Anomalous diffusion as modeled by a nonstationary extension of Brownian motion
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作者:
Cushman, John H.
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Purdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA
Purdue Univ, Dept Math, W Lafayette, IN 47907 USAPurdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA
Cushman, John H.
[1
,2
]
O'Malley, Daniel
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Purdue Univ, Dept Math, W Lafayette, IN 47907 USAPurdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA
O'Malley, Daniel
[2
]
Park, Moongyu
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Univ Alabama, Dept Math, Huntsville, AL 35899 USAPurdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA
Park, Moongyu
[3
]
机构:
[1] Purdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA
[2] Purdue Univ, Dept Math, W Lafayette, IN 47907 USA
[3] Univ Alabama, Dept Math, Huntsville, AL 35899 USA
If the mean-square displacement of a stochastic process is proportional to t(beta), beta not equal 1, then it is said to be anomalous. We construct a family of Markovian stochastic processes with independent nonstationary increments and arbitrary but a priori specified mean-square displacement. We label the family as an extended Brownian motion and show that they satisfy a Langevin equation with time-dependent diffusion coefficient. If the time derivative of the variance of the process is homogeneous, then by computing the fractal dimension it can be shown that the complexity of the family is the same as that of the Brownian motion. For two particles initially separated by a distance x, the finite-size Lyapunov exponent (FSLE) measures the average rate of exponential separation to a distance ax. An analytical expression is developed for the FSLEs of the extended Brownian processes and numerical examples presented. The explicit construction of these processes illustrates that contrary to what has been stated in the literature, a power-law mean-square displacement is not necessarily related to a breakdown in the classical central limit theorem (CLT) caused by, for example, correlation (fractional Brownian motion or correlated continuous-time random-walk schemes) or infinite variance (Levy motion). The classical CLT, coupled with nonstationary increments, can and often does give rise to power-law moments such as the mean-square displacement.