We develop a compositional model for the grain boundary (GB) diffusion creep of melt-bearing polycrystalline aggregates. This model is an extension of the GB diffusion control model by taking into account the effects of finite liquid diffusivity and finite reaction rates, which are important at small melt fractions (phi). For shear viscosity eta, there exists a critical melt fraction phi(eta)(c) below which the rate-limiting process changes from diffusion through GB to diffusion through the liquid, and for bulk viscosity xi, there exists a critical melt fraction phi(xi)(c) below which the rate-limiting process changes from diffusion through GB to reaction at the pore surface. The implication of the model results is that different processes may limit the kinetics of bulk and shear viscosities at small phi. The model also predicts that stress can cause compositional and hence volumetric asymmetry in pores. As melt fraction increases from zero to the critical melt fractions, rapid decreases occur in eta, from eta(cc) to 0.2 eta(cc), and in xi, from infinity to 0.4 eta(cc), where eta(cc) represents eta for Coble creep. In the GB diffusion control model, these decreases occur discontinuously at zero melt fraction, but this singularity is removed in the compositional model. For a typical grain size in the mantle (3 mm), the critical melt fractions are estimated semiquantitatively as phi(eta)(c) = 10(-4) and phi(xi)(c) < 6 x 10(-8), demonstrating the significant effect of very small amount of melt on the viscosities in the mantle.
464FTTimes Cited:2Cited References Count:19