A magnetorheological fluid consisting of colloidal silica spheres suspended
in an organic ferrofluid is described. Its linear viscoelastic behavior as
a function of frequency, magnetic field strength, and silica volume fracti
on was investigated with a specially designed magnetorheometer. The storage
modulus G' is at least an order of magnitude larger than the loss modulus
G " at all magnetic held strengths investigated, G' does depend only weakly
on frequency, and linearly on volume fraction. A model is presented for th
e high frequency limit of the storage modulus G(infinity)'. In the model ou
r system is heated as a collection of single noninteracting chains of parti
cles. Assuming a dipolar magnetic interaction, theory and experiment show r
easonable agreement at high frequencies. [S1063-651X(99)16510-3].