首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Aqueous alteration of nearly pure Nd-doped zirconolite (Ca0.8Nd0.2ZrTi1.8Al0.2O7) a passivating layer control
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Aqueous alteration of nearly pure Nd-doped zirconolite (Ca0.8Nd0.2ZrTi1.8Al0.2O7) a passivating layer control

机译:几乎纯净掺钕锆石(Ca0.8Nd0.2ZrTi1.8Al0.2O7)的钝化层控制

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摘要

Neodynium-doped zirconolite was fabricated by hydrolysing a mixture of alkoxide with nitrate solutions followed by a series of drying, calcination, pressing and sintering steps. The material obtained was essentially zirconolite (99.5 vol% Ca0.8Nd0.2ZrTi1.8Al0.2O7) with a minor ZrTiO4 phase (0.5 vol%). The microstructure and composition of the zirconolite was characterised, before and after durability experiments, by SEM/EDS, SIMS, AFM and TEM. Chemical durability testing was carried out using the standard MCC-2 test at 150 degrees C for a series of four test durations - 1, 7, 28 and 84 days. The pH of the leachates was fairly constant with time (pH 5), and elemental releases reached apparent steady-state conditions within the first day of leaching. Thermodynamic calculations indicated that attainment of these steady-state conditions at this point could not be explained by thermodynamic equilibrium being reached between the leachates and the primary zirconolite phase. However, thermodynamic equilibrium between a possible layer of secondary hydroxides or a decalcified zirconolite and the leachates could explain the steady state of Ti, Zr and Al releases. Moreover, it is suggested that the steady-state conditions achieved by Nd, theoretically undersaturated in the leachates, is due to adsorption of Nd to this secondary layer, and is not a result of precipitation of a hydroxide form. Anatase, commonly observed during leaching of zirconotitanates, is also theoretically undersaturated in the leachates. When observed, it is possibly a product of local condensation of the hydroxide layer and not due to simply a dissolution/precipitation process. SEM and AFM investigations confirmed the formation of a passivation layer on the surface of the zirconolite. The layer was of the order of 10 nm, in accordance with the thickness calculated from leachate results. (c) 2004 Elsevier Ltd. All rights reserved.
机译:通过水解醇盐与硝酸盐溶液的混合物,然后进行一系列的干燥,煅烧,压制和烧结步骤来制备掺钕锆石。得到的材料基本上是锆石(99.5体积%的Ca0.8Nd0.2ZrTi1.8Al0.2O7),具有次要的ZrTiO4相(0.5体积%)。在耐久性实验之前和之后,通过SEM / EDS,SIMS,AFM和TEM对锆石的微观结构和组成进行了表征。化学耐久性测试是使用标准MCC-2测试在150摄氏度下进行的,四个系列的测试持续时间分别为1天,7天,28天和84天。浸出液的pH值随时间(pH 5)相当恒定,并且元素释放在浸出的第一天达到了明显的稳态条件。热力学计算表明,此时的这些稳态条件无法通过浸出液和初级锆石相之间的热力学平衡来解释。然而,可能的仲氢氧化物层或脱钙锆石与渗滤液之间的热力学平衡可以解释Ti,Zr和Al释放的稳态。此外,建议通过Nd达到的稳态条件(理论上在渗滤液中不饱和)是由于Nd吸附到该第二层,而不是氢氧化物形式沉淀的结果。在浸出锆钛酸盐期间通常观察到的锐钛矿在理论上在浸出液中也不饱和。当观察到时,它可能是氢氧化物层局部凝结的产物,而不是仅仅由于溶解/沉淀过程所致。 SEM和AFM研究证实,在锆石表面上形成了钝化层。根据从渗滤液结果计算的厚度,该层约为10nm。 (c)2004 Elsevier Ltd.保留所有权利。

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