杭州某地区富水粉砂细砂地层物理力学特性研究

Huafeng Wang, Yangyi Zhang, Yanhua Gao, Yunfeng Guo, Fu-Shung Liu, Dongsheng Chen
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引用次数: 0

摘要

为深入探讨富水粉砂细层的基本物理力学特性,以杭州市富水粉砂层为工程背景,进行了密度、颗粒分析、直剪、无侧限压缩、三轴压缩等一系列物理力学试验。现场钻探表明,杭州地区主要由砂质粉砂和粉砂细砂混合粉砂组成。粉砂层土颗粒分析试验表明,粉砂细砂样品中大于0.075 mm的颗粒含量占50%~75%,多数分布范围为0.075~0.25mm。它是一种典型的粉砂细砂,粒度单一,级配差。室内土样力学试验表明,土样的无侧限压应力-应变曲线呈现弹塑性-延性特征。破坏方式为剪切破坏,剪切破碎带角度约为65°。直剪、未固结不排水和固结不排水三轴试验土样的黏聚角和摩擦角分别约为7.67~13.50KPa和36.35~41.54°。三者的结果较为接近,但均呈上升趋势。研究成果可为杭州地区的工程建设设计和施工提供参考意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on Physical and Mechanical Properties of the Water-rich Silt Fine Sand Stratum in an Area of Hangzhou
In order to deeply explore the basic physical and mechanical properties of the water-rich silt fine layer, taking the water-rich silt sand layer in Hangzhou city as the engineering background, a series of physical and mechanical tests including density, particle analysis, direct shear, unconfined compression and triaxial compression are carried out. On-site drilling reveals that the area in Hangzhou is mainly composed of sandy silt and silt fine sand mixed with silt. The particle analysis tests on the silt sand stratum soil show that the content of particles larger than 0.075 mm in the silt fine sand sample accounts for 50%~75% with a majority distribution range of 0.075~0.25mm. It is a typical silt fine sand with a single particle size and poor gradation. Laboratory mechanical tests of soil samples show that the unconfined compressive stress-strain curves of the soil sample show a characteristic of elastic-plastic-ductile. The failure mode is shear failure, and the angle of the shear fracture zone is about 65°. The cohesion and friction angle of the soil samples obtained from the direct shear, unconsolidated and undrained, and consolidated undrained triaxial tests are approximately 7.67~13.50KPa and 36.35~41.54° respectively. The results of three are closer but show an increasing trend. The research results can provide reference significance for engineering construction design and construction in Hangzhou area.
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