Taylor columns
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A Taylor column is a fluid dynamics phenomenon that occurs as a result of the
Coriolis effect In physics, the Coriolis force is an inertial or fictitious force that acts on objects in motion within a frame of reference that rotates with respect to an inertial frame. In a reference frame with clockwise rotation, the force acts to the ...
. It was named after
Geoffrey Ingram Taylor Sir Geoffrey Ingram Taylor OM FRS FRSE (7 March 1886 – 27 June 1975) was a British physicist and mathematician, and a major figure in fluid dynamics and wave theory. His biographer and one-time student, George Batchelor, described him as ...
. Rotating fluids that are perturbed by a solid body tend to form columns parallel to the axis of rotation called Taylor columns. An object moving parallel to the axis of rotation in a rotating fluid experiences more drag force than what it would experience in a non rotating fluid. For example, a strongly buoyant ball (such as a pingpong ball) will rise to the surface slower than it would in a non rotating fluid. This is because fluid in the path of the ball that is pushed out of the way tends to circulate back to the point it is shifted away from, due to the Coriolis effect. The faster the rotation rate, the smaller the radius of the inertial circle traveled by the fluid. In a non-rotating fluid the fluid parts above the rising ball and closes in underneath it, offering relatively little resistance to the ball. In a rotating fluid, the ball needs to push up a whole column of fluid above it, and it needs to drag a whole column of fluid along beneath it in order to rise to the surface. A rotating fluid thus displays some degree of rigidity.


History

Taylor columns were first observed by
William Thomson, Lord Kelvin William Thomson, 1st Baron Kelvin, (26 June 182417 December 1907) was a British mathematician, mathematical physicist and engineer born in Belfast. Professor of Natural Philosophy at the University of Glasgow for 53 years, he did important ...
, in 1868. Taylor columns were featured in lecture demonstrations by Kelvin in 1881 and by John Perry in 1890. The phenomenon is explained via the
Taylor–Proudman theorem In fluid mechanics, the Taylor–Proudman theorem (after Geoffrey Ingram Taylor and Joseph Proudman) states that when a solid body is moved slowly within a fluid that is steadily rotated with a high angular velocity \Omega, the fluid velocity will ...
, and it has been investigated by Taylor, Grace, Stewartson,Stewartson, K. (1952) "On the slow motion of a sphere along the axis of a rotating fluid," ''Proceedings of the Cambridge Philosophical Society'', vol. 48, pages 168–177. and MaxworthyMaxworthy, T. (1968) "The observed motion of a sphere through a short, rotating cylinder of fluid," ''Journal of Fluid Mechanics'', vol. 31, pages 643–655. See also: Maxworthy, T. (1970) "The flow created by a sphere moving along the axis of a rotating, slightly-viscous fluid," ''Journal of Fluid Mechanics'', vol. 40, pages 453–479.—among others.


Theory

Taylor columns have been rigorously studied. For '' Re''<<1, '' Ek''<<1, '' Ro''<<1, the drag equation for a cylinder of radius, ''a'', the following relation has been found. F=\frac\rho a^\Omega U To derive this, Moore and Saffman solved the linearised Navier–Stokes equation along in cylindrical coordinates, where some of the vertical and radial components of the viscous term are taken to be small relative to the Coriolis term: -2\Omega v=-\frac\frac 2\Omega u=\nu \left (\frac+\frac\frac-\frac \right ) 0=-\frac\frac+\nu \left (\frac+\frac\frac \right ) To solve these equations, we incorporate the volume conservation condition as well: \frac \frac+\frac=0 We use the Ekman compatibility relation for this geometry to restrict the form of the velocity at the disk surface: w-U=\pm\frac\sqrt\frac\frac The resultant velocity fields can be solved in terms of
Bessel function Bessel functions, first defined by the mathematician Daniel Bernoulli and then generalized by Friedrich Bessel, are canonical solutions of Bessel's differential equation x^2 \frac + x \frac + \left(x^2 - \alpha^2 \right)y = 0 for an arbitrar ...
s. u=-\frac\int\limits_^ k^2 A(k) J_1(kr)e^dk v=\int\limits_^ A(k) J_1(kr)e^dk w=-\int\limits_^ A(k) J_0(kr)e^dk whereby for '' Ek''<<1 the function ''A(k)'' is given by, A(k)=\frac\left ( \cos ka - \frac \right ) Integrating the equation for the ''v'', we can find the pressure and thus the drag force given by the first equation.


References


Further reading

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External links


Taylor columns
(Martha Buckley, MIT)
Record Player Fluid Dynamics: A Taylor Column Experiment
(UCLA Spin Lab) {{DEFAULTSORT:Taylor Column Fluid mechanics Physical oceanography