Systematics of helium diffusion sinks in apatite demonstrated by 4He/3He degassing experiments and modeling

IF 4.5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Hongcheng Guo , Marissa M. Tremblay , Peter K. Zeitler , Bruce D. Idleman , Annia K. Fayon
{"title":"Systematics of helium diffusion sinks in apatite demonstrated by 4He/3He degassing experiments and modeling","authors":"Hongcheng Guo ,&nbsp;Marissa M. Tremblay ,&nbsp;Peter K. Zeitler ,&nbsp;Bruce D. Idleman ,&nbsp;Annia K. Fayon","doi":"10.1016/j.gca.2025.05.036","DOIUrl":null,"url":null,"abstract":"<div><div>Widely reported overdispersion of apatite (U-Th)/He ages has encouraged efforts to explore He diffusion kinetics and systematics in apatite. Studies such as continuous ramped heating (CRH) of apatite have revealed complex laboratory He behavior that is often correlated with abnormally old (U-Th)/He ages. Stemming from these studies is a hypothesis that diffusion sinks within apatite grains can reversibly trap radiogenic <sup>4</sup>He over both geologic time and during laboratory heating. This sink-related trapping is further hypothesized to be temperature dependent and can hence potentially provide thermal-history information. In this work, we conducted <sup>4</sup>He/<sup>3</sup>He degassing experiments from proton-irradiated apatite samples using a CRH-like heating strategy. We demonstrate that the synthesized <sup>3</sup>He also exhibits complex release behavior which (1) confirms that the proposed sink-related trapping occurs during laboratory heating, and (2) provides foundational evidence for possibly qualifying the nature and quantifying the abundance and/or distribution of diffusion sinks. Our combined <sup>4</sup>He/<sup>3</sup>He observations show that an apatite sample’s thermal history controls the amount of trapping over geologic time. Building upon the dataset from one of the sink-bearing samples, we attempt to simulate the sink characteristics using a simple random-walk code that can simulate trapping. The forward modeling can reproduce the <sup>3</sup>He release observed in the laboratory experiment if multiple sinks characterized by different kinetics are present. Using such sink kinetics and the sample’s known thermal history, we find that the prediction of laboratory <sup>4</sup>He release, which reflects both geologic and laboratory volume diffusion and trapping processes, is comparable to our observations. This work confirms that a temperature-dependent trapping mechanism is required to explain the complex He diffusion behavior seen in many apatite grains, and also serves as a proof-of-concept that helium trapped in sinks can provide added thermal history information.</div></div>","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"400 ","pages":"Pages 115-128"},"PeriodicalIF":4.5000,"publicationDate":"2025-05-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochimica et Cosmochimica Acta","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0016703725002923","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

Abstract

Widely reported overdispersion of apatite (U-Th)/He ages has encouraged efforts to explore He diffusion kinetics and systematics in apatite. Studies such as continuous ramped heating (CRH) of apatite have revealed complex laboratory He behavior that is often correlated with abnormally old (U-Th)/He ages. Stemming from these studies is a hypothesis that diffusion sinks within apatite grains can reversibly trap radiogenic 4He over both geologic time and during laboratory heating. This sink-related trapping is further hypothesized to be temperature dependent and can hence potentially provide thermal-history information. In this work, we conducted 4He/3He degassing experiments from proton-irradiated apatite samples using a CRH-like heating strategy. We demonstrate that the synthesized 3He also exhibits complex release behavior which (1) confirms that the proposed sink-related trapping occurs during laboratory heating, and (2) provides foundational evidence for possibly qualifying the nature and quantifying the abundance and/or distribution of diffusion sinks. Our combined 4He/3He observations show that an apatite sample’s thermal history controls the amount of trapping over geologic time. Building upon the dataset from one of the sink-bearing samples, we attempt to simulate the sink characteristics using a simple random-walk code that can simulate trapping. The forward modeling can reproduce the 3He release observed in the laboratory experiment if multiple sinks characterized by different kinetics are present. Using such sink kinetics and the sample’s known thermal history, we find that the prediction of laboratory 4He release, which reflects both geologic and laboratory volume diffusion and trapping processes, is comparable to our observations. This work confirms that a temperature-dependent trapping mechanism is required to explain the complex He diffusion behavior seen in many apatite grains, and also serves as a proof-of-concept that helium trapped in sinks can provide added thermal history information.
通过4He/3He脱气实验和模型验证了磷灰石中氦扩散汇的系统
广泛报道的磷灰石(U-Th)/He年龄的过度分散促进了对磷灰石中He扩散动力学和系统的研究。诸如磷灰石的连续斜坡加热(CRH)等研究揭示了复杂的实验室He行为,这些行为通常与异常老(U-Th)/He年龄相关。这些研究提出了一种假设,即磷灰石颗粒内的扩散汇可以在地质时期和实验室加热期间可逆地捕获放射性成因的氦。这种与碳汇相关的捕获进一步假设与温度有关,因此可能提供热历史信息。在这项工作中,我们使用类似crh的加热策略对质子辐照磷灰石样品进行了4He/3He脱气实验。我们证明,合成的3He也表现出复杂的释放行为,这(1)证实了在实验室加热过程中所提出的与汇相关的捕获发生,(2)为可能确定扩散汇的性质和定量丰度和/或分布提供了基础证据。我们的4He/3He综合观测表明,在地质时期,磷灰石样品的热历史控制着捕获量。基于来自其中一个承载汇的样本的数据集,我们尝试使用可以模拟捕获的简单随机漫步代码来模拟汇特征。如果存在以不同动力学特征为特征的多个汇,则正演模拟可以再现实验室实验中观察到的3He释放。利用这种汇动力学和样品已知的热历史,我们发现实验室4He释放的预测反映了地质和实验室体积扩散和捕获过程,与我们的观察结果相当。这项工作证实,需要一个温度依赖的捕获机制来解释在许多磷灰石颗粒中看到的复杂的He扩散行为,并且也可以作为一个概念证明,在汇中捕获的氦可以提供额外的热历史信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta 地学-地球化学与地球物理
CiteScore
9.60
自引率
14.00%
发文量
437
审稿时长
6 months
期刊介绍: Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes: 1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids 2). Igneous and metamorphic petrology 3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth 4). Organic geochemistry 5). Isotope geochemistry 6). Meteoritics and meteorite impacts 7). Lunar science; and 8). Planetary geochemistry.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信