“…Soil scientists rapidly seized that opportunity (e.g., Jongerius et al, 1972;Murphy et al, 1977a,b). They continued to do so in the 1980s (e.g., Ringrose-Voase and Bullock, 1984), after the development of personal computers, and particularly in the 1990s, as inexpensive scanners, digital cameras, and versatile image manipulation software made it increasingly straightforward to acquire images and to analyze them (often with the help of fractal geometry), for a variety of purposes (e.g., Hallaire and Cointepas, 1993;Bielders et al, 1996;Deleporte et al, 1997;DeLeo et al, 1997;Beaudet-Vidal et al, 1998;Baveye, 2002;Ohrstrom et al, 2002;Dathe and Baveye, 2003;Ohrstrom et al, 2004;Morris and Mooney, 2004;Pendleton et al, 2005;Persson et al, 2005;Wantanaphong et al, 2006;Lipsius and Mooney, 2006;Vogel et al, 2006;Otten and Gilligan, 2006;Jacobson et al, 2007;Marcelino et al, 2007;Mooney and Morris, 2008;Papadopoulos et al, 2008;Persson and Olsson, 2008;Tarquis et al, 2008). In recent years, synchrotronbased X-ray computed tomography (CT) and table-top X-ray micro-CT scanners have allowed researchers to visualize in 3 dimensions the structure and composition of soils at micrometric resolutions, and have enabled significant advances to be made in our understanding of the functioning of soils at previously unexplored spatial scales (e.g., Garnier et al, 1998;Baveye et al, 2002;Elliot and Heck, 2007a,b;Sleutel et al, 2008).…”