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Physics for Geologists, Second edition

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Stress and strain 91<br />

Figure 9.1 Newton's concept of viscosity (seen in section). When the upper plate<br />

moves relative to the lower, the lubricant between them is assumed<br />

to have adhered to each plate, and to have sheared linearly between<br />

them.<br />

Coefficient of viscosity: absolute or dynamic viscosity<br />

Consider a liquid between two closely-spaced parallel plates (Figure 9.1) of<br />

which the top plate is moving with constant velocity, V, relative to the lower<br />

plate. Fluid adheres to each plate. The velocity of the fluid against the upper<br />

plate is V, while the fluid adhering to the lower plate does not move. Between<br />

the two, it is reasonable to assume that successive layers slip relative to those<br />

below and above it, so that the velocity is linearly distributed between the<br />

two plates. This is Newton's concept of viscosity, and it is called newtonian<br />

viscosity.<br />

The coefficient of viscosity, q, is defined as the ratio of shear stress to the<br />

rate of shear strain:<br />

In words, the coefficient of viscosity is the tangential <strong>for</strong>ce per unit area that<br />

maintains unit relative velocity between two parallel planes unit distance<br />

apart.<br />

The coefficient of viscosity is also known as absolute or dynamic viscosity.<br />

The SI unit is newton second per square metre (N s rnp2). Other units are the<br />

poise, P, which is grams per centimetre second (gcm-l s-l) in units of mass,<br />

length and time or dynes second per square centimetre in units of <strong>for</strong>ce,<br />

length and time. The poise is named after the French physician, J.-L.-M.<br />

Poiseuille (1799-1869) whose interest in blood flow led to a beautiful series<br />

of experiments on flow through small pipes.<br />

If the viscosity remains constant throughout the fluid, and at different<br />

strain rates, the fluid is said to be newtonian. Non-newtonian fluids are<br />

those with variable viscosity.<br />

Copyright 2002 by Richard E. Chapman

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