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Analysis of Adsorption Characteristics and Influencing Factors of Wufeng-Longmaxi Formation Shale in Sichuan Basin

机译:四川盆地武丰 - 龙丸地板页岩的吸附特性及影响因素分析

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摘要

Shale gas resources provide a new impetus to alleviate the contradiction between China’s oil and gas supply and demand. As an important part of shale gas, understanding the occurrence mechanism of adsorbed gas can help shale gas resources to be better developed and used. This time, a series of experiments, such as low-temperature nitrogen adsorption and methane isotherm adsorption, were conducted to discuss the pore structure, adsorption performance, and adsorption mechanism of shale. The results show the following: (1) Shale pores are dominated by nanopores, and pores with a pore width of less than 2 nm have the best relationship with the shale surface area and adsorption capacity. (2) Total organic carbon (TOC) plays an important role in controlling the specific surface area and methane adsorption capacity of shale. This is mainly due to the large number of micropores (pore size of 2 nm) developed in organic matter. Micropores provide the main specific surface area and adsorption sites for methane adsorption. (3) A variety of models were used to fit shale methane isotherm adsorption data. The results show that the SDR model and Langmuir model have the best fit. The methane adsorption performance of shale is controlled by many factors; the adsorption capacity becomes weaker as the temperature rises; and this influence is also affected by TOC. (4) In comparison to the adsorption capacity, the change of the adsorbed phase density is more complicated: overall, there is a weak positive correlation with TOC; as the temperature increases, the adsorbed phase density decreases. However, this law is not stable, and there are different performances in different experiments. (5) The adsorption comparison results show that the shale methane adsorption is mainly multilayer adsorption and micropore filling.
机译:页岩气资源提供了一种缓解中国石油和燃气供需矛盾的新推动力。作为页岩气的重要组成部分,了解吸附气体的发生机制可以帮助页岩气资源更好地发展和使用。这次是一系列实验,例如低温氮吸附和甲烷等温吸附,以探讨页岩的孔结构,吸附性能和吸附机制。结果表明以下:(1)页岩孔隙由纳米孔主导,孔径小于2nm的孔与页岩表面积和吸附容量具有最佳关系。 (2)总有机碳(TOC)在控制页岩的比表面积和甲烷吸附能力方面发挥着重要作用。这主要是由于有机物质中产生的大量微孔(孔尺寸的孔尺寸)。微孔提供了甲烷吸附的主要比表面积和吸附部位。 (3)各种模型用于配合页岩甲烷等温物吸附数据。结果表明,SDR模型和Langmuir模型具有最佳合适。页岩的甲烷吸附性能受到许多因素的控制;随着温度升高,吸附能力变弱;这种影响也受到TOC的影响。 (4)与吸附能力相比,吸附相密度的变化更复杂:总体而言,与TOC有弱阳性相关性;随着温度升高,吸附相密度降低。然而,这种法律不稳定,不同实验中存在不同的性能。 (5)吸附比较结果表明,页岩甲烷吸附主要是多层吸附和微孔填充。

著录项

  • 来源
    《Energy & fuels》 |2021年第6期|4925-4942|共18页
  • 作者单位

    CNOOC Research Institute Company Limited;

    School of Geosciences China University of Petroleum (East China);

    School of Geosciences China University of Petroleum (East China);

    CNOOC Research Institute Company Limited;

    Bohai Oilfield Research Institute Tianjin Branch of CNOOC Limited;

    Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education School of Earth Resources China University of Geosciences;

  • 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
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