| 研究生: |
李昕澄 Lee, Hsin-Cheng |
|---|---|
| 論文名稱: |
Zn(Nb1-xTax)2O6陶瓷材料其微波介電性質與結構之探討 Microwave Dielectric Properties and Structure of Zn(Nb1-xTax)2O6 Ceramics |
| 指導教授: |
黃啟原
Huang, Chi-Yuen |
| 學位類別: |
碩士 Master |
| 系所名稱: |
工學院 - 資源工程學系 Department of Resources Engineering |
| 論文出版年: | 2010 |
| 畢業學年度: | 98 |
| 語文別: | 中文 |
| 論文頁數: | 67 |
| 中文關鍵詞: | 鈳鐵礦 、鈳鉭鐵礦 、有序程度 、ZnNb2O6 |
| 外文關鍵詞: | ZnNb2O6, columbite, ixiolite, ordering degree |
| 相關次數: | 點閱:57 下載:4 |
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ZnNb2O6材料為鈳鐵礦結構 (columbite)。此材料之燒結溫度約在1000-1200°C,且具有良好的微波介電性質。
在近幾十年來有許多文獻探討鈳鐵礦結構 M+Nb2O6,但大多數研究均集中探討以不同元素取代 M+,所造成性質之改變。而過去研究指出,添加少量 Ta5+於 ZnNb2O6 中,能夠完全固溶於結構中並形成 Zn(Nb1-xTax)2O6 成份系統。
故本研究以 x=0-0.1 之Ta5+ 少量取代 Nb5+,形成純相之固溶體 Zn(Nb1-xTax)2O6,探討其晶體結構、微結構與微波介電性質的關係。
在本實驗燒結條件為升溫速率 5°C / min 升到 1150 °C,並持溫 2 小時情況下,不同成份點之微結構、粒徑大小和密度皆無明顯的改變 (相對密度變化在 96.1% 至 96.7% 之間),但其微波介電性質 Q×f 有大幅度的改變。
而介電常數 (r) 由 x=0 時 22.9 提升至 23.1 (x=0.05),雖有增加,但變化之幅度不明顯。但當x=0時 Q×f 值為 80,000,而在 x=0.05 時提升至 130,000 (at 8.81 GHz),而添加 Ta5+ 至 x=0.1 時,Q×f 值下降至 88,000。
在晶體結構部分:鈳鉭鐵礦 (ixiolite)具有鈳鐵礦類似之結構,且可視為鈳鐵礦之無序結構,而在前人文獻指出,當鈳鉭鐵礦轉變為鈳鐵礦時會出現 (040) 繞射面。從長時間 X 光繞射光譜計算可知,在 x=0.05 時,有序程度 (I040/ I040+ I031) 較 x=0 時有些微上升;從 9.84 升至13.41,故推測 Q×f 值上升與結構之有序程度有關。
ZnNb2O6 with a columbite crystal structure have good microwave dielectric properties and sintered temperature about 1000-1200°C. The binary niobate compounds with general formula M+Nb2O6 was interested in last decade, and most of articles focus how the M+ effects dielectric properties of M+Nb2O6. In the past study, it is substituting small amount Nb5+ with Ta5+ of the ZnNb2O6 ceramics can forming solid solution Zn(Nb1-xTax)2O6.
At this study sintering condition (sintering temperature 1150°C for 2 h), by increasing x, not only the microstructure, grain size but relative density (change from 96.1% to 96.7%) have not change obviously. But the Q×f (at 8.81 GHz) be tremendously boosted from 80,000 GHz at x= 0 to a maximum 130,000 GHz at x=0.05. On the other hand, Q×f decrease to the 88,000 GHz at x=0.1.
Structurally, ixiolite can be regarded as a disorder form of columbite, and in the past study, when the ixiolite structure changes to columbite, the peak (040) will appear. At this study, the ordering degree (I040/ I040+ I031) is increase from 9.84 at x=0 to 13.41 x=0.05, so we conjectures the reason of Q×f increase is the ordering degree increase.
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