“…However, they typically yield under a modest stress, often including the gravitational stress exerted by their own weight. It is therefore not surprising that many studies have been devoted to the sedimentation behavior of colloidal gels, revealing a wealth of fascinating but yet not fully understood phenomena, such as delayed sedimentation [4,5,6,7,8], creep [4,9,10,11,12], and fracture associated with complex flow patterns [4,9,13]. With a few notable exceptions [4,6,8], most previous work has focussed on the macroscopic behavior of the gels, typically by measuring the time evolution of the gel height, h(t).…”