Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9531194 | Journal of Volcanology and Geothermal Research | 2005 | 21 Pages |
Abstract
The rheological behavior of pyroclastic deposits during welding is incompletely understood and is based on a surprisingly small number of experimental studies. Here we present results from a new experimental apparatus comprising an automated uniaxial compression load frame that can run constant load (up to 1150 kg) or constant displacement rate (10â6 to 0.25 cm/s) tests at elevated temperatures (â¤1100 °C). Deformation experiments were performed on pre-fabricated cylinders (4.5 cm diameter, â¼6 cm length) of soda lime silica glass beads (N=32), sintered rhyolite ash (N=7) and cores of pumiceous rhyodacite (N=6). Experimental runs used strain rates from 10â5 to 10â3 sâ1 and stresses of â¼0 to 5.24 MPa. Temperatures varied from 535 to 650 °C for experiments on soda lime silica glass beads and 825 to 950 °C for natural materials. In all cases experimental cores showed a strain-dependent rheology that is more strongly affected by temperature than by load or strain rate. Results from these experiments are used to develop a relationship in which the effective viscosity (ηe) of the experimental cores is predicted by:ηe=ηoexpâ5.3(Ï f1âÏ f)where η0 is melt viscosity and Ïf is sample porosity. This rheological model provides a means for exploring the relative roles of emplacement temperature, load and glass transition temperature in welding of pyroclastic deposits.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Steven L. Quane, J.K. Russell,