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MPCVD低溫沉積金剛石薄膜及其特征

Low Temperature Deposition and Characterization of Diamond Thin Films by MPCVD

  • 摘要: 應用微波等離子體輔助的化學氣相沉積(MPCVD)工藝成功地實現了金剛石薄膜在700-790℃范圍內的低溫沉積.發現氧在CH4-H2系統中的引入不僅可以減小或消除Raman譜上位于1550cm-1的非金剛石特征峰,而且還使位于1332cm-1的金剛石特征峰半高寬顯著減小。正是由于原子態氧在較低溫度下具有遠比原子態氫強烈得多的對石墨和類金剛石碳的刻蝕作用,才用金剛石的低溫生長得以順利進行。本文詳細報導了金剛石薄膜低溫沉積工藝及其所得薄膜的表征結果,并就Bachmann等最近提出C-H-O金剛石相圖針對低溫沉積數據進行了討論。

     

    Abstract: Low temperature deposition of diamond thin films in the range of 700-300℃ has been successfully carried out by microwave plasma assisted CVD technique. It was found that the introduction of oxygen into the system of CH4-H2 not only lowered or even eliminated the diffused peak at 1550cm-1 caused by non-diamond phases, but also reduced the half height width of the diamond peak at 1332cm-1. It was because that the atomic oxygen did have a much stronger etching effect on graphite and diamond-like carbon than that of atomic hydrogen at relatively low temperatures, could the low temperature growth of diamond from the vapour phase become possible. Low temperature deposition and characterization of the resultant diamond films are reported in detail. An attempt to link the low temperature deposition data to the C-H-O phase diagram recently proposed by Bachmann et al. has also been made.

     

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