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研究生:洪國華
研究生(外文):Hung, Guo-Hwa
論文名稱:打樁引致土壤內孔隙水壓變化及地盤變位之量測
論文名稱(外文):In-situ measurement of pore water pressure and ground deformation induced by pile drivings
指導教授:黃俊鴻黃俊鴻引用關係
指導教授(外文):Hwang Jing-Hung
學位類別:碩士
校院名稱:國立中央大學
系所名稱:土木工程學系
學門:工程學門
學類:土木工程學類
論文種類:學術論文
論文出版年:1998
畢業學年度:86
語文別:中文
論文頁數:107
中文關鍵詞:打樁孔隙水壓地盤變位現地試驗
外文關鍵詞:pile drivingpore water pressureground deformationin-situ test
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本研究配合高鐵位於嘉義太保之基樁試驗計畫,事先於預鑄混凝土樁群(
樁徑80cm,樁長34m)周圍土壤內不同距離處埋設孔隙水壓計、傾度管及
水準點等監測儀器,以量測打樁所引致土壤內孔隙水壓變化及地盤變位。
根據量測結果可定性及定量地評估基樁打設之擠壓效應、影響範圍、及其
與地層剖面之相關性,可作為打樁施工控制及環境影響評估之基本參考資
料。本研究中發現,打樁所引致之最大超額孔隙水壓在砂土層中約為1.5
倍的現地有效覆土有效應力,而黏土層中則為3.5倍,此外超額孔隙水壓
隨著水壓計距離之增加而迅速遞減,約15倍樁徑後,超額孔隙水壓幾乎可
以忽略;而孔隙水壓消散以砂土層最快約3.5分鐘即消散完畢,而黏土層
約需18小時;在最大超額孔隙水壓的預測上,黏土層以Massarsch與
Ladanyi經驗法,砂土層則是以D'Appolonia and Lambe經驗法之分析結果
最為接近;若以孔穴擴張理論來評估孔隙水壓,只要慎選參數亦能獲得不
錯結果。而以彈性理論來模擬水平徑向位移,其位移隨距離增加而遞減之
趨勢與實際量測值有明顯差異,此外打樁造成地表最大隆起為4.5cm。由
打樁前後CPT剖面之對比,顯示打樁可使鬆砂變緊,緊砂變鬆,大致上以
qc=110∼135bar為分界值,而黏土層將因受擾動而使其強度降低約40%。

During the pile drivings of three precast concrete piles of
the Chiayi-Taipo Large Scale Pilot Pile Test for the High Speed
Rail Project, a network of piezometers, inclinometers and level
posts were deployed around the pile driving area to monitor the
variations of soil water pressure and the ground deformations
induced by pile drivings. Each of the piles driven has a
diameter of 80cm and a length of 34m. The results measured have
clearly revealed, qualitatively and quantitatively, the
squeezing phenomenon and its influencing area during the
penetration process of the piles. Besides, the correlation
between the resistance of pile driving and the geological
condition of the site has also been identified. The results of
measurement are very valuable and useful for engineering
applications. It is shown that in the vicinity of the pile
,very high excess pore pressure are developed, it approaching
1.5 times the in-situ vertical effective stress in sand and 3.5
times in clay and beyond 15 times pile diameters the excess pore
pressure are virtually negligible. The time of dissipation of
excess pore pressure in sand is about 3.5 minute and 18 hours in
clay. To predict the maximum excess pore pressure, the measured
results in clay agree well with the empirical method proposed by
Massarsch or Ladanyi and the results in sand agree well with
that proposed by D'Appolonia and Lambe. We also can get good
result from the "Cavity Expansion Theory" in both clay and sand
if we can choose the parameter carefully. If simulating the
lateral deformation with "Elastic Theory", the decreasing trend
is siginificantly different with the field measured value.

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