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Comparative studies on mechanical behavior of frozen natural saline silty sand and frozen desalted silty sand

机译:冷冻天然盐粉质砂和冷冻淡化粉质砂的力学性能比较研究

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To compare the mechanical behavior of natural frozen saline silty sand before and after a desalting process, the collected natural frozen saline silty sand with/without desalting is reconstituted to soil samples with water content at 13%. Triaxial compressive tests are carried out under confining pressures ranging from 0.3 to 3 MPa and at temperatures of -2 degrees C, -4 degrees C, and -6 degrees C. In the testing range of confining pressure and temperature, the natural frozen saline silty sand presents plastic failure and strain-hardening, whereas the desalted silty sand with the same water content exhibits brittle failure and obvious strain-softening. Thus, the experimental results show that the presence of salt obviously weakens soil brittleness. The strength of either the natural frozen saline silty sand or the desalted one increases with the increase of confining pressure but with the decrease of temperature. Additionally, the strength of the natural soil is lower than that of the desalted soil in all tests which indicates that the presence of salt can also reduce the strength of the frozen silty sand. The internal friction angle of the frozen natural soil first increases with the decrease of temperature and then maintains nearly at constant; adversely, the internal friction angle of the desalted soil sustains,as a constant within the testing temperature range. The cohesive force of both the natural and desalted frozen soil exhibits a linear growth as temperature decreases. Moreover, the cohesive force and the internal friction angle of the desalted soil are always higher than those of the natural soils. Lastly, the influence of temperature and confining pressure on initial tangent modulus (E-0) and secant modulus corresponding to half the strength (E-0.5) are analyzed. The E-0 and E-0.5 of the desalted frozen soil increase with the increase of confining pressure but with the decrease of temperature and are higher than the ones of the natural soil. Additionally, for either the natural or the desalted soil, E-0 is more sensitive to confining pressure compared with E-0.5. (C) 2016 Elsevier B.V. All rights reserved.
机译:为了比较天然冷冻盐水粉砂在脱盐之前和之后的机械性能,将收集的有/无脱盐的天然冷冻盐水粉砂重新配制为含水量为13%的土壤样品。三轴压缩试验是在0.3至3 MPa的围压下,在-2摄氏度,-4摄氏度和-6摄氏度的温度下进行的。在围压和温度的试验范围内,天然冷冻盐粉质砂岩表现出塑性破坏和应变硬化,而含水量相同的脱盐粉质沙石表现出脆性破坏和明显的应变软化。因此,实验结果表明,盐的存在明显减弱了土壤的脆性。天然冷冻盐粉质砂或脱盐砂的强度随围压的增加而增加,但随温度的降低而增加。另外,在所有测试中,天然土壤的强度均低于脱盐土壤的强度,这表明盐的存在也会降低冷冻粉质砂的强度。冷冻的天然土壤的内摩擦角首先随着温度的降低而增加,然后几乎保持恒定。不利地,脱盐土壤的内摩擦角在测试温度范围内保持恒定。天然和脱盐的冻土的内聚力都随温度降低而呈现线性增长。而且,脱盐土壤的内聚力和内摩擦角始终高于天然土壤。最后,分析了温度和围压对初始切线模量(E-0)和正切模量(对应于强度的一半)(E-0.5)的影响。脱盐冻土的E-0和E-0.5随围压的增加而增加,随温度的降低而增加,高于天然土。此外,对于天然土壤或脱盐土壤,E-0比E-0.5对围压更为敏感。 (C)2016 Elsevier B.V.保留所有权利。

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