The DOI matches its Crossref record; 69 of the 69 references it cites were found in a registry or an index.
The Fluid Mechanics Inside a Volcano
Abstract
The style and evolution of volcanic eruptions are dictated by the fluid mechanics governing magma ascent. Decompression during ascent causes dissolved volatile species, such as water and carbon dioxide, to exsolve from the melt to form bubbles, thus providing a driving force for the eruption. Ascent is influenced not only by the nucleation and growth of gas bubbles, but also magma rheology and brittle deformation (fragmentation). In fact, all processes and magma properties within the conduit interact and are coupled. Ultimately, it is the ability of gas trapped within growing bubbles to expand or to be lost by permeable gas flow, which determines whether ascending magmas can erupt nonexplosively. We review and integrate models of the primary conduit processes to show when each process or property dominates and how these interact within a conduit. In particular, we illustrate how and why ascent rate may control eruptive behavior: slowly ascending magmas erupt effusively and rapidly ascending magmas erupt explosively.
Overview
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
The self-check needs the paper’s full text.
Citations
Cites
Rowe, G. L. (2000) · Eos, Transactions American Geophysical Union · doi:10.1029/00eo00168 · Cited by 2,089
Flow of gases through porous media
Eisenklam, P. (1957) · Combustion and Flame · doi:10.1016/0010-2180(57)90038-x · Cited by 1,362
Flow of gases through porous media
Carman, P. C. (1956) · Medical Entomology and Zoology · Cited by 1,324
Wallace, P. J. (2005) · Journal of Volcanology and Geothermal Research · doi:10.1016/j.jvolgeores.2004.07.023 · Cited by 1,053
The dynamics of bubble formation and growth in magmas: A review and analysis
Sparks, R. S. J. (1978) · Journal of Volcanology and Geothermal Research · doi:10.1016/0377-0273(78)90002-1 · Cited by 987
Propagation of Magma-Filled Cracks
Rubin, A. M. (1995) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.ea.23.050195.001443 · Cited by 970
The 1980 eruptions of Mount St. Helens, Washington
Lipman, P. W., & Mullineaux, D. R. (1981) · Professional Paper · doi:10.3133/pp1250 · Cited by 664
Wilson, L., Sparks, R. S. J., & Walker, G. P. L. (1980) · Geophysical Journal International · doi:10.1111/j.1365-246x.1980.tb02613.x · Cited by 650
Non-explosive silicic volcanism
Eichelberger, J. C., Carrigan, C. R., Westrich, H. R., & Price, R. H. (1986) · Nature · doi:10.1038/323598a0 · Cited by 631
Viscosities of hydrous leucogranitic melts: A non-Arrhenian model
Hess, K., & Dingwell, D. B. (1996) · American Mineralogist · doi:10.2138/am-1996-9-1031 · Cited by 569
Cited by
Violent expiratory events: on coughing and sneezing
Bourouiba, L., Dehandschoewercker, E., & Bush, J. W. M. (2014) · Journal of Fluid Mechanics · doi:10.1017/jfm.2014.88 · Cited by 828
The fluid dynamics of disease transmission
Bourouiba, L. (2021) · Annual Review of Fluid Mechanics · doi:10.1146/annurev-fluid-060220-113712 · Cited by 366
Excess degassing from volcanoes and its role on eruptive and intrusive activity
Shinohara, H. (2008) · Reviews of Geophysics · doi:10.1029/2007rg000244 · Cited by 323
Accelerating geoscience and engineering system simulations on graphics hardware
Walsh, S. D. C., Saar, M. O., Bailey, P., & Lilja, D. J. (2009) · Computers & Geosciences · doi:10.1016/j.cageo.2009.05.001 · Cited by 63
Metadata
- Authors
- Gonnermann, H. M., & Manga, M.
- Venue
- Annual Review of Fluid Mechanics
- Publisher
- Annual Reviews
- Published
- 2007-01-01
- Volume
- 39
- Issue
- 1
- Pages
- 321-356
- ISSN
- 0066-4189 (ISSN-L)
- 1545-4479
- OpenAlex
- W2145853140
- Cited by
- 489
- References
- 69
- FWCI
- 2.34
- Type
- journal article
- Language
- en
- Open access
- closed
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review
How to cite
Cite CoChat for the checks on this page, and the paper for its own findings.
- This page
- CoChat. (2026). Citation check: The Fluid Mechanics Inside a Volcano. https://app.cochat.ai/papers/10.1146/annurev.fluid.39.050905.110207
- The paper
- Gonnermann, H. M., & Manga, M. (2007). The Fluid Mechanics Inside a Volcano. Annual Review of Fluid Mechanics. https://doi.org/10.1146/annurev.fluid.39.050905.110207
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
