吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (5): 1551-1559.doi: 10.13278/j.cnki.jjuese.20210041
桑松魁1,2, 王永洪1, 张明义1, 孔亮3, 吴文兵4, 陈志雄5, 李兆龙6, 张启军7
Sang Songkui1,2, Wang Yonghong1, Zhang Mingyi1, Kong Liang3, Wu Wenbing4, Chen Zhixiong5, Li Zhaolong6, Zhang Qijun7
摘要: 为研究层状黏性土在静压桩沉桩过程中桩土界面孔隙水压力的分布规律,依托山东东营某桩基工程开展了现场足尺静压桩试验,分析了桩土界面孔隙水压力的变化规律,探讨了桩土界面超孔隙水压力的分布特征,明确了桩土界面孔隙水压力和超孔隙水压力的消散特性,并结合水力压裂理论和孔穴扩张理论,揭示了沉桩过程中桩土界面沿桩长方向超孔隙水压力的分布形式。试验结果表明:孔隙水压力、超孔隙水压力与土层性质密切相关,二者均在粉土层中增长较慢,在粉质黏土层中增长较快;在同一深度处,两者均存在明显的消散现象,在粉土中的消散程度明显大于粉质黏土中;采用水力压裂理论结合孔穴扩张理论计算的超孔隙水压力沿桩长方向的变化规律与试验值相吻合;桩身贯入深度越大,超孔隙水压力理论计算值与现场实测值越接近。
中图分类号:
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