The formation of open-mode discontinuities is a common occurrence in soils. This family of discontinuities includes hydraulic fractures, gas-driven fractures, desiccation cracks, ice and hydrate lenses, and even roots. These discontinuities can be analysed at the particle scale or at the macroscale using constitutive models that are consistent with the effective stress-dependent behaviour of soils. Both analyses show that the medium is in compression everywhere and that growth is intimately related to unloading and expansion ahead of the tip. While these observations appear to be common to the development of all open-mode fractures in soils, there are pronounced invasion differences between miscible fluids and immiscible phases.
INTRODUCTIONThe analysis of open-mode discontinuities in soils, such as hydraulic fractures and desiccation cracks, is typically based on concepts derived from equivalent-continuum fracture mechanics, sometimes adjusted to account for various aspects of soil behaviour. However, this approach fails to recognise the inherent particulate nature of soils. In this context, the concept of fracture formation in a fully fractured medium is not immediately obvious. Furthermore, an effective stress tensile failure is impossible in cohesionless granular materials, and total stress analyses do not contribute physical understanding to the process.The mechanical analysis of open-mode discontinuities leads to an important first distinction pertaining to the miscibility of the invading fluid with the defending fluid that saturates the soil. Except for 'classical' hydraulic fracture, all the following examples refer to an immiscible invading phase (Fig. 1).(a) Fractures driven by the invasion of a miscible fluid ( Fig. 1(a)). This is the case of 'classical' hydraulic fractures in near-surface geotechnical applications, such as dams, where the invading fluid (e.g. water) is miscible with the saturating fluid (e.g. water). In general, these fractures develop normal to the least principal stress unless pronounced stratigraphic features play a dominant role (Bjerrum et al., 1972;Jaworski et al., 1981;de Pater et al., 1994). Fluid leakoff normal to the fracture planes is proportional to the permeability of the medium. (b) Fractures driven by the invasion of an immiscible fluid (Figs 1(b) and 1(c)). Gas invasion into water-saturated sediments or the forced invasion of water into oilsaturated reservoirs may cause open-mode discontinuities. There is no seepage or leak-off of the invading fluid into the formation normal to the fracture faces (end-member case) and the fracture advances normal to the minimum stress direction in homogeneous sediments. (c) Desiccation cracks ( Fig. 1(d) (Fig. 1(e)). The literature on frozen ground and the more recent publications on methane hydrate report extensively on ice and hydrate lenses found in fine-grained sediments. Ice lenses in near-surface frozen ground are temperature controlled and lenses align parallel to the isothermal front rather than normal to the minimum effectiv...