After an introduction describing the indentation techniques traditionally applied to the study of micromechanical properties of minerals and rocks, phenomena induced by the diamond tip's penetration into crystalline rocks are analyzed. Crystalline rocks are characterized by low values of the critical breakage load, i.e. the threshold load corresponding to the transition from a ductile to a brittle behavior. As a consequence, it seems more convenient to examine the mechanical behavior of crystalline rocks by using instrumented nanoindentations. Above the critical load, ranging from rock to rock, fractures occur, affecting the indentation results and thus invalidating the values of the rock mechanical properties obtained by indentation data processing. In order to determine the correct values of the hardness and elastic modulus of brittle rocks, an innovative measurement modality for rocks, i.e. Continuous Stiffness Measurement mode, is proposed. By providing the continuous evolution of the hardness and of the elastic modulus as a function of the indentation depth, it has proven particularly suited to analyze the effects of induced fracturing on the load versus displacement curve.
IntroductionCrystalline rocks consist of crystals of the same mineral or of aggregates of several mineral grains and contain discontinuities of different nature. Simmons and Richter (1976) and Kranz (1983) classified such microdiscontinuities into four types:• grain boundaries (following the contacts between the grains); • intergranular (intersecting grain boundaries);• multigranular (the longest cracks, crossing several grains and their boundaries).At the scale of the laboratory specimen, crystalline rocks are considered mostly continuous and homogeneous media and, when there is a marked iso-orientation of the grains, anisotropic. For a detailed analysis at the microscopic scale, they are revealed as discontinuous solids, affected by a dense network of cracks and grain boundary cavities. Figure 1 shows some examples of microdiscontinuities in a granite's sample. More generally, the discontinuous nature and heterogeneity of rocks at the grain scale are well described in Blair andCook (1998) andin Lan et al. (2010).Depending on their distribution, nature and statistically prevailing orientation more than grains iso-orientation, the defects affect the rock's mechanical behavior at a varying extent.The microdiscontinuities are surfaces along which the failure processes of the rock samples under critical state of stresses originate (Tapponnier and Brace 1976;Kranz 1979;Wong 1982). Consequently, to properly understand the mechanisms leading to the rock's macroscopic failure, analyses should be performed even at the micro and nanoscale (discontinuities scale), where the failure begins.The micro and nano scale analysis on the rock's mechanical response highlights the clear influence of the above mentioned discontinuities on the indentations performed with the different methods available today. Indeed, unlikely the observations in metals...