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Comparison of Hydrogen Isotope Retention in Divertor Tiles of JET with the ITER-Like Wall Following Campaigns in 2011-2012 and 2015-2016

机译:在2011-2012和2015-2016在竞选中与射门型射流器型射流瓷砖氢同位素保留的比较

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摘要

Hydrogen isotope retention and chemical state for the tiles exposed to plasma in the JET-ITER-like wall (ILW) during two campaigns in 2011-2012 (first campaign, ILW-1) and 2015-2016 (third campaign, ILW-3) were studied and compared by means of X-ray photoelectron spectroscopy and thermal desorption spectroscopy. In both campaigns the upper part of the inner divertor tiles was the deposition-dominated area, while erosion was observed on the outer divertor tiles. Therefore, higher deuterium retention was found on the inner divertor tiles. The major D desorption peak for the inner divertor tiles from ILW-3 was located at the temperature range of 470 degrees C to 520 degrees C, which was higher than measured after ILW-1: 370 degrees C to 430 degrees C. The XPS analyses showed the formation of a BeO layer on the ILW-3 inner divertor tiles, while after ILW-1 the layers also contained a significant amount of carbon. Deuterium retention was reduced toward the outer divertor tiles. The differences could be related to the difference in the power level in the two campaigns.
机译:在2011-2012(第一竞选活动,ILW-1)和2015-2016(第三次竞选,ILW-3)(第三次广告系列,ILW-3)(第三次广告系列)(第三次广告系列)(第三次广告系列)(第三次广告系列)(第三次广告系列)(第三次广告系列)(第三次竞选活动)中,陶瓷等瓷砖的保留和化学状态通过X射线光电子能谱和热解吸光谱进行了研究和比较。在两个竞选方面,内侧偏转器瓦片的上部是沉积主导区域,而在外部偏移瓦片上观察到侵蚀。因此,在内侧偏转器瓦片上发现了更高的氘留卷。来自ILW-3的内部偏移器瓦片的主要D解吸峰位于470℃至520℃的温度范围,高于ILW-1:370℃至430℃的测量。XPS分析显示在ILW-3内侧偏转器瓦上形成BEO层,而ILW-1之后,层还含有大量的碳。氘保留朝向外部偏转器瓷砖。差异可能与两个广告系列中的功率水平的差异有关。

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