Research on the New Method of Determining Subsurface Porosity of Unconsolidated Cores

G. Ping, Yuan Zhiwang, Wang Zhouhua, Y. Yiyi
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Abstract

Abstract In this paper, we have derived the transformational relationship between the porosity under triaxial, biaxial stress and uniaxial stress respectively. Moreover, porosity tests under biaxial and triaxial stress for 11 groups of parallel unconsolidated core samples are conducted. Based on the transformational relationship, we have converted the tested porosity under triaxial stress into the porosity under biaxial stress and then compared it with the tested porosity under biaxial stress. The results indicate that the theoretical porosity model is reliable and deformation of unconsolidated cores is approximate elastic deformation of the rock body. Therefore, the porosity under uniaxial stress can be converted from the porosity under biaxial stress, which can simplify the experimental procedure and equipment, and provide a new way of determining subsurface porosity of unconsolidated cores. Besides, the Poisson’s ratio of unconsolidated cores is much larger than that of the normal clastic rock, and the actual conversion factor should be used for the conversion.
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测定松散岩心地下孔隙度新方法研究
摘要本文分别推导了三轴、双轴和单轴应力作用下孔隙度的转换关系。并对11组平行松散岩心进行了双轴和三轴应力下的孔隙度测试。根据转换关系,将三轴应力下的孔隙度测试值转换为双轴应力下的孔隙度测试值,并与双轴应力下的孔隙度测试值进行对比。结果表明,理论孔隙度模型是可靠的,松散岩心的变形近似于岩体的弹性变形。因此,单轴应力作用下的孔隙度可以由双轴应力作用下的孔隙度转换而来,简化了实验程序和设备,为确定松散岩心的地下孔隙度提供了一种新的方法。另外,松散岩心的泊松比远大于正常碎屑岩的泊松比,应采用实际换算系数进行换算。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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