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Developing new in-situ approaches to characterize the hydraulic properties of discontinuities in a rock mass, ranging from individual fractures to complex fracture networks, is essential to improve our understanding of flow and transport processes in heterogeneous media and to further develop our ability to accurately model flow, solute and heat transport therein. Likewise, characterizing the nature and degree of hydraulic connection between intersecting fractures – where the bulk of fluid flow, mass and energy transport is generally constrained to a limited number of preferential flow paths – remains to date a difficult task to perform in the field, leaving therefore significant uncertainty in delineating the geometrical arrangement of such flow paths.

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Joint-analysis of single and cross-borehole hydraulic pressure transients to characterize the hydraulic properties and connectivity of fractured networks