Most man-made as well as natural materials of interest in engineering and physical sciences are intrinsically heterogeneous. Common examples are particle-reinforced composites, porous materials, and polycrystalline solids such as metals, ice, and many rocks. A fundamental problem in mechanics of materials is the estimation of the macroscopic response of such heterogeneous materials from the properties and geometrical arrangement (microstructure) of their constituents. In addition, incorporating the effect of local processes (e.g., microstructure evolution, damage, work hardening, recrystallization) on the macroscopic response requires statistical information about spatial distribution of the local fields within the material. To this end, we...