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Reactivity of dolomite in water-saturated supercritical carbon dioxide:Significance for carbon capture and storage and for enhanced oil and gas recovery

机译:白云石在水饱和超临界二氧化碳中的反应性:对于碳捕获和储存以及提高油气采收率的意义

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摘要

Carbon dioxide injection in porous reservoirs is the basis for carbon capture and storage, enhanced oil and gas recovery. Injected carbon dioxide is stored at multiple scales in porous media, from the pore-level as a residual phase to large scales as macroscopic accumulations by the injection site, under the caprock and at reservoir internal capillary pressure barriers. These carbon dioxide saturation zones create regions across which the full spectrum of mutual CO_2-H_2O solubility may occur. Most studies assume that geo-chemical reaction is restricted to rocks and carbon dioxide-saturated formation waters, but this paradigm ignores injection of anhydrous carbon dioxide against brine and water-alternating-gas flooding for enhanced oil recovery. A series of laboratory experiments was performed to evaluate the reactivity of the common reservoir mineral dolomite with water-saturated supercritical carbon dioxide. Experiments were conducted at reservoir conditions (55 and 110 ℃, 25 MPa) and elevated temperature (220 ℃, 25 MPa) for approximately 96 and 164 h (4 and 7 days). Dolomite dissolves and new carbonate mineral precipitates by reaction with water-saturated supercritical carbon dioxide. Dolomite does not react with anhydrous supercritical carbon dioxide. Temperature and reaction time control the composition, morphology, and extent of formation of new carbonate minerals. Mineral dissolution and re-precipitation due to reaction with water-saturated carbon dioxide may affect the contact line between phases, the carbon dioxide contact angle, and the relative permeability and permeability distribution of the reservoir. These changes influence fundamental properties of hysteresis of drainage and imbibition cycles, rock wettability, and capillary pressure. The efficacy of physical carbon dioxide trapping mechanisms, integrity of caprock, and injectivity of a carbon dioxide storage reservoir as well as the injectivity and production rate of an enhanced oil recovery operation may be affected.
机译:在多孔储层中注入二氧化碳是碳捕获和储存,提高油气采收率的基础。所注入的二氧化碳以多种尺度存储在多孔介质中,从孔隙水平作为残留相,到大规模地作为宏观的堆积(通过注入部位)存储在盖层下和储层内部毛细管压力屏障下。这些二氧化碳饱和区创建了一个区域,在该区域中可能会发生相互之间的完整CO_2-H_2O溶解度谱。大多数研究假设地球化学反应仅限于岩石和二氧化碳饱和的地层水,但是该范例忽略了向盐水注入无水二氧化碳和水替代气驱以提高采收率。进行了一系列实验室实验,以评估普通储层矿物白云石与水饱和超临界二氧化碳的反应性。在储层条件(55和110℃,25 MPa)和高温(220℃,25 MPa)下进行了约96和164 h(4和7天)的实验。白云石溶解,新的碳酸盐矿物与水饱和的超临界二氧化碳反应而沉淀。白云石不会与无水超临界二氧化碳反应。温度和反应时间控制着新的碳酸盐矿物的组成,形态和形成程度。与水饱和的二氧化碳反应而导致的矿物溶解和再沉淀可能会影响相之间的接触线,二氧化碳接触角以及储层的相对渗透率和渗透率分布。这些变化影响排水和吸水循环的滞后,岩石的润湿性和毛细压力的基本特性。可能会影响物理二氧化碳捕集机制的有效性,盖层的完整性以及二氧化碳存储油藏的注入能力,以及提高采油率的注入能力和生产率。

著录项

  • 来源
    《Energy Conversion & Management》 |2013年第1期|564-573|共10页
  • 作者单位

    Department of Geology and Geophysics, 1000 E. University Avenue, University of Wyoming, Laramie, WY 82071, USA,Petroleum Engineering Department, China University of Petro-leum-Beijing, 18 Fuxue Rd., Changping District, Beijing 102249, China;

    Department of Chemical and Petroleum Engineering, 1000 E. University Avenue, University of Wyoming, Laramie, WY 82071, USA;

    Department of Geology and Geophysics, 1000 E. University Avenue, University of Wyoming, Laramie, WY 82071, USA;

    Department of Geology and Geophysics, 1000 E. University Avenue, University of Wyoming, Laramie, WY 82071, USA,School of Energy Resources, 1000 E. University Avenue, University of Wyoming, Laramie, WY 82071, USA,Department of Geology and Geophysics, 1000 E.University Avenue, University of Wyoming, Laramie, WY 82071, USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    carbon capture and storage; enhanced oil recovery; enhanced gas recovery; fluid-rock interactions; supercritical carbon dioxide; mineralization;

    机译:碳捕集与封存;提高采油率;提高气体回收率;流体-岩石相互作用超临界二氧化碳矿化;

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