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Theoretical models of compaction processes, such as for example intergranularpressure-solution (IPS), focus on deformation occurring at the contacts betweenspherical grains that constitute an aggregate. In order to investigate theapplicability of such models, and to quantify the deformation of particleswithin an aggregate, isostatic experiments were performed in cold-sealedvessels on glass sphere aggregates at 200 MPa confining pressure and 350degrees C with varying amounts of fluid.

Influence of time, temperature, confining pressure and fluid content on the experimental compaction of spherical grains