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Explosive Volcanic Eruptions‐I The Rate of Fall of Pyroclasts

Research output: Contribution to Journal/Magazine › Journal article › peer-review

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Explosive Volcanic Eruptions‐I The Rate of Fall of Pyroclasts. / Wilson, L.; Bowell, E. L.G.
In: Geophysical Journal of the Royal Astronomical Society, Vol. 22, No. 4, 01.04.1971, p. 377-383.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Wilson, L & Bowell, ELG 1971, 'Explosive Volcanic Eruptions‐I The Rate of Fall of Pyroclasts', Geophysical Journal of the Royal Astronomical Society, vol. 22, no. 4, pp. 377-383. https://doi.org/10.1111/j.1365-246X.1971.tb03607.x

APA

Wilson, L., & Bowell, E. L. G. (1971). Explosive Volcanic Eruptions‐I The Rate of Fall of Pyroclasts. Geophysical Journal of the Royal Astronomical Society, 22(4), 377-383. https://doi.org/10.1111/j.1365-246X.1971.tb03607.x

Vancouver

Wilson L, Bowell ELG. Explosive Volcanic Eruptions‐I The Rate of Fall of Pyroclasts. Geophysical Journal of the Royal Astronomical Society. 1971 Apr 1;22(4):377-383. doi: 10.1111/j.1365-246X.1971.tb03607.x

Author

Wilson, L. ; Bowell, E. L.G. / Explosive Volcanic Eruptions‐I The Rate of Fall of Pyroclasts. In: Geophysical Journal of the Royal Astronomical Society. 1971 ; Vol. 22, No. 4. pp. 377-383.

Bibtex

@article{d6eb96b96990495a8a512104d834a00c,
title = "Explosive Volcanic Eruptions‐I The Rate of Fall of Pyroclasts",
abstract = "Analysis of an explosive volcanic eruption requires a knowledge of the rate of fall of ejected debris. Terminal velocities have been determined experimentally for pumice of various grain‐sizes and also for lithic fragments and sanidine crystals from two series of volcanic eruptions. Theoretical terminal velocities for cylinders and rough and smooth spheres of various grain‐sizes and densities have been computed. The results for cylinders agree very closely with the corresponding experimentally measured values. Computed terminal velocities for particles with various diameters, densities and shapes are presented graphically.",
author = "L. Wilson and Bowell, {E. L.G.}",
year = "1971",
month = apr,
day = "1",
doi = "10.1111/j.1365-246X.1971.tb03607.x",
language = "English",
volume = "22",
pages = "377--383",
journal = "Geophysical Journal of the Royal Astronomical Society",
issn = "0016-8009",
publisher = "Wiley-Blackwell",
number = "4",

}

RIS

TY - JOUR

T1 - Explosive Volcanic Eruptions‐I The Rate of Fall of Pyroclasts

AU - Wilson, L.

AU - Bowell, E. L.G.

PY - 1971/4/1

Y1 - 1971/4/1

N2 - Analysis of an explosive volcanic eruption requires a knowledge of the rate of fall of ejected debris. Terminal velocities have been determined experimentally for pumice of various grain‐sizes and also for lithic fragments and sanidine crystals from two series of volcanic eruptions. Theoretical terminal velocities for cylinders and rough and smooth spheres of various grain‐sizes and densities have been computed. The results for cylinders agree very closely with the corresponding experimentally measured values. Computed terminal velocities for particles with various diameters, densities and shapes are presented graphically.

AB - Analysis of an explosive volcanic eruption requires a knowledge of the rate of fall of ejected debris. Terminal velocities have been determined experimentally for pumice of various grain‐sizes and also for lithic fragments and sanidine crystals from two series of volcanic eruptions. Theoretical terminal velocities for cylinders and rough and smooth spheres of various grain‐sizes and densities have been computed. The results for cylinders agree very closely with the corresponding experimentally measured values. Computed terminal velocities for particles with various diameters, densities and shapes are presented graphically.

U2 - 10.1111/j.1365-246X.1971.tb03607.x

DO - 10.1111/j.1365-246X.1971.tb03607.x

M3 - Journal article

AN - SCOPUS:84984500559

VL - 22

SP - 377

EP - 383

JO - Geophysical Journal of the Royal Astronomical Society

JF - Geophysical Journal of the Royal Astronomical Society

SN - 0016-8009

IS - 4

ER -