The viscosity of basaltic magma; an analysis of field measurements in Makaopuhi lava lake, Hawaii

  • Shaw H
  • Wright T
  • Peck D
  • et al.
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Abstract

The methods of rotation viscometry have been applied in the fieldto a tholeiitic lava at 1130 degrees to 1135 degrees C containingabout 25 percent crystals and 2 to 5 percent gas bubbles, using astainless steel spindle inserted through the lava crust. The resultsagree well with the Bingham model. Yield values in the lava are 1200and 700 dynes cm (super -2) , and the plastic constants are 6500and 7500 poises. Laboratory studies in silicone fluid show gas bubblesenhance plastic behavior. In general, lavas must be treated as non-Newtonianfluids; the conditions that may cause different types of fluid behaviorin tholeiitic lava are outlined.

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Shaw, H. R., Wright, T. L., Peck, D. L., & Okamura, R. (1968). The viscosity of basaltic magma; an analysis of field measurements in Makaopuhi lava lake, Hawaii. American Journal of Science, 266(4), 225–264. https://doi.org/10.2475/ajs.266.4.225

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