Incorporation of Mg2+ in surface Ca2+ sites of aragonite : an ab initio study
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DOI[10.1186/s40645-015-0039-4]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 KawanoHiroshi SakumaTakaya Nagai
- 出版年月日等
- 2015-04-02
- 出版年(W3CDTF)
- 2015-04-02
- タイトル(掲載誌)
- Progress in earth and planetary science
- 巻号年月日等(掲載誌)
- 2(7)
- 掲載巻
- 2(7)
- 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/s40645-015-0039-4
- 国立国会図書館永続的識別子
- info:ndljp/pid/9381662
- 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)
- 2015-06-09T00:17:00+09:00
- 保存日(W3CDTF)
- 2015-04-20
- 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/9381655
- 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
- First-principles calculations of Mg2+-containing aragonite surfaces are important because Mg2+ can affect the growth of calcium carbonate polymorphs. New calculations that incorporate Mg2+ substitution for Ca2+ in the aragonite {001} and {110} surfaces clarify the stability of Mg2+ near the aragonite surface and the structure of the Mg2+-containing aragonite surface. The results suggest that the Mg2+ substitution energy for Ca2+ at surface sites is lower than that in the bulk structure and that Mg2+ can be easily incorporated into the surface sites; however, when Mg2+ is substituted for Ca2+ in sites deeper than the second Ca2+ layer, the substitution energy approaches the value of the bulk structure. Furthermore, Mg2+ at the aragonite surface has a significant effect on the surface structure. In particular, CO3 groups rotate to achieve six-coordinate geometry when Mg2+ is substituted for Ca2+ in the top layer of the {001} surface or even in the deeper layers of the {110} surface. The rotation may relax the atomic structure around Mg2+ and reduces the substitution energy. The structural rearrangements observed in this study of the aragonite surface induced by Mg2+ likely change the stability of aragonite and affect the polymorph selection of CaCO3.
- DOI
- 10.1186/s40645-015-0039-4
- オンライン閲覧公開範囲
- インターネット公開
- 著作権情報
- Creative Commons Attribution 4.0 International
- 関連情報(URI)
- 参照
- Observing crystal growth processes in computer simulationsStrong Coupling between Biomineral Morphology and Sr/Ca of Arctica islandica (Bivalvia)—Implications for Shell Sr/Ca-Based Temperature EstimatesSpeciation of magnesium in monohydrocalcite: XANES, ab initio and geochemical modelingRearing in strontium-enriched water induces vaterite otoliths in the Japanese rice fish, <i>Oryzias latipes</i>Synthesis of needle-like aragonite using carbonation method: A review
- 参照
- Atomic and electronic structures of CaCO<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:msub><mml:mrow/><mml:mn>3</mml:mn></mml:msub></mml:math>surfacesThe Arrangement of First- and Second-shell Water Molecules Around Metal Ions: Effects of Charge and SizePrinciples of Crystal Nucleation and GrowthMg/Ca Partitioning Between Aqueous Solution and Aragonite Mineral: A Molecular Dynamics StudyPrecipitation diagram of calcium carbonate polymorphs: its construction and significanceElectronic, optical and bonding properties of MgCO3Thermodynamics of solvation of ions. Part 5.—Gibbs free energy of hydration at 298.15 KMg/Ca Thermometry in Coral SkeletonsDifference in the Conformation and Dynamics of Aspartic Acid on the Flat Regions, Step Edges, and Kinks of a Calcite Surface: A Molecular Dynamics StudySurface Tension Alteration on Calcite, Induced by Ion SubstitutionEfficiency of ab-initio total energy calculations for metals and semiconductors using a plane-wave basis setHydration Energies and Structures of Alkaline Earth Metal Ions, M<sup>2+</sup>(H<sub>2</sub>O)<i><sub>n</sub></i>, <i>n</i> = 5−7, M = Mg, Ca, Sr, and BaThe Role of Mg <sup>2+</sup> as an Impurity in Calcite Growth<i>VESTA</i>: a three-dimensional visualization system for electronic and structural analysisAtomistic simulation of the differences between calcite and dolomite surfacesSurface–water interactions in the dolomite problem<i>Ab initio</i>molecular-dynamics simulation of the liquid-metal–amorphous-semiconductor transition in germaniumEnergetic clues to pathways to biomineralization: Precursors, clusters, and nanoparticlesThermodynamics of ion hydration and its interpretation in terms of a common modelFourier transform infrared spectroscopy (FTIR) and X-ray diffraction analyses of mineral and organic matrix during heating of mother of pearl (nacre) from the shell of the molluscPinctada maximaGeneralized Gradient Approximation Made SimpleEfficient iterative schemes for<i>ab initio</i>total-energy calculations using a plane-wave basis setFrom ultrasoft pseudopotentials to the projector augmented-wave methodGeneral model for calcite growth kinetics in the presence of impurity ionsElectronic, optical and bonding properties of CaCO3 calcite<i>Ab initio</i>molecular dynamics for liquid metalsThe role of magnesium in the growth of calcite: An AFM studySurface Structure and Morphology of Calcium Carbonate Polymorphs Calcite, Aragonite, and Vaterite: An Atomistic ApproachThe behavior of various inorganic ions in the separation of calcium carbonate from a bicarbonate solution
- 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
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossrefCiNii Articles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CrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID(NDLBibID)
- 9381662
- NII論文ID
- 120005677757