{"title":"300 GPa以下镍的Hugoniot状态方程:对地球固体内核密度缺陷的启示","authors":"Qing Zhang, Xun Liu, Yishi Wang, Yu Hu, Zehui Li, Haijun Huang","doi":"10.1016/j.pepi.2025.107454","DOIUrl":null,"url":null,"abstract":"<div><div>Hugoniot data for nickel (Ni) were extended to 305 GPa through plate-impact experiments using a two-stage light gas gun. Combining our results with previously published data, we determined the shock velocity (<em>Us</em>)–particle velocity (<em>Up</em>) Hugoniot relation for Ni to be: <span><math><msub><mi>U</mi><mi>s</mi></msub><mo>=</mo><mn>4.653</mn><mfenced><mn>62</mn></mfenced><mo>+</mo><mn>1.420</mn><mfenced><mn>23</mn></mfenced><msub><mi>U</mi><mi>p</mi></msub></math></span>. The thermodynamic parameters of Ni were derived through a joint analysis of the Hugoniot and static compression data, allowing us to extend the equation of state (EOS) to conditions relevant to Earth's inner core. Additionally, we reanalyzed the EOS of iron based on a recently published static compression data. Our study suggests that the density of pure iron is 0.59 (20) g/cm<sup>3</sup> higher than that of the inner core. Moreover, adding 10 wt% Ni to iron increases this density deficit by approximately 0.10 g/cm<sup>3</sup>.</div></div>","PeriodicalId":54614,"journal":{"name":"Physics of the Earth and Planetary Interiors","volume":"368 ","pages":"Article 107454"},"PeriodicalIF":1.9000,"publicationDate":"2025-09-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Hugoniot equation of state of nickel up to 300 GPa: Implication on the density deficit of earth's solid inner core\",\"authors\":\"Qing Zhang, Xun Liu, Yishi Wang, Yu Hu, Zehui Li, Haijun Huang\",\"doi\":\"10.1016/j.pepi.2025.107454\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Hugoniot data for nickel (Ni) were extended to 305 GPa through plate-impact experiments using a two-stage light gas gun. Combining our results with previously published data, we determined the shock velocity (<em>Us</em>)–particle velocity (<em>Up</em>) Hugoniot relation for Ni to be: <span><math><msub><mi>U</mi><mi>s</mi></msub><mo>=</mo><mn>4.653</mn><mfenced><mn>62</mn></mfenced><mo>+</mo><mn>1.420</mn><mfenced><mn>23</mn></mfenced><msub><mi>U</mi><mi>p</mi></msub></math></span>. The thermodynamic parameters of Ni were derived through a joint analysis of the Hugoniot and static compression data, allowing us to extend the equation of state (EOS) to conditions relevant to Earth's inner core. Additionally, we reanalyzed the EOS of iron based on a recently published static compression data. Our study suggests that the density of pure iron is 0.59 (20) g/cm<sup>3</sup> higher than that of the inner core. Moreover, adding 10 wt% Ni to iron increases this density deficit by approximately 0.10 g/cm<sup>3</sup>.</div></div>\",\"PeriodicalId\":54614,\"journal\":{\"name\":\"Physics of the Earth and Planetary Interiors\",\"volume\":\"368 \",\"pages\":\"Article 107454\"},\"PeriodicalIF\":1.9000,\"publicationDate\":\"2025-09-20\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Physics of the Earth and Planetary Interiors\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0031920125001487\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physics of the Earth and Planetary Interiors","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0031920125001487","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Hugoniot equation of state of nickel up to 300 GPa: Implication on the density deficit of earth's solid inner core
Hugoniot data for nickel (Ni) were extended to 305 GPa through plate-impact experiments using a two-stage light gas gun. Combining our results with previously published data, we determined the shock velocity (Us)–particle velocity (Up) Hugoniot relation for Ni to be: . The thermodynamic parameters of Ni were derived through a joint analysis of the Hugoniot and static compression data, allowing us to extend the equation of state (EOS) to conditions relevant to Earth's inner core. Additionally, we reanalyzed the EOS of iron based on a recently published static compression data. Our study suggests that the density of pure iron is 0.59 (20) g/cm3 higher than that of the inner core. Moreover, adding 10 wt% Ni to iron increases this density deficit by approximately 0.10 g/cm3.
期刊介绍:
Launched in 1968 to fill the need for an international journal in the field of planetary physics, geodesy and geophysics, Physics of the Earth and Planetary Interiors has now grown to become important reading matter for all geophysicists. It is the only journal to be entirely devoted to the physical and chemical processes of planetary interiors.
Original research papers, review articles, short communications and book reviews are all published on a regular basis; and from time to time special issues of the journal are devoted to the publication of the proceedings of symposia and congresses which the editors feel will be of particular interest to the reader.