LIA-QMS method for the quantity analysis of the hydrogen isotopes retention in first-wall components of Globus-M2 tokamak

[Display omitted] •LIA-QMS quantitative analysis give the same results to conventional TDS analysis.•LIA-QMS detect a comparable deuterium density in co-deposits as LID-QMS.•The LIA-QMS signal is several times higher, which is important for large machines like ITER. The technique based on quadrupole...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Nuclear materials and energy 2024-12, Vol.41, p.101829, Article 101829
Hauptverfasser: Medvedev, O.S., Razdobarin, A.G., Shubina (Smirnova), E.V., Grishaev, M.V., Elets, D.I., Snigirev, L.A., Kolomiytsev, A.S., Nikolaev, A.V.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:[Display omitted] •LIA-QMS quantitative analysis give the same results to conventional TDS analysis.•LIA-QMS detect a comparable deuterium density in co-deposits as LID-QMS.•The LIA-QMS signal is several times higher, which is important for large machines like ITER. The technique based on quadrupole mass spectrometry of the material ejected by laser-induced ablation – LIA-QMS is proposed as a tool to measure H/D/T content in carbon co-deposits in the first wall and divertor regions of tokamak reactors. Tungsten tiles exposed in Globus-M2 tokamak were taken for validation experiments. Measurement accuracy was determined by comparison with the results obtained by laser-induced desorption – LID-QMS and conventional thermal desorption spectroscopy (TDS). Total amount of deuterium in hydrocarbon deposits was found to be 2.8 × 1017 D/cm2, when measured by – LIA-QMS, 3.0 × 1017 D/cm2 for LID-QMS and 2.9 × 1017 D/cm2 for TDS. The main uncertainty of D surface concentration are caused by inhomogeneity of the deposit thickness over the sample area or by presence of hydrocarbon species in the released gas.
ISSN:2352-1791
2352-1791
DOI:10.1016/j.nme.2024.101829