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Crystal fractionation by crystal-driven convection

Crystal fractionation by crystal-driven convection
Crystal fractionation by crystal-driven convection
Fractional crystallization is an essential process proposed to explain worldwide compositional abundances of igneous rocks. It requires crystals to precipitate from the melt and segregate from its residual melt, or experience crystal fractionation. The compositional abundances of volcanic systems show a bell curve distribution suggesting that the process has variable efficiencies. We test crystal fractionation efficiency in convective flow in low to intermediate crystallinity regime. We simulate the physical segregation of crystals from their residual melt at the scale of individual crystals, using a direct numerical method. We find that at low particle Reynolds numbers, crystals sink in clusters. The relatively rapid motion of clusters strips away residual melt. Our results show cluster settling can imprint observational signatures at the crystalline scale. The collective crystal behavior results in a crystal convection that governs the efficiency of crystal fractionation, providing a possible explanation for the bell curve distribution in volcanic systems.
0094-8276
Culha, Cansu
fb70d46d-e069-44ee-9472-7eb540f1235a
Suckale, Jenny
2f422629-845e-4186-bf3a-c00dd1a417d6
Keller, Tobias
d8dfcfa5-89d1-4203-aa2d-8c142c00a169
Qin, Zhipeng
e45392ee-5cc0-41f1-9eaf-7072c83882b9
Culha, Cansu
fb70d46d-e069-44ee-9472-7eb540f1235a
Suckale, Jenny
2f422629-845e-4186-bf3a-c00dd1a417d6
Keller, Tobias
d8dfcfa5-89d1-4203-aa2d-8c142c00a169
Qin, Zhipeng
e45392ee-5cc0-41f1-9eaf-7072c83882b9

Culha, Cansu, Suckale, Jenny, Keller, Tobias and Qin, Zhipeng (2020) Crystal fractionation by crystal-driven convection. Geophysical Research Letters. (doi:10.1029/2019GL086784).

Record type: Article

Abstract

Fractional crystallization is an essential process proposed to explain worldwide compositional abundances of igneous rocks. It requires crystals to precipitate from the melt and segregate from its residual melt, or experience crystal fractionation. The compositional abundances of volcanic systems show a bell curve distribution suggesting that the process has variable efficiencies. We test crystal fractionation efficiency in convective flow in low to intermediate crystallinity regime. We simulate the physical segregation of crystals from their residual melt at the scale of individual crystals, using a direct numerical method. We find that at low particle Reynolds numbers, crystals sink in clusters. The relatively rapid motion of clusters strips away residual melt. Our results show cluster settling can imprint observational signatures at the crystalline scale. The collective crystal behavior results in a crystal convection that governs the efficiency of crystal fractionation, providing a possible explanation for the bell curve distribution in volcanic systems.

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Published date: 7 February 2020

Identifiers

Local EPrints ID: 488274
URI: http://eprints.soton.ac.uk/id/eprint/488274
ISSN: 0094-8276
PURE UUID: 072d106e-2773-4dba-8e40-6bcd97c3ca88
ORCID for Tobias Keller: ORCID iD orcid.org/0000-0002-6121-5377

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Date deposited: 19 Mar 2024 17:53
Last modified: 21 Mar 2024 03:16

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Contributors

Author: Cansu Culha
Author: Jenny Suckale
Author: Tobias Keller ORCID iD
Author: Zhipeng Qin

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