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A unified theory for sharp dissolution front propagation inchemical dissolution of fluid-saturated porous rocks
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  • 英文篇名:A unified theory for sharp dissolution front propagation inchemical dissolution of fluid-saturated porous rocks
  • 作者:ZHAO ; ChongBin ; HOBBS ; Bruce ; ORD ; Alison
  • 英文作者:ZHAO ChongBin;HOBBS Bruce;ORD Alison;Computational Geosciences Research Centre, Central South University;School of Earth and Environment, The University of Western Australia;
  • 英文关键词:sharp dissolution front;;stationary/steady state;;transient state;;acid dissolution capacity;;acidization dissolution;;porous rocks
  • 中文刊名:JEXG
  • 英文刊名:中国科学:技术科学(英文版)
  • 机构:Computational Geosciences Research Centre, Central South University;School of Earth and Environment, The University of Western Australia;
  • 出版日期:2019-01-01
  • 出版单位:Science China(Technological Sciences)
  • 年:2019
  • 期:v.62
  • 基金:supported by the National Natural Science Foundation of China(Grant No.11272359)
  • 语种:英文;
  • 页:JEXG201901016
  • 页数:12
  • CN:01
  • ISSN:11-5845/TH
  • 分类号:167-178
摘要
This paper presents a unified theory to deal with when, why and how a sharp acidization dissolution front(ADF), which is represented by the porosity distribution curve, can take place in an acidization dissolution system composed of fluid-saturated porous rocks. The theory contains the following main points:(1) A reaction rate of infinity alone can lead to a sharp ADF of the Stefan-type in the acidization dissolution system. This sharp front is unstable when permeability in the downstream region is smaller than that in the upstream region.(2) For a finite reaction rate, when the acid dissolution capacity number approaches zero,the ADF can have a sharp profile of the Stefan-type either on a much smaller time scale or on a much larger time scale than the dissolution time scale. In the former case, the ADF may become unstable on a much larger time scale than the transport time scale, while in the latter case, it may become unstable if the growth rate of a small perturbation is greater than zero.(3) On the dissolution time scale, even if both the reaction rate is finite and the acid dissolution capacity number approaches zero, the profile of an ADF may not be sharp because it is in a transient state. In this case, not only can an ADF change its profile with time, but also its morphology can grow if the growth rate of a small perturbation is greater than zero. Due to the involvement of both the change rate and the growth rate of the ADF profile, it is necessary to conduct a transient linear stability analysis for determining whether or not a time-dependent ADF is stable in the acidization dissolution system.
        This paper presents a unified theory to deal with when, why and how a sharp acidization dissolution front(ADF), which is represented by the porosity distribution curve, can take place in an acidization dissolution system composed of fluid-saturated porous rocks. The theory contains the following main points:(1) A reaction rate of infinity alone can lead to a sharp ADF of the Stefan-type in the acidization dissolution system. This sharp front is unstable when permeability in the downstream region is smaller than that in the upstream region.(2) For a finite reaction rate, when the acid dissolution capacity number approaches zero,the ADF can have a sharp profile of the Stefan-type either on a much smaller time scale or on a much larger time scale than the dissolution time scale. In the former case, the ADF may become unstable on a much larger time scale than the transport time scale, while in the latter case, it may become unstable if the growth rate of a small perturbation is greater than zero.(3) On the dissolution time scale, even if both the reaction rate is finite and the acid dissolution capacity number approaches zero, the profile of an ADF may not be sharp because it is in a transient state. In this case, not only can an ADF change its profile with time, but also its morphology can grow if the growth rate of a small perturbation is greater than zero. Due to the involvement of both the change rate and the growth rate of the ADF profile, it is necessary to conduct a transient linear stability analysis for determining whether or not a time-dependent ADF is stable in the acidization dissolution system.
引文
1 Gow P A,Upton P,Zhao C,et al.Copper-gold mineralisation in New Guinea:Numerical modelling of collision,fluid flow and intrusionrelated hydrothermal systems.Aust J Earth Sci,2002,49:753-771
    2 Schaubs P M,Zhao C.Numerical models of gold-deposit formation in the Bendigo-Ballarat Zone,Victoria.Aust J Earth Sci,2002,49:1077-1096
    3 Sorjonen-Ward P,Zhang Y,Zhao C.Numerical modelling of orogenic processes and gold mineralisation in the southeastern part of the Yilgarn Craton,Western Australia.Aust J Earth Sci,2002,49:935-964
    4 Ju M,Zhao C,Dai T,et al.Finite element modeling of pore-fluid flow in the Dachang ore district,Guangxi,China:Implications for hydrothermal mineralization.Geosci Front,2011,2:463-474
    5 Liu Y,Dai T.Numerical modeling of pore-fluid flow and heat transfer in the Fushan iron ore district,Hebei,China:Implications for hydrothermal mineralization.J Geochem Explor,2014,144:115-127
    6 Chadam J,Hoff D,Merino E,et al.Reactive infiltration instabilities.IMA J Appl Math,1986,36:207-221
    7 Chadam J,Ortoleva P,Sen A.A weakly nonlinear stability analysis of the reactive infiltration interface.IAM J Appl Math,1988,48:1362-1378
    8 Ormond A,Ortoleva P.Numerical modeling of reaction-induced cavities in a porous rock.J Geophys Res,2000,105:16737-16747
    9 Ortoleva P,Chadam J,Merino E,et al.Geochemical self-organization II:The reactive-infiltration instability.Am J Sci,1987,287:1008-1040
    10 Chen J S,Liu C W.Numerical simulation of the evolution of aquifer porosity and species concentrations during reactive transport.Comput Geosci,2002,28:485-499
    11 Chen J S,Liu C W.Interaction of reactive fronts during transport in a homogeneous porous medium with initial small non-uniformity.JContam Hydrol,2004,72:47-66
    12 Zhao C,Hobbs B E,Hornby P,et al.Theoretical and numerical analyses of chemical-dissolution front instability in fluid-saturated porous rocks.Int J Numer Anal Meth Geomech,2008,32:1107-1130
    13 Chen J S,Liu C W,Lai G X,et al.Effects of mechanical dispersion on the morphological evolution of a chemical dissolution front in a fluidsaturated porous medium.J Hydrol,2009,373:96-102
    14 Zhao C,Hobbs B E,Ord A,et al.Effects of mineral dissolution ratios on chemical-dissolution front instability in fluid-saturated porous media.Transp Porous Media,2010,82:317-335
    15 Sherwood J D.Stability of a plane reaction front in a porous medium.Chem Eng Sci,1987,42:1823-1829
    16 Hinch E J,Bhatt B S.Stability of an acid front moving through porous rock.J Fluid Mech,1990,212:279-288
    17 Fredd C N,Fogler H S.Influence of transport and reaction on wormhole formation in porous media.Aiche J,1998,44:1933-1949
    18 Golfier F,Zarcone C,Bazin B,et al.On the ability of a Darcy-scale model to capture wormhole formation during the dissolution of a porous medium.J Fluid Mech,2002,457:213-254
    19 Panga M K R,Ziauddin M,Balakotaiah V.Two-scale continuum model for simulation of wormholes in carbonate acidization.Aiche J,2005,51:3231-3248
    20 Kalia N,Balakotaiah V.Modeling and analysis of wormhole formation in reactive dissolution of carbonate rocks.Chem Eng Sci,2007,62:919-928
    21 Kalia N,Balakotaiah V.Effect of medium heterogeneities on reactive dissolution of carbonates.Chem Eng Sci,2009,64:376-390
    22 Cohen C E,Ding D,Quintard M,et al.From pore scale to wellbore scale:Impact of geometry on wormhole growth in carbonate acidization.Chem Eng Sci,2008,63:3088-3099
    23 Zhao C,Hobbs B E,Ord A.Theoretical analyses of acidization dissolution front instability in fluid-saturated carbonate rocks.Int J Numer Anal Meth Geomech,2013,37:2084-2105
    24 Wangen M.Stability of reaction-fronts in porous media.Appl Math Model,2013,37:4860-4873
    25 Szymczak P,Ladd A J C.Reactive-infiltration instabilities in rocks.Part 2.Dissolution of a porous matrix.J Fluid Mech,2014,738:591-630
    26 Zhao C B,Hobbs B,Ord A.A new alternative approach for investigating acidization dissolution front propagation in fluid-saturated carbonate rocks.Sci China Tech Sci,2017,60:1197-1210
    27 Zhao C,Hobbs B E,Ord A.Theoretical analyses of the effects of solute dispersion on chemical-dissolution front instability in fluidsaturated porous media.Transp Porous Media,2010,84:629-653
    28 Carman P C.Flow of Gases Through Porous Media.New York:Academic Press,1956
    29 Ortoleva P,Merino E,Moore C,et al.Geochemical self-organization I:Reaction-transport feedbacks and modeling approach.Am J Sci,1987,287:979-1007
    30 Lai K H,Chen J S,Liu C W,et al.Effect of permeability-porosity functions on simulated morphological evolution of a chemical dissolution front.Hydrol Process,2014,28:16-24
    31 Lai K H,Chen J S,Liu C W,et al.Effect of medium permeability anisotropy on the morphological evolution of two non-uniformities in a geochemical dissolution system.J Hydrol,2016,533:224-233

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