittle technological materials [6,7] and geologic media [8], waiting times between earthquakes [915], wind speed [16] and annual hydrological maxima [17]. We study the impact of the randomness (heterogeneity) of the Weibull link parameters on the system survival function by introducing doubly-stochastic representations analogous to superstatistics [18]. We also investigate weakest-link scaling with non-exponential link survival functions. In this context, we introduce a modified gamma distribution, and we provide theoretical arguments for the κ-Weibull distribution, which exhibits power-law tails in finite-sized systems.

1.1. Mathematical Preliminaries

We will use the capital letter X to denote a random variable (e.g., tensile strength, wind speed, earthquake return time, maximum annual rainfall or river discharge) and the lowercase x to denote values of the random variable, where x ∈ [0, ). We will assume that the random variable represents the property of interest for a particular spatial or temporal window (support), the size of which we will denote by . The probability density function (pdf) will be denoted by f(x). It is customary to use fX(x) to denote the pdf of X when more than one random variable is involved. In this case, however, there is no risk of confusion, and thus, we replace X with the support scale, which is relevant in our analysis. The integral of the pdf, i.e., the cumulative distribution function (cdf), will be denoted by:
F ( x ) = x d x f ( x ) .
Another useful probability function, which is mostly used in reliability analysis, is the survival function or complementary cumulative distribution function, defined by:
R ( x ) = 1 F ( x ) .
The survival function R(x) gives the probability that the system has not “failed” when the variable X has reached the level x. The survival function is equal to one for x = xmin and tends to zero for x → ∞. A characteristic property of the survival function is that its integral equals the expectation of X, i.e.,
E [ X ] = 0 d x R ( x ) .
The above is based on dR(x)/dx = −f(x), which follows from (1) and integration by parts.
  • In the case of fracture strength, R(x) is the probability that the system has not failed if the external load takes values that do not exceed x.
  • In the case of earthquake return times, the survival function is the probability that there are no successive earthquakes separated by a time interval less than or equal to x.
  • In the case of annual rainfall maxima, R(x) gives the probability that the maximum rainfall over the support area for the duration of one year does not exceed the value x.
Finally, the hazard rate or hazard function h(x) is the conditional probability that the system will fail at time x* > x within the infinitesimal time window x < x* ≤ x + δx, given that the system has not failed during the interval [0, x]. Let A denote the event that the system has not failed at x and B the event that the system fails at x < x* ≤ x + δx. Then, h(x) = Prob(B|A) = Prob(B A)/Prob(A), which leads to the following:
h ( x ) = Prob ( x < x x + δ x ) R ( x ) δ x = f ( x ) R ( x ) .
The asymptotic dependence of the hazard rate is a matter of interest. For example, in the case of earthquakes, it is often desired to estimate the probability of the time until the next big earthquake. If the particular hazard rate tends to infinity as x → ∞, the probability that an earthquake will occur increases with the time elapsed since the last earthquake [19]. In contrast, a decreasing or constant hazard rate indicates that the probability of a new occurrence is reduced or remains constant, respectively, as time elapses, and no event takes place.

5. Finite-Sized System with κ-Weibull Distribution

5.1. The κ-exponential and κ-logarithm Functions

The definition of the κ-exponential function for κ ≥ 0 is given by [3135]:
exp κ ( z ) = ( 1 + z 2 κ 2 + z κ ) 1 / κ .
The κ-exponential tends asymptotically to the standard exponential at the limits z → 0 or κ → 0, i.e.,
exp κ ( z ) z 0 exp ( z ) ,
exp κ ( z ) κ 0 exp ( z ) .
The inverse function of the κ-exponential is the κ-logarithm, which is defined by:
ln κ ( z ) = z κ z κ 2 κ .

5.2. The κ-Weibull Function

If κ = 1/N, where N is the number of links in a system, we can define a system survival function based on:
R N ( x ) = exp κ [ ( x x s ) m ] .
The κ-Weibull admits explicit expressions for the cdf, the survival function and the pdf, which are given respectively by the following expressions:
F κ ( x ) = 1 exp κ ( [ x / x s ] m ) ,
R κ ( x ) = exp κ ( [ x / x s ] m ) ,
f κ ( x ) = m x s ( x x s ) m 1 exp κ ( [ x / x s ] m ) 1 + κ 2 ( x / x s ) 2 m .
The κ-Weibull hazard function is obtained from (31) using (37) and (38) as follows:
h κ ( x ) = m x s ( x / x s ) m 1 1 + κ 2 ( x / x s ) 2 m .
The κ-Weibull quantile function is defined by means of the survival function as follows:
T κ ( R κ ) = 1 x s [ ln κ ( 1 R κ ) ] 1 / m .

5.3. Motivation and Properties

The κ-Weibull is motivated by the non-exponential link ansatz discussed in Section 3.2. In particular, we assume that ϕ(x) is the following monotonically increasing function with link-size dependence:
ϕ ( x ) = 1 N ( x / x s ) m .
Then, the link survival function is given according to (20) by the function:
R 0 ( x ) = 1 + 1 N 2 ( x x s ) 2 m 1 N ( x x s ) m .
The κ-Weibull system survival function (35) is then obtained from the above link survival function and the WLS principle (5).
Based on the properties of the κ-exponential, the survival function (35) corresponds to an extension of the Weibull survival function. The term κ-Weibull is due to the presence of the κ-exponential. This distribution has been used in economics to model the distribution of income [32,34] and in statistical physics as a model of earthquake recurrence times [27]. Other potential applications include the fracture strength of quasi-brittle materials, which exhibit deviations from Weibull scaling [7,28], and reliability models that involve the Pareto distribution.
The κ-exponential function can describe heavy-tailed processes, because for κ > 0, it decays asymptotically as a power-law function, i.e.,
exp κ ( z ) z ± | 2 κ z | ± 1 / κ .
The κ-Weibull pdf also exhibits a power-law tail, which is inherited by the κ-exponential and is relevant in applications where such heavy tails are observed. In addition, if we define the κ-Weibull plot by means of the function Φ′κ(x) = ln lnκ(1/Rκ(x)), it follows that Φ′κ(x) = m ln (x/xs). Hence, Φ′κ(x) is independent of κ and regains the logarithmic scaling of the double logarithm of the inverse survival function. This means that the κ-Weibull plot, in which Φ′κ(x) is plotted instead of Φκ(x), can be used to visually detect the κ-Weibull scaling.
Plots of the κ-Weibull pdf for xs = 1 and two values of m (m < 1 and m > 1) are shown in Figure 7. The plots also include the Weibull pdf (κ = 0) for comparison. For both m, lower N lead to a heavier right tail. For m = 2.5 the mode of the pdf moves to the right as N increases (for m = 0.7 the mode is at zero independently of N, since the distribution is zero-modal for m ≤ 1) [34]. To the right of the mode, higher N correspond, at first, to higher pdf values. This is reversed at a crossover point beyond which the lower-N pdfs exhibit slower power-law decay, i.e., limx→∞ fκ(x) ∝ x−α, where α = 1 + m/κ [34]. The crossover point occurs at 1.5xs for m = 2.5, whereas for m = 0.7 at 5 xs.
Figure 7. Semi-logarithmic plots of κ-Weibull pdfs for xs = 1, different values of N (shown by different line types), and Weibull modulus equal to (a) m = 2.5 (b) m = 0.7.

6. Conclusions

We investigated the statistical implications of the principle of weakest-link scaling. This type of scaling is used to model the probability distributions of extreme events, including the failure strength of various heterogeneous materials, wind speed, earthquake recurrence times and hydrological maxima. We have focused on various statistical mechanisms leading to deviations from the Weibull distribution, which is commonly used in weakest-link scaling systems. Our motivation stems from empirical distributions that deviate from the Weibull in physical systems expected to follow weakest-link scaling, e.g., [7,15,27,28,36]. Our results include a modified gamma distribution, the κ-Weibull distribution and weakest-link scaling distributions with non-homogeneous links that have random (possibly correlated) parameters. The distributions proposed above modify the tail behavior in comparison with the classical Weibull dependence. We thus believe that they are of interest to both statistical physicists and reliability or systems engineers.
The modified gamma distribution, which we introduce herein, is derived by applying weakest-link scaling to systems with a finite number of links. The modified gamma distribution has a heavier tail than the respective Weibull for m > 1 and a lighter tail for m < 1. The κ-Weibull distribution is also shown to follow from weakest-link scaling. A notable property of the κ-Weibull distribution is its ability to exhibit a power-law tail, whereas the modified gamma distribution is dominated by exponential decay at large values. The power-law dependence of the κ-Weibull is derived from the interaction between the system and the links, expressed in terms of a finite-valued scaling factor N in the link survival function. For N, the κ-Weibull tends to the Weibull model, and the power-law decay at x ≫ 1 is replaced by the exponential Weibull dependence. We have argued in [27] that the κ-Weibull distribution can be observed in the case of earthquake recurrence times if the monitored area comprises a finite number of faults. We have also linked the number of effective units in this system to the inverse of κ. This type of behavior can also be observed if the system under study does not include all of the units (e.g., faults) of an interdependent system. In this case, events that are outside the boundaries of the observed system are not taken into account, thus leading to longer recurrence times, which generate the power-law tail. The heavy tail of the κ-Weibull may also find applications in biology, e.g., in modeling the inter-spike interval distributions of cortical neurons, which is known to follow a power law [37].
We have also proposed a different approach for inserting correlations in weakest-link scaling systems by means of a variable scaling factor in the link survival function. If this factor is random (but possibly correlated between links), the observed random variable X is described by an appropriate superstatistics formulation. In the case of Weibull link scaling, we have shown that if the scale parameter is uniformly distributed and uncorrelated across links, the observable probability distribution is controlled by three factors: the width of the scale parameter distribution, the Weibull modulus and the mixing ratio, which determines the balance between the number of links and the values contributed by each link to the observed sample. In the limit of a very large sample, it is also shown that the system’s survival function regains the Weibull form, albeit with a renormalized scale, provided that the distribution of the scale parameter has a compact support. In further research, we will investigate the impact of correlations between link distribution parameters on the observed system survival function, as well as applications of this formalism to environmental extreme events that exhibit weakest-link scaling.
Another extreme value distribution that fits within the weak-scaling formalism is the Gumbel distribution [38]. The Gumbel distribution is of the general form F (x) = exp(− exp(−x)) and belongs to the family of generalized extreme value distributions. The Gumbel is characterized by a different mathematical expression and size scaling than the Weibull distribution. There is both theoretical and experimental evidence (e.g., in the fracture of brittle ceramics) that in certain cases, the Gumbel is a more suitable asymptotic form than the Weibull [22,38]. One may therefore wonder if the same arguments that led to the κ-Weibull distribution also apply to the Gumbel distribution. At this point, however, we lack insight into how this construction should be implemented. Hence, we will leave this as an open subject for future research.
PACS classifications: 02.50.-r; 02.50.Ey; 02.60.Ed; 89.20.-a; 89.60.-k

Author Contributions

All authors contributed to the research and the writing. All authors have read and approved the final manuscript.

Conflicts of Interest

The authors declare no conflict of interest.

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