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Bubble coalescence in basaltic lava : its impact on the evolution of bubble populations.

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Bubble coalescence in basaltic lava : its impact on the evolution of bubble populations. / Herd, Richard A.; Pinkerton, Harry.
In: Journal of Volcanology and Geothermal Research, Vol. 75, No. 1-2, 01.1997, p. 137-157.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

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Herd RA, Pinkerton H. Bubble coalescence in basaltic lava : its impact on the evolution of bubble populations. Journal of Volcanology and Geothermal Research. 1997 Jan;75(1-2):137-157. doi: 10.1016/S0377-0273(96)00039-X

Author

Herd, Richard A. ; Pinkerton, Harry. / Bubble coalescence in basaltic lava : its impact on the evolution of bubble populations. In: Journal of Volcanology and Geothermal Research. 1997 ; Vol. 75, No. 1-2. pp. 137-157.

Bibtex

@article{c768f7ae42e34887ad810364de4cd2ac,
title = "Bubble coalescence in basaltic lava : its impact on the evolution of bubble populations.",
abstract = "Morphological properties (bubble number density, porosity, mean radius, specific surface area) of vesicular rocks provide quantitative information on the rates of bubble nucleation, growth and coalescence in magmas when measured as a function of time. Such data are useful in constraining the timing and style of gas release during volcanic eruptions. Volcanic rocks commonly show strong zonation with respect to bubble size and porosity, indicating a variation in the amount of bubble growth and coalescence preserved within a single sample. Morphological properties and bubble size distributions (BSD's) were measured in a suite of zoned alkali basalts using image analysis and the data were compared to theoretical predictions. Our data indicate that at porosities greater than 35%, extensive coalescence occurred during the growth of bubbles with restricted nucleation; at lower porosities, vesiculation is dominated by nucleation and diffusion with no coalescence. The interiors of many of our samples have undergone 4–7 binary coalescence events after eruption in a time of around 15 min. The Ostwald ripening effect has not significantly modified the BSD's.",
keywords = "bubble coalescence, bubble population, morphological properties, basaltaic lava, magma degassing",
author = "Herd, {Richard A.} and Harry Pinkerton",
year = "1997",
month = jan,
doi = "10.1016/S0377-0273(96)00039-X",
language = "English",
volume = "75",
pages = "137--157",
journal = "Journal of Volcanology and Geothermal Research",
issn = "0377-0273",
publisher = "Elsevier Science B.V.",
number = "1-2",

}

RIS

TY - JOUR

T1 - Bubble coalescence in basaltic lava : its impact on the evolution of bubble populations.

AU - Herd, Richard A.

AU - Pinkerton, Harry

PY - 1997/1

Y1 - 1997/1

N2 - Morphological properties (bubble number density, porosity, mean radius, specific surface area) of vesicular rocks provide quantitative information on the rates of bubble nucleation, growth and coalescence in magmas when measured as a function of time. Such data are useful in constraining the timing and style of gas release during volcanic eruptions. Volcanic rocks commonly show strong zonation with respect to bubble size and porosity, indicating a variation in the amount of bubble growth and coalescence preserved within a single sample. Morphological properties and bubble size distributions (BSD's) were measured in a suite of zoned alkali basalts using image analysis and the data were compared to theoretical predictions. Our data indicate that at porosities greater than 35%, extensive coalescence occurred during the growth of bubbles with restricted nucleation; at lower porosities, vesiculation is dominated by nucleation and diffusion with no coalescence. The interiors of many of our samples have undergone 4–7 binary coalescence events after eruption in a time of around 15 min. The Ostwald ripening effect has not significantly modified the BSD's.

AB - Morphological properties (bubble number density, porosity, mean radius, specific surface area) of vesicular rocks provide quantitative information on the rates of bubble nucleation, growth and coalescence in magmas when measured as a function of time. Such data are useful in constraining the timing and style of gas release during volcanic eruptions. Volcanic rocks commonly show strong zonation with respect to bubble size and porosity, indicating a variation in the amount of bubble growth and coalescence preserved within a single sample. Morphological properties and bubble size distributions (BSD's) were measured in a suite of zoned alkali basalts using image analysis and the data were compared to theoretical predictions. Our data indicate that at porosities greater than 35%, extensive coalescence occurred during the growth of bubbles with restricted nucleation; at lower porosities, vesiculation is dominated by nucleation and diffusion with no coalescence. The interiors of many of our samples have undergone 4–7 binary coalescence events after eruption in a time of around 15 min. The Ostwald ripening effect has not significantly modified the BSD's.

KW - bubble coalescence

KW - bubble population

KW - morphological properties

KW - basaltaic lava

KW - magma degassing

U2 - 10.1016/S0377-0273(96)00039-X

DO - 10.1016/S0377-0273(96)00039-X

M3 - Journal article

VL - 75

SP - 137

EP - 157

JO - Journal of Volcanology and Geothermal Research

JF - Journal of Volcanology and Geothermal Research

SN - 0377-0273

IS - 1-2

ER -