Antonio Said Webbe Sales, Airton Natanael Coelho Dias, Sandro Guedes, Marcela Guinther Medeiros, Vinicius de Queirós Pereira
{"title":"巴西Serra Geral火山杂岩ZAD锆石诱导裂变径迹的热退火动力学","authors":"Antonio Said Webbe Sales, Airton Natanael Coelho Dias, Sandro Guedes, Marcela Guinther Medeiros, Vinicius de Queirós Pereira","doi":"10.1007/s00269-025-01323-x","DOIUrl":null,"url":null,"abstract":"<div>\n \n <p>This study investigates the thermal annealing kinetics of induced fission tracks in ZAD zircon from the Serra Geral Volcanic Complex, Brazil, and compares results with previously studied ZPC zircon. Both samples underwent identical pre-annealing treatment (1100 °C for 1 h) to remove fossil fission tracks before neutron irradiation and heating experiments at temperatures between 500 and 800 °C for durations of 1–100 h. Comprehensive statistical analysis, including Kolmogorov–Smirnov tests and effect size calculations, confirmed that observed differences between samples reflect genuine material properties rather than measurement bias. ZAD exhibited significantly higher annealing rates and lower activation energy (62 ± 14 kcal/mol) compared to ZPC (80 ± 20 kcal/mol), despite both samples undergoing identical laboratory procedures. This differential behavior is attributed to ZAD’s 20% higher accumulated α-recoil damage (3.34 × 10<sup>16</sup> vs. 2.67 × 10<sup>16</sup> decays/g), which persists as residual damage even after pre-annealing treatment. Calculations of displacements per atom (dpa) further quantified this difference (1.07 × 10<sup>−3</sup> for ZAD vs. 8.5 × <sup>−4</sup> for ZPC). The study demonstrates how radiation damage accumulated over different timescales (134 Ma for ZAD vs. 80 Ma for ZPC) creates distinct microstructural defect patterns that significantly influence fission track annealing kinetics, with important implications for zircon thermochronology interpretations and geological thermal history reconstruction.</p>\n </div>","PeriodicalId":20132,"journal":{"name":"Physics and Chemistry of Minerals","volume":"52 3","pages":""},"PeriodicalIF":1.6000,"publicationDate":"2025-07-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Thermal annealing kinetics of induced fission tracks in ZAD zircon from the Serra Geral Volcanic Complex, Brazil\",\"authors\":\"Antonio Said Webbe Sales, Airton Natanael Coelho Dias, Sandro Guedes, Marcela Guinther Medeiros, Vinicius de Queirós Pereira\",\"doi\":\"10.1007/s00269-025-01323-x\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div>\\n \\n <p>This study investigates the thermal annealing kinetics of induced fission tracks in ZAD zircon from the Serra Geral Volcanic Complex, Brazil, and compares results with previously studied ZPC zircon. Both samples underwent identical pre-annealing treatment (1100 °C for 1 h) to remove fossil fission tracks before neutron irradiation and heating experiments at temperatures between 500 and 800 °C for durations of 1–100 h. Comprehensive statistical analysis, including Kolmogorov–Smirnov tests and effect size calculations, confirmed that observed differences between samples reflect genuine material properties rather than measurement bias. ZAD exhibited significantly higher annealing rates and lower activation energy (62 ± 14 kcal/mol) compared to ZPC (80 ± 20 kcal/mol), despite both samples undergoing identical laboratory procedures. This differential behavior is attributed to ZAD’s 20% higher accumulated α-recoil damage (3.34 × 10<sup>16</sup> vs. 2.67 × 10<sup>16</sup> decays/g), which persists as residual damage even after pre-annealing treatment. Calculations of displacements per atom (dpa) further quantified this difference (1.07 × 10<sup>−3</sup> for ZAD vs. 8.5 × <sup>−4</sup> for ZPC). The study demonstrates how radiation damage accumulated over different timescales (134 Ma for ZAD vs. 80 Ma for ZPC) creates distinct microstructural defect patterns that significantly influence fission track annealing kinetics, with important implications for zircon thermochronology interpretations and geological thermal history reconstruction.</p>\\n </div>\",\"PeriodicalId\":20132,\"journal\":{\"name\":\"Physics and Chemistry of Minerals\",\"volume\":\"52 3\",\"pages\":\"\"},\"PeriodicalIF\":1.6000,\"publicationDate\":\"2025-07-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Physics and Chemistry of Minerals\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s00269-025-01323-x\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"MATERIALS SCIENCE, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physics and Chemistry of Minerals","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s00269-025-01323-x","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"MATERIALS SCIENCE, MULTIDISCIPLINARY","Score":null,"Total":0}
Thermal annealing kinetics of induced fission tracks in ZAD zircon from the Serra Geral Volcanic Complex, Brazil
This study investigates the thermal annealing kinetics of induced fission tracks in ZAD zircon from the Serra Geral Volcanic Complex, Brazil, and compares results with previously studied ZPC zircon. Both samples underwent identical pre-annealing treatment (1100 °C for 1 h) to remove fossil fission tracks before neutron irradiation and heating experiments at temperatures between 500 and 800 °C for durations of 1–100 h. Comprehensive statistical analysis, including Kolmogorov–Smirnov tests and effect size calculations, confirmed that observed differences between samples reflect genuine material properties rather than measurement bias. ZAD exhibited significantly higher annealing rates and lower activation energy (62 ± 14 kcal/mol) compared to ZPC (80 ± 20 kcal/mol), despite both samples undergoing identical laboratory procedures. This differential behavior is attributed to ZAD’s 20% higher accumulated α-recoil damage (3.34 × 1016 vs. 2.67 × 1016 decays/g), which persists as residual damage even after pre-annealing treatment. Calculations of displacements per atom (dpa) further quantified this difference (1.07 × 10−3 for ZAD vs. 8.5 × −4 for ZPC). The study demonstrates how radiation damage accumulated over different timescales (134 Ma for ZAD vs. 80 Ma for ZPC) creates distinct microstructural defect patterns that significantly influence fission track annealing kinetics, with important implications for zircon thermochronology interpretations and geological thermal history reconstruction.
期刊介绍:
Physics and Chemistry of Minerals is an international journal devoted to publishing articles and short communications of physical or chemical studies on minerals or solids related to minerals. The aim of the journal is to support competent interdisciplinary work in mineralogy and physics or chemistry. Particular emphasis is placed on applications of modern techniques or new theories and models to interpret atomic structures and physical or chemical properties of minerals. Some subjects of interest are:
-Relationships between atomic structure and crystalline state (structures of various states, crystal energies, crystal growth, thermodynamic studies, phase transformations, solid solution, exsolution phenomena, etc.)
-General solid state spectroscopy (ultraviolet, visible, infrared, Raman, ESCA, luminescence, X-ray, electron paramagnetic resonance, nuclear magnetic resonance, gamma ray resonance, etc.)
-Experimental and theoretical analysis of chemical bonding in minerals (application of crystal field, molecular orbital, band theories, etc.)
-Physical properties (magnetic, mechanical, electric, optical, thermodynamic, etc.)
-Relations between thermal expansion, compressibility, elastic constants, and fundamental properties of atomic structure, particularly as applied to geophysical problems
-Electron microscopy in support of physical and chemical studies
-Computational methods in the study of the structure and properties of minerals
-Mineral surfaces (experimental methods, structure and properties)