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The evolution of the pore space of mudrocks induced by drying shrinkage and effective stresses is of importance to several areas of research. Drying is a prerequisite for most mudrock characterization methods, while effective stresses have a direct impact on mudrocks properties such as permeability, compressibility, and strength. Mercury porosimetry intrusion has been widely utilized to show that drying shrinkage and effective stresses lead to the collapse of large pores only (~> 50 nm), while small pores (~< 50 nm) remain unaffected. However, the validity of mercury porosimetry intrusion-derived pore size distributions is greatly doubted in the literature due to the fact that most pores in mudrocks are not directly accessible to the surrounding mercury. This study follows a different approach by utilizing a suite of methods including imaging by transmission electron microscopy and scanning electron microscopy at cryogenic temperature after high-pressure freezing (cryoSEM), and gravimetric porosity measurements to investigate the influence of volumetric changes on the pore space of mudrocks. Contrary to previously published results, we show that volumetric changes induced by drying and effective stresses lead to the collapse of pores of all sizes. Furthermore, we show that porosity measured from SEM images is dependent on SEM resolution and reveals only a fraction of the actual porosity. These results provide valuable insights used to interpret the results of characterization methods requiring drying and modeling of effective stress influence on the properties of mudrocks.

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