含二氧化碳水合物沉积物的时间特性及弹粘塑性本构模型的应用

Hiromasa Iwai, Y. Konishi, S. Kimoto
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引用次数: 2

摘要

人们已经认识到,由于天然气水合物的粘塑性,含天然气水合物的沉积物明显表现出时间依赖性,如长期固结、应变速率依赖性和蠕变变形。本研究的主要目的是通过一系列的实验来了解含气水合物沉积物的时间依赖行为,并建立一个可以描述含气水合物土壤时间依赖行为的本构方程。首先,对含co2合成水合土进行了一系列应变速率阶变的不排水三轴压缩试验,研究了含co2合成水合土的应变速率依赖性。其次,根据实验结果建立了弹粘塑性本构方程。将该模型应用于实验结果,发现该模型能较好地再现含co2水合物试件的力学行为。主要研究结果如下:①含co2水合物的砂样与不含co2水合物的砂样均存在独特的应力-应变-应变速率关系,即等压关系;此外,含CO 2水合物的试样具有明显的应变速率依赖性,且随水合物饱和度的增加而增大。其次,从实验结果来看,在应变速率较慢的情况下,水合物饱和度对强度和刚度都没有依赖性。这是因为含cdh沉积物的强度可能取决于水合物的硬化效应和粘塑性的平衡。在应变速率较慢的情况下,粘塑性对含cdh砂力学行为的影响大于硬化效应。通过引入效应,所建立的本构模型能较好地表达含co2水合物试件的力学响应
本文章由计算机程序翻译,如有差异,请以英文原文为准。
TIME-DEPENDENT BEHAVIOR OF CO2-HYDRATE-BEARING SEDIMENTS AND APPLICATION OF ELASTO-VISCOPLASTIC CONSTITUTIVE MODEL
It has been recognized that gas hydrate-bearing sediments clearly exhibit time-dependent behavior such as long-term consolidation, strain rate dependency, and creep deformation due to its viscoplasticity of gas hydrates. The main objective of the present study is to understand the time-dependent behavior of gas-hydrate-bearing sediments by a series of experiment and to establish a constitutive equation that can de-scribe the time-dependent behavior of gas-hydrate-bearing soils. First, a series of undrained triaxial compression tests with step-changed strain rate is conducted on synthetic CO 2 -hydrate-bearing sand specimens in order to investigate the strain rate dependency of the hydrate-bearing soils. Second, the elasto-viscoplastic constitutive equation has been developed based on the obtained experimental results. The proposed model is then applied to the experimental results to find that the model can reproduce the mechanical behavior of the CO 2 -hydrate-bearing specimens. The main findings obtained from the present study are as follows: First, the unique stress-strain-strain rate relations, namely, Isotaches, is observed for both the CO 2 -hydrate-bearing sand specimens and the sand sample without hydrates. In addition, the CO 2 -hydrate-bearing specimens clearly show the strain rate dependency, and it increases with increase in the hydrate saturation. Second, from the experimental results, it is found that dependency of hydrate saturation on both the strength and the stiffness does not appear in the case where the strain rate is quite slow. This is because the strength of the CDH-bearing sediments may be determined by the balance of the hardening effect and viscoplasticity of the hydrates. In the case of the slow strain rate, the viscoplasticity is more dominant on the mechanical behavior of the CDH-bearing sand than the hardening effect. The proposed constitutive model can well express those mechanical responses of the CO 2 -hydrate-bearing specimens by introducing the effect
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