透過您的圖書館登入
IP:18.217.144.32
  • 學位論文

邊坡管湧之臨界水力坡降值推估

The Assessment of Critical Hydraulic Gradient for Sloping Fields Piping

指導教授 : 張德鑫

摘要


管湧現象是指土體中的細小顆粒通過粗大顆粒間孔隙,並發生移動或被水流帶出的情形。管湧發生的位置會在滲流出口附近,也會發生在土體內部。一般傳統判斷邊坡破壞時水力梯度,是以整體的方式來取得數據,所得到的數據皆為一個範圍的平均水力梯度;另一方面砂土在含有水分時具有凝聚力,但傳統上卻忽略其值,而使管湧發生時推估得到的水力梯度並不精確。本研究利用臨界水力坡降公式及數值模擬方法觀察微小顆粒土壤在滲流坡面的受力情形,探討在不同坡度及粒徑下微小土壤顆粒所能承受的水力梯度值。 本研究首先進行實驗室管湧現象模型試驗,所選用材料第一組為過50號篩停60號篩之標準砂,第二組為混合砂。其次,利用運動方程式推導發生管湧時,微小土壤顆粒在坡面上之臨界水力梯度。再利用FEMWATER模式模擬管湧試驗,根據實驗結果所得到之參數條件及邊界條件代入模式進行模擬,得到水流速度及水力梯度值。最後,分析三方面在不同條件下之結果差異,並根據模擬結果反推求其非飽和情況下凝聚力及有效摩擦角。本研究由管湧試驗、理論公式及數值模擬三者比較,在臨界水力梯度方面三者相當接近;修正未飽和砂層之凝聚力在0.0660~0.0891(N/cm2)之間,而有效摩擦角在土壤含水時比乾砂略大0.8~2.0度,可供工程上參考。

並列摘要


The piping phenomenon means that soil particles move along the pathway among particles of the soil-body framework or when soil particles are taken out from the soil-body. The position of piping phenomenon occurs seepage outlet or inside of siol-body.In general, We come to obtain the hydraulic gradient by way of whole, but the data we got that is the average hydraulic gradient; On the other hand the sandy soil when includes the moisture content has the cohesive force, but in the tradition actually neglects this value, it causes the hydraulic gradient not to be certainly precise when piping phenomenon occurrence. The research uses critical hydraulic gradient equation and GMS to observe the hydraulic gradient of soil particle in the piping phenomenon. Firstly, this research involves the model experiment on lab piping phenomenon. Selects the material first group for pass 50 sieve and stops 60 sieve of standard sand, the second group for mixes sand.Secondly, we build critical Hydraulic Gradient equation that is derived from movement equations. Thirdly, according to parameter condition and boundary condition which were got from the experimental result, that bring into GMS and get the velocity of fluid and the hydraulic gradient by GMS. Finally, the research analyzes the different result under different conditions between three methods, and revises its cohesive strength and effective friction angle.The research uses piping phenomenon experiment, the theory formula and GMS to analyze the hydraulic gradient, and compares each other, three quite approaches in the critical hydraulic gradient aspect; obtains the cohesive strength scope between 0.0660and 0.0891(N/cm2),as for the effective friction angle, dank sand is slightly bigger than dry sand for 0.8°~2.0°, may supply in the project to refer.

參考文獻


24. 林繼立(2005),「坡地裂縫位置對邊坡穩定之影響」,私立中原大學土木工程學系碩士論文,P.34-55。
20. 林勝鴻(2005),「邊坡管湧現象及坡地安全之探討」,私立中原大學土木工程學系碩士論文,P.10-26。
1. 鄭建志(2006),「斜坡均質土體滲流之實驗研究」,國立中央大學土木工程學系碩士論文,P.4-17。
21. 鄭世才(2007),「邊坡管湧現象及水力坡降關係之探討」,私立中原大學土木工程學系碩士論文,P.20-34。
15. 詹坤哲(2004),「滲流作用引發土石流」,國立中興大學水土保持學系碩士論文,P.8-38。

被引用紀錄


曹書瑋(2016)。水平透水帶對邊坡管湧現象減緩之探討〔碩士論文,中原大學〕。華藝線上圖書館。https://doi.org/10.6840/cycu201600703
鄧雍瀚(2010)。不同級配砂對邊坡管湧現象之探討〔碩士論文,中原大學〕。華藝線上圖書館。https://doi.org/10.6840/cycu201000911
王欣雅(2009)。非均質邊坡管湧現象之探討〔碩士論文,中原大學〕。華藝線上圖書館。https://doi.org/10.6840/cycu200901072

延伸閱讀