TY - JOUR
T1 - Quantitative measurement of bubble textures in pumice clasts using a digital stereo microscope with low-angled ring illumination
AU - Ohashi, Masatoshi
AU - Ichihara, Mie
AU - Maeno, Fukashi
AU - Kennedy, Ben
AU - Gravley, Darren
N1 - Funding Information:
The authors are grateful to Takeshi Hasegawa, Lydia Harmon, and Gilles Seropian for helping us collect pumice clasts in Taupo. We also thank Atsushi Yasuda and Natsumi Hokanishi for the measurement with SEM. The manuscript has been improved by the appropriate handling by T. Yamamoto, the associate editor, and constructing comments by two anonymous reviewers. The present study was supported by Grant-in-Aid for JSPS Research Fellowship 17J05094 and the Joint Usage Program of the Earthquake Research Institute, University of Tokyo (2017B01).
Funding Information:
This work is supported by Grant-in-Aid for JSPS Research Fellowship 17J05094, the Joint Usage Program of the Earthquake Research Institute, University of Tokyo (2017B01), and MEXT “Integrated Program for Next Generation Volcano Research and Human Resource Development”. BK acknowledges the ECLIPSE Program supported by the New Zealand Ministry for Business, Innovation and Employment.
Funding Information:
The authors are grateful to Takeshi Hasegawa, Lydia Harmon, and Gilles Seropian for helping us collect pumice clasts in Taupo. We also thank Atsushi Yasuda and Natsumi Hokanishi for the measurement with SEM. The manuscript has been improved by the appropriate handling by T. Yamamoto, the associate editor, and constructing comments by two anonymous reviewers. The present study was supported by Grant-in-Aid for JSPS Research Fellowship 17J05094 and the Joint Usage Program of the Earthquake Research Institute, University of Tokyo (2017B01).
Publisher Copyright:
© 2020, The Author(s).
PY - 2020/12
Y1 - 2020/12
N2 - Quantitative analysis of bubble textures in a large number of volcanic pyroclasts is critical to investigating the eruption dynamics in a volcanic conduit. Here, we used a digital stereo microscope with low-angled ring illumination (DSM-LaRI) to measure bubble textures on unpolished cutting surfaces of pumice clasts. As the DSM-LaRI enhances brightness contrast between the bubbles (pores) and the matrix, we easily obtained the two-dimensional data on the size and shape of bubbles by image analysis. The DSM-LaRI imaging provided the distributions of size and shape of bubbles at least 50 µm across. We applied the DSM-LaRI to analyze more than 1000 pumice clasts from the 232 AD Taupo eruption and measured the mean bubble radius (R¯ ) and the mean deformation degree (D¯ ) in the individual clasts. The distribution of R¯ and D¯ in each layer showed a distinctive difference between the fallout and the flow deposits. These quantitative data are consistent with a qualitative classification in a previous study. Although the new DSM-LaRI method has the disadvantage of the low spatial resolution, it allows for the analysis of a large number of pumice clasts in a short time, which can address larger scale heterogeneity, by efficiently generating a large representative suite of bubble size and shape data to link bubble textures to conduit processes. This provides vital information for quantitatively modeling eruption dynamics.[Figure not available: see fulltext.].
AB - Quantitative analysis of bubble textures in a large number of volcanic pyroclasts is critical to investigating the eruption dynamics in a volcanic conduit. Here, we used a digital stereo microscope with low-angled ring illumination (DSM-LaRI) to measure bubble textures on unpolished cutting surfaces of pumice clasts. As the DSM-LaRI enhances brightness contrast between the bubbles (pores) and the matrix, we easily obtained the two-dimensional data on the size and shape of bubbles by image analysis. The DSM-LaRI imaging provided the distributions of size and shape of bubbles at least 50 µm across. We applied the DSM-LaRI to analyze more than 1000 pumice clasts from the 232 AD Taupo eruption and measured the mean bubble radius (R¯ ) and the mean deformation degree (D¯ ) in the individual clasts. The distribution of R¯ and D¯ in each layer showed a distinctive difference between the fallout and the flow deposits. These quantitative data are consistent with a qualitative classification in a previous study. Although the new DSM-LaRI method has the disadvantage of the low spatial resolution, it allows for the analysis of a large number of pumice clasts in a short time, which can address larger scale heterogeneity, by efficiently generating a large representative suite of bubble size and shape data to link bubble textures to conduit processes. This provides vital information for quantitatively modeling eruption dynamics.[Figure not available: see fulltext.].
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U2 - 10.1186/s40623-020-01320-0
DO - 10.1186/s40623-020-01320-0
M3 - Article
AN - SCOPUS:85097049492
VL - 72
JO - Earth, Planets and Space
JF - Earth, Planets and Space
SN - 1343-8832
IS - 1
M1 - 185
ER -