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[1]佘 敏*,寿建峰,沈安江,等.从表生到深埋藏环境下有机酸对碳酸盐岩溶蚀的实验模拟[J].地球化学,2014,43(03):276-286.
 SHE Min*,SHOU Jian-feng,SHEN An-jiang,et al.Experimental simulation of dissolution for carbonate rocks in organic acid under the conditions from epigenesis to deep burial environments[J].Geochimica,2014,43(03):276-286.
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从表生到深埋藏环境下有机酸对碳酸盐岩溶蚀的实验模拟

参考文献/References:

[1] Gledhill D K, Morse J W.Calcite dissolution kinetics in Na-Ca-Mg-Cl brines[J].Geochim Cosmochim Acta, 2006, 70(23): 5802-5813.
[2] 罗平, 张静, 刘伟, 宋金民; 周刚, 孙萍, 王道串.中国海相碳酸盐岩油气储层基本特征[J].地学前缘, 2008, 15(1): 36-50.
Luo Ping, Zhang Jing, Liu Wei, Song Jin-min, Zhou Gang, Sun Ping, Wang Dao-chuan.Characteristics of marine carbonate hydrocarbon reservoirs in China[J].Earth Sci Front, 2008, 15(1): 36-50 (in Chinese with English abstract).
[3] Plummer L N, Wigley T M L, Parkhurst D L.The kinetics of calcite dissolution in CO2-water systems at 5 to 60 ℃ and 0.0 to 1.0 atm CO2[J].Am J Sci, 1978, 278(2): 179-216.
[4] Sj?berg E L, Rickard D T.Temperature dependence of calcite dissolution kinetics between 1 and 62 ℃ at pH 2.7 to 8.4 in aqueous solutions[J].Geochim Cosmochim Acta, 1984, 48(3): 485-493.
[5] Svensson U, Dreybrodt W.Dissolution kinetics of natural calcite minerals in CO2-water systems approaching calcite equilibrium[J].Chem Geol, 1992, 100(1/2): 129-145.
[6] Alkattan M, Oelkers E H, Dandur J L, Schott J.An experi-mental study of calcite and limestone dissolution rates as a function of pH from -1 to 3 and temperature from 25 to 80 ℃[J].Chem Geol, 1998, 151(1-4): 199-214.
[7] Eisenlohr L, Meteva K, Gabrov?ek F, Dreybrodt W.The inhibiting action of intrinsic impurities in natural calcium carbonate minerals to their dissolution kinetics in aqueous H2O-CO2 solutions[J].Geochim Cosmochim Acta, 1999, 63(7/8): 989-1002.
[8] Liu Z H, Yuan D X, Dreybrodt W.Comparative study of dissolution rate-determining mechanism of limestone and dolomite[J].Environ Geol, 2005, 49(2): 274-279.
[9] Rauch H W, White W.Dissolution kinetics of carbonate rocks: 1.Effects of lithology on dissolution rate[J].Water Resour Res, 1977, 13(2): 181-194.
[10] 陈景山, 李忠, 王振宇, 谭秀臣, 李凌, 马青.塔里木盆地奥陶系碳酸盐岩古岩溶作用与储层分布[J].沉积学报, 2007, 25(6): 858-868.
Chen Jing-shan, Li Zhong, Wang Zhen-yu, Tan Xiu-chen, Li Ling, Ma Qing.Paleokarstification and reservoir distribution of Ordovician carbonates in Tarim Basin[J].Acta Sedimentol Sinica, 2007, 25(6): 858-868 (in Chinese with English abstract).
[11] 王一刚, 文应初, 洪海涛, 夏茂龙, 何颋婷, 宋蜀筠.四川盆地三叠系飞仙关组气藏储层成岩作用研究拾零[J].沉积学报, 2007, 25(6): 831-838.
Wang Yi-gang, Wen Ying-chu, Hong Hai-tao, Xia Mao-long, He Ting-ting, Song Shu-jun.Diagenesis of Triassic Feixianguan Formation in Sichuan Basin, Southwest China[J].Acta Sedimentol Sinica, 2007, 25(6): 831-838 (in Chinese with English abstract).
[12] 朱光有, 张水昌, 梁英波.川东北飞仙关组H2S的分布与古环境的关系[J].石油勘探与开发, 2005, 32(4): 65-69.
Zhu Guang-you, Zhang Shui-chang, Liang Ying-bo.Rela-tionship between palaeoenvironment and the distribution of H2S in Feixianguan Formation, NE Sichuan Province[J].Pet Explor Develop, 2005, 32(4): 65-69 (in Chinese with English abstract).
[13] 朱光有, 张水昌, 梁英波, 马永生, 戴金星, 周国源.TSR对深部碳酸盐岩储层的溶蚀改造—— 四川盆地深部碳酸盐岩优质储层形成的重要方式[J].岩石学报, 2006, 22(8): 2182-2194.
Zhu Guang-you, Zhang Shui-chang, Liang Ying-bo, Ma Yong-sheng, Dai Jin-xing, Zhou Guo-yuan.Dissolution and alteration of the deep carbonate reservoirs by TSR: An important type of deep-buried high-quality carbonate reservoirs in Sichuan basin[J].Acta Petrol Sinica, 2006, 22(8): 2182-2194 (in Chinese with English abstract).
[14] Langhorne B, Smithe J, Davies G R.Structurally controlled hydrothermal alteration of carbonate reservoirs: Introduction [J].AAPG Bull, 2006, 90(11): 1635-1640.
[15] Chou L, Garrels R M, Wollast R.Comparative study of the kinetics and mechanisms of dissolution of carbonate minerals [J].Chem Geol, 1989, 78(3/4): 269-282.
[16] Pokrovsky O S, Sergey V G, Schott J, Castillo A.Calcite, do-lomite and magnesite dissolution kinetics in aqueous solu-tions at acid to circumneutral pH, 25 to 150 ℃ and 1 to 55 atm pCO2: New constraints on CO2 sequestration in sedimentary basins[J].Chem Geol, 2009, 265(1/2): 20-32.
[17] Cubilias P, K?hler S, Prieto M, Causserand C, Oelkers E H.How do mineral coatings affect dissolution rates? An experimental study of coupled CaCO3 dissolution-CdCO3 precipitation[J].Geochim Cosmochim Acta, 2005, 69(23): 5459-5476.
[18] Pokrovsky O S, Golubev S V, Schott J.Dissolution kinetics of calcite, dolomite and magnesite at 25 ℃ and 0 to 50 atm pCO2 [J].Chem Geol, 2005, 217(3/4): 239-255.
[19] Gong Q J, Deng J, Wang, Q F, Yang L Q, She M.Calcite dissolution in deionized water from 50 ℃ to 250 ℃ at 10 MPa: Rate equation and reaction order[J].Acta Geol Sinica, 2008, 82(5): 994-1001.
[20] Alkattan M, Oelkers E H, Dandurand J-L, Schott J.An experimental study of calcite dissolution rates at acidic conditions and 25 ℃ in the presence of NaPO3 and MgCl2[J].Chem Geol, 2002, 190(1-4): 291-302.
[21] Fredd C N.The influence of transport and reaction of worm-hole formation in carbonate porous media: A study of alternative stimulation fluids[D].Ann Arbor: University of Michigan, 1997: 45-87.
[22] 黄康俊, 王炜, 鲍征宇, 谢淑云, 万能, 梅廉夫, 钱一雄.埋藏有机酸性流体对四川盆地东北部飞仙关组储层的溶蚀改造作用: 溶解动力学实验研究[J].地球化学, 2011, 40(3): 289-300.
Huang Kang-jun, Wang Wei, Bao Zheng-yu, Xie Shu-yun, Wan Neng, Mei Lian-fu, Qian Yi-xiong.Dissolution and alteration of Feixianguan Formation in the Sichuan Basin by organic acid fluids under burial condition: Kinetic dissolution experiments[J].Geochimica, 2011, 40(3): 289-300 (in Chinese with English abstract).
[23] 范明, 胡凯, 蒋小琼, 刘伟新, 张建勇, 陈宏宇.酸性流体对碳酸盐岩储层的改造作用[J].地球化学, 2009, 38(1): 20-26.
Fan Ming, Hu Kai, Jiang Xiao-qiong, Liu Wei-xin, Zhang Jian-yong, Chen Hong-yu.Effect of acid fluid on carbonate reservoir reconstruction[J].Geochimica, 2009, 38(1): 20-26 (in Chinese with English abstract).
[24] Taylor K C, Nasr-El-Din H A, Mehta S, Aramco S.Anomalous acid reaction rates in carbonate reservoir rocks[J].Soc Petrol Eng, 2006, 11(4): 488-496.
[25] Berner R A.Rate control of mineral dissolution under earth surface condition[J].Am J Sci, 1978, 278(9): 1235-1252.
[26] 佘敏, 朱吟, 沈安江, 郑兴平, 贺训云.塔中北斜坡鹰山组碳酸盐岩溶蚀的模拟实验研究[J].中国岩溶, 2012, 31(3): 234-239.
She Min, Zhu Yin, Shen An-jiang, Zheng Xing-ping, He Xun-yun.Simulation experiment for the dissolution of carbonate rocks of the Yingshan formation on the northern slope of Tazhong uplift[J].Carsol Sinica, 2012, 31(3): 234-239 (in Chinese with English abstract).
[27] Lee S W, Kim Y I, Ahn J W.The use of iminodiacetic acid for low-temperature synthesis of aragonite crystal microrods: Correlation between aragonite crystal microrods and stereo-chemical effects[J].Int J Miner Process, 2009, 92(3/4): 190-195.
[28] Guo H X, Qin Z P, Qian P, Yu P, Cui S P, Wang W.Crystalli-zation of aragonite CaCO3 with complex structures[J].Adv Powder Tech, 2011, 22(6): 777-783.
[29] Santos R M, Ceulemans P, Gerven T V.Synthesis of pure aragonite by somochemical mineral carbonate[J].Chem Eng Res Des, 2012, 90(6): 715-725.
[30] 周根陶, 郑永飞.文石-水体系氧同位素分馏系数的低温实验研究[J].高校地质学报, 2000, 6(1): 89-105.
Zhou Gen-tao, Zheng Yong-fei.Experimental studies of oxygen isotope fractionation factors between aragonite and water at low temperatures[J].Geol J China Univ, 2000, 6(1): 89-105 (in Chinese with English abstract).
[31] 张波, 张刚生.利用羧酸盐的水解脱羧反应合成纯文石晶须[J].陶瓷, 2007 (11): 23-26.
Zhang Bo, Zhang Gang-sheng.Preparation of pure aragonite whiskers by hydrolysis and decarboxylation of carboxylate[J].Ceramics, 2007 (11): 23-26 (in Chinese with English abstract).

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备注/Memo

收稿日期(Received): 2013-06-18; 改回日期(Revised): 2013-10-10; 接受日期(Accepted): 2013-11-01
基金项目: 国家油气专项(2011ZX05004-002)
作者简介: 佘敏(1983-), 男, 工程师、硕士, 主要从事油气储层实验地质方面的研究工作。
* 通讯作者(Corresponding author): SHE Min, E-mail: shem_hz@petrochina.com.cn; Tel: +86-571-85224994

更新日期/Last Update: 2014-05-30