T14 Unconventional Energy Resources: Advances and Evolution in Tight Reservoir Assessment and Production
Sunday, 22 October 2017
8:00 AM - 12:00 PM
Room 3B
EFFECT OF PORE STRUCTURE AND COMPOSITION ON GAS SORPTION CAPACITY OF TRANSITIONAL SHALES, NW CHINA
Paper number: T14-3
Program: Technical Sessions
Time: 8:30 AM – 8:45 AM
Authors
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Mohammad Amin AmooieCollege of Arts and Sciences, COLUMBUS, OH
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Mohamad Reza SoltanianUniversity of Cincinnati, Cincinnati, OH
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Zhenxue JiangChina University of Petroleum-Beijing, Beijing
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Joachim MoortgatCollege of Arts and Sciences, COLUMBUS, OH
Abstract
The results show that total organic carbon (TOC) content ranges 0.781-3.82 wt%. Shanxi shale comprises of type III OM and is at over-mature stage. The dominant composition is Clay minerals, averaging 54.6%, and the second is quartz with an average of 39.7%. Feldspar, plagioclase, siderite and pyrite can be observed. The prevailing pore type is silt-shaped, with a smaller amount of ink-bottle-shaped pores, as observed by N2 adsorption-desorption hysteresis loops. TOC is not the only controlling factor, and clay minerals also contributed to the specific surface area for gas sorption. The relationship between quartz and soft composite (clays and OM) is also observed to impact the gas sorption capacity. In addition, the Langmuir, supercritical Dubinin-Radushkevich (SDR) and Ono-Kondo (OK) model were employed and compared to derive Langmuir volume. The fitting performance demonstrates that the Langmuir model is applicable for shales with measured maxima of excess sorption capacity (MESC) less than 2.36 m3/t, while the SDR model better fits the data for shales with MESC larger than 2.89 m3/t.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-299178
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