Improved ERO modelling of beryllium erosion at ITER upper first wall panel using JET-ILW and PISCES-B experience

•The earlier ERO erosion modelling [1] for the beryllium ITER FW element was significantly revisited.•The revisit utilizes the recent experience of ERO application to the Be erosion experiments at JET-ILW tokamak and PISCES-B linear device.•The net erosion gets stronger by a factor of ∼2 mostly due...

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Veröffentlicht in:Nuclear materials and energy 2019-05, Vol.19, p.510-515
Hauptverfasser: Borodin, D., Romazanov, J., Pitts, R.A., Lisgo, S.W., Brezinsek, S., Borodkina, I., Eksaeva, A., Safi, E., Nordlund, K., Kirschner, A., Linsmeier, Ch
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Sprache:eng
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Zusammenfassung:•The earlier ERO erosion modelling [1] for the beryllium ITER FW element was significantly revisited.•The revisit utilizes the recent experience of ERO application to the Be erosion experiments at JET-ILW tokamak and PISCES-B linear device.•The net erosion gets stronger by a factor of ∼2 mostly due to the new semi-analytic approach [10] for the sputtering ion trajectories in the surface sheath.•The paper shows the status of the underlying sputtering data including the most recent MD-OKMC simulations [11] and the role of CAPS. ERO is a 3D Monte-Carlo impurity transport and plasma-surface interaction code. In 2011 it was applied for the ITER first wall (FW) life time predictions [1] (critical blanket module BM11). After that the same code was significantly improved during its application to existing fusion-relevant plasma devices: the tokamak JET equipped with an ITER-like wall and linear plasma device PISCES-B. This has allowed testing the sputtering data for beryllium (Be) and showing that the “ERO-min” fit based on the large (50%) deuterium (D) surface content is well suitable for plasma-wetted areas (D plasma). The improved procedure for calculating of the effective sputtering yields for each location along the plasma-facing surface using the recently developed semi-analytical sheath approach was validated. The re-evaluation of the effective yields for BM11 following the similar revisit of the JET data has indicated significant increase of erosion and motivated the current re-visit of ERO simulations.
ISSN:2352-1791
2352-1791
DOI:10.1016/j.nme.2019.03.016