Low-frequency shear and structural relaxation in rhyolite melt
โ 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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โฆ 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.
๐ SIMILAR VOLUMES
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