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南黄海中部海底沉积物剪切波速度测量及其与物理力学性质参数的关系 被引量:5
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作者 阚光明 张一凡 +2 位作者 苏远峰 李官保 孟祥梅 《海洋科学进展》 CAS CSCD 北大核心 2014年第3期335-342,共8页
采用弯曲元剪切波测试方法对在南黄海中部采集到的沉积物样品进行了剪切波速度测试,基于所获得的剪切波速度数据,分析了研究区沉积物剪切波速度特性及分布规律.分析表明,沉积物剪切波速度为12.05~74.55 m/s,总体相对较低.浅表层沉积物... 采用弯曲元剪切波测试方法对在南黄海中部采集到的沉积物样品进行了剪切波速度测试,基于所获得的剪切波速度数据,分析了研究区沉积物剪切波速度特性及分布规律.分析表明,沉积物剪切波速度为12.05~74.55 m/s,总体相对较低.浅表层沉积物剪切波速度呈现出分区域分布特征,可分为东北部低速区、西南部高速区、北西-南东向梯度带以及测区东南部的低速背景上的串珠状高速异常区四个区域.通过回归分析,建立了剪切波速度与密度、含水率、孔隙比、孔隙度、液限、塑限、压缩系数、抗剪强度等沉积物物理力学参数之间相互关系的经验回归公式.回归分析结果表明,海底沉积物剪切波速度与上述物理力学参数之间均具有较好的相关性,相关系数R均大于0.80. 展开更多
关键词 海底沉积物 剪切波速度 弯曲元系统 经验回归公式 南黄海
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土工试验中弯曲单元量测系统的开发
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作者 丁金伟 刘海笑 胡黎明 《实验技术与管理》 CAS 2007年第2期56-60,共5页
弯曲单元量测系统是一种实验室内用于无损检测土样最大剪切模量的土工试验手段。在综合研究国外同类系统的基础上,对弯曲单元测量系统进行了一系列的改进,简化了其硬件组成,用带声卡的电脑实现了示波器和信号发生器的相关功能;同时... 弯曲单元量测系统是一种实验室内用于无损检测土样最大剪切模量的土工试验手段。在综合研究国外同类系统的基础上,对弯曲单元测量系统进行了一系列的改进,简化了其硬件组成,用带声卡的电脑实现了示波器和信号发生器的相关功能;同时开发了配套的软件系统,使土工试验中可以进行实时检测和信号处理。该系统成本低廉、界面友好、操作方便,已经被安装到清华大学动三轴试验系统上,并且在天津新港软粘土动三轴试验中得到应用。 展开更多
关键词 土工试验 弯曲单元量测系统 压电传感器 最大剪切模量 LABVIEW
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Laboratory investigation on relationship between degree of saturation, B-value and P-wave velocity 被引量:4
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作者 GU Xiao-qiang YANG Jun HUANG Mao-song 《Journal of Central South University》 SCIE EI CAS 2013年第7期2001-2007,共7页
Laboratory tests were performed on Toyoura sand specimens to investigate the relationship between degree of saturation Sr, B-value and P-wave velocity Vp. Different types of pore water (de-aired water or tap water) ... Laboratory tests were performed on Toyoura sand specimens to investigate the relationship between degree of saturation Sr, B-value and P-wave velocity Vp. Different types of pore water (de-aired water or tap water) and pore gas (air or CO2) as well as different magnitudes of back pressure were used to achieve different Sr (or B-value). The measured relationship between B-value and Vp was not consistent with the theoretical prediction. The measurement shows that the Vp value in the specimen flushed with de-aired water is independent of B-value (or St) and is always around the one in fully saturated condition. However, the Vp value in the specimen flushed with tap water increases with B-value, but the shape of the relationship between Vp and B-value is quite different from the theoretical prediction. The possible explanation for the discrepancy between laboratory measurement and theoretical prediction lies in that the air exists in the water as air bubbles and therefore the pore fluid (air-water mixture) is heterogeneous instead of homogenous assumed in the theoretical prediction. 展开更多
关键词 degree of saturation B-VALUE P-wave velocity bender element
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Shear wave velocity in granular soil considering effects of inherent and stress-induced anisotropy
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作者 Bayat MEYSAM 《Journal of Central South University》 SCIE EI CAS CSCD 2021年第5期1476-1492,共17页
The aim of this research was to explain the effects of relative density,mean effective stress,grading characteristics,consolidation stress ratio and initial fabric anisotropy produced during specimen preparation on sh... The aim of this research was to explain the effects of relative density,mean effective stress,grading characteristics,consolidation stress ratio and initial fabric anisotropy produced during specimen preparation on shear wave velocity(Vs).It is shown that the Vs of the consolidated specimens under anisotropic compression stress is greater than that of the consolidated specimens under isotropic or anisotropic extension stress states at a given relative density and effective confining stress.It is also shown that the depositional technique that was used to create reconstituted specimens has important effect on the Vs.A parallel comparison of measured values from the resonant column and bender element tests is also presented.These results of the tests have been employed to develop a generalized relationship for predicting Vs of granular soils.The Vs model is validated using data collected from literatures.Based on the results,it can be conducted that the proposed model has a good performance and is capable of evaluating the Vs of granular soil. 展开更多
关键词 ANISOTROPY SAND GRAVEL bender element resonant column shear wave velocity
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