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Detailed Reference Information |
Meerschaert, M.M., Kozubowski, T.J., Molz, F.J. and Lu, S. (2004). Fractional Laplace model for hydraulic conductivity. Geophysical Research Letters 31: doi: 10.1029/2003GL019320. issn: 0094-8276. |
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Based on an examination of K data from four different sites, a new stochastic fractal model, fractional Laplace motion, is proposed. This model is based on the assumption of spatially stationary ln(K) increments governed by the Laplace PDF, with the increments named fractional Laplace noise. Similar behavior has been reported for other increment processes (often called fluctuations) in the fields of finance and turbulence. The Laplace PDF serves as the basis for a stochastic fractal as a result of the geometric central limit theorem. All Laplace processes reduce to their Gaussian analogs for sufficiently large lags, which may explain the apparent contradiction between large-scale models based on fractional Brownian motion and non-Gaussian behavior on smaller scales. |
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Abstract |
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Keywords
Hydrology, Groundwater hydrology, Hydrology, Stochastic processes, Mathematical Geophysics, Fractals and multifractals |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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