In situ observation of CH4-H2O binary system at high temperature and high pressure by diamond anvil cell and Raman spectroscopy

被引：4
|
作者：
Zheng, Haifei [1 ]
Duan, Tiyu [1 ]
Sun, Qiang [1 ]
机构：
[1] Peking Univ, Dept Geol, Key Lab Orogen Belts & Crustal Evolut, Beijing, Peoples R China
来源：
EXPERIMENTAL THERMAL AND FLUID SCIENCE | 2012年 / 38卷
关键词：
Methane; Water; Molecule interaction; Raman spectroscopy; High temperature and high pressure (HTHP); EQUATION-OF-STATE; WATER PLUS METHANE; VIRIAL-COEFFICIENTS; MOLECULAR-DYNAMICS; CH4-CO2-H2O SYSTEM; FLUID INCLUSIONS; HYDRATE; CH4; 1000-DEGREES-C; DENSITIES;
D O I：
10.1016/j.expthermflusci.2011.11.005
中图分类号：
O414.1 [热力学];
学科分类号：
摘要：
Phases and pressure-temperature (P-T) relationship of CH4-H2O binary system were observed in situ by diamond anvil cell (DAC) and Raman spectroscopy under various temperature and pressure. The system shows three states: (1) State I: methane in low density and immiscible with water at 75-150 degrees C and 80-189 MPa; (2) State II: methane in high density and immiscible with water at 175-220 degrees C and 265-303 MPa; and (3) State III: methane dissolved in water at above 225 degrees C and 303 MPa. Pressure drops by about 100 MPa in the system when the state transforms from II to III, indicating negative excess volume during the transition. Raman spectra of methane show discontinuity between State II and III, indicating multi-component interactions and system property variations during the phase transition. (C) 2011 Elsevier Inc. All rights reserved.
引用
收藏
页码：262 / 265
页数：4
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