Climate Change Data Portal
DOI | 10.1016/j.epsl.2021.117008 |
Origin of hydrogen isotopic variations in chondritic water and organics | |
Piani L.; Marrocchi Y.; Vacher L.G.; Yurimoto H.; Bizzarro M. | |
发表日期 | 2021 |
ISSN | 0012821X |
卷号 | 567 |
英文摘要 | Chondrites are rocky fragments of asteroids that formed at different times and heliocentric distances in the early solar system. Most chondrite groups contain water-bearing minerals, attesting that both water-ice and dust were accreted on their parent asteroids. Nonetheless, the hydrogen isotopic composition (D/H) of water in the different chondrite groups remains poorly constrained, due to the intimate mixture of hydrated minerals and organic compounds, the other main H-bearing phase in chondrites. Building on our recent works using in situ secondary ion mass spectrometry analyses, we determined the H isotopic composition of water in a large set of chondritic samples (CI, CM, CO, CR, and C-ungrouped carbonaceous chondrites) and report that water in each group shows a distinct and unique D/H signature. Based on a comparison with literature data on bulk chondrites and their water and organics, our data do not support a preponderant role of parent-body processes in controlling the D/H variations among chondrites. Instead, we propose that the water and organic D/H signatures were mostly shaped by interactions between the protoplanetary disk and the molecular cloud that episodically fed the disk over several million years. Because the preservation of D-rich interstellar water and/or organics in chondritic materials is only possible below their respective sublimation temperatures (160 and 350–450 K), the H isotopic signatures of chondritic materials depend on both the timing and location at which their parent body formed. © 2021 Elsevier B.V. |
关键词 | chondritediskhydrogen isotopesmolecular cloudorganic matterwater |
英文关键词 | Hydrogen bonds; Isotopes; Meteorites; Organic compounds; Secondary ion mass spectrometry; Water; Disk; Heliocentric distances; Hydrogen isotope; Hydrogen isotopic; Isotopic variations; Molecular clouds; Organic matter; Organics; Parent bodies; Time-distance; Hydrogen |
语种 | 英语 |
来源期刊 | Earth and Planetary Science Letters
![]() |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/203253 |
作者单位 | Université de Lorraine, CNRS, CRPG, UMR 7358, Vandoeuvre les Nancy, France; Laboratory for Space Sciences, the Department of Physics, Washington University in St. Louis, St. Louis, MO 63130, United States; Department of Natural History Sciences, Faculty of Science, Hokkaido University, Sapporo, Japan; StarPlan - Centre for Star and Planet Formation, GLOBE Institute, University of Copenhagen, Øster Voldgade 5-7, Copenhagen, DK-1350, Denmark |
推荐引用方式 GB/T 7714 | Piani L.,Marrocchi Y.,Vacher L.G.,et al. Origin of hydrogen isotopic variations in chondritic water and organics[J],2021,567. |
APA | Piani L.,Marrocchi Y.,Vacher L.G.,Yurimoto H.,&Bizzarro M..(2021).Origin of hydrogen isotopic variations in chondritic water and organics.Earth and Planetary Science Letters,567. |
MLA | Piani L.,et al."Origin of hydrogen isotopic variations in chondritic water and organics".Earth and Planetary Science Letters 567(2021). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。