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在8.6米处对含硫矿物、涂有赤铁矿或覆盖有玄武岩粉尘的矿物进行远程激光诱导击穿光谱(LIBS)和拉曼光谱联用分析。

Combined remote LIBS and Raman spectroscopy at 8.6m of sulfur-containing minerals, and minerals coated with hematite or covered with basaltic dust.

作者信息

Sharma S K, Misra A K, Lucey P G, Wiens R C, Clegg S M

机构信息

Hawaii Institute of Geophysics and Planetology, SOEST, University of Hawaii, Honolulu, HI 96822, USA.

出版信息

Spectrochim Acta A Mol Biomol Spectrosc. 2007 Dec 15;68(4):1036-45. doi: 10.1016/j.saa.2007.06.046. Epub 2007 Aug 1.

Abstract

Combined remote laser-induced breakdown spectroscopy (LIBS) and Raman spectroscopy investigations at a distance of 8.6m have been carried out in air and under a simulated Martian atmosphere of 933Pa (7Torr) CO(2) on calcite (CaCO(3)), gypsum (CaSO(4).2H(2)O), and elemental sulfur (S), and LIBS investigations on chalcopyrite (CuFeS(2)) and pyrite (FeS(2)). Both Raman and LIBS techniques have also been used sequentially in air on hematite-coated calcite crystals and on a sample of anhydrite covered with basaltic dust. These experiments demonstrate that by using a frequency-doubled Nd:YAG pulsed laser co-radiating 1064 nm and 532 nm laser beams with a 5x beam expander, it is possible to measure simultaneously both the Raman and LIBS spectra of calcite, gypsum and elemental sulfur by adjusting the laser power electronically. The spectra of calcite, gypsum, and elemental sulfur contain fingerprint Raman lines; however, it was not possible to measure the remote Raman spectra of pyrite and chalcopyrite because of low intensities of Raman lines. In the cases of CuFeS(2), FeS(2), and elemental sulfur, S atomic emission lines in the LIBS spectra were detected only in 7Torr of CO(2) pressure and not in air. No S atomic emission lines were detected for gypsum in air or in CO(2). In the case of coated/dusted minerals, it was possible to remove the coating or dust with the focused LIBS laser and measure the Raman spectra of subsurface minerals with a 532 nm laser excitation. The complementary nature of these two techniques is highlighted and discussed.

摘要

已在空气中以及在933Pa(7托)二氧化碳的模拟火星大气条件下,对方解石(CaCO₃)、石膏(CaSO₄·2H₂O)和元素硫(S)进行了距离为8.6米的远程激光诱导击穿光谱(LIBS)和拉曼光谱联合研究,并对黄铜矿(CuFeS₂)和黄铁矿(FeS₂)进行了LIBS研究。拉曼光谱和LIBS技术还先后在空气中用于涂有赤铁矿的方解石晶体以及覆盖有玄武岩粉尘的硬石膏样品。这些实验表明,通过使用倍频Nd:YAG脉冲激光器,其同时辐射1064纳米和532纳米激光束,并配备5倍扩束器,通过电子方式调节激光功率,就能够同时测量方解石、石膏和元素硫的拉曼光谱和LIBS光谱。方解石、石膏和元素硫的光谱包含指纹拉曼谱线;然而,由于拉曼谱线强度较低,无法测量黄铁矿和黄铜矿的远程拉曼光谱。在CuFeS₂、FeS₂和元素硫的情况下,仅在7托二氧化碳压力下的LIBS光谱中检测到S原子发射线,而在空气中未检测到。在空气中或二氧化碳中均未检测到石膏的S原子发射线。对于涂覆/沾尘的矿物,可以用聚焦的LIBS激光去除涂层或粉尘,并用532纳米激光激发测量地下矿物的拉曼光谱。突出并讨论了这两种技术的互补性。

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