Coalescence of Growing Bubbles in Highly Viscous Liquids

نویسندگان

چکیده

Abstract Bubble coalescence in ascending magma is a key process that controls the eruption violence and texture of volcanic pyroclasts. In present study, we performed situ experiments to investigate two growing bubbles highly viscous liquids (102 1,020 Pa ⋅ s). A new experimental apparatus enables us directly observe drainage film between three dimensions. We combined results simple scaling analysis reveal dynamics terms capillary number depending on liquid viscosity η , bubble growth rate surface tension σ . The represents interplay force arising from force. At Ca ≪ 1, adjacent retain their spherical shapes until ruptures, forces control timescale. contrast, at ≫ largely flatten itself drives drainage. also provide general formula for timescale over wide range numbers (10 −3 < 10 1 ). Our highlight importance process. variations shape density during decompression can be explained by number.

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ژورنال

عنوان ژورنال: Geochemistry Geophysics Geosystems

سال: 2022

ISSN: ['1525-2027']

DOI: https://doi.org/10.1029/2022gc010618