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首页> 外文期刊>South african journal of chemical engineering >Methane hydrate phase behaviour in EMIM-Cl water based mud (WBM): An experimental and modelling study
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Methane hydrate phase behaviour in EMIM-Cl water based mud (WBM): An experimental and modelling study

机译:eMIM-CL水基泥浆(WBM)中的甲烷水合物相行为:实验和建模研究

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Gas hydrate sediments are known as future energy source and potential technique for the storage CO2. However, the drilling of hydrate sediments are challenged with inappropriate drilling mud systems. Ionic liquids are introduced as novel drilling mud agents that can enhance the rheology of water-based mud and at the same time manage hydrate formation risk during hydrate sediments drilling. However, the disturbances of ionic liquid water-based mud filtrate on hydrate in-situ rocks is not well understood. To achieve this, the phase behaviour of methane hydrates in 1-Ethyl-3-methy-limidazolium chloride (EMIM-Cl) water-based mud at different EMIM-Cl concentrations were measured using the isochoric T-cycle technique in a high-pressure hydrate cell within the temperatures and pressures and ranges from 273.68 – 286.10 K and 3.60 – 9.70 MPa, respectively. The rheological properties of the EMIM-Cl mud systems were tested using a TA rheometer at 271.15 K – 313.15 K. The presence of EMIM-Cl had very minimal disturbances (less than 0.5 K shift) on methane hydrate at the studied concentrations. The disturbance of EMIM-Cl of methane hydrates in pure water system is reduced by 74% in drilling mud systems. The use of EMIM-Cl at 3 wt.% could reduce the methane hydrate disturbance effect 2 times as methanol. EMIM-Cl reduced the thermal degradation of the mud by 55% at 1 wt.% with very low viscosity. The viscosity reduction of the mud occurs at lower EMIM-Cl concentrations. Suggesting that, using ionic liquids water-based mud to drill hydrate sediments will reduce the risk of releasing compacted methane gas into the borehole while drilling. In addition, an attempt is made to predict the methane hydrate equilibrium curve in the presence of the EMIM-Cl using the Dickens and Quinby-Hunt, (1997) model.
机译:气体水合物沉积物被称为未来的存储器CO2的能源和潜在技术。然而,在不适当的钻井泥浆系统中挑战水合物沉积物的钻井。将离子液体引入新型钻井泥剂,可增强水性泥浆的流变学,同时在水合物沉积物钻井期间管理水合物形成风险。然而,对原位岩石上的离子液水基泥炭滤液的干扰尚不清楚。为此,在高压中使用等因素T循环技术测量在不同eMIM-CL浓度下的1-乙基-3-甲状腺沸石氯化物(emim-Cl)水基泥浆中甲烷水合物的相位行为水合物细胞在温度和压力内,分别为273.68-286.10k和3.60-9.70mPa的范围。使用Ta流变仪在271.15k-313.15k中测试eMIM-CL泥系统的流变性质。在研究浓度下,eMIM-CL的存在在甲烷水合物上具有非常小的扰动(小于0.5k偏移)。钻井泥浆系统中甲烷水合物甲烷水合物的eMIM-CL扰动减少了74%。使用3重量%的eMIM-Cl。%可以将甲烷水合物干扰效应降低2次作为甲醇。 emim-cl将泥浆的热降解降低55%,1重量%,粘度非常低。泥浆的粘度降低在较低的emim-Cl浓度下发生。暗示,使用离子液体水基泥浆钻水合物沉积物将使钻孔时将压实甲烷气体释放到钻孔中的风险。此外,尝试使用Dickens和Quinby-Hunt(1997)模型在emim-cl的存在下预测甲烷水合物平衡曲线。

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