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Ion irradiation damage in geikielite (MgTiO3)

机译:Geikielite(MgTiO3)中的离子辐照损伤

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A series of ion-irradiation experiments were conducted to explore the radiation response of the ilmenite-group oxide geikielite (MgTiO3). In these experiments, oriented single crystals were irradiated with either 200 keV Ar2+ or 400 keV Xe2+ and Rutherford back-scattering spectrometry combined with ion channelling (RBS/C) was used to characterize consequent radiation damage. In the 200 keV Ar2+ experiments, the sample was held at 100 K and a buried amorphous layer 55 nm thick formed underneath a defective crystalline layer 90 nm thick after exposure to a fluence of 2 x 10(15) ions cm(-2). More detailed experiments with 400 keV Xe2+ employed incremental ion irradiation followed by RBS/C to determine the extent and rate of radiation damage at temperatures of 170, 300 and 470 K. These irradiations show that there is a strong temperature dependence for damage accumulation and that critical amorphization fluences increase from 2 x 10(15) Xe2+ cm(-2) (170 K) to 6 x 10(15) Xe2+ cm(-2) (300 K) to greater than 2.5 x 10(16) Xe2+ cm(-2) (470 K). Damage appears to accumulate in several stages, with a rapid initial growth that levels at an intermediate stage. This is followed by an increase in and, eventually, saturation in the damage rare. At 170 and 300 K the damage fraction saturates at 100%, whereas saturation occurs at about 80% at 470 K. RBS/C data suggest the possible formation of a radiation-induced metastable phase in the damaged region, which may be analogous to pressure- or temperature-induced phase transformations in other ilmenite-group oxides. In particular, these materials transform to either the lithium niobate or the orthorhombic perovskite structure at high pressures and temperatures. The results presented in this study and similar investigations on the olivine system suggest that ionicity, composition and melting temperature may play important roles in the radiation response of ceramics, and particularly in predicting the relative radiation tolerance of materials within a solid-solution series. [References: 42]
机译:进行了一系列的离子辐照实验,以探索钛铁矿型氧化物Geikielite(MgTiO3)的辐射响应。在这些实验中,用200 keV Ar2 +或400 keV Xe2 +照射取向的单晶,并使用结合离子通道(RBS / C)的卢瑟福背散射光谱法来表征随后的辐射损伤。在200 keV Ar2 +实验中,将样品保持在100 K,然后在暴露于2 x 10(15)离子cm(-2)的通量后,在55纳米厚的有缺陷晶体层下方形成55纳米厚的掩埋非晶层。使用400 keV Xe2 +进行的更详细的实验采用增量离子辐照,然后采用RBS / C确定170、300和470 K温度下的辐射损伤程度和速率。这些辐照表明,损伤积累与温度有很强的相关性,并且临界非晶化通量从2 x 10(15)Xe2 + cm(-2)(170 K)增加到6 x 10(15)Xe2 + cm(-2)(300 K)至大于2.5 x 10(16)Xe2 + cm( -2)(470 K)。损害似乎在多个阶段累积,初期快速增长到中间阶段。其次是罕见的损害增加,并最终达到饱和。在170和300 K时,损伤分数以100%饱和,而在470 K时,饱和度约为80%。RBS/ C数据表明在损伤区域可能形成辐射诱导的亚稳相,这可能与压力相似。 -或温度引起的其他钛铁矿型氧化物的相变。特别地,这些材料在高压和高温下转变成铌酸锂或斜方钙钛矿结构。这项研究以及对橄榄石系统的类似研究提出的结果表明,离子性,组成和熔化温度可能在陶瓷的辐射响应中,特别是在预测固溶系列中材料的相对辐射耐受性方面起重要作用。 [参考:42]

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