Article ID Journal Published Year Pages File Type
9531194 Journal of Volcanology and Geothermal Research 2005 21 Pages PDF
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 (10−6 to 0.25 cm/s) tests at elevated temperatures (≤1100 °C). Deformation experiments were performed on pre-fabricated cylinders (4.5 cm diameter, ∼6 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 10−5 to 10−3 s−1 and stresses of ∼0 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=ηoexp−5.3(ϕ f1−ϕ f)where η0 is melt viscosity and ϕf 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.
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