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Low-frequency shear and structural relaxation in rhyolite melt

โœ Scribed by Sharon L. Webb


Publisher
Springer-Verlag
Year
1992
Tongue
English
Weight
570 KB
Volume
19
Category
Article
ISSN
0342-1791

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โœฆ Synopsis


The frequency-dependence of the shear viscosity and modulus of rhyolite melt has been determined over a 10-14 loglo Pa s viscosity range and a 0.03-63 rad s-1 angular frequency range. The frequency-dependent viscosity determined at high frequencies is 5 orders of magnitude lower than the Newtonian viscosity. At lower frequencies, a frequency-independent viscosity identical with the Newtonian viscosity is observed. The measured shear modulus increases from zero to 30.5___2.5 GPa with increasing frequency. The viscoelastic regime consists of a maximum in viscous loss centered on the Maxwell relaxation time. The width and height of the loss modulus as a function of frequency is inconsistent with a single relaxation-time. The frequency-dependent shear modulus is best described by a distribution of relaxationtimes with a sharp cutoff at times slightly longer than the Maxwell relaxation time, and a long tail at shorter times extending up to 5 orders of magnitude less than the Maxwell relaxation time. This distribution of relaxation-times is in contrast with the single-relaxation-time behavior observed in low viscosity silicate melts.


๐Ÿ“œ SIMILAR VOLUMES


Structural relaxation in silicate melts
โœ Donald B. Dingwell; Sharon L. Webb ๐Ÿ“‚ Article ๐Ÿ“… 1989 ๐Ÿ› Springer-Verlag ๐ŸŒ English โš– 1020 KB

The timescale of structural relaxation in a silicate melt defines the transition from liquid (relaxed) to glassy (unrelaxed) behavior. Structural relaxation in silicate melts can be described by a relaxation time, z, consistent with the observation that the timescales of both volume and shear relaxa