Randomized trial models tungsten erosion in L-mode helium plasma, indicating significant influence from helium ions.
Due to its unavoidable presence in thermonuclear DT plasmas and to its peculiar effects on materials, investigating the role of helium (He) in plasma-wall interaction (PWI) in current tokamaks is fundamental. In this work, PWI in L-mode He plasma discharges in ASDEX Upgrade (AUG) is modelled by exploiting simplified analytical approaches and two state-of-the-art codes. SOLPS-ITER is employed both to provide a suitable background plasma for erosion simulations and to interpret diagnostics measurements in terms of He+/2+ fraction. In particular, a 50-50% concentration of the two He ions is found in the proximity of the strike-points, while He2+ represents the dominant population farther in the scrape-off layer (SOL). The role of He ion fraction on AUG tungsten divertor erosion is first estimated by means of a simple analytical model and, afterwards, by exploiting ERO2.0, showing the major impact of He2+ in common AUG plasma temperatures. The potential influence of extrinsic impurities on divertor erosion is inferred from the preliminary comparison of ERO2.0 simulation results with experimental erosion measurements in the strike-point region. A comparison between the multi-fluid and kinetic approaches for simulating W erosion and migration reveals significant discrepancies in the predicted tungsten source and transport. In particular, he routinely adopted perfect entrainment assumption in SOLPS-ITER, i.e. setting the same velocity at the magnetic pre-sheath entrance for both main ions and impurities, is found to substantially overestimate the W source compared to ERO2.0 results. Moreover, ERO2.0 predicts a stronger tungsten transport towards the X-point than current SOLPS-ITER simulations without drifts. Comparable W influx into the core can, however, be reproduced in ERO2.0 by reducing the anomalous diffusivity.
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Alberti et al. (2026) studied this question.
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