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首页> 外文期刊>IEEE Transactions on Applied Superconductivity >Sub-Micron Non-Superconducting Deposits That Fail to Act as Pinning Centers in Textured YBCO Superconductor
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Sub-Micron Non-Superconducting Deposits That Fail to Act as Pinning Centers in Textured YBCO Superconductor

机译:亚微米非超导沉积物,无法在带纹理的YBCO超导体中充当钉扎中心

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摘要

A conundrum is observed where one type of small, non-superconducting particles fails to provide pinning, in textured YBCO superconductor, while other non-superconducting particles of comparable size and number density, pin very well. Pinning centers in high temperature superconductors (HTS) have been shown to greatly enhance critical current density $(J_{C})$. An experiment was performed in which large grain YBCO doped with uranium (U), but no platinum (Pt), was produced. Profuse deposits of a U-Y-Ba-O compound were formed during texturing. These U-rich deposits have an almost spherical morphology with an average diameter of $sim$300 nm and are uniformly distributed inside the YBCO. Conventional wisdom dictates that the U-Y-Ba-O sub-micron deposits should act as pinning centers and increase $J_{C}$. However, in tests of $J_{C}$ via trapped magnetic flux density at 77 K, no increase was measured. This result is especially surprising because chemically similar and morphologically indistinguishable deposits of U-Pt-Y-Ba-O, found in $({rm U}+{rm Pt})$-doped YBCO, increased $J_{C}$ by a factor exceeding 2. The deposits compared had the same size and number density. Neither deposits significantly affected critical temperature $(T_{C})$. One difference between these two compounds is that the non-pinning U-Y-Ba-O deposits have a single perovskite structure, while the U-Pt-Y-Ba-O pinning centers are a double perovskite. Data are presented on the remarkably similar morphology and strikingly different ability to trap magnetic flux density of the U-Y-Ba-O and U-Pt-Y-Ba-O deposits.
机译:观察到一个难题,在带纹理的YBCO超导体中,一种类型的小的非超导颗粒无法提供固定作用,而尺寸和数量密度相当的其他非超导颗粒则可以很好地固定。高温超导体(HTS)的钉扎中心已显示出可大大提高临界电流密度((J_ {C})$)。进行了实验,其中生产了掺有铀(U)但没有铂(Pt)的大晶粒YBCO。在纹理化过程中形成了U-Y-Ba-O化合物的大量沉淀。这些富含U的沉积物具有近乎球形的形态,平均直径为$ sim $ 300 nm,并且均匀地分布在YBCO内部。传统观点认为,U-Y-Ba-O亚微米沉积物应充当固定中心并增加$ J_ {C} $。但是,在通过$ 77 K捕获的磁通密度测试$ J_ {C} $时,未测量到增加。这个结果尤其令人惊讶,因为在掺杂$({rm U} + {rm Pt})$的YBCO中发现的U-Pt-Y-Ba-O的化学相似且在形态上无法区分的沉积增加了$ J_ {C} $因子超过2。所比较的沉积物具有相同的大小和数量密度。两种沉积物均未严重影响临界温度$(T_ {C})$。这两种化合物之间的区别是非钉扎U-Y-Ba-O沉积物具有单个钙钛矿结构,而U-Pt-Y-Ba-O钉扎中心是双钙钛矿。数据呈现出非常相似的形态和截然不同的捕获U-Y-Ba-O和U-Pt-Y-Ba-O矿床磁通密度的能力。

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