In situ Raman spectroscopy,as a non-destructive measurement method,is a powerful tool for hydrate research,which can provide important information of hydrate such as cage occupancy,guest molecule and structure.In this work,a series of fundenmental experiments are conducted that focus on the structural transition and the transfer behavior of gas molecule in structure I,II hyrates and water layer during the gas hydrate decomposition by using Raman spectroscopy,including the hydrate decomposition behavior below ice point,transfer of gas molecule in typical structure II hydrate,the effect of small molecule on CH4 hydrate decomposition and the evaluation of stability of CO2 hydrate.The results of these experiments can provide theoretical support for the hydrate exploitation,and have guiding significance for gas storage,gas separation and CO2sequestration.The main achievements are summarized as follows.(1)Study on the dissociation behavior of methant-ethane hydrate below ice point.Besides of the self-preservation,structural transition is also an important feature during the decomposition of CH4-C2H6 hydrate at atmospheric pressure and below ice point.The influences of hydrate-forming gas composition and temperature on the hydrate decomposition behaviors are examined in this work.The CH4-C2H6 hydrates are found to transform from structure I to structure II over the CH4 composition range of 50~68%.The structural transition occurs at the decomposition temperatures below 270.15 K.Furthermore,the hydrate dissociation is retarded upon decreasing the temperature.The above conclusion is important for understanding the hydrate decomposition mechanism,and is helpful for the hydrate exploitation by depressurization in permafrost zones.(2)Study on the transfer behavior of small molecular gas in structure II hydrate.The diffusion process of CH4,CO2 and H2 molecules in a typical structure II,tetrahydrofuran hydrate,is observed by in situ Raman spectroscopy.It is found that H2can penetrate a 5 mm tetrahydrofuran hydrate layer through migrating between the clathrate cages,while CH4 and CO2 molecules cannot penetrate the hydrate layer.The diffusion coefficient of H2 molecule in the tetrahydrofuran hydrate is calculated by Fick’s first law,which is 6.1×10-12 m2/s.The minimum pressure of H2 to enter the tetrahydrofuran hydrate lattice and migrate between small cages is 2.9 MPa.The difference of diffusion behavior of gas molecules in structure II hydrate can be used for gas separation and purification.(3)Study on the effect of small molecular gas on the decomposition of CH4 hydrate.The gas recovery can be significantly enhanced by adding small-molecule gases such as N2or H2to the injecting gas mixtures.To evaluate the independent effect of the small-molecule gas on the CH4 hydrate decomposition,the depressurization of CH4hydrate after the injection of H2/N2 is compared with the pure depressurization.The experimental results show that the addition of small molecule gases lead to the change of the hydrate phase equilibrium,which results in the increase of the hydrate decomposition pressure.Moreover,the content of small molecule gas and the hydrate decomposition pressure are positive correlation.The diffusion coefficients of H2 and N2in CH4 hydrate are calculated by the Raman peak area data,which are 6.6×10-10 and1.8×10-10 m2/s respectively.The injection of H2promotes the hydrate decomposition to a greater extent because of the higher diffusion coefficient.(4)CO2 hydrate is not only one of the hydrate exploitation products,but also an effective medium to store the green house gases.The stability of CO2 hydrate in marine environment is a significant index to evaluate the feasibility of these technologies.In this work,the dissolution rates of CO2 hydrate in under-saturated water are quantified to evaluate the stabilities of CO2 hydrate in different environments.The results show that the dissolution rates are related to the CO2 solubility in different solutions.Meanwhile,there is a linear relationship between the dissolution rate of CO2 hydrate and the water flow rate. |