Evidence for hydrogen flux dependence of the apparent chemical erosion yield of 
graphite under high flux conditions

Kallenbach, A.; Thoma, A.; Bard, A.; Behringer, K. H.; Schmidtmann, K.; Weinlich, M.; ASDEX Upgrade Team

doi:10.1088/0029-5515/38/7/311

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Evidence for hydrogen flux dependence of the apparent chemical erosion yield of graphite under high flux conditions

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Kallenbach, A.
Experimental Plasma Physics 4 (E4), Max Planck Institute for Plasma Physics, Max Planck Society;

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Bard, A.
Experimental Plasma Physics 4 (E4), Max Planck Institute for Plasma Physics, Max Planck Society;

Behringer, K. H.
Max Planck Society;

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Schmidtmann, K.
Experimental Plasma Physics 4 (E4), Max Planck Institute for Plasma Physics, Max Planck Society;

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Weinlich, M.
Tokamak Theory (TOK), Max Planck Institute for Plasma Physics, Max Planck Society;
Experimental Plasma Physics 3 (E3), Max Planck Institute for Plasma Physics, Max Planck Society;

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Kallenbach, A., Thoma, A., Bard, A., Behringer, K. H., Schmidtmann, K., Weinlich, M., et al. (1998). Evidence for hydrogen flux dependence of the apparent chemical erosion yield of graphite under high flux conditions. Nuclear Fusion, 38(7), 1097-1103. doi:10.1088/0029-5515/38/7/311.

Cite as: https://hdl.handle.net/11858/00-001M-0000-0027-883B-A

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