研究生: |
李昱成 Yu-Cheng Lee |
---|---|
論文名稱: |
以土壤波速與基質吸力探討不飽和夯實紅土視凝聚力與應變相依模數 A Study on Apparent Cohesion and Strain-dependent Modulus of Unsaturated Lateritic Soil Based on Wave Velocity and Matric Suction |
指導教授: |
林宏達
Horn-Da Lin |
口試委員: |
王建智
Chien-Chih Wang 拱祥生 Hsiang-Sheng Kung 鄧福宸 Fu-Chen Teng |
學位類別: |
碩士 Master |
系所名稱: |
工程學院 - 營建工程系 Department of Civil and Construction Engineering |
論文出版年: | 2020 |
畢業學年度: | 108 |
語文別: | 中文 |
論文頁數: | 154 |
中文關鍵詞: | 不飽和土壤 、基質吸力 、土壤波速 、視凝聚力 、應變相依模數 |
外文關鍵詞: | unsaturated soil, matric suction, wave velocity, apparent cohesion, strain-dependent modulus |
相關次數: | 點閱:212 下載:4 |
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夯實土壤長時間處於不飽和狀態,可能受日曬及降雨等天氣因素而改變土壤內部含水量,進而影響強度及勁度等。本研究針對不飽和夯實紅土進行一系列室內試驗,包括土壤基本物性試驗、無圍壓縮試驗、超音波試驗及不飽和三軸暨彎曲元件試驗。然後根據這些試驗結果,探討基質吸力對土壤波速、視凝聚力及應變相依模數之影響,並建立簡易方法來評估不飽和土壤性質。
試驗結果顯示,隨著基質吸力提升,土壤波速、視凝聚力及應變相依模數皆隨之提升。深入探討土壤波速與視凝聚力關係,發現兩者呈線性相關。以此為根據,建立波速推估視凝聚力評估式,推估結果良好,MAPE值約為20%。因此,工程上以簡易的非破壞性試驗來評估不飽和土壤之剪力強度應屬可行。夯實土壤應變相依模數探討結果顯示,在相同吸力下模數大小為濕側大於OMC,乾側最小。原因為乾側飽和過程中吸收水體積最多,導致顆粒間隙較大。而三側之不飽和土壤模數衰減皆較飽和土壤快。以γ0.7作為模數衰減指標值,發現強度越高其γ0.7值隨之遞減,也就是模數衰減越快。故基質吸力提高,無圍壓縮強度也隨之提高,進而使模數衰減越快。
Compacted soil is often in an unsaturated state. Weather factors such as sunlight and rainfall will change the water content of the soil, thereby affecting its strength and stiffness. This research conducted a series of tests on unsaturated compacted lateritic soils, including the soil basic property test, the unconfined compression test, the ultrasonic test and the unsaturated triaxial test with bender element. Test results were used to study the influence of the matric suction on the soil wave velocity, the apparent cohesion and the strain-dependent modulus. Simplified methods were developed to evaluate the properties of unsaturated soil.
The test results show that when the matric suction increases, the soil wave velocity, the apparent cohesion, and the strain-dependent modulus all increase. And the apparent cohesion is linearly related to the soil wave velocity. Based on this, the wave velocity is used to estimate the apparent cohesion. The estimation result is good, the value of MAPE is about 20%. Therefore, it should be feasible to use simple non-destructive tests to evaluate the shear strength of unsaturated soils. The results of the strain-dependent modulus of compacted soils show that the modulus is larger than the OMC on the wet side and the smallest on the dry side under the same suction. The reason is that the volume of absorbed water is the largest during the saturation process of the dry side, resulting in a larger particle spacing. The modulus of unsaturated soils of the three compaction conditions degrade faster than that of the saturated soil. Taking γ_0.7 as the modulus degradation index value, it is found that the value of γ_0.7 decreases with strength increases. As the results, matric suction increases, the unconfined compression strength increases, and the modulus degrades faster.
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