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 , Marissa M. Tremblay , Peter K. Zeitler , Bruce D. Idleman , 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.
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.