Toward a general viscosity equation for natural anhydrous and hydrous silicate melts

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Diffusion of H, C, and O Components in Silicate Melts (2010, methodology): “The dotted line is Eyring diffusivity calculated using the viscosity model of Hui and Zhang (2007) at 0.1 MPa to 1 GPa assuming a jumping distance of 2.8×10−10 m. 212 Zhang & Ni m2/s to the oxygen diffusivity.”
The rheology of two-phase magmas: A review and analysis (2013, methodology): “The rheology of silicate melts has been well-studied for a wide range of melt compositions and conditions (e.g. Hess and Dingwell, 1996; Giordano et al., 2006; Neuville, 2006; Poe et al., 2006; Vetere et al., 2006; Hui and Zhang, 2007; Giordano et al., 2008, 2009; Vetere et al., 2009; Whittington et”
Viscosity of magmatic liquids: A model (2008, methodology): “(A) Values of A representing the high-T limits to silicate melt viscosity (i.e. log η ∞ ) implicit in the SH model (Shaw, 1972), the HZ model (Hui and Zhang, 2007 ) and our model (GRD).”
The Role of Volatiles in Reactive Melt Transport in the Asthenosphere (2015, unknown): “The liquid viscosity varies with composition to capture leading-order effects of the polymerization state of a magma with variable silica and volatile content (Bottinga & Weill, 1972; Kushiro et al., 1976; Giordano & Dingwell, 2003; Hui & Zhang, 2007).”