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Definition of viscosity

The transport properties of fluid materials (either solid or liquid) are determined by their viscosity, which defines the resistance of the material to fluid flow (i.e., how “runny” it is). Viscosity, η, describes the time dependence of material motion through the ratio of applied shear stress, σ, to strain rate, via

The Earth's liquid outer core will have a relatively low viscosity compared to that of the solid inner core, which deforms on a much longer timescale. In geophysics, the quantity η is referred to as the dynamic viscosity, which, when normalized by the density, ρ, is termed the kinematic viscosity, ν:

Viscosity is a quantity dependent on the properties of the fluid at a molecular level. Therefore, both the viscosities defined above may also be referred to as “molecular viscosity.” In the outer core, fluid motion occurs over a range of length scales from that at a molecular level to large‐scale motion with characteristic distances comparable with the...

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© 2007 Springer-Verlag

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Vočadlo, L. (2007). Core Viscosity. In: Gubbins, D., Herrero-Bervera, E. (eds) Encyclopedia of Geomagnetism and Paleomagnetism. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-4423-6_42

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