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Experimental Study of the NMR Characteristics of Shale Reservoir Rock

  • SUN Junchang;CHEN Jingping;YANG Zhengming;LIU Xuewei;LIU Yuanjun
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  • 1. Institute of Porous Flow and Fluid Mechanics, Chinese Academy of Sciences, Langfang 065007, Hebei Province, China;2. The First Operation Department, The Second Mud Logging Branch, CNPC Bohai Drilling Engineering Company Limited, Langfang 065007, Hebei Province, China;3. Langfang Branch, Research Institute of Petroleum Exploration and Development of CNPC, Langfang 065007, Hebei Province, China;4. Engineering & Technology College, Yangtze University Jingzhou 434023, Hubei Province, China

Received date: 2011-04-03

  Revised date: 2011-05-07

  Online published: 2012-05-18

Abstract

It is very important to systematically study the NMR characteristics of the shale core sample before the NMR logging technology can be used in the development of the shale gas reservoir. This paper studies the NMR characteristics, the NMR porosity, the movable fluid T2cutoff and other NMR properties of the shale rock sample. The experimental results demonstrate that the shale T2 spectrum can be divided into three types, the single peak T2 spectrum, the two peak T2 spectrum containing one isolated right peak and the two peak T2 spectrum containing continuous left and right peaks. The T2 relaxation of the shale is mostly less than 10ms. The fracture porosity is only about 9.16% of the total pore space. The surface area per unit volume of the shale gas reservoir ranges mainly from 3.59 to 80.51μm-1. The shale NMR porosity is generally less than its conventional porosity. The average error is about 22.33%. The movable fluid T2cutoff value is in the range from 3.87 to 16.68ms and its average value is 8.29ms. The free gas saturation of the shale gas reservoir obtained from the centrifugal experiment is about 9.72%.

Cite this article

SUN Junchang;CHEN Jingping;YANG Zhengming;LIU Xuewei;LIU Yuanjun . Experimental Study of the NMR Characteristics of Shale Reservoir Rock[J]. Science & Technology Review, 2012 , 30(14) : 25 -30 . DOI: 10.3981/j.issn.1000-7857.2012.14.002

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