Hydrogen in the Earth core inferred from neutron imaging and diffraction | Research Square window.SnipcartSettings = { analytics: { enabled: false } }; (function() { var accessVector = localStorage.getItem('access_vector') || ''; window.dataLayer = window.dataLayer || []; if (accessVector) { window.dataLayer.push({ user: { profile: { profileInfo: { snid: accessVector } } } }); } })(); (function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start':new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0],j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src='https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f);})(window,document,'script','dataLayer','GTM-K279D39R'); Browse Preprints In Review Journals COVID-19 Preprints AJE Video Bytes Research Tools Research Promotion AJE Professional Editing AJE Rubriq About Preprint Platform In Review Editorial Policies Our Team Advisory Board Help Center Sign In Submit a Preprint Cite Share Download PDF Physical Sciences - Article Hydrogen in the Earth core inferred from neutron imaging and diffraction Naoki Takahashi, Tatsuya Sakamaki, Takanori Hattori, Ken-ichi Funakoshi, and 4 more This is a preprint; it has not been peer reviewed by a journal. https://doi.org/ 10.21203/rs.3.rs-6011893/v1 This work is licensed under a CC BY 4.0 License Status: Under Review Version 1 posted You are reading this latest preprint version Abstract The density of the Earth’s core is lower than that of pure iron; this is considered to be caused by the presence of light elements in the core. Hydrogen is one of the most important light elements in the Earth’s core because of its high cosmochemical abundance and its nature as a siderophile element under high pressure. Thus, the hydrogen content in liquid iron under high pressure is required to constrain the chemical composition of the Earth’s core. However, this value has been estimated based on the observation of quench products, and the true hydrogen content in liquid iron remains unclear. Here, we performed high-pressure and high-temperature neutron diffraction and imaging experiments in situ to determine the hydrogen content in liquid iron. We observed that liquid iron contains 0.17(3) wt.% H at 3.4 GPa and 1400 K, indicating that liquid iron is hydrogenated in the magma ocean during core formation. For the hydrogen content in the liquid iron at the base of the magma ocean, we estimated that the outer and inner cores contain 0.60–0.72 and 0.30–0.44 wt.% H, corresponding to 70–85 and 1.9–2.7 times the mass of hydrogen in the ocean, respectively. This suggests that hydrogen can contribute more than half of the density deficit in the outer core. For the magma ocean equilibrating with the hydrogen-rich primary atmosphere, the study findings show that liquid iron plays a crucial role in transporting a large amount of hydrogen into the core. Earth and environmental sciences/Solid Earth sciences/Core processes Earth and environmental sciences/Solid Earth sciences/Mineralogy Earth and environmental sciences/Planetary science/Core processes Earth and environmental sciences/Solid Earth sciences/Geochemistry Full Text Additional Declarations There is NO Competing Interest. Cite Share Download PDF Status: Under Review Version 1 posted You are reading this latest preprint version Research Square lets you share your work early, gain feedback from the community, and start making changes to your manuscript prior to peer review in a journal. As a division of Research Square Company, we’re committed to making research communication faster, fairer, and more useful. We do this by developing innovative software and high quality services for the global research community. Our growing team is made up of researchers and industry professionals working together to solve the most critical problems facing scientific publishing. Also discoverable on Platform About Our Team In Review Editorial Policies Advisory Board Help Center Resources Author Services Accessibility API Access RSS feed Manage Cookie Preferences © Research Square 2026 | ISSN 2693-5015 (online) Privacy Policy Terms of Service Do Not Sell My Personal Information {"props":{"pageProps":{"initialData":{"identity":"rs-6011893","acceptedTermsAndConditions":true,"allowDirectSubmit":false,"archivedVersions":[],"articleType":"Physical Sciences - Article","associatedPublications":[],"authors":[{"id":420357590,"identity":"e38fe415-e9e5-4762-8375-206af200c5a4","order_by":0,"name":"Naoki Takahashi","email":"data:image/png;base64,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","orcid":"https://orcid.org/0009-0002-7831-7588","institution":"Tohoku University","correspondingAuthor":true,"prefix":"","firstName":"Naoki","middleName":"","lastName":"Takahashi","suffix":""},{"id":420357591,"identity":"70f32443-67d6-4aed-89b2-12b1dcad10a4","order_by":1,"name":"Tatsuya Sakamaki","email":"","orcid":"https://orcid.org/0000-0002-1158-844X","institution":"Department of Earth Science, Tohoku University","correspondingAuthor":false,"prefix":"","firstName":"Tatsuya","middleName":"","lastName":"Sakamaki","suffix":""},{"id":420357592,"identity":"a5f03826-d3e8-43c4-8154-0ab108009859","order_by":2,"name":"Takanori Hattori","email":"","orcid":"https://orcid.org/0000-0002-1968-3732","institution":"Japan Atomic Energy Agency","correspondingAuthor":false,"prefix":"","firstName":"Takanori","middleName":"","lastName":"Hattori","suffix":""},{"id":420357593,"identity":"8109ddef-dccb-412b-be34-badda2644fb5","order_by":3,"name":"Ken-ichi Funakoshi","email":"","orcid":"","institution":"Research Center for Neutron Science and Technology","correspondingAuthor":false,"prefix":"","firstName":"Ken-ichi","middleName":"","lastName":"Funakoshi","suffix":""},{"id":420357594,"identity":"d9967291-52a4-4c40-9929-c512c71b1b63","order_by":4,"name":"Hiroshi Arima-Osonoi","email":"","orcid":"","institution":"Kyoto University","correspondingAuthor":false,"prefix":"","firstName":"Hiroshi","middleName":"","lastName":"Arima-Osonoi","suffix":""},{"id":420357595,"identity":"97d577e6-5022-4d79-ade2-8a3d016228c6","order_by":5,"name":"Asami Sano-Furukawa","email":"","orcid":"https://orcid.org/0000-0002-1652-1623","institution":"J-PARC Center, Japan Atomic Energy Agency","correspondingAuthor":false,"prefix":"","firstName":"Asami","middleName":"","lastName":"Sano-Furukawa","suffix":""},{"id":420357596,"identity":"21e61261-7c1d-4265-b1e7-e58c2fe642f9","order_by":6,"name":"Jun Abe","email":"","orcid":"","institution":"Comprehensive Research Organization for Science and Society","correspondingAuthor":false,"prefix":"","firstName":"Jun","middleName":"","lastName":"Abe","suffix":""},{"id":420357597,"identity":"124eedf4-42db-43dc-93db-461fc9ff3909","order_by":7,"name":"Akio Suzuki","email":"","orcid":"","institution":"Tohoku University","correspondingAuthor":false,"prefix":"","firstName":"Akio","middleName":"","lastName":"Suzuki","suffix":""}],"badges":[],"createdAt":"2025-02-12 05:10:11","currentVersionCode":1,"declarations":"","doi":"10.21203/rs.3.rs-6011893/v1","doiUrl":"https://doi.org/10.21203/rs.3.rs-6011893/v1","draftVersion":[],"editorialEvents":[],"editorialNote":"","failedWorkflow":false,"files":[{"id":78128809,"identity":"697ce88f-87ae-4f17-be92-fa37f3b46afb","added_by":"auto","created_at":"2025-03-10 08:26:31","extension":"pdf","order_by":1,"title":"","display":"","copyAsset":false,"role":"manuscript-pdf","size":1279342,"visible":true,"origin":"","legend":"","description":"","filename":"FinalFilemanuscripttakahashi.pdf","url":"https://assets-eu.researchsquare.com/files/rs-6011893/v1_covered_37766759-6ed7-4b7f-94e9-b9fa14524107.pdf"}],"financialInterests":"There is \u003cb\u003eNO\u003c/b\u003e Competing Interest.","formattedTitle":"Hydrogen in the Earth core inferred from neutron imaging and diffraction","fulltext":[],"fulltextSource":"","fullText":"","funders":[],"hasAdminPriorityOnWorkflow":false,"hasManuscriptDocX":false,"hasOptedInToPreprint":true,"hasPassedJournalQc":"","hasAnyPriority":true,"hideJournal":false,"highlight":"","institution":"","isAcceptedByJournal":false,"isAuthorSuppliedPdf":true,"isDeskRejected":"","isHiddenFromSearch":false,"isInQc":false,"isInWorkflow":false,"isPdf":true,"isPdfUpToDate":true,"isWithdrawnOrRetracted":false,"journal":{"display":true,"email":"
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