HR: 0830h
AN: ED41C-1184 [PDF]
TI: Student Experiments for Investigations of Physical Controls on Viscosity and the Implications for
Volcanic Hazards
AU: * Edwards, B R
EM: edwardsb@dickinson.edu
AF: Department of Geology, Dickinson College, Carlisle, PA 17013 United States
AU: Teasdale, R
EM: Teasdale@asu.edu
AF: Department of Earth Sciences, University of Bristol, Bristol, BS8 1RJ
United Kingdom
AU: Myers, J
EM: magma@uwyo.edu
AF: Department of Geology and Geophysics, University of Wyoming, Laramie, WY 82071 United States
AB:
Interactive laboratory investigations and demonstrations using analog materials can be used to introduce students to the
rheologic properties of magmas and lavas. Using such an approach, students investigate the physical, compositional, and
thermodynamic controls on viscosity through observations, experimental investigations, calculations, and computer
simulations. During lab exercises, which are typically preceded by a reading assignment and brief introduction, students use
analog materials (e.g. corn syrup) to experiment with parameters controlling viscosity. They prepare a set of syrup solutions
at 3 (or more) temperatures, another set of syrup solutions with varying proportions of particles (e.g. sand), and a final
set of syrup solutions mixed with water. A fourth experiment, which produces somewhat more complex results, can be prepared
by using a hand mixer to make syrup with varying proportions of bubbles. Students make qualitative observations of the
relative force required to blow bubbles into the syrup solutions with a straw as an analog for comparing the effects of
viscosity on the formation and bursting behavior of gas bubbles in magma. During class, students observe syrup "lava flows"
flowing on a slope. Measured flow characteristics are used to calculate viscosities for each "lava" using a dynamic visual
equation (DVE) of the Jeffries equation. The DVE, which was created in Flash MX, allows students to explore interactively and
visually how changing various parameters in the Jeffries equation affects fluid viscosity. Before each experiment, a
critical set of questions lead students to make predictions and hone their observational skills. The questions also help
students generate graphs and sketches and write brief reports to synthesize their observations. Additional activities
incorporating volcanic hazards associated with low versus high viscosity flows and highly viscous explosive eruptions bring
students back to very real applications of the principles investigated. In some cases, classroom activities have led students
to independent research. One such project used analog flow materials to illustrate the effect of the shape and abundance of
crystals on lava flow morphology. Students report having a clearer understanding of the viscous properties of lavas and
magma, allowing more advanced discussions of volcanologic and petrologic principles such as conduit flow dynamics,
crystallization of magmas, and volcanic hazards.
DE: 3640 Igneous petrology
DE: 8400 VOLCANOLOGY
DE: 8429 Lava rheology and morphology
DE: 8439 Physics and chemistry of magma bodies
SC: Education and Human Resources [ED]
MN: 2003 Fall Meeting