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Topochemical Nitridation with Anion Vacancy-Assisted N~(3-)/O~(2-) Exchange

机译:阴离子空位辅助N〜(3-)/ O〜(2-)交换的拓扑化学氮化

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摘要

We present how the introduction of anion vacancies in oxyhydrides enables a route to access new orynitrides, by conducting ammonolysis of perovskite oxyhydride EuTiO_(3-x)H_x (x ~ 0.18). At 400 ℃, similar to our studies on BaTiO_(3-x)H_x, hydride lability enables a low temperature direct ammonolysis of EuTi~(3.82+)O_(2.82)H_(0.18), leading to the N~(3-)/H~--exchanged product EuTi~(4+)O_(2.82)N_(0.12)□_(0.06). When the ammonolysis temperature was increased up to 800 ℃, we observed a further nitridation involving N~(3-)/O~(2-) exchange, yielding a fully oxidized Eu~(3+)Ti~(4+)O_2N with the GdFeO_3-type distortion (Pnma) as a metastable phase, instead of pyrochlore structure. Interestingly, the same reactions using the oxide EuTiO_3 proceeded through a 1:1 exchange of N~(3-) with O~(2-) only above 600 ℃ and resulted in incomplete nitridation to EuTiO_(2.25)N_(0.75), indicating that anion vacancies created during the initial nitridation process of EuTiO_(2.82)H_(0.18) play a crucial role in promoting anion (N~(3-)/O~(2-)) exchange at high temperatures. Hence, by using (hydride-induced) anion-deficient precursors, we should be able to expand the accessible anion composition of perovskite oxynitrides.
机译:我们介绍了如何通过进行钙钛矿型氢氧化物EuTiO_(3-x)H_x(x〜0.18)的氨解反应,在氢氧根中引入阴离子空位,从而使一条途径获得新的氰化物。在400℃下,类似于我们对BaTiO_(3-x)H_x的研究,氢化物不稳定性使EuTi〜(3.82+)O_(2.82)H_(0.18)在低温下直接氨解,导致N〜(3-) / H〜-交换产物EuTi〜(4+)O_(2.82)N_(0.12)□_(0.06)。当氨解温度提高到800℃时,我们观察到进一步的氮化反应涉及N〜(3-)/ O〜(2-)交换,产生了完全氧化的Eu〜(3+)Ti〜(4+)O_2N GdFeO_3型畸变(Pnma)为亚稳相,而不是烧绿石结构。有趣的是,使用氧化物EuTiO_3进行的相同反应仅在600℃以上通过N〜(3-)与O〜(2-)1:1交换进行,导致未完全氮化为EuTiO_(2.25)N_(0.75),表明EuTiO_(2.82)H_(0.18)的初始氮化过程中产生的阴离子空位在高温下促进阴离子(N〜(3-)/ O〜(2-))交换中起关键作用。因此,通过使用(氢化物诱导的)阴离子缺陷前体,我们应该能够扩大钙钛矿型氮氧化物的可及阴离子组成。

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  • 来源
    《Journal of the American Chemical Society》 |2016年第9期|3211-3217|共7页
  • 作者单位

    Department of Energy and Hydrocarbon Chemistry, Graduate School of Engineering Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan;

    Department of Energy and Hydrocarbon Chemistry, Graduate School of Engineering Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan;

    Department of Energy and Hydrocarbon Chemistry, Graduate School of Engineering Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan;

    Department of Energy and Hydrocarbon Chemistry, Graduate School of Engineering Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan;

    Department of Energy and Hydrocarbon Chemistry, Graduate School of Engineering Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan;

    Department of Energy and Hydrocarbon Chemistry, Graduate School of Engineering Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan;

    Department of Material Chemistry, Graduate School of Engineering, Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan;

    Department of Material Chemistry, Graduate School of Engineering, Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan;

    Department of Material Chemistry, Graduate School of Engineering, Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan;

    Electron Microscopy for Materials Research (EMAT), University of Antwerp, Groenenborgerlaan 171, B-2020 Antwerp, Belgium;

    Electron Microscopy for Materials Research (EMAT), University of Antwerp, Groenenborgerlaan 171, B-2020 Antwerp, Belgium,Skoltech Center for Electrochemical Energy Storage, Skolkovo Institute of Science and Technology, 143026 Moscow, Russia;

    Center for Neutron Research, National Institute of Standards and Technology, Gaithersburg, MD 20899, United States;

    Department of Energy and Hydrocarbon Chemistry, Graduate School of Engineering Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan,PRESTO Japan Science and Technology Agency (JST), Kawaguchi, Saitama 332-0012, Japan;

    Department of Energy and Hydrocarbon Chemistry, Graduate School of Engineering Kyoto University, Nishikyo-ku, Kyoto 615-8510, Japan,CREST, Japan Science and Technology Agency (JST), Kawaguchi, Saitama 332-0012, Japan;

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  • 入库时间 2022-08-18 03:08:44

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