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Ono-Kondo Model for Supercritical Shale Gas Storage: A Case Study of Silurian Longmaxi Shale in Southeast Chongqing, China

机译:页岩超临界储气的Ono-Kondo模型:以重庆东南志留系龙马溪组页岩为例

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摘要

Shale gas storage is a dominant factor to economically evaluate the shale play. A series of Lower Silurian Longmaxi marine shale samples in southeast Chongqing, China, were collected to investigate the reservoir characteristics, and a suit of methane adsorption isotherms were fitted using a supercritical Ono-Kondo model to better understand the adsorption capacity of Longmaxi shale. The saturated adsorption of a monolayer presents a greatly positive relationship with the total organic carbon (TOC) content. A negative relationship with clay was observed due to the predominant influence of organic matter on the methane adsorption. Methane adsorption also increases with increasing pressure and decreases with increasing temperature. On the basis of the relationships, one new estimation algorithm related to TOC content, pressure, and temperature was established to calculate the methane adsorption capacity on the basis of the Ono-Kondo model. Furthermore, with higher TOC content, the adsorption capacity of shales correspondingly increases and the maximum of the adsorption capacity tends to a deeper depth. Considering geological characteristics of Longmaxi shale, one new gas-in-place (GIP) model was proposed to apply, considering the controlling factors, TOC, porosity, gas saturation, pressure, and temperature. The relationships of GIP, adsorbed gas, and free gas with increasing depth shows that (1) free gas increases rapidly and equally; (2) adsorbed gas initially increases rapidly at less than 1000 m, and then decreases with depth increases; and (3) GIP rapidly increases at shallow depths, and then gently increases more than 1000 m.
机译:页岩气储量是从经济角度评估页岩游隙的主要因素。收集了中国重庆东南部一系列志留系龙马溪组海相页岩样品,以研究储层特征,并使用超临界Ono-Kondo模型拟合了一套甲烷吸附等温线,以更好地了解龙马溪组页岩的吸附能力。单层的饱和吸附与总有机碳(TOC)含量呈极大的正相关。由于有机物对甲烷吸附的主要影响,因此观察到与粘土的负相关关系。甲烷吸附也随压力增加而增加,而随温度增加而减少。基于这些关系,建立了一种与TOC含量,压力和温度相关的新估算算法,以Ono-Kondo模型为基础来计算甲烷的吸附量。此外,随着TOC含量的增加,页岩的吸附容量相应地增加,并且吸附容量的最大值趋于更深的深度。考虑到龙马溪组页岩的地质特征,考虑控制因素,总有机碳,孔隙度,气体饱和度,压力和温度,提出了一种新的GIP模型。随着深度的增加,GIP,吸附气体和游离气体之间的关系表明:(1)游离气体迅速而均匀地增加; (2)吸附气体在1000m以下开始迅速增加,然后随深度增加而减少; (3)GIP在浅深度迅速增加,然后逐渐增加超过1000 m。

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  • 来源
    《Energy & fuels》 |2017年第3期|2755-2764|共10页
  • 作者单位

    PetroChina, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China;

    China Univ Petr, Unconvent Gas Res Inst, Fuxue Rd 18, Beijing, Peoples R China;

    PetroChina, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China;

    Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA;

    PetroChina, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China;

    China Univ Petr, Unconvent Gas Res Inst, Fuxue Rd 18, Beijing, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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