基于结构屈服压力的黄土湿陷性评价

    LOESS COLLAPSIBILITY ASSESSMENT BASED ON STRUCTURAL YIELD PRESSURE

    • 摘要: 随着黄土地区工程建设层次和标准的提高,对黄土湿陷性评价提出了更高的要求。本文以城际铁路西安-韩城线合阳段的湿陷性黄土为研究对象,现场开挖一30 m深的探井,按1 m间距取样,通过双线法湿陷试验测得12.5~4000 kPa下的天然与饱和黄土的压缩曲线,计算得到湿陷系数-压力曲线。从曲线上可以看出黄土湿陷系数随压力变化呈先增大后减小的趋势,湿陷系数随压力变化存在着一个峰值,与峰值湿陷系数相应的压力为天然黄土的结构屈服压力,湿陷起始压力为饱和黄土的结构屈服压力。为此提出用天然黄土结构屈服压力下的峰值湿陷系数评价黄土地基的湿陷量。同时发现,黄土湿陷性随深度的变异性大,湿陷性、非湿陷性及弱膨胀黄土在剖面上都有出现,当少量湿陷性土夹在非湿陷性或弱膨胀黄土之间时,湿陷变形可能被周围土层吸收,为此建议湿陷土层底界深度不宜按湿陷性土样的最大深度来确定,以湿陷性明显的土层底面确定较为合适。

       

      Abstract: With promotion of the level and standard of engineering construction in loess region,more strict demands are arisen to loess collapsibility evaluation. In this paper,collapsibility of the loess on the railway line from Xi'an to Hancheng was investigated. A sampling shaft of 30 m depth was excavated on the site of Heyang Loess Platform where the railway passes through. The samples were collected at 1 m interval. The basic physical indexes of the samples at each depth were measured first,and the collapsibility of them was measured with double-odometer test. The compression of the intact loess samples with both original water content and saturated were tested under the pressures of 12.5~4000 kPa respectively. The void ratios and the equivalent coefficients of collapsibility vs logarithmic pressure curves were obtained with the test results. The curves show that the coefficient of the loess collapsibility increases first and then decreases with the pressure increment. The coefficient of collapsibility exhibits a peak value with respect to pressure. The corresponding pressure to the peak collapsibility coefficient represents the structural yield pressure of natural loess,while the initial collapse pressure corresponds to the structural yield pressure of saturated loess. Therefore,the peak coefficient of collapsibility is proposed to evaluate the collapsibility of loess foundation. Meanwhile,it is found that the collapsibility of loess varies greatly with depth,collapsible loess,non-collapsible loess and weak expansive loess all exist on a profile. When a small amount of collapsible loess is interbedded in non-collapsible or weak expansive loess,the collapsible deformation may be balanced by the surrounding loess. Therefore,the depth of the lower boundary of collapsible loess layer should not be determined according to a single value of a loess sample,it is suggested that the base of the loess with obvious and continuous collapsibility should be recognized as the lower boundary of collapsible loess.

       

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