Homogeneous bubble nucleation in H2O- and H2O-CO2-bearing basaltic melts: results of high temperature decompression experiments - Archive ouverte HAL Access content directly
Journal Articles Journal of Volcanology and Geothermal Research Year : 2016

Homogeneous bubble nucleation in H2O- and H2O-CO2-bearing basaltic melts: results of high temperature decompression experiments

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Abstract

High pressure and temperature decompression experiments were conducted to provide experimental information on the conditions of homogeneous bubble nucleation in basaltic melts. Experiments were performed on H2O- and H2O-CO2-bearing natural melts from Stromboli. Three starting volatile compositions were investigated: series #1 (4.91 wt.% H2O, no CO2), series #2 (2.37–2.45 wt.% H2O, 901–1011 ppm CO2) and series #3 (0.80–1.09 wt.% H2O, 840–923 ppm CO2). The volatile-bearing glasses were first synthesized at 1200°C and 200 MPa, and second continuously decompressed in the pressure range 150–25 MPa and rapidly quenched. A fast decompression rate of 78 kPa/s (or 3 m/s) was applied to limit the water loss from the glass cylinder and the formation of a H2O-depleted rim. Post-decompression glasses were characterized texturally by X-ray microtomography. The results demonstrate that homogenous bubble nucleation requires supersaturation pressures (difference between saturation pressure and pressure at which homogeneous bubble nucleation is observed, ∆ PHoN) ≤ 50–100 MPa. ∆ PHoN varies with the dissolved CO2 concentration, from << 50 MPa (no CO2, series #1) to ≤ 50 MPa (872 ± 45 ppm CO2, series #3) to < 100 MPa (973 ± 63 ppm CO2, series #2). In series #1 melts, homogeneous bubble nucleation occurs as two distinct events, the first at high pressure (200 < P < 150 MPa) and the second at low pressure (50 < P < 25 MPa), just below the fragmentation level. In contrast, homogenous nucleation in series #2 and #3 melts is a continuous process. As well, chemical near-equilibrium degassing occurs in the series #1 melts, unlike in the series #2 and #3 melts which retain high CO2 concentrations even for higher vesicularities (up to 23% at 25 MPa). Thus, our experimental observations underline a significant effect of CO2 on the physical mechanisms of bubble vesiculation in basaltic melts. Our experimental decompression textures either reproduce or approach the characteristics of explosive basaltic eruptions, in terms of vesicularity, bubble shapes, sizes and number densities. Unimodal, exponential to power law bubble size distributions were encountered and correlated with the different melt series, textural characteristics and types of degassing.
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Dates and versions

insu-01378576 , version 1 (11-10-2016)

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Attribution - NonCommercial - NoDerivatives - CC BY 4.0

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Nolwenn Le Gall, Michel Pichavant. Homogeneous bubble nucleation in H2O- and H2O-CO2-bearing basaltic melts: results of high temperature decompression experiments. Journal of Volcanology and Geothermal Research, 2016, 327, pp.604-621. ⟨10.1016/j.jvolgeores.2016.10.004⟩. ⟨insu-01378576⟩
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