Existence of a detachment cliff at ASDEX Upgrade

Luca Scotti, M. Cavedon, Matthias Bernert, D. Brida, Bernd Kurzan, Ralph Dux
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Abstract

The detachment cliff is a bifurcative transition to partial detachment recently discovered at the DIII-D tokamak. This work presents a database analysis of target parameters in L-mode and H-mode discharges to search for a detachment cliff at ASDEX Upgrade (AUG). Most of the transitions from attached to partially detached divertor conditions observed in H- and L-mode discharges in AUG show bifurcative-like characteristics that are consistent with the properties of the detachment cliff if the Bx∇B drift is directed towards the active X-point. In the operational space of power and density, the bifurcative transitions identified during an L-mode discharge occur at injected power and density higher than a threshold value Ptot > 0.7 MW and ne > 1.6 x 1019 m-3, respectively). Furthermore, the temperatures at which the transitions start are found to be insensitive to the injected impurity, to the injected power and to the value of the upstream density. Finally, the study of the evolution of the target parameters, of the intensity of the Dα line and of specific manometers and bolometer lines of sights shows that the physical process underlying the detachment cliff and the self-sustained divertor oscillations might be the same.
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ASDEX 升级版存在支队悬崖
脱离悬崖是最近在 DIII-D 托卡马克发现的向部分脱离的分叉过渡。这项工作对 L 模式和 H 模式放电中的目标参数进行了数据库分析,以寻找 ASDEX 升级(AUG)中的脱离悬崖。在AUG的H模式和L模式放电中观察到的从附着到部分分离的分流条件过渡,大部分都显示出类似分叉的特征,如果Bx∇B漂移指向活动X点,这些特征与分离悬崖的特性是一致的。在功率和密度的操作空间中,在 L 模式放电过程中发现的分岔转换发生在注入功率和密度分别高于临界值 Ptot > 0.7 MW 和 ne > 1.6 x 1019 m-3 时)。此外,研究还发现跃迁开始时的温度对注入的杂质、注入功率和上游密度值都不敏感。最后,对目标参数、Dα 线强度以及特定压力计和螺栓计视线演变的研究表明,脱离崖和自持憩息器振荡的物理过程可能是相同的。
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