Dynamic particle-scale numerical simulations are used to show that the shear thickening observed in dense colloidal, or Brownian, suspensions is of a similar nature to that observed in noncolloidal suspensions, i.e., a stress-induced transition from a flow of lubricated near-contacting particles to a flow of a frictionally contacting network of particles. Abrupt (or discontinuous) shear thickening is found to be a geometric rather than hydrodynamic phenomenon; it stems from the strong sensitivity of the jamming volume fraction to the nature of contact forces between suspended particles. The thickening obtained in a colloidal suspension of purely hard frictional spheres is qualitatively similar to experimental observations. However, the agreement cannot be made quantitative with only hydrodynamics, frictional contacts, and Brownian forces. Therefore, the role of a short-range repulsive potential mimicking the stabilization of actual suspensions on the thickening is studied. The effects of Brownian and repulsive forces on the onset stress can be combined in an additive manner. The simulations including Brownian and stabilizing forces show excellent agreement with experimental data for the viscosity η and the second normal stress difference N 2 .soft matter | colloidal suspensions | shear thickening | rheology | jamming T he rheology of dense suspensions is of considerable theoretical and technological importance, yet the shear rheology of even the simplest case of a suspension of hard spheres in a Newtonian suspending fluid is incompletely understood (1). Many of the features observed in these suspensions, including shear thinning (2) or thickening (3, 4) and the magnitudes and even the algebraic signs of normal stress differences (5), are at best understood at a qualitative level, and a general theoretical framework is lacking. Furthermore, there has been a tendency to treat the rheology of Brownian (colloidal) suspensions and nonBrownian suspensions as distinct.Recently, a picture has emerged in which central aspects of the rheology of non-Brownian dense suspensions are interpreted as manifestations of proximity to jamming transitions in the parameter space. These transitions are singularities whose locations in the volume fraction ϕ and shear stress σ-plane depend on the details of the microscopic interactions (shape of the particles, friction, interparticle forces). In turn, the locations of these singularities shape the large ϕ-portion of the rheological landscape, i.e., the effective viscosity and the normal stresses as functions of ϕ and σ. In particular, in the "stress-induced friction" scenario (4, 6-13), shear thickening is a transition from a rheological response dominated by frictionless jamming to one controlled by frictional jamming upon increase of the shear stress. This transition is argued to be due to the creation of frictional contacts between particles at high stresses; the contacts are prevented at low stresses by a short-range stabilizing repulsive force, as would be expected to be present to...