石英砂中甲烷溶解运移体系水合物生成与聚集实验分析

建立了可模拟海底天然气水合物形成环境的大型三维成藏实验模拟装置,其主体高压反应釜内径500 mm,高1000 mm。在此基础上,采用填砂模型,进行了甲烷溶解运移体系下甲烷水合物生成与聚集过程的实验模拟分析。实验流程为：甲烷溶解于NaCl溶液中,再泵送进入高压反应釜,在沉积层中渗流并生成甲烷水合物。通过30个电阻率传感器监测甲烷水合物的生成和聚集过程。实验结果表明,甲烷溶解运移体系下甲烷水合物生成之后首先分散在溶液中,当溶液的总甲烷浓度（溶解的甲烷及水合物分散相中的甲烷）达到操作条件下盐溶液体系甲烷饱和溶解度后,甲烷水合物从溶液中析出。电阻率分布实验结果表明,析出甲烷水合物的聚集区域受溶液流动控制。     

世界甲烷水合物研究开发现状

分析了甲烷水合物的结构与相平衡以及资源潜力和资源特点,综述了由甲烷水合物生产天然气的方法,详细介绍了日本和美国研究开发甲烷水合物的历程与现状.     

独立探头3ω法表征甲烷水合物热导率和热扩散率

甲烷水合物热物性参数的测量一般是基于时域信号测量,测量方法没有考虑探测器与试样之间的接触热阻。基于频域信号测量原理,研发的3ω独立探头大大拓展了该方法的应用范围。建立了低温高压甲烷水合物合成测量系统。利用独立探头3ω法实时测量甲烷水合物热导率、热扩散率、探头和甲烷水合物之间的接触热阻。分析了甲烷水合物热导率、热扩散率随温度的变化规律;比较了测量值与国内外学者测量数据的不同;发现接触热阻对甲烷水合物热导率有显著影响。     

盐水体系中环戊烷-甲烷水合物的相平衡及分解热

利用可视化水合物相平衡实验装置,采用恒温压力搜索法,测定了284～303K内环戊烷(CP)-甲烷在NaCl溶液中的水合物相平衡数据,并采用Clausius-Clapeyron方程计算了其生成/分解热数据。实验结果表明,CP-甲烷水合物生成条件远低于纯甲烷水合物;采用甲烷辅助气体可使CP在高于其纯水合物四相点的更高温度范围内生成CP-甲烷水合物;CP-甲烷水合物相平衡压力随温度增大而升高;随着NaCl浓度的增大,相平衡压力线性升高,且温度越高,温度和NaCl浓度对相平衡压力的影响越大。CP-甲烷水合物的生成/分解热随着温度的升高而逐渐减小,随NaCl浓度的增加而减小。     

独立探头3ω法表征甲烷水合物热导率和热扩散率

甲烷水合物热物性参数的测量一般是基于时域信号测量,测量方法没有考虑探测器与试样之间的接触热阻。基于频域信号测量原理,研发的3ω独立探头大大拓展了该方法的应用范围。建立了低温高压甲烷水合物合成测量系统。利用独立探头3ω法实时测量甲烷水合物热导率、热扩散率、探头和甲烷水合物之间的接触热阻。分析了甲烷水合物热导率、热扩散率随温度的变化规律;比较了测量值与国内外学者测量数据的不同;发现接触热阻对甲烷水合物热导率有显著影响。     

低温常压条件下水合物法储存甲烷的实验研究

利用水合物法实现对天然气的工业储运,需要提高水合物的储气量并解决水合物的分解速度问题。为此,文章研究了在十二烷基硫酸钠（SDS）体系中,甲烷水合物的储气量和在冰点以下的常压分解规律。研究发现,SDS浓度为650 mg/L时甲烷水合物储气量达到最高值,约为170 V/V。分解温度为268.2~272.2 K区域内,甲烷水合物的分解速率随温度的降低而降低;在268.2 K时,甲烷水合物分解速率最低。     

甲烷水合物生成和分解的实验研究

利用水合物法实现对天然气的工业储运,需要提高水合物的储气量并解决水合物的分解速度问题。为此,文章研究了在十二烷基硫酸钠(SDS)体系中,甲烷水合物的储气量和在冰点以下的常压分解规律。研究发现,SDS浓度为650 mg/L时甲烷水合物储气量达到最高值,约为170 V/V。分解温度为268.2~272.2 K区域内,甲烷水合物的分解速率随温度的降低而降低;在268.2 K时,甲烷水合物分解速率最低。     

聚乙烯己内酰胺链端改性及其对甲烷水合物形成的抑制作用研究

注入动力学抑制剂是一种有效缓解天然气水合物管道堵塞的方法。本文以动力学抑制剂聚乙烯基己内酰胺(PVCap)结构为基础,将氧乙基和酯基引入PVCap的分子链端,合成了新抑制剂PVCap-XA1,在高压定容反应釜内评价了PVCap-XA1对甲烷水合物形成的抑制作用,并采用粉末X射线衍射、低温激光拉曼光谱和冷冻扫描电子显微镜研究了抑制剂对甲烷水合物结构和形态的影响。实验结果表明,相同实验条件下PVCap-XA1比PVCap具有更好的抑制作用;微观测试表明PVCap-XA1的加入没有改变甲烷水合物的晶体结构,但会使甲烷水合物晶面扭曲变形,可以降低水合物大小笼占有比(I_L/I_S),使得甲烷分子更难进入水合物大笼,同时PVCap-XA1的加入使甲烷水合物的微观形貌由多孔有序变得更致密而不利于气体通过。     

氨水在冰粉法合成甲烷水合物中的作用

利用冰粉法在低温高压冰态环境中合成甲烷水合物,通过压缩因子修正理想气体消耗量的PVT理论研究甲烷水合物饱和度随着氨水体积的变化规律,进而探索液态氨与固体甲烷水合物的作用关系。结果表明,在冰粉直径为200μm,温度为-4℃,甲烷气体压力为4.7MPa的条件下,随着氨水体积从0mL增加到24mL,甲烷水合物饱和度从3.8%降低到0.3%,起到了抑制生成甲烷水合物作用。研究为完善冻土带天然气水合物的性质及其开发利用提供了依据。     

盐水体系中环戊烷-甲烷水合物相平衡测定与模拟

利用恒温搜索法测定了温度284.4~303.8 K、NaCl质量浓度0~9.978%水溶液中环戊烷-甲烷水合物(II型)的相平衡条件. 结果表明,该体系水合物相平衡压力远低于纯甲烷水合物,且随温度升高和盐度增大逐渐升高. 在Van der Waals-Platteeuw等温吸附模型和Pitzer活度模型的基础上建立了环戊烷-甲烷水合物在盐水体系中的相平衡理论模型,模拟预测值与实验测定值的吻合度较好,平均相对误差为4.07%,能较好地预测盐水体系中环戊烷-甲烷水合物(II型)的相平衡条件.     

客体分子数对甲烷水合物导热性能影响的分子动力学模拟

本文通过采用EMD方法Green-Kubo理论计算263.15 K 晶穴占有率0-100% sI甲烷水合物导热系数,研究客体分子数对甲烷水合物导热性能的影响。模拟结果显示,甲烷水合物的低导热性能由主体分子构建的笼型结构决定。而在相同温压条件下,随着客体分子甲烷进入晶胞数目增多,晶穴占有率增大后,密度增大,同时客体分子对声子的散射也增强,二者均导致导热性能增强。     

X射线衍射分析聚乙烯吡咯烷酮对水合物分解过程的影响

深水油气资源的勘探开发以及开采过程中的环保要求,使得天然气水合物动力学抑制剂使用不可避免,含动力学抑制剂的分解研究对水合物生成后的解堵具有重要的指导意义。本文在高压反应釜内采用甲烷和丙烷混合气,合成天然气水合物,并用X射线粉晶衍射仪分析了含动力学抑制剂聚乙烯吡咯烷酮的水合物分解过程。结果显示甲烷和丙烷气体会形成SⅡ型水合物,但伴随有SⅠ型甲烷水合物的生成;添加动力学抑制剂后,水合物的分解速率变慢,在-60℃,添加0.5%的聚乙烯吡咯烷酮后,分解起始的20 min内,无抑制剂体系水合物分解可达69%,而在含抑制剂体系分解约18%;SⅡ型甲烷丙烷混合气水合物分解过程中晶胞各晶面分解速率相同,没有偏好性,水合物笼作为一个整体分解,添加抑制剂不改变这种分解方式,仍以整体分解。     

甲烷+氨水体系水合物生成条件实验测定及计算

甲烷在氨水体系中生成水合物的实验数据对于开发水合法回收合成氨驰放气工艺以及操作条件的确定具有重要意义。本文测定了氨摩尔分数为1.018、3.171、5.278氨水溶液中甲烷气体水合物的生成条件。结果表明：氨的加入对甲烷水合物的生成起着明显抑制作用,而且随着氨浓度的增加,生成压力越高。采用Chen-Guo模型对甲烷在氨水中生成水合物的数据进行了计算,得到了较为满意的计算结果,平均误差为2.71%,说明Chen-Guo模型能够较好地预测该类体系的水合物的生成条件。     

Methane hydrate formation and dissociation behaviors in montmorillonite

The methane hydrate formation and the methane hydrate dissociation behaviors in montmorillonite are experimentally studied. Through the analyses of the microstructure characteristic, the study obtains the porous characteristic of montmorillonite. It is indicated that methane hydrate in montmorillonite forms the structure I(sI) crystal.Meanwhile, molecular dynamics simulation is carried out to study the processes of the methane hydrate formation and the methane hydrate dissociation in montmorillonite. The microstructure and microscopic properties are analyzed. The methane hydrate formation and methane hydrate dissociation mechanisms in the montmorillonite nanopore and on the montmorillonite surface are expounded. Combining the experimental and simulating analyses,the results indicate the methane hydrate formation and methane hydrate dissociation processes have little influence upon the crystal structure of porous media from either micro-or macro-analysis. It is beneficial to the fundamental researches on the exploitation and security control technologies of natural gas hydrate in deep-sea sediments.     

Characterization of gas hydrates with PXRD, DSC, NMR, and Raman spectroscopy

Structure I (sI) and H (sH) hydrates containing methane were synthesized and characterized with PXRD, DSC, NMR, and Raman spectroscopy. Three well-known large molecule guest substances (LMGSs) were selected as sH hydrate formers: 2,2-dimetylbutane (NH), methylcyclohexane (MCH), and tert-butyl methyl ether (TBME). The solid phase analysis confirmed the presence of sH hydrate whenever a LMGS was present. The presence of a non-hydrate former (n-heptane) did not affect the methane hydrate structure or cage occupancies. Ice to hydrate conversion was limited when the LMGS amount was less than stoichiometric and synthesized at low methane pressure, but nearly complete conversion was achieved with temperature ramping and excess LMGS. The methane occupancies were found to depend on the type of LMGS and increased with pressure. The hydrate with TBME was found to have the smallest methane content followed by the hydrates with NH and MCH. Both NMR and Raman identified methane and LMGS signals from the hydrate phase, however, the cage occupancy values of sH hydrate can only be obtained from NMR spectroscopy. The hydrate structures, ice to hydrate conversion, gas content in hydrate and cage occupancy from the various measurements are consistent with each other.     

甲烷水合物分解动力学

根据两种测量水合物分解动力学的方法———恒定分解压力法及压力变化法 ,采用气体水合物静力学实验装置测定了甲烷水合物的分解动力学数据 .由建立的分解动力学模型计算了甲烷水合物的分解速率 ,较好地拟合了所测得的实验数据 .实验数据验证了分解速率和水合物平衡压力下的逸度与实验压力下的逸度之差有关 ,计算的分解活化能为 73.3kJ·mol^-1(甲烷 ) .     

甲烷水合物在纯水中的生成动力学

引言一些低分子量气体,如石油和天然气中C_1～C_4轻烃、氮气、硫化氢、二氧化碳和惰性气体等,在一定压力和温度的条件下可与水形成一类笼形结构的冰状晶体,即所谓的气体水合物．气体水合物是一类较为特殊的包络化合物：主体水分子通过氢键相互结合形成一种内含空隙的笼形框架,客体分子则被笼罩于这些空隙中．主、客体分子之间的作用力为vanderWaals力．水合物晶体最为常见的两种结构分别称为结构I（体心立方构型）和结构Ⅱ（金刚石构型）．甲烷和水形成结构I水合物．文献阐述了开展水合物生成动力学研究的重要意义．但由于水合物生成…     

甲烷水合物在纯水中的生成动力学

The kinetic behavior of methane hydrate formation in pure water was investigated.12 sets of experimental data on methane hydrate formation were determined at temperatures ranging from 273.65 to 276.15K and pressures ranging from 4.47 to 8.47MPa.The duration of three stages in methane hydrate formation,known as the dissolution,nucleation and growth periods,that are lacking in open literature,was obtained.The effect of pressure and temperature on the kinetics of methane hydrate formation was also studied.     

Phase behavior and structure transition of the mixed methane and nitrogen hydrates

Pure methane and nitrogen form structure I and II hydrate, respectively, and therefore the structure type of mixed gas hydrate was found to largely depend on their relative gas composition. In addition to the structural difference of size and shape, each hydrate structure shows different capacity to store the guest molecules. In this study, we investigated phase and structural behaviors according to the composition of methane+nitrogen gas mixture. Three-phase (H-Lw-V) equilibria of solid hydrate, water-rich liquid and vapor phase containing 25.24 mol%, 28.51 mol%, 31.23 mol% and 40.39 mol% of methane were determined at various temperatures (in the range from 273.30 K to 285.05 K) and pressures (from 8.325 MPa to 20.700 MPa). 13C solid-state NMR spectroscopy and powder XRD method were performed to identify the formed structure of hydrate samples. The experimental results showed that gas hydrate of the methane+nitrogen mixture changes its structure from sI to sII between 25.24 mol% and 28.51 mol% of methane concentration. These results of phase behavior and structure identification for the mixed gas hydrates are expected to be very helpful in evaluating the feasibility of exploitation of methane gas from natural gas hydrate and the separation process using gas hydrate as a storage-media     

Nonstationary Absorption of Methane by a Quiescent Aqueous Phase

Nonequilibrium dissolution of methane in unstirred water was investigated. The experiments were carried out in the ranges of temperatures, pressures, and concentrations corresponding to the existence of methane hydrate in an equilibrium state. The experimental data were satisfactorily described by a model taking into account the methane transfer both through the gas–liquid interface layer and in the liquid phase. Calculations using the model and the experimental data showed that the methane diffusivity in water is lower than in the interface layer. This can be associated with the formation of methane hydrate in the aqueous phase, since methane hydrate molecules are larger than methane molecules.