完整后设资料纪录
DC 栏位语言
dc.contributor.author张友诚en_US
dc.contributor.authorChang, Yu-Chengen_US
dc.contributor.author林志平en_US
dc.contributor.authorLin, Chih-Pingen_US
dc.date.accessioned2014-12-12T02:37:31Z-
dc.date.available2014-12-12T02:37:31Z-
dc.date.issued2012en_US
dc.identifier.urihttp://140.113.39.130/cdrfb3/record/nctu/#GT070051264en_US
dc.identifier.urihttp://hdl.handle.net/11536/73298-
dc.description.abstract  为了提升软弱地盘之强度与劲度,大地工程师们常用高压喷射灌浆或是挤压砂桩等地盘改良工法以达到上述目的,由于改良后会在地中形成固结物,使得土壤为高度非均质性。现有一课题值得探讨:如何决定改良成效?传统检核方法如钻孔取样、标准贯入试验因取样空间小、耗时且成本高等限制,想要取得此地盘整体平均的改良率有相当的难度,相反的表面波震测具有大范围取样,非破坏性及快速施作等优点,其反算得到的剪力波速剖面实质上反映了复合土体之弹性行为,但表面波方法有一基本假设是测线下方为水平一维层状地层,使得非均质土壤在剪力波速量测上却有均质化的特性,为此文献进行了二维数值模拟探讨,评估地盘改良率与剪力波速提升率之关系,但二维模拟建立的地层模型无法反映实际地盘改良场址,加上表面波震测会因侧向地层变化造成讯号收录有一定程度之影响,进行三维数值模拟有其必要性。
  本研究采用三维波谱元素法进行探讨,研究成果显示,表面波于改良后场址之行为,若是简化墙状地层模型,其剪力波速之均质化会遵守一维等效波速理论之下限;若于柱状地层模型,剪力波速之均质化不再遵守一维等效波速理论之下限,而是在等效模数理论之上下限之间,可根据模拟资料提出均质化等效速度与改良率之关系。表面波的侧向影响范围约为波长的1.3倍,在同样范围内,测线外异质土壤与测线内原土壤的速度比越大,量测速度受到的影响越大;当速度比相同的情况下,原土壤速度越低,量测速度受到的影响也越大。
zh_TW
dc.description.abstractSoft ground is often improved to increase strength and stiffness by methods such as jet grouting and stone column which result in heterogeneous ground with improved columns. Conventional methods used to assess such ground improvement are subjected to several limitations such as small sampling volume, time-consuming, and cost ineffectiveness. It’s difficult to assess the average property of the improved ground and the actual replacement ratio of ground improvement. The use of seismic surface wave method (i.e. multi-station analysis of surface wave, MASW) for such a purpose seems to be a good candidate. But the surface wave method is essentially a 1-D method assuming horizontally-layered medium. What MASW measures in the highly heterogeneous improved ground remains to be investigated. The feasibility of MASW in characterizing the heterogeneous ground with improved columns has been demonstrated and the relationship between replacement ratio and velocity increase has been studied by 2D model. This study aims to investigate the homogenization of shear wave velocity measured by MASW in real 3D condition. Testing results may also be affected by the survey line location relative to the improved columns. The lateral sampling space of the surface wave testing was also investigated by 3D modeling.
3D spectral element method was utilized for the numerical investigation. Numerical results show that the effective shear velocity can be derived based on lower bound of equivalent velocity model when the heterogeneous ground is a 2D wall-like structure. However, in real 3D column-embedded structure, the relation between the effective shear wave velocity and replacement ratio falls between upper bound and lower bound of the equivalent modulus model. A predictive model is derived based on the numerical simulations. The lateral sampling range is about 1.3 wavelength. In the same spatial range, the measured velocity is affected more by offline heterogeneous material for higher velocity contrast. At constant velocity contrast, lower velocity material along the survey line is affected more by offline heterogeneity.
en_US
dc.language.isozh_TWen_US
dc.subject表面波zh_TW
dc.subject表面波震测zh_TW
dc.subject波谱元素法zh_TW
dc.subject均质化zh_TW
dc.subject侧向变化地层zh_TW
dc.subjectsurface waveen_US
dc.subjectseismic surface wave methoden_US
dc.subjectspectral element methoden_US
dc.subjecthomogenizationen_US
dc.subjectlateral heterogeneous layeren_US
dc.title应用三维波传模拟表面波震测于复合土体有效剪力波速量测之探讨zh_TW
dc.titleThe study of effective shear wave velocity measurement in composite soil by application of three-dimensional simulation of surface waveen_US
dc.typeThesisen_US
dc.contributor.department土木工程系所zh_TW
显示于类别:Thesis


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