Abstract:
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.