The role of hydrogen bonds in hydrous minerals stable at lower mantle pressure conditions
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DOI[10.1186/s40645-022-00521-3]のデータに遷移します
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- 資料種別
- 記事
- 著者・編者
- Jun TsuchiyaElizabeth C. Thompson
- 出版年月日等
- 2022-11-17
- 出版年（W3CDTF）
- 2022-11-17
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 9(63)
- 掲載巻
- 9(63)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-022-00521-3
- 国立国会図書館永続的識別子
- info:ndljp/pid/12998704
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- コレクション（個別）
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2023-09-27T14:40:47+09:00
- 保存日（W3CDTF）
- 2023-04-11
- 記録形式（IMT）
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否（NDL）
- 可
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/12307811
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- 要約等
- コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- DOI
- 10.1186/s40645-022-00521-3
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報（URI）
- 参照
- Nuclear quantum effect on the elasticity of ice VII under pressure: A path-integral molecular dynamics studyRole of water in dynamics of slabs and surrounding mantle
- 参照
- Compressional behavior and spin state of δ-(Al,Fe)OOH at high pressuresSymmetrization driven spin transition in ε-FeOOH at high pressureStability of a hydrous δ-phase, AlOOH–MgSiO2(OH)2, and a mechanism for water transport into the base of lower mantleFirst principles prediction of a new high‐pressure phase of dense hydrous magnesium silicates in the lower mantleDirect observation of symmetrization of hydrogen bond in δ-AlOOH under mantle conditions using neutron diffractionFirst principles calculation of the elasticity of ice VIII and XFirst‐Principles Determination of the Dissociation Phase Boundary of Phase H MgSiO<sub>4</sub>H<sub>2</sub>Reassigning Hydrogen-Bond Centering in Dense IceThe influence of δ-(Al,Fe)OOH on seismic heterogeneities in Earth’s lower mantleRefinement of the crystal structure of groutite – MnOOHHigh‐Pressure Elasticity of δ‐(Al,Fe)OOH Single Crystals and Seismic Detectability of Hydrous MORB in the Shallow Lower MantleStructural independence of hydrogen-bond symmetrisation dynamics at extreme pressure conditionsAbsence of proton tunneling during the hydrogen-bond symmetrization in <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:mi>δ</mml:mi><mml:mo>−</mml:mo><mml:mi>AlOOH</mml:mi></mml:math>Stability and Solid Solutions of Hydrous Alumino-Silicates in the Earth’s MantleThe Crystal Structure of the Tetragonal Modification of YbOOH.Single crystal synthesis of δ-(Al,Fe)OOHNew aluminium hydroxide at multimegabar pressures: Implications for water reservoirs in deep planetary interiorsIn situ X-ray diffraction studies of dense hydrous magnesium silicates at mantle conditionsPhase transformations in serpentine at high pressures and temperatures and implications for subducting lithosphereThe Pyrite-Type High-Pressure Form of SilicaPressure-Induced Hydrogen Bond Symmetrization in Iron OxyhydroxideStability of dense hydrous magnesium silicate phases and water storage capacity in the transition zone and lower mantleThe role of water in Earth's mantleVibrational anisotropy of <i>δ</i>-(Al,Fe)OOH single crystals as probed by nuclear resonant inelastic X-ray scatteringStability of hydrous silicate at high pressures and water transport to the deep lower mantleSound velocities of δ‐AlOOH up to core‐mantle boundary pressures with implications for the seismic anomalies in the deep mantleElastic Properties of the Pyrite‐Type FeOOH‐AlOOH System From First‐Principles CalculationsHydrous mantle transition zone indicated by ringwoodite included within diamondStructure Refinement of Deuterated BoehmiteLower-mantle water reservoir implied by the extreme stability of a hydrous aluminosilicateLinear response approach to the calculation of the effective interaction parameters in the<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mrow><mml:mi>LDA</mml:mi><mml:mo>+</mml:mo><mml:mi mathvariant="normal">U</mml:mi></mml:mrow></mml:math>methodFirst principles calculation of a high‐pressure hydrous phase, δ‐AlOOHFirst-principles study of hydrogen bond symmetrization of phase D under high pressureNeutron and X-Ray Crystallographic Studies on Indium Oxide Hydroxide.Stability limits of hydrous minerals in sediment and mid‐ocean ridge basalt compositions: Implications for water transport in subduction zonesCalculated Elasticity of Al-Bearing Phase DSingle‐Crystal Elasticity of High‐Pressure Ice up to 98 GPa by Brillouin ScatteringStability of hydrous phase H MgSiO<sub>4</sub>H<sub>2</sub> under lower mantle conditionsElasticity of superhydrous phase, B, Mg10Si3O14(OH)4Experimentally based water budgets for dehydrating slabs and consequences for arc magma generationNeutron diffraction study of -AlOOD at high pressure and its implication for symmetrization of the hydrogen bondWhole-mantle convection and the transition-zone water filterCompression of<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mrow><mml:msub><mml:mtext>H</mml:mtext><mml:mn>2</mml:mn></mml:msub><mml:mtext>O</mml:mtext></mml:mrow></mml:math>ice to 126 GPa and implications for hydrogen-bond symmetrization: Synchrotron x-ray diffraction measurements and density-functional calculationsAluminous hydrous mineral <i>δ</i>‐AlOOH as a carrier of hydrogen into the core‐mantle boundaryIsotope effects in the bonds of β-CrOOH and β-CrOOD<i>Ab initio</i> investigation of H-bond disordering in δ-AlOOHSpectroscopic evidence for the Fe3+ spin transition in iron-bearing δ-AlOOH at high pressureA single crystal neutron diffraction study of diaspore, AlO(OH)Infrared absorption study of the hydrogen-bond symmetrization in ice to 110 GPaStability field of new hydrous phase, δ‐AlOOH, with implications for water transport into the deep mantleFirst principles centroid molecular dynamics simulation of high pressure icesCompression of Ice to 210 Gigapascals: Infrared Evidence for a Symmetric Hydrogen-Bonded PhaseStability of phase H in the MgSiO 4 H 2 –AlOOH–SiO 2 systemInfrared investigation on ice VIII and the phase diagram of dense icesHydrogen Bonding and Jahn–Teller Distortion in Groutite,α-MnOOH, and Manganite,γ-MnOOH, and Their Relations to the Manganese Dioxides Ramsdellite and PyrolusiteBrillouin scattering of H2O ice to megabar pressuresNew high-pressure phases in MOOH (M = Al, Ga, In)First-principles prediction of a high-pressure hydrous phase of AlOOHElastic properties of δ-AlOOH under pressure: First principles investigationQUANTUM ESPRESSO: a modular and open-source software project for quantum simulations of materialsVolatile accretion history of the terrestrial planets and dynamic implicationsA new hydrous phase δ-AlOOH synthesized at 21 GPa and 1000 °CHigh-pressure form of pyrite-type germanium dioxideHigh pressure phase transitions and hydrogen-bond symmetry in ice polymorphsWater in Earth’s mantleTransition from the<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="normal">Rh</mml:mi><mml:mn>2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn>3</mml:mn></mml:msub><mml:mrow><mml:mo>(</mml:mo><mml:mn>II</mml:mn><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math>-to-<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mrow><mml:mi mathvariant="normal">Ca</mml:mi><mml:mi mathvariant="normal">Ir</mml:mi><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn>3</mml:mn></mml:msub></mml:mrow></mml:math>structure and the high-pressure-temperature phase diagram of aluminaObservation of nuclear quantum effects and hydrogen bond symmetrisation in high pressure iceElastic properties of phase D (MgSi2O6H2) under pressure: Ab initio investigationDehydrogenation of goethite in Earth’s deep lower mantleOn the geometry of O–H...O hydrogen bondsPhonons and related crystal properties from density-functional perturbation theoryEtude par diffraction neutronique de la forme haute pression de FeOOHVibrational properties of -AlOOH under pressureDynamical Instabilities of Ice XMorphology of synthetic sub-microscopic crystals of α and γFeOOH and of γFe<sub>2</sub>O<sub>3</sub>prepared from FeOOHWATER, MELTING, AND THE DEEP EARTH H<sub>2</sub>O CYCLERaman Spectroscopy of Dense<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant="normal">H</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow><mml:mi mathvariant="normal">O</mml:mi></mml:math>and the Transition to Symmetric Hydrogen BondsSolubility behavior of δ-AlOOH and ε-FeOOH at high pressuresHigh-pressure reconnaissance investigations in the system Mg2SiO4 - MgO - H2OTunnelling and zero-point motion in high-pressure iceThe lattice parameters of natural single crystal and synthetically produced goethite (α-FeOOH)On the Symmetry of the Hydrogen Bonds in Ice VIIPhase transitions in ε-FeOOH at high pressure and ambient temperatureFirst principles prediction of new high-pressure phase of InOOH地球内部の水 マントル遷移層は水のリザバーか？
- 参照（URI）
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossref
- 書誌ID（NDLBibID）
- 12998704