Huang Chenggang, Yuan Jianying, Cao Zhenglin, Zhang Shiming, Wang Ying, She Min, Mi Haijie. Simulation experiment for ankerite dissolution in clastic reservoir of saline lacustrine basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(5): 650-655. doi: 10.11781/sysydz201405650
Citation: Huang Chenggang, Yuan Jianying, Cao Zhenglin, Zhang Shiming, Wang Ying, She Min, Mi Haijie. Simulation experiment for ankerite dissolution in clastic reservoir of saline lacustrine basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(5): 650-655. doi: 10.11781/sysydz201405650

Simulation experiment for ankerite dissolution in clastic reservoir of saline lacustrine basin

doi: 10.11781/sysydz201405650
  • Received Date: 2013-08-10
  • Rev Recd Date: 2014-07-03
  • Publish Date: 2014-09-28
  • It is generally believed that carbonate minerals can easily dissolve. This process will lead to the formation of secondary pores, thereby enlarging the reservoir space and improving the permeability of reservoir rocks. In the Qaidam Basin, clastic reservoirs of the Lower Eocene Gancaigou Formation are deposits of saline lacustrine basin, with plaster and ankerite well developed in rock flacks as revealed by polarized light microscopy and scanning electron microscope. Experimental results of fluid-rock dynamic stimulation show that the ankerite dissolution can generate secondary pores, and gypsum catalyzes the dissolution. The iron and magnesium ions generated are reactants in the transformation from koalinite to chlorite. The foliated chlorite easily blocks thin throat, leading to the decrease of permeability, while the dissolution of easily soluble minerals like ankerite increases porosity.

     

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  • [1]
    沈照理,王焰新.水—岩相互作用研究的回顾与展望[J].地球科学:中国地质大学学报,2002,27(2):127-133. Shen Zhaoli,Wang Yanxin.Review and outlook of water-rock interaction studies[J].Earth Science:Journal of China University of Geosciences,2002,27(2):127-133.
    [2]
    Carothers W W,Kharaka Y K.Aliphatic acid anions in oil-fields waters:implications for origin of natural gas[J].AAPG Bulletin,1978,62(12):2441-2453.
    [3]
    蔡春芳,梅博文,李伟.塔里木盆地油田水文地球化学[J].地球化学,1996,25(6):614-622. Cai Chunfang,Mei Bowen,Li Wei.The hydro geochemistry of oil-fields in Tarim Basin[J].Geochimica,1996,25(6):614-622.
    [4]
    李义连,杨玉环,卢学实.水—岩相互作用模拟的研究进展[J].水文地质工程地质,2003,40(3):95-99. Li Yilian,Yang Yuhuan,Lu Xueshi.Research advance on modeling study of water-rock interaction[J].Hydrogeology and Engineering Geology,2003,40(3):95-99.
    [5]
    张枝焕,常象春,曾溅辉.水—岩相互作用研究及其在石油地质中的应用[J].地质科技情报,1998,17(3):69-74. Zhang Zhihuan,Chang Xiangchun,Zeng Jianhui.Research on water-rock interaction and its application on petroleum geology[J].Geo-logical Science and Technology Information,1998,17(3):69-74.
    [6]
    郑兴平,刘永福,张杰,等.塔里木盆地塔中隆起北坡鹰山组白云岩储层特征与成因[J].石油实验地质,2013,35(2):157-161. Zheng Xingping,Liu Yongfu,Zhang Jie,et al.Characteristics and origin of dolomite reservoirs in Lower Ordovician Yingshan Formation,northern slope of Tazhong uplift,Tarim Basin[J].Petroleum Geology & Experiment,2013,35(2):157-161.
    [7]
    Sjoeberg E L,Riekard D T.Temperature dependence of calcite dissolution kinetics between 1 and 62℃ pH 2.7 to 8.4 in aqueous solutions[J].Geochimica et Cosmochimica Acta,1984,48:485-493.
    [8]
    Amrhein C,Jurinak J J,Moore W M.Kinetics of calcite dissolution as affected by carbon dioxide partial pressure[J].Soil Science Society of America Journal,1985,49(6):1393-1398.
    [9]
    Pokrovsky O S,Golubev S V,Sehott J.Dissolution kinetics of calcite,dolomite and magnesite at 25 ℃ and 0 to 50 atm Pco2[J].Chemical Geology,2005,217(3/4):239-255.
    [10]
    Buhmann D,Dreybrodt W.Calcite dissolution kinetics in the system H2O-CO2-CaCO3 with participation of foreign ions[J].Chemical Geology,1987,64(1/2):89-102.
    [11]
    Svensson U,Dreybrodt W.Dissolution kinetics of natural calcite mi-nerals in CO2-water systems approaching calcite equilibrium[J].Chemical Geology,1992,100(1/2):129-145.
    [12]
    王琪,史基安,薛莲花,等.碎屑储集岩成岩演化过程中流体—岩石相互作用特征:以塔里木盆地西南坳陷地区为例[J].沉积学报,1999,17(4):584-590. Wang Qi,Shi Jian,Xue Lianhua,et al.Characteristics of fluid-rock interaction in clastic reservoir controlled by evolution of diagenetic environment :Taking the southwest depression of Tarim basin as an example[J].Acta Sedimentologica Sinica,1999,17(4):584-590.
    [13]
    Huang Sijing,Xiao Linping,Yang Junjie,et al.Experimental simulation of dolomite dissolution under burial diagenesis conditions and thermodynamic interpretation[J].Chinese Journal of Geochemistry,2000,19(1):58-64.
    [14]
    黄思静,杨俊杰,张文正,等.石膏对白云岩溶解影响的实验模拟研究[J].沉积学报,1996,14(1):103-109. Huang Sijing,Yang Junjie,Zhang Wenzheng,et al.Effects of gypsum(or anhydrite) on dissolution of dolomite under different temperatures and pressures of epigenesis and burial diage-nesis[J].Acta Sedimentologica Sinica,1996,14(1):103-109.
    [15]
    郭春清,沈忠明,张林晔.等.砂岩储层中有机酸对主要矿物的溶蚀作用及机理研究综述[J].地质地球化学,2003,31(3):53-57. Guo Chunqing,Shen Zhongming,Zhang Linye,et al.The corrosion and its mechanism of organic acids on main minerals in oil-gas reservoir sand rocks[J].Geology-Geochemistry,2003,31(3):53-57.
    [16]
    邱楠生,顾先觉,丁丽华,等.柴达木盆地西部新生代的构造—热演化研究[J].地质科学,2000,35(4):456-464. Qiu Nansheng,Gu Xianjue,Ding Lihua,et al.Tectono-thermal evolution of western Qaidam basin,Northwest China[J].Scientia Geologica Sinica,2000,35(4):456-464.
    [17]
    Surdam R C,Crossey L J,Hagen E S,et al.Organic-inorganic and sandstone diagenesis[J].AAPG Bulletin,1989,73(1):1-23.
    [18]
    Surdam R C,Boese S W,Crossey L J.The chemistry of secondary porosity[M]//McDonald D A,Surdam R C.Clastic diagenesis:AAPG Mem37.Tulsa:AAPG,1984:127-149.
    [19]
    Helgeson H C,Knox A M,Owens C E,et al.Petroleum,oil field waters,and authigenic mineral assemblages:are they in metastable equili brium in hydrocarbon reservoirs?[J].Geochimica et Cosmochimica Acta,1993,57(14):3295-3339.
    [20]
    Lundegard P D,Land L S,Galloway W E.Problem of secondary porosity:Frio Formation (Oligocene),Texas Gulf Coast[J].Geology,1984,12(7):399-402.
    [21]
    Mcshri I D.On there activity of carbonic and organic acid sand generation of secondary porosity[M]//Gautier D.Roles of Organic matters in sediment diagenesis:SEPM Spec Publ 38,1986:147-155.
    [22]
    MacGowan D B,Surdan R C,Ewing R E.油层中羧酸阴离子对骨架矿物颗粒稳定性的影响[C]//向廷生,译.储层地球化学译文集.西安:西北大学出版社,1990:83-94. MacGowan D B,Surdan R C,Ewing R E.The effection of carboxylic acid carboxylic anions on the steadty of framework particles[C]//Reservoir geochemistry translations.Xi'an:Northwest University Press,1990:83-94.
    [23]
    季汉成,徐珍.深部碎屑岩储层溶蚀作用实验模拟研究[J].地质学报,2007,81(2):212-216. Ji Hancheng,Xu Zhen.Experimental simulation for dissolution in clastic reservoirs of the deep zone[J].Acta Geologica Sinica,2007,81(2):212-216.
    [24]
    蒋小琼,王恕一,范明,等.埋藏成岩环境碳酸盐岩溶蚀作用模拟实验研究[J].石油实验地质,2008,30(6):643-646. Jiang Xiaoqiong,Wang Shuyi,Fan Ming,et al.Study of simulation experiment for carbonate rocks dissolution in burial diagenetic environment [J].Petroleum Geology & Experiment,2008,30(6):643-646.
    [25]
    张天付,鲍征宇,崔振昂,等.碳酸盐岩埋藏溶蚀的热力学分析及其地质意义[J].新疆石油地质,2012,33(2):179-181. Zhang Tianfu,Bao Zhengyu,Cui Zhen'ang,et al.Thermodynamic analysis of burial dissolution of carbonate rocks and its geological ignificance[J].Xinjiang Petroleum Geology,2012,33(2):179-181.
    [26]
    曹正林,袁剑英,黄成刚,等.高温高压碎屑岩储层中石膏溶解对方解石沉淀的影响[J].石油学报,2014,35(3):450-454. Cao Zhenglin,Yuan Jianying,Huang Chenggang,et al. Influence of plaster dissolution on calcite precipitation in clastic reservoirs under high-temperature and high-pressure conditions[J].Acta Petrolei Sinica,2014,35(3):450-454.
    [27]
    闫志为,张志卫.氯化物对方解石和白云石矿物溶解度的影响[J].水文地质工程地质,2009,36(1):113-118. Yan Zhiwei,Zhang Zhiwei.The effect of chloride on the solubility of calcite and dolomite[J].Hydrogeology and Engineering Geology,2009,36(1):113-118.
    [28]
    金强,朱光有.中国中新生代咸化湖盆烃源岩沉积的问题及相关进展[J].高校地质学报,2006,12(4):483-492. Jin Qiang,Zhu Guangyou.Progress in research of deposition of oil source rocks in saline lakes and their hydrocarbon generation[J].Geological Journal of China Universities,2006,12(4):483-492.
    [29]
    金强.柴达木盆地西部第三系蒸发岩微量元素组成及其地球化学特征[J].石油大学学报:自然科学版,2003,27(2):1-5. Jin Qiang.Geochemistry characteristics of trace elements in evaporates of the tertiary in western Qaidam basin[J].Journal of the University of Petroleum,China,2003,27(2):1-5.
    [30]
    张晓宝,胡勇,马立元,等.柴达木盆地西部第三系盐湖相天然气碳同位素特征、成因与分布[J].中国科学:D辑:地球科学,2002,32(7):598-608. Zhang Xiaobao,Hu Yong,Ma Liyuan,et al.Carbon isotope compositions of natural gases from saline sediments in Qaidam Basin and their origin and distribution[J].China Science:Ser D:Ear th Science,2002,32(7):598-608.
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