{"title":"Phase equilibria and crystallographic structure of clathrate hydrate formed with carbon dioxide and cyclohexanone","authors":"Leo Kamiya , Ryonosuke Kasai , Satoshi Takeya , Ryo Ohmura","doi":"10.1016/j.fluid.2024.114175","DOIUrl":null,"url":null,"abstract":"<div><p>This paper reports the phase equilibrium and crystallographic data of the hydrate formed in the CO<sub>2</sub> + cyclohexanone + water system. We measured the phase equilibrium condition and conducted the powder X-ray diffraction measurements. The formation of the structure II hydrate in the system of CO<sub>2</sub> + cyclohexanone + water was observed at the temperature from 270.0 K to 275.6 K, under the pressure from 0.62 MPa to 1.70 MPa.</p><p>At 270.0 K – 275.6 K and 0.62 MPa – 1.70 MPa, the structure II hydrate formed, and the phase equilibrium condition alleviated in the system of CO<sub>2</sub> + cyclohexanone + water, while the hydrate formed at 276.5 K - 280.7 K and 2.02 MPa – 3.33 MPa, displayed structure I and cyclohexanone acted as an inhibitor. Equilibrium conditions were measured using the isochoric method, revealing different <em>p-T</em> slopes at high and low temperatures. The high-temperature slope closely resembled that of structure I CO<sub>2</sub> hydrate reported previously. We continuously monitored temperature and pressure during the structural phase transition, resulting in a slope change. To directly determine the hydrate structure, PXRD measurements were conducted on two samples: one from the high-temperature side and the other from the low-temperature side. The sample from the high-temperature side exhibited structure I with a lattice constant of 11.8749 (9) <strong>Å</strong> at 153 K, while the low-temperature sample displayed structure II with a lattice constant of 17.443(1) Å at 153 K.</p></div>","PeriodicalId":12170,"journal":{"name":"Fluid Phase Equilibria","volume":"585 ","pages":"Article 114175"},"PeriodicalIF":2.8000,"publicationDate":"2024-07-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S0378381224001511/pdfft?md5=cd3f6e0c37faa01d9777676ef3142d64&pid=1-s2.0-S0378381224001511-main.pdf","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Fluid Phase Equilibria","FirstCategoryId":"5","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0378381224001511","RegionNum":3,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"CHEMISTRY, PHYSICAL","Score":null,"Total":0}
引用次数: 0
Abstract
This paper reports the phase equilibrium and crystallographic data of the hydrate formed in the CO2 + cyclohexanone + water system. We measured the phase equilibrium condition and conducted the powder X-ray diffraction measurements. The formation of the structure II hydrate in the system of CO2 + cyclohexanone + water was observed at the temperature from 270.0 K to 275.6 K, under the pressure from 0.62 MPa to 1.70 MPa.
At 270.0 K – 275.6 K and 0.62 MPa – 1.70 MPa, the structure II hydrate formed, and the phase equilibrium condition alleviated in the system of CO2 + cyclohexanone + water, while the hydrate formed at 276.5 K - 280.7 K and 2.02 MPa – 3.33 MPa, displayed structure I and cyclohexanone acted as an inhibitor. Equilibrium conditions were measured using the isochoric method, revealing different p-T slopes at high and low temperatures. The high-temperature slope closely resembled that of structure I CO2 hydrate reported previously. We continuously monitored temperature and pressure during the structural phase transition, resulting in a slope change. To directly determine the hydrate structure, PXRD measurements were conducted on two samples: one from the high-temperature side and the other from the low-temperature side. The sample from the high-temperature side exhibited structure I with a lattice constant of 11.8749 (9) Å at 153 K, while the low-temperature sample displayed structure II with a lattice constant of 17.443(1) Å at 153 K.
本文报告了 CO2 + 环己酮 + 水体系中形成的水合物的相平衡和晶体学数据。我们测量了相平衡条件,并进行了粉末 X 射线衍射测量。在 270.0 K - 275.6 K 和 0.62 MPa - 1.70 MPa 压力下,观察到 CO2 + 环己酮 + 水体系中结构 II 水合物的形成。在 270.0 K - 275.6 K 和 0.62 MPa - 1.70 MPa 条件下,形成结构 II 水合物,CO2 + 环己酮 + 水体系中的相平衡条件得到缓解;而在 276.5 K - 280.7 K 和 2.02 MPa - 3.33 MPa 条件下,形成的水合物显示结构 I,环己酮起抑制作用。使用等时法测量了平衡条件,发现在高温和低温下存在不同的 p-T 斜率。高温斜率与之前报告的结构 I CO2 水合物的斜率非常相似。我们在结构相变过程中持续监测温度和压力,结果发现斜率发生了变化。为了直接确定水合物结构,我们对两个样品进行了 PXRD 测量:一个来自高温侧,另一个来自低温侧。高温侧的样品在 153 K 时显示出晶格常数为 11.8749 (9) Å 的结构 I,而低温侧的样品在 153 K 时显示出晶格常数为 17.443 (1) Å 的结构 II。
期刊介绍:
Fluid Phase Equilibria publishes high-quality papers dealing with experimental, theoretical, and applied research related to equilibrium and transport properties of fluids, solids, and interfaces. Subjects of interest include physical/phase and chemical equilibria; equilibrium and nonequilibrium thermophysical properties; fundamental thermodynamic relations; and stability. The systems central to the journal include pure substances and mixtures of organic and inorganic materials, including polymers, biochemicals, and surfactants with sufficient characterization of composition and purity for the results to be reproduced. Alloys are of interest only when thermodynamic studies are included, purely material studies will not be considered. In all cases, authors are expected to provide physical or chemical interpretations of the results.
Experimental research can include measurements under all conditions of temperature, pressure, and composition, including critical and supercritical. Measurements are to be associated with systems and conditions of fundamental or applied interest, and may not be only a collection of routine data, such as physical property or solubility measurements at limited pressures and temperatures close to ambient, or surfactant studies focussed strictly on micellisation or micelle structure. Papers reporting common data must be accompanied by new physical insights and/or contemporary or new theory or techniques.