循環(huán)荷載作用下海積軟土動力特性及細(xì)觀結(jié)構(gòu)試驗研究
[Abstract]:The site formed by sand blowing and reclamation is usually covered with thick layer of marine silt soft soil, and the coastal area is an area where earthquakes occur frequently. The poor engineering characteristics of soft soil have a great influence on earthquake action. Therefore, from the point of view of engineering earthquake prevention and disaster reduction, the dynamic characteristics of Beihai marine soft soil under the influence of three different factors are studied by dynamic triaxial test, and the mercury injection test and scanning electron microscope test are carried out on the soil samples before and after cyclic loading. The variation law of soil micro-structure and the influence of three elements on the micro-structure are studied quantitatively. The relationship between the characteristic parameters of meso-structure and the macro-property parameters is established, and the mechanical behavior of soil displacement and deformation is explained from the point of view of meso. The main results of this paper are as follows: (1) Beihai marine soft soil is sandy clay, and the main mineral components are quartz and kaolin. Under the action of overburden load, the maximum vertical settlement deformation is 44%, and the settlement deformation rate slows down gradually with the increase of load grade, and finally tends to be stable. The prepared soil samples have the characteristics of high porosity and high saturation. (2) in dynamic triaxial tests, with the increase of dynamic load amplitude, the dynamic deformation of Beihai marine soft soil evolves from elastic stable state to plastic expansion state. And different factors have different influence on soil dynamic characteristics. The strength and stiffness of marine soft soil will be decreased with the increase of consolidation ratio, and the effect of consolidation ratio on soil deformation is relatively small. The increase of consolidation confining pressure can obviously improve the deformation resistance of soil and reduce the energy transfer consumption in soil. When the vibration frequency is 0.05Hz~1Hz, the deformation curve of soil sample is hyperbolic and stable, and when the frequency is 2Hz, the deformation curve is hardening. The lower the vibration frequency is, the more favorable the dynamic deformation is, and the decrease of frequency will weaken the strength and stiffness of soil. (3) according to the pore characteristics of marine soft soil, the pore size is divided into four grades, and the pore size of the undisturbed sample is distributed as a single peak. The mesopore has the absolute advantage. It is found that the total pore volume of soil samples increases after cyclic loading, but the main pore content is medium pore content, the distribution of pore size in each group is adjusted, the small pore content decreases and the macropore content increases. The larger the consolidation ratio is, the smaller the macroporous content is, the smaller the total pore volume is, and the higher the consolidation confining pressure is, the less the pore volume of soil is. The effect of vibration frequency on pore distribution is complex under the coupling of various factors. (4) qualitative analysis of SEM images shows that the soft clay in Beihai Sea is a scaffold mosaic structure with surface to surface contact and a small amount of surface to edge contact. The basic unit is mainly composed of "clay domain" stacked by flat granular fragments, which interlaced in space to form aerial and inlaid pores, with obvious pore development, and most of them show banded fractures. Extremely irregular shape and poor connectivity. Under the action of large overburden load, the soil structure element presents a certain directional arrangement. (5) the meso-structure parameters of each unit are extracted from the SEM binary image by using IPP software, and the variation law of the meso-structure under the influence of three elements is analyzed. Combined with the dynamic characteristics of Beihai marine soft soil, the evolution law of soil meso-structure before and after cyclic loading is studied, and the evolution process of meso-structure is summarized: structure fine-tuning, structural stress concentration and overall structural instability. It corresponds to three stages of macroscopic deformation: elastic deformation, stress yield and plastic deformation. The relationship between pore structure characteristic parameter and macroscopic characteristic parameter is established, and the influence mechanism of each factor on soil dynamic characteristic is analyzed from the viewpoint of meso.
【學(xué)位授予單位】:廣西大學(xué)
【學(xué)位級別】:碩士
【學(xué)位授予年份】:2017
【分類號】:TU447
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