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Mixtures of ammonia and water and of methane and water at high pressures.

机译:氨和水以及甲烷和水的高压混合物。

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I have examined the phase relations of mixtures of ammonia and water, {dollar}rm (NHsb3)sb{lcub}X{rcub}Hsb2O)sb{lcub}1-X{rcub},{dollar} with compositions 0.32 {dollar}<{dollar} X {dollar}<{dollar} 0.51, at pressures from 0 to 6.5 GPa, and at temperatures from 125 to 400 K. Sample pressures were determined by the ruby luminescence technique. The sample temperature was controlled by mounting the diamond cell in a vacuum cryostat where the diamond cell was cooled by a static heat sink and heated electrically. Microscopic observations were made in situ and were recorded on video tape. Polarizing filters were used to observe and record birefringence and other optical effects. I found that the congruent melting curve of ammonia dihydrate, {dollar}rm NHsb3{lcub}cdot{rcub}2Hsb2O,{dollar} extends from 0.06 GPa and 179 K to 1.4 GPa and 243 K and conforms to the equation, T = 176 + 60P {dollar}-{dollar} 8.5P{dollar}sp2{dollar} where T is temperature in K and P is pressure in GPa. Above 1.4 GPa, {dollar}rm NHsb3{lcub}cdot{rcub}2Hsb2O{dollar} was found to melt incongruently to form Ice VII and fluid. The congruent melting curve of ammonia monohydrate, {dollar}rm NHsb3{lcub}cdot{rcub}Hsb2O,{dollar} was found to extend from atmospheric pressure to 4.8 GPa and 350 K and to conform to the equation, T = 194 + 37P {dollar}-{dollar} P{dollar}sp2{dollar}. At higher pressures, it is presumed that {dollar}rm NHsb3{lcub}cdot{rcub}Hsb2O{dollar} melts incongruently to form Ice VII and fluid. A phase diagram for the high-pressure ice polymorphs and the ammonia hydrates in the water-rich region is presented.; I have examined samples of methane and water which were loaded into a diamond cell as methane hydrate clathrate using optical observations and Raman spectroscopy at conditions ranging from 296 to 323 K and at pressures from 0.4 to 5.0 GPa. The spectral results indicate that methane hydrate decomposes to high pressure ices and solid methane at pressure above 2.0 GPa at 295 {dollar}pm{dollar} 5 K. Microscopic examination indicates the presence of a single phase at pressures above 2.3 GPa which tends to contradict the spectral data. The transition from methane hydrate to ice and solid methane seems to cover a broad range of pressure, from 1.0 to 2.0 GPa.
机译:我检查了氨和水的混合物的相位关系,{rmal} rm(NHsb3)sb {lcub} X {rcub} Hsb2O)sb {lcub} 1-X {rcub},{dollar}的组成为0.32 {dollar} <{美元} X {美元} <{美元} 0.51,压力为0至6.5 GPa,温度为125至400K。样品压力通过红宝石发光技术测定。通过将金刚石池安装在真空低温恒温器中来控制样品温度,在真空低温池中,金刚石池通过静态散热器冷却并电加热。显微镜观察原位进行,并记录在录像带上。偏振滤光片用于观察和记录双折射和其他光学效应。我发现氨水合物{美元} rm NHsb3 {lcub} cdot {rcub} 2Hsb2O,{美元}的全同熔融曲线从0.06 GPa和179 K扩展到1.4 GPa和243 K,并符合方程式T = 176 + 60P {美元}-{美元} 8.5P {美元} sp2 {美元}其中T是K的温度,P是GPa的压力。高于1.4 GPa,发现{美元} rm NHsb3 {lcub} cdot {rcub} 2Hsb2O {美元}融化不均匀,形成冰VII和流体。发现一水合氨(美元)rms NHsb3 {lcub} cdot {rcub} Hsb2O {美元}的全同熔融曲线从大气压扩展到4.8 GPa和350 K,并符合方程T = 194 + 37P {dollar}-{dollar} P {dollar} sp2 {dollar}。假定在较高压力下,{rm} rm NHsb3 {lcub} cdot {rcub} Hsb2O {dollar}熔融不均匀,形成Ice VII和流体。给出了富水区中高压冰晶型和氨水合物的相图。我检查了甲烷和水的样品,这些样品以甲烷水合物包合物的形式通过光学观察和拉曼光谱法在296至323 K的条件下和0.4至5.0 GPa的压力下作为金刚石水合物包合物装载到钻石电池中。光谱结果表明,甲烷水合物在295 {pm} {5} 5 K时,在高于2.0 GPa的压力下分解为高压冰和固体甲烷。显微镜检查表明,在高于2.3 GPa的压力下存在单相,这往往是矛盾的。光谱数据。从甲烷水合物到冰和固态甲烷的过渡似乎涵盖了从1.0 GPa到2.0 GPa的广泛压力范围。

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