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Wei Wei

Researcher at China University of Geosciences (Wuhan)

Publications -  43
Citations -  1580

Wei Wei is an academic researcher from China University of Geosciences (Wuhan). The author has contributed to research in topics: Fractal & Fractal dimension. The author has an hindex of 14, co-authored 39 publications receiving 1065 citations. Previous affiliations of Wei Wei include Chinese Academy of Sciences & China University of Petroleum.

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Electrical conductivity models in saturated porous media: A review

TL;DR: A review of the electrical conductivity models developed using fractal, percolation and effective medium theories is presented in this paper, where the results obtained by comparing experiential and theoretical models with experiments/simulations are analyzed.
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Fractal characterization of dynamic fracture network extension in porous media

TL;DR: In this article, the authors measured the fractal dimension of fracture network in porous media under drying process by the improved box-counting technique, and fractal dimensions were respectively related to drying time, average aperture, moisture content and fracture porosity.
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An electrical conductivity model for fractal porous media

TL;DR: In this article, a theoretical electrical conductivity equation is derived based on the fractal characteristics of porous media, which is expressed in terms of the tortuosity fractal dimension (DT), the pore fractal dimensions (Df), and the electrical conductivities of pore liquid.
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Recent developments on fractal-based approaches to nanofluids and nanoparticle aggregation

TL;DR: The properties of nanoparticles and its aggregation as well as convective heat transfer of nanofluids have received great attentions over the last few decades as discussed by the authors, and the recent investigations on the fractal models and fractal-based approaches are summarized.
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Shale gas transport model in 3D fractal porous media with variable pore sizes

TL;DR: In this article, a model for gas transport in shale is proposed by accounting for three major fluid flow mechanisms in shale stratum, which is modeled as a 3D fractal media.