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• W2071373230 abstract "The microstructure of sedimentary rocks is studied by small-angle neutron scattering for length scales between 5 and 500 AA{}. In limestones and dolomites, we find that the pore surfaces are effectively smooth above 50 AA{}, but there is evidence for roughening on shorter length scales. In sandstones and shales, the pore surfaces show fractal character due to the presence of clay. The fractal dimension is nonuniversal. We attribute these observations to impurity effects, which can lower the surface tension and maximize the surface area." @default.
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• W2071373230 date "1986-08-04" @default.
• W2071373230 modified "2023-10-18" @default.
• W2071373230 title "Surface Roughening and the Fractal Nature of Rocks" @default.
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• W2071373230 doi "https://doi.org/10.1103/physrevlett.57.637" @default.
• W2071373230 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/10034113" @default.
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