Research article Topical Sections

Lateral growth of xenon hydrate films on mica

  • Received: 13 September 2021 Accepted: 19 October 2021 Published: 26 October 2021
  • In this paper, we report an in situ optical microscopy study of lateral growth of xenon (Xe) hydrate thin films on mica at sub-zero temperatures. The interactions between a solid surface and water molecules can strongly affect the alignment of water molecules and induce ice-like ordered structures within the water layer at the water-surface interface. Mica was chosen as a model surface to study the surface effect of hydrophilic sheet silicates on the lateral growth of Xe hydrate films. Under the experimental conditions, the lateral growth of Xe hydrate films was measured to be at an average rapid rate of ~200 μm/s and 400 μm/s under two different pressures of Xe. Mass transfer estimation of the Xe-water system revealed that the increasing trend of lateral film growth rates followed the increase in the net mass flux and aqueous solubility of Xe. However, as the supercooling temperature increased, the trend of lateral film growth rates attained a plateau region where little change in the rate was observed. This unique feature in the lateral film growth trend, the fast lateral growth kinetics, and the short induction time for hydrate film growth hinted at the assistance of the mica surface to aid the lateral growth process of Xe hydrate films at low Xe mass flux and at a low degree of subcooling. A mechanism based on the reported structured water layer at the interface on mica was proposed to rationalize a postulated surface-promotional effect of mica on the nucleation and lateral growth kinetics of Xe hydrate films.

    Citation: Avinash Kumar Both, Chin Li Cheung. Lateral growth of xenon hydrate films on mica[J]. AIMS Materials Science, 2021, 8(5): 776-791. doi: 10.3934/matersci.2021047

    Related Papers:

  • In this paper, we report an in situ optical microscopy study of lateral growth of xenon (Xe) hydrate thin films on mica at sub-zero temperatures. The interactions between a solid surface and water molecules can strongly affect the alignment of water molecules and induce ice-like ordered structures within the water layer at the water-surface interface. Mica was chosen as a model surface to study the surface effect of hydrophilic sheet silicates on the lateral growth of Xe hydrate films. Under the experimental conditions, the lateral growth of Xe hydrate films was measured to be at an average rapid rate of ~200 μm/s and 400 μm/s under two different pressures of Xe. Mass transfer estimation of the Xe-water system revealed that the increasing trend of lateral film growth rates followed the increase in the net mass flux and aqueous solubility of Xe. However, as the supercooling temperature increased, the trend of lateral film growth rates attained a plateau region where little change in the rate was observed. This unique feature in the lateral film growth trend, the fast lateral growth kinetics, and the short induction time for hydrate film growth hinted at the assistance of the mica surface to aid the lateral growth process of Xe hydrate films at low Xe mass flux and at a low degree of subcooling. A mechanism based on the reported structured water layer at the interface on mica was proposed to rationalize a postulated surface-promotional effect of mica on the nucleation and lateral growth kinetics of Xe hydrate films.



    加载中


    [1] Koh CA, Sloan ED, Sum AK, et al. (2011) Fundamentals and applications of gas hydrates. Annu Rev Chem Biomol 2: 237–257. doi: 10.1146/annurev-chembioeng-061010-114152
    [2] Both AK, Gao Y, Zeng XC, et al. (2021) Gas hydrates in confined space of nanoporous materials: new frontier in gas storage technology. Nanoscale 13: 7447–7470. doi: 10.1039/D1NR00751C
    [3] Koh CA, Sum AK, Sloan ED (2009) Gas hydrates: Unlocking the energy from icy cages. J Appl Phys 106: 061101. doi: 10.1063/1.3216463
    [4] Max MD (2003) Natural Gas Hydrate in Oceanic and Permafrost Environments, Dordrecht, Netherlands: Kluwer Academic Publishers.
    [5] Miller SL (1961) The occurence of gas hydrates in the solar system. P Natl Acad Sci USA 47: 1798. doi: 10.1073/pnas.47.11.1798
    [6] Gudipati MS, Castillo-Rogez J (2012) The Science of Solar System Ices, New York, USA: Springer Science & Business Media.
    [7] Chong ZR, Yang SHB, Babu P, et al. (2016) Review of natural gas hydrates as an energy resource: Prospects and challenges. Appl Energy 162: 1633–1652. doi: 10.1016/j.apenergy.2014.12.061
    [8] Kargel JS, Lunine JI (1998) Clathrate hydrates on earth and in the solar system. In: Schmitt B, De Bergh C, Festou M, Solar System Ices. Dordrecht, Netherlands: Springer, 97–117.
    [9] Fu X, Waite WF, Cueto-Felgueroso L, et al. (2019) Xenon hydrate as an analog of methane hydrate in geologic systems out of thermodynamic equilibrium. Geochem Geophy Geosy 20: 2462–2472. doi: 10.1029/2019GC008250
    [10] Kobelev A, Yashin V, Penkov N, et al. (2019) An optical microscope study of the morphology of xenon hydrate crystals: Exploring new approaches to cryopreservation. Crystals 9: 215. doi: 10.3390/cryst9040215
    [11] Shishova NV, Fesenko EE (2015) The prospects of the application of gases and gas hydrates in cryopreservation. Biophysics 60: 782–804. doi: 10.1134/S0006350915050218
    [12] Mousis O, Lunine JI, Picaud S, et al. (2010) Volatile inventories in clathrate hydrates formed in the primordial nebula. Faraday Discuss 147: 509–525. doi: 10.1039/c003658g
    [13] Owen T, Bar-Nun A, Kleinfeld I (1992) Possible cometary origin of heavy noble gases in the atmospheres of Venus, Earth and Mars. Nature 358: 43–46. doi: 10.1038/358043a0
    [14] Shcheka SS, Keppler H (2012) The origin of the terrestrial noble-gas signature. Nature 490: 531–534. doi: 10.1038/nature11506
    [15] Kvamme B, Aromada SA, Saeidi N, et al. (2020) Hydrate nucleation, growth, and induction. ACS Omega 5: 2603–2619. doi: 10.1021/acsomega.9b02865
    [16] Kvamme B, Zhao J, Wei N, et al. (2020) Hydrate—A mysterious phase or just misunderstood? Energies 13: 880. doi: 10.3390/en13040880
    [17] Broseta D, Ruffine L, Desmedt A (2017) Gas Hydrates 1: Fundamentals, Characterization and Modeling, Hoboken, NJ, USA: John Wiley & Sons.
    [18] Ma R, Zhong H, Li L, et al. (2020) Molecular insights into the effect of a solid surface on the stability of a hydrate nucleus. J Phys Chem C 124: 2664–2671. doi: 10.1021/acs.jpcc.9b09704
    [19] Aman ZM, Koh CA (2016) Interfacial phenomena in gas hydrate systems. Chem Soc Rev 45: 1678–1690. doi: 10.1039/C5CS00791G
    [20] Nguyen NN, Galib M, Nguyen AV (2020) Critical review on gas hydrate formation at solid surfaces and in confined spaces—Why and how does interfacial regime matter? Energ Fuel 34: 6751–6760. doi: 10.1021/acs.energyfuels.0c01291
    [21] Shen YR, Ostroverkhov V (2006) Sum-frequency vibrational spectroscopy on water interfaces: polar orientation of water molecules at interfaces. Chem Rev 106: 1140–1154. doi: 10.1021/cr040377d
    [22] You K, Flemings PB, Malinverno A, et al. (2019) Mechanisms of methane hydrate formation in geological systems. Rev Geophys 57: 1146–1196. doi: 10.1029/2018RG000638
    [23] Deer WA, FRS, Howie RA, Zussman J (2013) An Introduction to the Rock-Forming Minerals, London, UK: Mineralogical Society of Great Britain and Ireland.
    [24] Nguyen AN, Zinner E (2004) Discovery of ancient silicate stardust in a meteorite. Science 303: 1496. doi: 10.1126/science.1094389
    [25] Messenger S, Keller LP, Stadermann FJ, et al. (2003) Samples of stars beyond the solar system: silicate grains in interplanetary dust. Science 300: 105. doi: 10.1126/science.1080576
    [26] de Poel W, Pintea S, Drnec J, et al. (2014) Muscovite mica: Flatter than a pancake. Surf Sci 619: 19–24. doi: 10.1016/j.susc.2013.10.008
    [27] Fukuma T, Ueda Y, Yoshioka S, et al. (2010) Atomic-scale distribution of water molecules at the mica-water interface visualized by three-dimensional scanning force microscopy. Phys Rev Lett 104: 016101. doi: 10.1103/PhysRevLett.104.016101
    [28] Odelius M, Bernasconi M, Parrinello M (1997) Two dimensional ice adsorbed on mica surface. Phys Rev Lett 78: 2855–2858. doi: 10.1103/PhysRevLett.78.2855
    [29] Bluhm H, Inoue T, Salmeron M (2000) Formation of dipole-oriented water films on mica substrates at ambient conditions. Surf Sci 462: L599–L602. doi: 10.1016/S0039-6028(00)00595-1
    [30] Miranda PB, Xu L, Shen YR, et al. (1998) Icelike water monolayer adsorbed on mica at room temperature. Phys Rev Lett 81: 5876–5879. doi: 10.1103/PhysRevLett.81.5876
    [31] Cheng L, Fenter P, Nagy KL, et al. (2001) Molecular-scale density oscillations in water adjacent to a mica surface. Phys Rev Lett 87: 156103. doi: 10.1103/PhysRevLett.87.156103
    [32] Peng BZ, Dandekar A, Sun CY, et al. (2007) Hydrate film growth on the surface of a gas bubble suspended in water. J Phys Chem B 111: 12485–12493. doi: 10.1021/jp074606m
    [33] Ballard AL, Sloan ED (2004) The next generation of hydrate prediction: Part Ⅲ. Gibbs energy minimization formalism. Fluid Phase Equilibr 218: 15–31. doi: 10.1016/j.fluid.2003.08.005
    [34] Lang C, Zhao J, Yuan C, et al. (2019) Growth patterns of xenon hydrate on surfaces with varying wettability. International Conference on Applied Energy 2019.
    [35] Khurana M, Yin Z, Linga P (2017) A review of clathrate hydrate nucleation. ACS Sustain Chem Eng 5: 11176–11203. doi: 10.1021/acssuschemeng.7b03238
    [36] Sun CY, Peng BZ, Dandekar A, et al. (2010) Studies on hydrate film growth. Annu Rep Prog Chem, Sect C: Phys 106: 77–100. doi: 10.1039/b811053k
    [37] Fray N, Marboeuf U, Brissaud O, et al. (2010) Equilibrium data of methane, carbon dioxide, and xenon clathrate hydrates below the freezing point of water. Applications to astrophysical environments. J Chem Eng Data 55: 5101–5108. doi: 10.1021/je1006604
    [38] Sanloup C, Mao H-k, Hemley RJ (2002) High-pressure transformations in xenon hydrates. P Natl Acad Sci USA 99: 25. doi: 10.1073/pnas.221602698
    [39] Sugahara K, Sugahara T, Ohgaki K (2005) Thermodynamic and Raman spectroscopic studies of Xe and Kr hydrates. J Chem Eng Data 50: 274–277. doi: 10.1021/je0496692
    [40] Carey DM, Korenowski GM (1998) Measurement of the Raman spectrum of liquid water. J Chem Phys 108: 2669–2675. doi: 10.1063/1.475659
    [41] Nagashima HD, Oshima M, Jin Y (2020) Film-growth rates of methane hydrate on ice surfaces. J Cryst Growth 537: 125595. doi: 10.1016/j.jcrysgro.2020.125595
    [42] Barrer RM, Edge AVJ (1967) Gas hydrates containing argon, krypton and xenon: kinetics and energetics of formation and equilibria. Proc R Soc Lond A 300: 1–24. doi: 10.1098/rspa.1967.0154
    [43] Cox JL (1983) Natural Gas Hydrates: Properties, Occurrence and Recovery. USA: Butterworth.
    [44] Ohmura R, Kashiwazaki S, Mori YH (2000) Measurements of clathrate-hydrate film thickness using laser interferometry. J Cryst Growth 218: 372–380. doi: 10.1016/S0022-0248(00)00564-9
    [45] Hirai S, Tabe Y, Kuwano K, et al. (2000) MRI measurement of hydrate growth and an application to advanced CO2 sequestration technology. Ann Ny Acad Sci 912: 246–253. doi: 10.1111/j.1749-6632.2000.tb06778.x
    [46] Liang H, Guan D, Shi K, et al. (2022) Characterizing mass-transfer mechanism during gas hydrate formation from water droplets. Chem Eng J 428: 132626. doi: 10.1016/j.cej.2021.132626
    [47] Sun W, Brown S, Leach R (2012) An overview of industrial X-ray computed tomography. NPL Report ENG 32.
    [48] Wilson P, Williams MA, Warnett JM, et al. (2017) Utilizing X-ray computed tomography for heritage conservation: The case of Megalosaurus bucklandii. 2017 IEEE International Instrumentation and Measurement Technology Conference.
    [49] Wilson PF, Smith MP, Hay J, et al. (2018) X-ray computed tomography (XCT) and chemical analysis (EDX and XRF) used in conjunction for cultural conservation: the case of the earliest scientifically described dinosaur Megalosaurus bucklandii. Herit Sci 6: 58. doi: 10.1186/s40494-018-0223-0
    [50] Hermanek P, Carmignato S (2016) Reference object for evaluating the accuracy of porosity measurements by X-ray computed tomography. Case Stud Nondestruct Test Eval 6: 122–127. doi: 10.1016/j.csndt.2016.05.003
    [51] Lifton JJ, Malcolm AA, McBride JW (2015) An experimental study on the influence of scatter and beam hardening in X-ray CT for dimensional metrology. Meas Sci Technol 27: 015007. doi: 10.1088/0957-0233/27/1/015007
    [52] Esmail S, Beltran JG (2016) Methane hydrate propagation on surfaces of varying wettability. J Nat Gas Sci Eng 35: 1535–1543. doi: 10.1016/j.jngse.2016.06.068
    [53] Guo Y, Xiao W, Pu W, et al. (2018) CH4 nanobubbles on the hydrophobic solid-water interface serving as the nucleation sites of methane hydrate. Langmuir 34: 10181–10186. doi: 10.1021/acs.langmuir.8b01900
    [54] Bai D, Chen G, Zhang X, et al. (2015) How properties of solid surfaces modulate the nucleation of gas hydrate. Sci Rep 5: 12747. doi: 10.1038/srep12747
    [55] Buch V, Devlin JP (2003) Water in Confining Geometries. New York, USA: Springer Science & Business Media.
    [56] Striolo A, Phan A, Walsh MR (2019) Molecular properties of interfaces relevant for clathrate hydrate agglomeration. Curr Opin Chem Eng 25: 57–66. doi: 10.1016/j.coche.2019.08.006
    [57] Both AK, Cheung CL (2019) Growth of carbon dioxide whiskers. RSC Adv 9: 23780–23784. doi: 10.1039/C9RA04583J
    [58] Kennan RP, Pollack GL (1990) Pressure dependence of the solubility of nitrogen, argon, krypton, and xenon in water. J Chem Phys 93: 2724–2735. doi: 10.1063/1.458911
    [59] He Z, Linga P, Jiang J (2017) CH4 hydrate formation between silica and graphite surfaces: insights from microsecond molecular dynamics simulations. Langmuir 33: 11956–11967. doi: 10.1021/acs.langmuir.7b02711
    [60] He Z, Mi F, Ning F (2021) Molecular insights into CO2 hydrate formation in the presence of hydrophilic and hydrophobic solid surfaces. Energy 234: 121260. doi: 10.1016/j.energy.2021.121260
    [61] Bai D, Chen G, Zhang X, et al. (2011) Microsecond molecular dynamics simulations of the kinetic pathways of gas hydrate formation from solid surfaces. Langmuir 27: 5961–5967. doi: 10.1021/la105088b
    [62] Mori YH (2001) Estimating the thickness of hydrate films from their lateral growth rates: application of a simplified heat transfer model. J Cryst Growth 223: 206–212. doi: 10.1016/S0022-0248(01)00614-5
    [63] Takeya S, Hachikubo A (2019) Structure and density comparison of noble gas hydrates encapsulating Xenon, Krypton and Argon. ChemPhysChem 20: 2518–2524. doi: 10.1002/cphc.201900591
  • matersci-08-05-047-s01.pdf
  • Reader Comments
  • © 2021 the Author(s), licensee AIMS Press. This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0)
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Metrics

Article views(3195) PDF downloads(100) Cited by(0)

Article outline

Figures and Tables

Figures(7)

Other Articles By Authors

/

DownLoad:  Full-Size Img  PowerPoint
Return
Return

Catalog