Bubbles to Chondrites-I. Evaporation and condensation experiments, and formation of chondrules

Abstract We propose a simple model of chondrule formation that is supported by our new experiments. With a laser-heating and inert-gas-cooling technique, we obtained evaporation and condensation pathways starting with chondritic compositions till ends, and extracted ‘relative volatilities’ of elemen...

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Main Authors: Yuki Nakano, Akihiko Hashimoto
Format: Article
Language:English
Published: SpringerOpen 2020-09-01
Series:Progress in Earth and Planetary Science
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40645-020-00335-1
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spelling doaj-892b004d5ec849859adaa1c7b0bdd9f02020-11-25T02:41:54ZengSpringerOpenProgress in Earth and Planetary Science2197-42842020-09-017113710.1186/s40645-020-00335-1Bubbles to Chondrites-I. Evaporation and condensation experiments, and formation of chondrulesYuki Nakano0Akihiko Hashimoto1Department of Cosmosciences, Hokkaido UniversitySuns & Fishermen SocietyAbstract We propose a simple model of chondrule formation that is supported by our new experiments. With a laser-heating and inert-gas-cooling technique, we obtained evaporation and condensation pathways starting with chondritic compositions till ends, and extracted ‘relative volatilities’ of elements from them. Above boiling points, we observed numerous silicate droplets being ejected from collapsed cavities of vapor bubbles on the surface of molten sample, known as jet-droplets. We postulate jet-droplets as origin of chondrules. The formation mechanism of jet-droplets requires a dense and large solid body (>3 cm across), named ‘duston’, for chondrule precursors. Our chondrule formation model presumes dustons having CI-like composition. Upon boiling, a duston ejects jet-droplets from its molten surface and simultaneously forms an adiabatically expanding vapor cloud around it. The jet-droplets supercool and incorporate the supersaturated vapor and fine condensates while they travel through the cloud, thus completing their makeup as chondrules. The compositions and the mixing ratio of the three components (jet-droplet, vapor and condensate) can be exactly predicted by using relative volatilities of elements, given the chondrule composition to be fitted and the conditions: vaporization degree (VD) and redox state (f s ) of the duston. We attempt to reproduce bulk compositions of chondrules in total of 600. About 75% chondrules are successfully matched with specific combinations of VD and f s for each chondrule. The model altogether explains 3.5 features of chondrules: maximum size and size-frequency distribution; chemical variety; and textural variety.http://link.springer.com/article/10.1186/s40645-020-00335-1EvaporationCondensationExperimentChondruleChemical fractionationBoiling
collection DOAJ
language English
format Article
sources DOAJ
author Yuki Nakano
Akihiko Hashimoto
spellingShingle Yuki Nakano
Akihiko Hashimoto
Bubbles to Chondrites-I. Evaporation and condensation experiments, and formation of chondrules
Progress in Earth and Planetary Science
Evaporation
Condensation
Experiment
Chondrule
Chemical fractionation
Boiling
author_facet Yuki Nakano
Akihiko Hashimoto
author_sort Yuki Nakano
title Bubbles to Chondrites-I. Evaporation and condensation experiments, and formation of chondrules
title_short Bubbles to Chondrites-I. Evaporation and condensation experiments, and formation of chondrules
title_full Bubbles to Chondrites-I. Evaporation and condensation experiments, and formation of chondrules
title_fullStr Bubbles to Chondrites-I. Evaporation and condensation experiments, and formation of chondrules
title_full_unstemmed Bubbles to Chondrites-I. Evaporation and condensation experiments, and formation of chondrules
title_sort bubbles to chondrites-i. evaporation and condensation experiments, and formation of chondrules
publisher SpringerOpen
series Progress in Earth and Planetary Science
issn 2197-4284
publishDate 2020-09-01
description Abstract We propose a simple model of chondrule formation that is supported by our new experiments. With a laser-heating and inert-gas-cooling technique, we obtained evaporation and condensation pathways starting with chondritic compositions till ends, and extracted ‘relative volatilities’ of elements from them. Above boiling points, we observed numerous silicate droplets being ejected from collapsed cavities of vapor bubbles on the surface of molten sample, known as jet-droplets. We postulate jet-droplets as origin of chondrules. The formation mechanism of jet-droplets requires a dense and large solid body (>3 cm across), named ‘duston’, for chondrule precursors. Our chondrule formation model presumes dustons having CI-like composition. Upon boiling, a duston ejects jet-droplets from its molten surface and simultaneously forms an adiabatically expanding vapor cloud around it. The jet-droplets supercool and incorporate the supersaturated vapor and fine condensates while they travel through the cloud, thus completing their makeup as chondrules. The compositions and the mixing ratio of the three components (jet-droplet, vapor and condensate) can be exactly predicted by using relative volatilities of elements, given the chondrule composition to be fitted and the conditions: vaporization degree (VD) and redox state (f s ) of the duston. We attempt to reproduce bulk compositions of chondrules in total of 600. About 75% chondrules are successfully matched with specific combinations of VD and f s for each chondrule. The model altogether explains 3.5 features of chondrules: maximum size and size-frequency distribution; chemical variety; and textural variety.
topic Evaporation
Condensation
Experiment
Chondrule
Chemical fractionation
Boiling
url http://link.springer.com/article/10.1186/s40645-020-00335-1
work_keys_str_mv AT yukinakano bubblestochondritesievaporationandcondensationexperimentsandformationofchondrules
AT akihikohashimoto bubblestochondritesievaporationandcondensationexperimentsandformationofchondrules
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