水-岩作用对储层渗透性影响的数值模拟研究——以鄂尔多斯盆地东北部上古生界砂岩储层为例
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摘要
油气储层的质量及演化往往受沉积作用和成岩作用的共同制约,成岩作用是影响储层孔渗最直接的因素,水-岩反应贯穿于整个成岩作用阶段,决定了孔渗的演化过程。本次研究以鄂尔多斯盆地东北部上古生界陆源碎屑岩储层下石盒子组—山西组为对象,运用多相流反应溶质运移数值模拟的方法,定量研究水-岩化学作用对含油气盆地储层渗透性能的影响,再现水-岩反应所造成的储层矿物溶解、沉淀以及储层渗透性的变化。结果表明:在成岩作用初期,矿物溶解过程占主导地位,模型运行50 Ma时,储层孔隙度由初始的0.30增至0.36,渗透率由初始的5.00×10_-15 m_2增至8.70×10_-15 m_2;在油气充注阶段(气体CO~2为主),整个成岩作用矿物的沉淀量大于矿物的溶解量,导致固相体积增加,模型运行20 Ma时,储层孔隙度由0.20降低至约0.15,渗透率由5.00×10_-13 m_2下降至约2.00×10_-13 m_2。
The quality and evolution of oil and gas reservoirs are often controlled by sedimentation and diagenesis.Diagenesis is the most direct factor affecting porosity and permeability of reservoirs.The evolution of porosity and permeability is determined by water-rock reaction throughout the whole process of diagenesis.The clastic rock reservoir of Lower Shihezi-Shanxi Group in the northeast Ordos basin was taken as the study object.Reactive transport modeling was used to carry out the quantitative research on the effects of water-rock interaction on the permeable properties of the reservoir in oil,gas bearing basin and on the changes of reservoir permeability and reservoir mineral dissolution,precipitation.The results show that in the early stage of diagenesis,mineral dissolution was dominant,which increased porosity of reservoir from 0.30 to 0.36 and permeability of reservoir from 5.00×10-15 m2 to 8.70×10-15 m2 respectively.During the oil and gas filling stage(mainly CO2),the precipitation of mineral was dominant in the whole geochemical reaction,resulting in the decrement of porosity(from 0.20 to 0.15)and permeability(from 5.00×10-13 m2 to 2.00×10-13 m2).
The quality and evolution of oil and gas reservoirs are often controlled by sedimentation and diagenesis.Diagenesis is the most direct factor affecting porosity and permeability of reservoirs.The evolution of porosity and permeability is determined by water-rock reaction throughout the whole process of diagenesis.The clastic rock reservoir of Lower Shihezi-Shanxi Group in the northeast Ordos basin was taken as the study object.Reactive transport modeling was used to carry out the quantitative research on the effects of water-rock interaction on the permeable properties of the reservoir in oil,gas bearing basin and on the changes of reservoir permeability and reservoir mineral dissolution,precipitation.The results show that in the early stage of diagenesis,mineral dissolution was dominant,which increased porosity of reservoir from 0.30 to 0.36 and permeability of reservoir from 5.00×10-15 m2 to 8.70×10-15 m2 respectively.During the oil and gas filling stage(mainly CO2),the precipitation of mineral was dominant in the whole geochemical reaction,resulting in the decrement of porosity(from 0.20 to 0.15)and permeability(from 5.00×10-13 m2 to 2.00×10-13 m2).
引文
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[9]Alhelal A B,Whitaker F,Xiao Y.Controls from Formation of Early Replacement Dolomites and Diagenetic Anhydrite:Reactive Transport Modeling of Dynamic Interactions Between Geothermal and Reflux Circulation[J].Drugs,2011,58(1):39-50.
[10]Xiao Y,Jones G D,Whitaker F F,et al.Fundamental Approaches to Dolomitisation and Carbonate Diagenesis in Different Hydrogeological Systems and the Impact on Reservoir Quality Distribution[C]//International Petroleum Technology Conference.Beijing:[s.n.],2013:16579-MS.
[11]Gabellone T,Whitaker F,Katz D,et al.Controls on Reflux Dolomitisation of Epeiric-Scale Ramps:Insights from Reactive Transport Simulations of the Mississippian Madison Formation(Montana and Wyoming)[J].Sedimentary Geology,2016,345:85-102.
[12]Xu T,Spycher N,Sonnenthal E L,et al.TOUGHREACT Version 2.0:A Simulator for Subsurface Reactive Transport Under Non-Isothermal Multiphase Flow Conditions[J].Computers and Geosciences,2011,37(6):763-774.
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[14]刘俊吉,周亚平,李松林.物理化学[M].北京:高等教育出版社,2009:529-530.Liu Junji,Zhou Yaping,Li Songlin.Physical Chemistry[M].Beijing:Higher Education Press,2009:529-530.
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[16]闵琪,付金华,席胜利,等.鄂尔多斯盆地上古生界天然气运移聚集特征[J].石油勘探与开发,2000,27(4):26-29.Min Qi,Fu Jinhua,Xi Shengli,et al.Characteristics of Natural Gas Migration and Accumulation in the Upper Paleozoic of Ordos Basin[J].Petroleum Exploration and Development,2000,27(4):26-29.
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[18]付金华.鄂尔多斯盆地上古生界天然气成藏条件及富集规律[D].西安:西北大学,2004.Fu Jinhua.The Gas Reservoir-Forming Conditions and Accumulation Rules of Upper Paleozoic Ordos Basin[D].Xi’an:Northwestern University,2004.
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[20]杨华,杨奕华,石小虎,等.鄂尔多斯盆地周缘晚古生代火山活动对盆内砂岩储层的影响[J].沉积学报,2007,25(4):526-534.Yang Hua,Yang Yihua,Shi Xiaohu,et al.Influence of the Late Paleozoic Volcanic Activity on the Sandstone Reservoir in the Interior of Ordos Basin[J].Acta Sedimentologica Sinica,2007,25(4):526-534.
[21]高胜利,任战利.鄂尔多斯盆地剥蚀厚度恢复及其对上古生界烃源岩热演化程度的影响[J].石油与天然气地质,2006,27(2):180-186.Gao Shengli,Ren Zhanli.Restoration of Eroded Thickness and Its Influence on Thermal Evolution of Upper Paleozoic Source Rocks in Ordos Basin[J].Oil&Gas Geology,2006,27(2):180-186.
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