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Discussion of “Accelerated motion of a spherical particle”
Author(s) -
Brooks Norman H.,
Carstens M. R.
Publication year - 1953
Publication title -
eos, transactions american geophysical union
Language(s) - English
Resource type - Journals
eISSN - 2324-9250
pISSN - 0002-8606
DOI - 10.1029/tr034i006p00947
Subject(s) - spheres , simple harmonic motion , motion (physics) , displacement (psychology) , classical mechanics , physics , particle (ecology) , harmonic , added mass , mechanics , mathematical analysis , mathematics , vibration , acoustics , psychology , oceanography , astronomy , psychotherapist , geology
In considering the accelerated motion of spheres in a viscous fluid, the author has restricted himself to consideration of only simple harmonic motions of the fluid field and the sphere. The author's equation of motion (Eq. 11) for a suspended sphere is true only when the solution yields a relative displacement (x ‐ a) which is sinusoidal in time. Otherwise, the apparent mass factor k, and the damping coefficient A have no meaning, because they are both based on the Stokes solution for an oscillating sphere given in LAMB [1945, see References at end of published paper, p. 721]. Both k and A are functions of the circular frequency w as they are defined by (1), (2), and (3).

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