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Hydrogen retention and depth profile in divertor tiles of Jt-60 exposed to hydrogen discharges

机译:暴露于氢放电的Jt-60转向器瓦中的氢保留和深度分布

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摘要

Depth profile and retention properties of hydrogen in the graphite armor tiles of JT-60 open-divertor used for HH discharge period were investigated by secondary ion mass spectroscopy and thermal desorption spectroscopy. Two tiles were investigated, one at the inner divertor area covered with the re-deposited layers of the largest thickness (70 μm) and the other at the private flux region near the outer divertor striking point hardly covered with the re-deposited layers (only 1-2 μm). In the former, hydrogen was retained uniformly in the carbon re-deposited layers with H/C of 0.03, which was significantly smaller than H/C observed in the re-deposited layers of other tokamaks. Such small hydrogen retention in the re-deposited layers is attributed to the temperature rise of the re-deposited layers during discharges due to their poor thermal contact to the substrate. The latter retained rather large amount of hydrogen only in the shallow surface layers and its depth profile decayed sharply to 1.3 x 10~(-4) in H/C of the bulk retention as expected from the very thin re-deposited layers and observed temperature rise above 900 K.
机译:通过二次离子质谱和热脱附光谱研究了用于HH放电期的JT-60开放式偏滤器的石墨铠装砖中氢的深度分布和保留特性。对两块瓷砖进行了研究,一块位于内分流器区域,覆盖有最大厚度(70μm)的再沉积层,另一块位于外分流器撞击点附近的私有通量区域,几乎没有被再沉积层覆盖(仅1-2微米)。在前者中,氢均匀地保留在碳的再沉积层中,H / C为0.03,该值明显小于在其他托卡马克的再沉积层中观察到的H / C。在再沉积层中如此小的氢保留归因于在放电期间由于再沉积层与基板的不良热接触而导致的温度升高。后者仅在浅表层中保留了相当数量的氢,并且其深度分布以非常薄的再沉积层和观察到的温度预期为准,在大体积保留的H / C中急剧下降至1.3 x 10〜(-4)。超过900K。

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