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页岩中丙烷的降解特征及对页岩气组成的影响
Degradation characteristics of propane in shale rocks and its implication to shale gas composition

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徐建兵 1,2   梁允干 1,2   邓倩 1,2   程斌 1   廖泽文 1 *  
文摘 为探讨高过成熟阶段页岩中小分子烃类的降解对页岩气组成的影响,选取了丙烷和页岩(取自四川盆地龙马溪组同一钻井、不同深度)开展不同系列的模拟实验。对C_3H_8、C_3H_8+页岩、C_3H_8+页岩+水在360 ℃、50 MPa条件下进行黄金管限定体系恒温热模拟实验,恒温时间包括72,216,360,720 h;同时为探讨更高演化程度条件下页岩中小分子烃类的降解特征,对C_3H_8、C_3H_8+页岩分别在400,450,500,550 ℃和50 MPa条件下恒温热模拟72 h。结果显示,360 ℃恒温实验条件下,C_3H_8+页岩体系中CH_4、C_2H_6生成量及CH_4/C_2H_6值比相应的C_3H_8对照实验高,且黏土矿物含量高的S1系列实验生成的CH_4、C_2H_6及CH_4/C_2H_6值基本较S2系列高。提高模拟实验温度后,丙烷的转化率显著提高,C_3H_8+页岩实验中的CH_4、C_2H_6产率均高于对照实验,且CH_4的产率高于C_2H_6。2个系列的模拟实验结果均说明黏土矿物能催化C_3H_8的裂解,且有利于CH_4的产生。含水体系中CH_4、C_2H_6生成量及CH_4/C_2H_6值比无水体系高,说明水能促进页岩中C_3H_8的裂解,且有利于CH_4的富集。页岩中黏土矿物和水对C_3H_8裂解的促进作用导致页岩气向干燥系数高的方向演化,页岩中小分子烃类的降解对高过成熟阶段页岩气的组成具有重要影响,在此过程中水分子起到重要作用,其对高过成熟页岩气资源的评价值得更多关注。
其他语种文摘 Propane and shale samples taken from the same well and different depths in the Longmaxi Formation in the Sichuan Basin were selected to carry out different series of simulation experiments in order to investigate the influence of the degradation of small molecular hydrocarbons on the composition of shale gas in the shale during the over-mature stage. The constant temperature thermal simulation experiments of a gold tube-restricted system were carried out on C_3H_8, C_3H_8 + shale, C_3H_8 + shale + water at 360 ℃ and 50 MPa for 72, 216, 360, 720 h. Other pyrolysis experiments were performed using C_3H_8 and C_3H_8 + shale samples at 400, 450, 500 and 550 ℃ with a pressure of 50 MPa for 72 h in order to increase the degradation degree of C_3H_8. The results showed that the CH_4, C_2H_6 yields and the CH_4/C_2H_6 ratio of C_3H_8 + shale at 360 ℃ are higher than those of C_3H_8 alone. The experiments with S1 shale rock which contains more clay minerals generated more CH_4 and C_2H_6 than those with S2 rock sample, and generally showed higher CH_4/C_2H_6 ratios. After increasing the simulation temperature, the conversion of C_3H_8 was significantly increased. The yields of CH_4 and C_2H_6 in the C_3H_8 + shale experiment were all higher than those in the control experiment, and the yield of CH_4 was higher than that of C_2H_6. These results indicated that clay minerals can catalyze C_3H_8 degradation and produce more CH_4. The yields of CH_4 and C_2H_6, and the CH_4/C_2H_6 ratio from the hydrous experiments were higher than those from anhydrous experiments, which indicated that water can promote the cracking of C_3H_8 to produce more CH_4. The positive effect of clay mineral and water in shale on C_3H_8 cracking increased the dryness index of shale gas. The degradation of small hydrocarbon molecules had an important influence on the composition of shale gas particularly in high- to over-mature shale rocks. It seems that water played a significant role and its effect on the evaluation of shale gas reserve should be thoroughly investigated especially for high- to over-mature shale rocks.
来源 石油实验地质 ,2018,40(3):389-396 【核心库】
DOI 10.11781/sysydz201803389
关键词 丙烷裂解 ; 矿物催化 ; 干燥系数 ; 页岩气
地址

1. 中国科学院广州地球化学研究所, 有机地球化学国家重点实验室, 广州, 510640  

2. 中国科学院大学, 北京, 100049

语种 中文
文献类型 研究性论文
ISSN 1001-6112
学科 石油、天然气工业
基金 国家自然科学基金面上项目 ;  中科院页岩气先导专项(B类)
文献收藏号 CSCD:6256744

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