| NUCLEAR PHYSICS |
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Deuterium Retention in the Co-Deposition Carbon Layers Deposited by Radio-Frequency Magnetron Sputtering in D2 Atmosphere |
| ZHANG Wei-Yuan1,2, SHI Li-Qun1,2**, ZHANG Bin1,2, HU Jian-Sheng3 |
1Applied Ion Beam Physics Laboratory, Institute of Modern Physics, Fudan University, Shanghai 200433
2Department of Nuclear Science and Technology, Fudan University, Shanghai 200433
3Institute of Plasma Physics, Chinese Academic of Sciences, Hefei 230031
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| Cite this article: |
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ZHANG Wei-Yuan, SHI Li-Qun, ZHANG Bin et al 2014 Chin. Phys. Lett. 31 052901 |
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Abstract Carbon is deposited on C and Si substrates by rf magnetron plasma sputtering in a D2 atmosphere. The deposited layers are examined with ion beam analysis and thermal desorption spectroscopy (TDS). The growth rates of the layers deposited on Si decrease with increasing substrate temperature, while increase significantly with the increase of D2 pressure. Meanwhile, the deuterium concentrations in the layers deposited on the Si substrates decrease from 30% to 2% and from 31% to 1% on the C substrates, respectively, when the substrate temperature varies from 350 K to 900 K. Similarly, the D concentration in the layer on the Si substrates increases from 3.4% to 47%, and from 8% to 35% on the C substrates when the D2 pressure increases from 0.3 Pa to 8.0 Pa. D desorption characterized by TDS is mainly in the forms of D2, HD, HDO, CD4, and C2D4, and a similar release peak occurs at 645 K. The release peak of D2 molecules at 960 K can be attributed to the escaped gas from the thin co-deposited deuterium-rich carbon layer in the form of C–D bonding.
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Published: 24 April 2014
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| PACS: |
29.25.-t
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(Particle sources and targets)
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29.27.-a
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(Beams in particle accelerators)
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29.40.Wk
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(Solid-state detectors)
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