A new portable penetrometer for measuring the viscosity of active lava

Viscosity is a fundamental physical property of lava that dictates style and rate of effusive transport. Studies of lava viscosity have predominantly focused on measuring re-melted rocks in the laboratory. While these measurements are well-constrained in temperature, shear rate, and oxygen fugacity,...

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Bibliographic Details
Main Authors: Harris, M. A., Kolzenburg, S., Sonder, I., /Chevrel, Magdalena Oryaelle
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://www.documentation.ird.fr/hor/fdi:010090759
Description
Summary:Viscosity is a fundamental physical property of lava that dictates style and rate of effusive transport. Studies of lava viscosity have predominantly focused on measuring re-melted rocks in the laboratory. While these measurements are well-constrained in temperature, shear rate, and oxygen fugacity, they cannot reproduce the complexities of the natural emplacement environment. Field viscosity measurements of active lava are the only way to fully capture lava's properties, but such measurements are scarce, largely due to a lack of easy-to-use, portable, and accurate measurement devices. Thus, there is a need for developing suitable field instruments to help bolster the understanding of lava. Here, we present a new penetrometer capable of measuring a material's viscosity under the harsh conditions of natural lava emplacement. This device uses a stainless-steel tube with a semi-spherical tip fixed to a load cell that records axial force when pushed into a material, while simultaneously measuring the penetration depth via a free-moving tube that is pushed backward along the penetration tube. The device is portable (1.5 m long, 5.5 kg in weight) and uses a single-board computer for data acquisition. The penetrometer has an operational range from 2.5 x 10(2) to 2.1 x 10(5) Pa s and was calibrated for viscosities ranging from 5.0 x 10(2) to 1.6 x 10(5) Pa s. It was deployed to the 2023 Litli-Hr & uacute;tur eruption in Iceland. These field measurements successfully recorded the in situ viscosities of the lava in the range of 1.2 x 10(4)-3.4 x 10(4) Pa s, showcasing it as an efficient method of measuring natural lava viscosity.