58
C.
De Campos et al.
Previous numerical simulations
of
mixing between basalt and granite,
in the same proportions as in this work (95% granite
+ 5% basalt) and
the same viscosity contrast, point towards mixing probabilities around
zero (Jellinek et aI., 1999). The combination
of
convection and chaotic
dynamics, however, greatly enhances the diffusive processes in molten
silicate melts over filament or lamellae dimensions.
Preliminary analytical results reveal different mobility and mixing
efficiency for different elements, which are presented in this work
as
oxides. This way, despite very low diffusion coefficients and a very
short mixing time (154 min),
CaO and MgO may reach mixing
efficiency coefficients around 5% while
K
2
0 and Na20 come closer to
50% (0.43 and 0.48).
The application
of
this device under geologically relevant conditions
has demonstrated that chaotic mixing processes are very efficient ways
to mix silicate melts.
Acknowledgements: Thanks
to
Philippe Courtialfor REE-rich glasses used
in
sample preparation and INGV /Unrest / Italy forfunding.
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