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Study on Consolidation Behaviors of Peaty Soils Using a Viscoelastic Rheological-Consolidation Model in Kunming, China

机译:基于粘弹性流变-固结模型的泥炭土固结特性研究

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Due to the presence of organic matters, peaty soils have a highly compressible nature, and the consolidation process is complicated by the occurrence of rheological deformation. This paper presents the behaviors of the peaty soils sampled from the city of Kunming, the capital of Yunnan province in southwestern China. A series of one-dimensional compression tests are carried out on the peaty soil specimens with different organic matter contents. Considering the rheological properties of peaty soils, the three-element viscoelastic rheological model is introduced into the consolidation equation, then the analytical solution is derived for the viscoelastic rheological-consolidation model. Finally, the influences of consolidation pressures and organic matter contents on the model parameters determined by test data fitting are investigated. It has been shown that the model is coinciding fairly well with test results, and the consolidation pressure and organic matter content have a remarkable effect on the model parameters.
机译:由于存在有机物,所以豌豆土具有高度可压缩的性质,并且流变变形的发生使固结过程变得复杂。本文介绍了从中国西南部云南省省会昆明市采样的豌豆土壤的行为。对不同有机质含量的豌豆土壤标本进行了一系列的一维压缩试验。考虑到粉土的流变特性,将三元粘弹性流变模型引入固结方程,然后导出粘弹性流变固结模型的解析解。最后,研究了固结压力和有机质含量对试验数据拟合确定的模型参数的影响。结果表明,该模型与试验结果吻合得很好,固结压力和有机物含量对模型参数有显着影响。

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