Experimental study on methane hydrate formation in quartz sand under tri-axial condition
Experimental study on methane hydrate formation in quartz sand under tri-axial condition
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DOI:
10.1016/j.jngse.2020.103707
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发表时间:
2020-11
影响因子:
--
通讯作者:
Q. Gao;Jianzhong Zhao;Zhenyuan Yin;Dong Yang;Chi Zhang
中科院分区:
文献类型:
--
作者:
Q. Gao;Jianzhong Zhao;Zhenyuan Yin;Dong Yang;Chi Zhang
Methane hydrate (MH) has been considered as one of the cleanest energy resources. Its huge resource reserve and high energy density have attracted widespread attention in the scientific field. The dynamic behavior of MH formation and the resulting hydrate saturation are greatly influenced by the conditions of the formation process, such as water-gas ratio (WGR), pressure (P), temperature (T), and the mass fraction of NaCl (XNaCl). To gain a better understanding of the kinetic behavior of the in-situ MH deposits, a novel tri-axial horizon fixed bed reactor was set up to synthesize MH samples under typical marine conditions. A series of MH formation experiments were conducted under similar initial stress conditions (initial tri-axial stress of 16.50 MPa to simulate the overburden stress of marine MH) while perturbing the other key factors (WGR,P,T,andXNaCl) to investigate their effects. The results show that MH saturation attained at the end of formation from an initial water-gas mixing condition was negatively affected by initial WGR,T,and the existence of NaCl. MH formation in the fixed bed reactor increases initialXNaCl= 3.0 wt% to a maximum ofXNaCl= 5.29 wt% and shifts the MH equilibrium curve to a more stringent condition for MH formation. Higher pressure promotes CH4conversion to MH and increases MH saturation from the start of gas injection to the time when the pressure of the reactor was stable (ΔP< 20 kPa/h). Larger initial WGRs (above MH hydration number = 5.75) and higher pressures result in a reduction of the induction time. Increasing temperature and the presence of NaCl increase the induction time.