A new method for synthesizing fluid inclusions in fused silica capillaries containing organic and inorganic material

被引:142
作者
Chou, I-Ming [1 ]
Song, Yucai [2 ]
Burruss, R. C. [1 ]
机构
[1] US Geol Survey, Reston, VA 20192 USA
[2] Nanjing Univ, Dept Earth Sci, Nanjing 210093, Peoples R China
关键词
D O I
10.1016/j.gca.2008.07.030
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Considerable advances in our understanding of physicochernical properties of geological fluids and their roles in many geological processes have been achieved by the use of synthetic fluid inclusions. We have developed a new method to synthesize fluid inclusions containing organic and inorganic material in fused silica capillary tubing. We have used both round (0.3 mm OD and 0.05 or 0.1 mm ID) and square cross-section tubing (0.3 x 0.3 mm with 0.05 x 0.05 mm or 0.1 x 0.1 mm cavities). For micro thermometric measurements in a USGS-type heating-cooling stage, sample capsules must be less than 25 mm in length. The square-sectioned capsules have the advantage of providing images without optical distortion. However, the maximum internal pressure (P; about 100 MPa at 22 degrees C and temperature (T; about 500 degrees C) maintained by the square-sectioned capsules are less than those held by the round-sectioned capsules (about 300 MPa. at room T, and T up to 650 degrees C). The fused silica capsules can be applied to a wide range of problems of interest in fluid inclusion and hydrothertnal research, such as creating standards for the calibration of thermocouples in heating-cooling stages and frequency shifts in Raman spectrometers. The fused silica capsules can also be used as containers for hydrothermal reactions, especially for organic samples, including individual hydrocarbons, crude oils, and gases, such as cracking of C18H38 between 350 and 400 degrees C, isotopic exchanges between C18H38 and D2O and between C19D40 and H2O at similar temperatures. Results of these types of studies provide information on the kinetics of oil cracking and the changes of oil composition under thermal stress. When compared with synthesis of fluid inclusions formed by healing fractures in quartz or other minerals or by overgrowth of quartz at elevated P-T conditions, the new fused-silica method has the following advantages: (1) it is simple; (2) fluid inclusions without the presence of water can be formed; (3) synthesized inclusions are large and uniform, and they are able to tolerate high internal P; (4) it is suitable for the study of organic material; and (5) redox control is possible due to high permeability of the fused silica to hydrogen. Published by Elsevier Ltd.
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页码:5217 / 5231
页数:15
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