静剪模量与动剪模量的对比分析

Udota S. Benjamin, T. I., Horsfall I. Opiriyabo, Mogaba P.
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The results of soil dynamic modulus (shear, young and bulk modulus) and Poisson ratio recorded from DST conducted in BH1, BH2 and BH3 ranges from 7300 KPa to 72390 KPa, 0.31 to 0.41 for the Poisson ratio. Meanwhile, soil static modulus and Poisson’s ratio recorded from SPT conducted in BH1, BH2 and BH3 ranges from 2520 to 44687.0 KPa, 0.20 to 0.55 for the Poisson ratio respectively. The results of this study have shown that there is a wide variation between geomechanical properties derived from geotechnical investigations (static properties) and geophysical investigations (dynamic properties). Based on depth trend analysis, the dynamic and static soil elastic properties all increases with depth. Generally, the dynamic soil properties were significantly higher than the static elastic properties. At shallow depths (<12.0 m), the difference between static and dynamic soil modulus was relatively small, but increased with increasing depth. Meanwhile, the difference between static and dynamic Poisson ratio was high at shallow depth and it decreased with increased depths where they almost overlap. Correlation between the derived static and dynamic properties all revealed positive correlation trends. The strength of the correlation was highest for young modulus (r=0.87) which was closely followed by the shear modulus (r=0.63). Meanwhile, Poisson ratio (r=0.40) and bulk modulus (r=0.23) revealed weak positive correlation trends. The regression models generated from this study were used to derive static elastic properties and compared with the static properties obtained from geotechnical investigation thereby deriving the equations Dynamic Shear Modulus = (1.4207 x Static Shear Modulus) + 5022, Dynamic Young Modulus = (2.0241 x static young modulus) + 5054.8, Dynamic Bulk Modulus = (1.7852 x static bulk modulus) + 15458, Dynamic Poisson’s ratio = (0.1812 x Static Poisson’s ratio) + 0.3154. 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引用次数: 0

摘要

由于地震的发生会导致地基振动,可能导致建筑物和道路的破坏,因此了解和掌握地质力学土壤特性对于基础设计、风险评估和工程结构和道路建设中的缓解计划建议非常重要。在Assa内共钻了3口井,进行了标准穿透测试(SPT)和井下地震测试(DST),以研究该地区的地质力学土壤特性。在物探方面,进行了井下地震试验,确定了纵波和横波。利用地震成像程序对结果进行了广义倒数法(GRM)处理。在BH1、BH2和BH3进行DST测得的土体动模量(剪切、幼嫩和体积模量)和泊松比变化范围为7300 ~ 72390 KPa,泊松比变化范围为0.31 ~ 0.41。同时,BH1、BH2和BH3的土壤静模量和泊松比的变化范围为2520 ~ 44687.0 KPa,泊松比为0.20 ~ 0.55。这项研究的结果表明,在岩土工程调查(静态属性)和地球物理调查(动态属性)中得出的地质力学属性之间存在很大差异。基于深度趋势分析,土的动、静弹性特性均随深度增加而增加。一般情况下,土的动力特性显著高于静弹性特性。在较浅深度(<12.0 m),土壤动静态模量差异较小,但随深度增加而增大。静态泊松比与动态泊松比的差异在浅水深处较大,随着深度的增加而减小,两者几乎重合。所得的静、动态性能均呈现正相关趋势。杨模量的相关强度最高(r=0.87),其次是剪切模量(r=0.63)。泊松比(r=0.40)与体积模量(r=0.23)呈弱正相关趋势。利用本研究建立的回归模型推导静力弹性特性,并与岩土工程调查得到的静力特性进行比较,得到:动剪切模量= (1.4207 x静剪切模量)+ 5022,动杨氏模量= (2.0241 x静杨氏模量)+ 5054.8,动体积模量= (1.7852 x静体积模量)+ 15458,动泊松比= (0.1812 x静泊松比)+ 0.3154。结果表明,静力(岩土)剪切模量与静力(回归模型)剪切模量、静力(岩土)杨龄模量与静力(回归模型)杨龄模量具有较好的匹配关系。总体而言,体模量与泊松比没有很好的匹配,但在较浅的深度(< 12 m),泊松比显示出良好的匹配。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
COMPARATIVE ANALYSIS OF STATIC SHEAR MODULUS AND DYNAMIC SHEAR MODULUS DETERMINED BY GEOPHYSICAL AND GEOTECHNICAL INVESTIGATION
Due to the occurrence of earth tremors which leads to the vibrations of foundations and perhaps failure of buildings and roads, it is therefore important to understand and have knowledge of the geomechanical soil properties for foundation design, assessment of risks and suggestion of mitigation plans in engineering structures and road construction. A total of 3 boreholes were drilled with the Standard Penetration Test (SPT) performed and Downhole Seismic Test (DST) carried out in the boreholes located within Assa to investigate the Geomechanical soil properties in the area. For the geophysical survey, the downhole seismic test was carried out to determine the P-wave and S-wave. The results were processed using the generalized reciprocal method (GRM) with the Seisimager program. The results of soil dynamic modulus (shear, young and bulk modulus) and Poisson ratio recorded from DST conducted in BH1, BH2 and BH3 ranges from 7300 KPa to 72390 KPa, 0.31 to 0.41 for the Poisson ratio. Meanwhile, soil static modulus and Poisson’s ratio recorded from SPT conducted in BH1, BH2 and BH3 ranges from 2520 to 44687.0 KPa, 0.20 to 0.55 for the Poisson ratio respectively. The results of this study have shown that there is a wide variation between geomechanical properties derived from geotechnical investigations (static properties) and geophysical investigations (dynamic properties). Based on depth trend analysis, the dynamic and static soil elastic properties all increases with depth. Generally, the dynamic soil properties were significantly higher than the static elastic properties. At shallow depths (<12.0 m), the difference between static and dynamic soil modulus was relatively small, but increased with increasing depth. Meanwhile, the difference between static and dynamic Poisson ratio was high at shallow depth and it decreased with increased depths where they almost overlap. Correlation between the derived static and dynamic properties all revealed positive correlation trends. The strength of the correlation was highest for young modulus (r=0.87) which was closely followed by the shear modulus (r=0.63). Meanwhile, Poisson ratio (r=0.40) and bulk modulus (r=0.23) revealed weak positive correlation trends. The regression models generated from this study were used to derive static elastic properties and compared with the static properties obtained from geotechnical investigation thereby deriving the equations Dynamic Shear Modulus = (1.4207 x Static Shear Modulus) + 5022, Dynamic Young Modulus = (2.0241 x static young modulus) + 5054.8, Dynamic Bulk Modulus = (1.7852 x static bulk modulus) + 15458, Dynamic Poisson’s ratio = (0.1812 x Static Poisson’s ratio) + 0.3154. The results showed fairly good match between static (geotechnical) shear modulus and static (from regression model) shear modulus, static (geotechnical) young modulus and static (from regression model) young modulus. There was no good match obtained for bulk modulus and Poisson ratio generally, except at shallow depth (< 12 m depth) where Poisson ratio revealed a good match.
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