南海北部深海软土压缩特性试验研究

    EXPERIMENTAL STUDY ON COMPRESSION CHARACTERISTICS OF DEEP-SEA SOFT SOIL IN NORTHERN SOUTH CHINA SEA

    • 摘要: 深海软土由于具有高压缩性常常导致海洋工程构筑物的沉降破坏。近年来,我国在南海进行了一系列工程建设及资源开发,但由于对深海软土认识不足造成深海工程建设及资源开发面临严峻挑战。为此,本文通过全岩分析、固结压缩、压缩-回弹-再压缩试验,研究了中国南海深海沉积软土压缩特性,分析了初始孔隙比、应力历史和含水率对压缩的影响。试验结果表明:该软土为高液塑限黏土,矿物成分中以方解石和伊利石为主,颗粒级配不良;饱和土在固定荷载下沉降量与时间之间的关系可用双曲线模型描述;压缩系数基本大于0.5 MPa-1,压缩指数整体呈现线性增加,200~400 kPa时增长速度变得缓慢,随后加快;e-lg p曲线呈现“前缓后陡”形态,且存在一个明显转折点(屈服应力),屈服前变形量很小,屈服后变形迅速增大;初始含水率与屈服应力的关系可通过幂函数表示。

       

      Abstract: Deep-sea soft soil often leads to settlement failure of marine engineering structures due to its high compressibility. China has carried out a series of engineering constructions and resource developments in the South China Sea in recent years. However,due to insufficient understanding of deep-sea soft soil,deep-sea engineering construction and resource development face severe challenges. Through whole-rock analysis,consolidation compression,and compression-rebound-recompression tests,this work studies the compression properties of deep-sea sedimentary soft soil in the South China Sea and analyzes the effects of initial void ratio,stress history,and water content on compression. The results indicate that the soft soil is clay with a high liquid plastic limit,and the mineral components are mainly calcite and illite,which have poor particle gradation. The relationship between settlement and time of saturated soil under fixed load can be described by a hyperbolic model. The compression coefficient is much larger than 0.5 MPa-1. The compression index first increases linearly and then slowly increases when 200~400 kPa,and rapidly increases in the last. The e-lgp curve presents a slow front and steep back shape,and there is an obvious turning point(yield stress). The deformation before yielding is small and increases rapidly after yielding. The relationship between initial water content and yield stress can be described as a power function.

       

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