Skip navigation

DSpace

機構典藏 DSpace 系統致力於保存各式數位資料(如:文字、圖片、PDF)並使其易於取用。

點此認識 DSpace
DSpace logo
English
中文
  • 瀏覽論文
    • 校院系所
    • 出版年
    • 作者
    • 標題
    • 關鍵字
    • 指導教授
  • 搜尋 TDR
  • 授權 Q&A
    • 我的頁面
    • 接受 E-mail 通知
    • 編輯個人資料
  1. NTU Theses and Dissertations Repository
  2. 工學院
  3. 應用力學研究所
請用此 Handle URI 來引用此文件: http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/19322
標題: 固液界面性質與表面熱滲流成因之研究
Research on Solid-Liquid Interface Properties and Constitution of Thermo-Osmosis
作者: Shih-Yun Lin
林詩芸
指導教授: 江宏仁(Hong-Ren Jiang)
關鍵字: 熱滲流,熱泳,表面張力,多孔薄膜,滑移流,
Thermo-osmosis,Thermophoresis,Surface Tension,Membrane,Slip Flow,
出版年 : 2016
學位: 碩士
摘要: 熱滲流為溫度梯度而產生的流動,此流動在多孔物質材料中已被研究探討多年,迄今仍沒有完整且通用的模型與機制。同樣因溫度梯度產生物質流現象的膠體粒子熱泳研究中指出,將膠體粒子固定於一溫度梯度中,該粒子的周圍會產生一流動稱為滑移流,其方向與該粒子本身熱泳方向相反,但此文獻中並未對滑移流作直接的量測。本實驗希望利用在平板表面製造一溫度梯度,進而了解溫度梯度所造成的流動與多孔物質材料中的熱滲流、膠體粒子表面之滑移流間的關聯性及成因。本實驗著重於表面性質對於該流動所產生的影響,研究方法為對基材表面作氧電漿表面改質及改變其表面電荷密度,觀察不同表面特性所對應的流動情形,並且利用二氧化矽粒子來追蹤因基材表面溫度梯度而產生流場現象。在本實驗的主要結果中,當基材表面巨觀的接觸角不同時,其因溫度梯度而產生的表面流動現象也會有所不同,並且隨著表面親水程度越強(接觸角越小),其流動速度會逐漸變小,甚至發生流動方向相反(原流動方向為低溫至高溫)的情形。熱滲流相關文獻中提及,不同多孔薄膜其形成的熱滲流方向相反,在疏水薄膜上其流動由低溫流向高溫;膠體粒子熱泳中,聚苯乙烯粒子表面疏水,其熱泳方向由高溫處往低溫移動,若其表面確實有所謂滑移流,則該流動方向由低溫流向高溫,這些結果皆與本實驗相符,因此溫度梯度而產生的物質流動,確實與表面性質有極大的相關。
Thermophoresis is a phenomenon when there exists a temperature gradient, and it would cause a matter flow. Previous research on thermophoresis suggests that it is caused by the slip flow which has been observed around particles. When a particle is fixed in an area with a temperature gradient, the flow happens in the opposite direction against thermophoresis. However, the research does not go any further and does not suggest how and why slip flow is generated. We are interested in if these two phenomena caused by the temperature gradient alike are related. If a particle is huge enough, a tiny part of the surface can be treated as a plane. Thus, the problem can be simplified and we need to consider what happens in the solid-liquid interface. In addition, slip flow is equivalent to thermos-osmosis which is defined as the flow generated by temperature gradient in the interface. The results shows that the wettability has a significant effect on the flow: here in after, the contact angle is used as the index of wettability. When θ = 30∘, driving forces equilibrated and no flow occurred. When θ > 30∘, the flow from the cold side to the hot side occurred. Reversely when θ < 30∘, the flow from the hot side to the cold side occurred. This result accords with the research of thermos-osmosis in porous materials. In addition, changing the property of particle surface shows that the direction of thermophoresis is related to its surface property. Hydrophobic PS (polystyrene) particle escapes from hot side in usual. Neither thermophoresis nor thermos-osmosis have been understand fully and almost do experiment indirectly. In our research, thermos-osmosis would not only follow the prediction but also thermophoresis. This suggest will make the research on the mechanism of thermophoresis simpler.
URI: http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/19322
DOI: 10.6342/NTU201600950
全文授權: 未授權
顯示於系所單位:應用力學研究所

文件中的檔案:
檔案 大小格式 
ntu-105-1.pdf
  未授權公開取用
6.65 MBAdobe PDF
顯示文件完整紀錄


系統中的文件,除了特別指名其著作權條款之外,均受到著作權保護,並且保留所有的權利。

社群連結
聯絡資訊
10617臺北市大安區羅斯福路四段1號
No.1 Sec.4, Roosevelt Rd., Taipei, Taiwan, R.O.C. 106
Tel: (02)33662353
Email: ntuetds@ntu.edu.tw
意見箱
相關連結
館藏目錄
國內圖書館整合查詢 MetaCat
臺大學術典藏 NTU Scholars
臺大圖書館數位典藏館
本站聲明
© NTU Library All Rights Reserved