1. College of Physics Science and Technology, China University of Petroleum, Dongying 257061, China 2. College of Science, Beijing Information Science and Technology University, Beijing 100085, China 3. College of Storage and Architecture Engineering, China University of Petroleum, Dongying 257061, China
Abstract:In the present paper, the authors examined some oily core by Raman spectral imaging methods. Those methods can be classified into two categories, referred to as “parallel or direct imaging” (Imaging) and “series or indirect imaging” (Mapping) techniques. The observed oily core samples which belong to siltstone that was from LONG-HU-PAO structure in SONG-LIAO basin. The samples were made from quartz (~60%), feldspar (~25%) and other impurity, a little recrystallized calcite (~1%) was in the pore, and the argillaceous matter was distributed along the edge of a pore. The experimental work was accomplished using Renishaw MKI2000 Model Raman spectrometer including System 1 000 plus filter wheel and filter set. The experimental condition is as follows: room temperature, back-scattering geometry, and excitation wavelength 514.5 nm (Ar ion laser). In organic matter region, the microscopic Raman spectrum shows that there are two strong scattering peaks at 1 587.2 and 1 334.5 cm-1, respectively. The former corresponds to intralayer bi-carbon-atomic stretch mode, referred to as “graphite peak”; the latter is disorder-induced feature because of the relaxation of the wave-vector selection rule resulting from finite crystal size effects, referred to as “disorder peak”. In pure core substrate region, we observed a sharper peak at 462.7 cm-1, corresponding to Raman active nonpolar optical mode of quartz crystal. On the basis of the above-mentioned experimental result, we accomplished Raman spectral imaging using mapping (indirect-imaging) procedure and imaging (direct-imaging) procedure, separately. In mapping (indirect-imaging) procedure, although the Raman spectra possess a high spectral resolution (~1 cm-1) in every spatial dot, the restructured picture shows a low spatial resolution power (~1 micrometer) because the smallest laser beam radius on the sample plane was restricted by objective lens NA. In imaging (direct-imaging) procedure, the Raman spectra possess a low spectral resolution power (~10-20 cm-1), but the picture shows a high spatial resolution power (~0.25-0.30 micrometer) because we need not restructure the picture whose spatial resolution power was only restricted by the optical wavelength. According to the specific structural and spectral properties of sample, and the practical research goal, the authors should select either imaging (direct-imaging) procedure or mapping (indirect-imaging) procedure.
Key words:Core;Microscopic Raman spectral imaging;Spatial resolution power;Spectral resolution power
[1] ZHENG Zhe, CHEN Xuan-hua(郑 辙,陈宣华). Science in China(Series B)(中国科学,B辑),1994,24(6):640. [2] CHEN Ru-qing, CAO Chang-chun, YUAN Gui-hua(陈儒庆,曹长春,阮贵华). Journal of Guilin Institute of Technology(桂林工学院学报),1996,16(4):362. [3] WANG Yu, ZHENG Hai-fei(王 宇,郑海飞). Spectroscopy and Spectral Analysis(光谱学与光谱分析),2005,25(9):1426. [4] WANG Rong, FENG Min, WU Wei-hong, et al(王 荣,冯 敏,吴卫红,等). Spectroscopy and Spectral Analysis(光谱学与光谱分析),2005,25(9): 1422. [5] WEN Chao, LI Xun, SUN De-yu, et al(文 潮,李 迅,孙德玉, 等). Spectroscopy and Spectral Analysis(光谱学与光谱分析),2005,25(1): 54. [6] XIAO Wan-sheng, ZHANG Hong, TAN Da-yong, et al(肖万生,张 红,谭大勇, 等). Spectroscopy and Spectral Analysis(光谱学与光谱分析),2007,27(7): 1340. [7] Turrell G, Corset J. Raman Microscopy: Development and Applications. San Diego: Academic Press Inc., 1996. [8] Wolfe W. Introduction to Imaging Spectrometers, Bellinghan, Waslington: SPIE Optical Engineering Press, 1997. [9] LANG Dong-sheng,YUE Xing-ju,et al(朗东升,岳兴举, 等). The Quantitative Evaluation for Crude Oil, Gas and Water Layer: Logging New Technologies(油气水层定量评价:录井新技术). Beijing: Publishing House of Petroleum Industry(北京:石油工业出版社),2004. 9. [10] HE Mou-chun, L Xin-biao, YAO Shu-zhen, et al(何谋春,吕新彪,姚书振,等). Geological Science and Technology Information(地质科技情报),2005,24(3): 67. [11] DUAN Jing-chun, ZHUANG Xin-guo, HE Mou-chun(段菁春,庄新国,何谋春). Geological Science and Technology Information(地质科技情报),2002, 21(2): 65. [12] CHEN Jin-yang, ZHANG Hong, XIAO Wan-sheng, et al(陈晋阳,张 红,肖万生,等). Chinese Journal of Spectroscopy Laboratory(光谱实验室),2004,21(6): 1060. [13] Tuinstra F, Koenig J L. The Journal of Chemical Physics, 1970,53(3): 1126. [14] Lespade P, Marchand A, Couzi M, et al. Carbon, 1984,22(4/5): 375. [15] Nikiel L, Jagodzinski P W. Carbon, 1993,31(8): 1313. [16] Batonneau Y,Bremard C, Laureyns J, et al. Journal of Raman Spectroscopy, 2000, 31: 1113. [17] Matthaus C, Boydston-white S, Miljkovic M, et al. Applied Spectroscopy,2006,60(1): 1. [18] Wabomba M, Sulub Y, Small G W. Applied Spectroscopy, 2007, 61(4): 349. [19] Sasic S. Applied Spectroscopy, 2007, 61(3): 239. [20] HUANG Qiao-song, XU Xiao-xuan, XU Jia-lin, et al(黄乔松,徐晓轩,许家林, 等). Chinese Journal of Luminescence(发光学报),2004,25(2):202. [21] HUANG Qiao-song, YU Zhao-xian, ZHANG Lin-can, et al(黄乔松,于肇贤,张林灿, 等). Chinese Journal of Luminescence(发光学报),2007,28(4):604. [22] XU Xiao-xuan, WANG Ji-you, ZHU Jian, et al (徐晓轩,王吉友,朱 箭, 等). Chnese Journal of Infrared and Millimeter Waves(红外与毫米波学报),2001,20(3):169.