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杨钢, 杨庆, 李吴刚. 平行试样土水特征曲线及其力学性质的试验研究[J]. 岩土工程学报, 2018, 40(S1): 224-228. DOI: 10.11779/CJGE2018S1036
引用本文: 杨钢, 杨庆, 李吴刚. 平行试样土水特征曲线及其力学性质的试验研究[J]. 岩土工程学报, 2018, 40(S1): 224-228. DOI: 10.11779/CJGE2018S1036
YANG Gang, YANG Qing, LI Wu-gang. Experimental research on soil water characteristic curve of parallel specimens and its influence on mechanical behavior[J]. Chinese Journal of Geotechnical Engineering, 2018, 40(S1): 224-228. DOI: 10.11779/CJGE2018S1036
Citation: YANG Gang, YANG Qing, LI Wu-gang. Experimental research on soil water characteristic curve of parallel specimens and its influence on mechanical behavior[J]. Chinese Journal of Geotechnical Engineering, 2018, 40(S1): 224-228. DOI: 10.11779/CJGE2018S1036

平行试样土水特征曲线及其力学性质的试验研究

Experimental research on soil water characteristic curve of parallel specimens and its influence on mechanical behavior

  • 摘要: 基于压力板仪对相同制样参数的8个三轴试样进行SWCC试验,对比试样土水特征曲线的差异,并对试验完成后的7个有效三轴试样进行无侧限抗压强度试验。通过对比研究剪切力与剪切位移关系、峰值强度与饱和度关系等内容,对试样的力学性质进行研究,并通过饱和度时程曲线对其结果进一步分析。研究结果表明:即便是相同条件制备的试样,其SWCC之间也会存在差异性,并与一定基质吸力范围相对应,但随着基质吸力增大,SWCC趋于一致;在SWCC试验后,由于高基质吸力下试样的平衡饱和度差异极小,试样的峰值强度与平衡饱和度没有必然联系;在一定基质吸力范围内,饱和度时程曲线相近的试样,最终的力学特性也相近,考虑这一基质吸力范围对应的孔隙在试样中占主导地位,因此这段时程曲线可以为试样均一性的研究提供一定思路。

     

    Abstract: The drying tests on eight triaxial specimens with the same remolding condition are carried out for soil water characteristic curve (SWCC). The differences of SWCC are compared. The unconfined compressive strength tests on seven effective specimens after SWCC tests are carried out. The relationships of shear force-shear displacement, peak strength-saturation degree, and saturation degree-time are investigated for analyzing the mechanical behavior of specimens. The results show that there are significant differences for SWCC in a certain range of matric suction, and with the increase of matrix suction SWCC will tend to be uniform. After SWCCs tests are finished, differences of equilibrium saturation degree between parallel specimens are very small because of high matrix suction, and then the peak strength and equilibrium saturation degree do not have necessary connection. At a certain range of matric suction, the specimens with similar curves of saturation degree versus time have approximate mechanical behavior. Because the pore ranges corresponding to this range of matric suction play a leading role in the specimens, the uniformity of specimens will be studied by the corresponding curves of saturation degree versus time.

     

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