A lower bound on the rheological evolution of magmatic liquids during the 2018 Kilauea eruption
A lower bound on the rheological evolution of magmatic liquids during the 2018 Kilauea eruption
复制标题
2018 年基拉韦厄火山喷发期间岩浆液体流变演化的下限
DOI:
10.1016/j.chemgeo.2021.120272
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发表时间:
2021
期刊:
影响因子:
3.9
通讯作者:
Dingwell, D.B.
中科院分区:
文献类型:
--
作者:
Soldati, A.;Houghton, B.F.;Dingwell, D.B.
During the four month-long 2018 Kilauea Lower East Rift Zone (LERZ) eruption, the bulk chemical compositions of magma ranged from basalt to andesite. This compositional variety was reflected in eruptive style, which ranged from Hawaiian fountaining to Strombolian explosions. Here, we quantified the evolution of the melt viscosity of the eruptive products through high-temperature laboratory experiments performed on a representative sample set that was collected in the field immediately after the eruptive series. This suite of 18 samples comprises all major eruptive phases (early phase I, late phase I, phase II, phase III, fissure 17). The results illustrate the significant rheological variability of the eruptive products, and appear to link to variations in eruption dynamics. We propose a new standard for the rheological study of a multi-episode effusive eruption, whereby precise, near-real-time viscosity results are obtained during ongoing eruptions will become a routine component of volcano monitoring during future eruptive events.Plain language summaryDuring the 2018 eruption of Kilauea, emerging magma spanned a wider compositional range than ever previously observed during a single eruption. This compositional diversity was matched by a variety in eruptive styles, which ranged from more persistent fountaining to short-lived explosions. Immediately after the eruption ceased, we collected a representative suite of 18 samples in the field, which comprises all major eruptive phases (early phase I, late phase I, phase II, phase III, fissure 17). We measured the melt viscosity of such samples through high-temperature laboratory experiments. The results illustrate a significant variability in viscosity, which is linked to the highly variable eruption dynamics. Here we propose a new standard for the study of multi-episode effusive eruptions from a viscosity standpoint. We hope and expect that this methodology will become routine practice during future eruption.
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影响因子:
2.3
作者:
G. Meerlender
通讯作者:
G. Meerlender
影响因子:
--
作者:
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通讯作者:
S. Arellano
影响因子:
56.9
作者:
Gansecki, Cheryl;Lee, R. Lopaka;Parcheta, Carolyn
通讯作者:
Parcheta, Carolyn
影响因子:
5.3
作者:
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通讯作者:
C. Losq;D. Neuville;R. Moretti;P. Kyle;C. Oppenheimer
影响因子:
1
作者:
Harris, Andrew J. L.;Chevrel, Magdalena Oryaelle;Gurioli, Lucia
通讯作者:
Gurioli, Lucia