Author:
Abe Steffen,Deckert Hagen
Abstract
Abstract. We investigate the influence of stress conditions during fracture formation on
the geometry and roughness of fracture surfaces. Rough fracture surfaces have
been generated in numerical simulations of triaxial deformation experiments
using the discrete element method and in a small number of laboratory
experiments on limestone and sandstone samples. Digital surface models of the
rock samples fractured in the laboratory experiments were produced using
high-resolution photogrammetry. The roughness of the surfaces was analyzed in terms
of absolute roughness measures such as an estimated joint roughness
coefficient (JRC) and in terms of its scaling properties. The results show
that all analyzed surfaces are self-affine but with different Hurst exponents
between the numerical models and the real rock samples. Results from numerical
simulations using a wide range of stress conditions to generate the fracture
surfaces show a weak decrease of the Hurst exponents with increasing confining
stress and a larger absolute roughness for transversely isotropic stress
conditions compared to true triaxial conditions. Other than that, our results
suggest that stress conditions have little influence on the surface roughness
of newly formed fractures.
Funder
Bundesministerium für Bildung und Forschung
Subject
Paleontology,Stratigraphy,Earth-Surface Processes,Geochemistry and Petrology,Geology,Geophysics,Soil Science
Cited by
11 articles.
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