基于Hapke模型的矿物红外发射光谱随粒度与发射角的变异规律

闫柏琨; 陈伟涛; 王润生; 杨苏明; 孙卫东; 陈建明

Volume 34 Issue 6

Jun. 2009

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Article Navigation > Earth Science > 2009 > 34(6): 946-954

YAN Bo-kun, CHEN Wei-tao, WANG Run-sheng, YANG Su-ming, SUN Wei-dong, CHEN Jian-ming, 2009. Variation Law of Mineral Emissivity Spectra with Mineral Granularity and Emission Angle Based on Hapke Model. Earth Science, 34(6): 946-954.

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Variation Law of Mineral Emissivity Spectra with Mineral Granularity and Emission Angle Based on Hapke Model

1.
Laboratory of the Earth Observation Tech no logy, China Aero Geophysical Survey and Remote Sensing Center for Land and Resources, Beijing 100083, China
2.
Department for Crust Dynamics & Deep Space Exploitation of NRSCC & Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Information Center, Xinjiang Bureau of Exploration & Development of Geology & Mineral Resources, Urumqi 830000, China

Received Date: 2008-12-09
Publish Date: 2009-11-25

Abstract

Abstract

One of basic issues in thermal infrared remote sensing geology is the variation law of mineral emissivity spectra with mineral granularity and emission angle, and the law is required when several kinds of ground information are retrieved such as temperature, emissivity and mineral. However, the law is still unknown because it is difficult to measure the mineral emissivity spectra in the laboratory. In this experiment, emissivity spectra of quartz, muscovite and anorthite are calculated using Hapke radiative transfer model, and the calculation results are compared with measured spectra. Finally, the variation law of mineral emissivity spectra with granularity and emission angle is summarized, and the problem of Hapke emissivity model is analyzed. Research results show that, Hapke radiative transfer model could be used to simulate minerals emissivity spectral and variation, and some fine spectral features are different from measured spectral probably owing to Hapke model hypothesis in which multiscattering radiation is isotropic. The variation of spectral with granularity is complicated and the variation law is different to different minerals. The common law is that, with the increase of granularity, reststrahlen features strengthen, reststrahlen features and wavelength change, and Christensen features remain stable. With increase of emission angle, emssivity becomes lower, reststrahlen and transparency features become more obvious, and the whole spectral feature and wavelength of some features such as transparency, reststrahlen and Christensen features keep stable.
- emissivity,
- mineral,
- infrared spectroscopy

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References(45)

References

Aronson, J. G., Strong, P. F., 1975. Optical constants of minerals and rocks. Applied Optics, 14 (12): 2914-2920. doi: 10.1364/AO.14.002914

Bandfield, J. L., 2002. Global mineral distributions on Mars. Journal of Geophysical Research, 107 (E6): 5042-5063. doi: 10.1029/2001JE001510

Bandfield, J. L., Hamilton, V. E., Christensen, P. R., 2000. A global view of Martian surface composition from MGS-TES. Science, 287 (5458): 1626-1630. doi: 10.1126/science.287.5458.1626

Buratti, B. J., Hicks, M. D., Soderblom, L. A., et al., 2004. Deep space 1 photometry of the nucleus of Comet19P/Borrelly. Icarus, 167 (1): 16-29. doi: 10.1016/j.icarus.2003.05.002

Christensen, P. R., Bandfield, J. L., Hamilton, V. E., et al., 2000. Athermal emission spectral library of rock-forming minerals. Journal of Geophysical Research, 105 (E4): 9735-9739. doi: 10.1029/1998JE000624

Clark, R. N., Swayzer, G. A., Livo, K. E., et al., 2003. I maging spectroscopy: Earth and planetary remote sensing with the USGS Tetracorder and expert system. Journalof Geophysical Research, 108 (E2): 5131.

Conel, J. E., 1969. Infrared emissivities of silicates: Experimental results and a cloudy at mosphere model of spectral emission from condensed particulate mediums. Journal of Geophysical Research, 74 (6): 1614-1634. doi: 10.1029/JB074i006p01614

Copper, B. L., Salisbury, J. W., Killen, R. M., et al., 2002. Midinfared spectral features of rocks and their powders. Journal of Geophysical Research, 107 (E4): 5017. doi: 10.1029/2000JE001462

Cruikshank, D. P., Dalle-Ore, C. M., Roush, T. L., et al., 2001. Constraints on the composition of Trojan asteroid 624 Hector. Icarus, 153 (2): 348-360. doi: 10.1006/icar.2001.6703

Dozier, J., Warren, S. G., 1982. Effect of viewing angle on infrared brightness temperature of snow. Water Resources Research, 18 (5): 1424-1434. doi: 10.1029/WR018i005p01424

Hamilton, V. E., 2000. Thermal infrared emission spectroscopy of the pyroxene mineral series. Journal of Geo-physical Research, 105 (E4): 9701-9716. doi: 10.1029/1999JE001112

Hansen, J. E., Travis, L. D., 1974. Light scattering in planetary at mospheres. Space Science Review, 16 (4): 527-610. doi: 10.1007/BF00168069

Hapke, B., 1981. Bidirectional reflectance spectroscopy 1. Theory. Journal of Geophysical Research, 86 (B4): 3039-3054. doi: 10.1029/JB086iB04p03039

Hapke, B., 1984. Bidirectional reflectance spectroscopy: 3. Correction for macroscopic roughness. Icarus, 59 (1): 41-59. doi: 10.1016/0019-1035(84)90054-X

Hapke, B., 1986. Bidirectional reflectance spectroscopy: 4. The extinction coefficient and the opposition effect. Icarus, 67 (2): 264-280. doi: 10.1016/0019-1035(86)90108-9

Hapke, B., 1993a. Combined theory of reflectance and emit-tance spectroscopy. In: Remote geochemical analysis: Elemental and mineralogical composition. CambridgeUniversity Press, London, 31-41.

Hapke, B., 1993b. Theory of reflectance and emittance spectroscopy. Cambridge University Press, London.

Hapke, B., 1999. Scattering and diffraction of light by particles in planetary regoliths. Journal of Quantitative Spectroscopy of Radiative and Transfer, 61 (5): 565-581. doi: 10.1016/S0022-4073(98)00042-9

Hapke, B., 2002. Bidirectional reflectance spectroscopy: 5. The coherent backscatter opposition effect and anisotropic scattering. Icarus, 157 (2): 523-534. doi: 10.1006/icar.2002.6853

Hapke, B., Nelson, R., Smythe, W., 1998. The oppositio neffect of the moon: Coherent backscatter and shadow hiding. Icarus, 133 (1): 89-97. doi: 10.1006/icar.1998.5907

Hudson, R. S., Ostro, S. J., 1999. Physical model of asteroid 1620 Geographos from radar and optical data. Icarus, 140 (2): 369-378. doi: 10.1006/icar.1999.6142

Kahle, A. B., Alley, R. E., 1992. Separation of temperature and emittance in remotely sensed radiance measurements. Remote Sensing of Environment, 42 (2): 107-111. doi: 10.1016/0034-4257(92)90093-Y

Kirkland, L., Herr, K., Keim, E., et al., 2002. First use of an airborne thermal infrared hyperspectral scanner for compositional mapping. Remote Sensing of Environment, 80 (3): 447-459. doi: 10.1016/S0034-4257(01)00323-6

Klingelh fer, G., Morris, R. V., Bernhardt, B., et al., 2004. Jarosite and hematite at Meridiani planum from opportunity's MÖssbauer spectrometer. Science, 306 (5702): 1740-1745. doi: 10.1126/science.1104653

Lane, M. D., Christensen, P. R., 1997. Thermal infrared emission spectroscopy of anhydrous carbonates. Journal of Geophysical Research, 102 (E11): 25581-25592. doi: 10.1029/97JE02046

Li, X. W., Wang, J. D., Strahler, A. H., 1999. Scale effects of Planck's law over nonisothermal blackbody surface. Science in China (Series E), 42 (6): 652-656. doi: 10.1007/BF02917003

Liu, L. W., Zheng, H. B., Jian, Z. M., 2005. Visible reflectance record of South China Sea sediments during the past 220 ka and its implications for East Asian monsoon variation. Earth Science—Journal of China University of Geosciences, 30 (5): 543-549 (in Chinesewith English abstract).

Liu, Z. F., Christophe, C., Alain, T., 2005. Application of Fourier transform infrared (FTIR) spectroscopy in quantitative mineralogy of the South China Sea: Example of core MD01-2393. Earth Science—Journal of China University of Geosciences, 30 (1): 25-29 (inChinese with English abstract).

Mallama, A., Wand, D., Howard, R. A., 2002. Photometry of mecury from SOHU/LASCO and earth: The phase function from 2 to 170°. Icarus, 155 (2): 253-264. doi: 10.1006/icar.2001.6723

McGuire, A. F., Hapke, B. W., 1995. An experimental study of light scattering by large, irregular particles. Icarus, 113 (1): 134-155. doi: 10.1006/icar.1995.1012

Melissa, L. W., Christensen, P. R., 1996. Optical constants of minerals derived from emission spectroscopy: Application to quartz. Journal of Geophysical Research, 107 (B7): 15921-15931.

Moersch, J. E., Christensen, P. R., 1995. Thermal emission from particulate surfaces: A comparison of scattering models with measured spectra. Journal of GeophysicalResearch, 100 (E4): 7465-7477.

Pit man, K. M., Wolff, M. J., Clayton, G. C., 2005. Application of modern radiative transfer tools to model laboratory quartz emissivity. Journal of Geophysical Research, 110 (E08003): 1-15.

Poulet, F., Cuzzi, J. N., Cruikshank, D. P., et al., 2002. Comparison between the Shkuratov and Hapke scattering theories for solid planetary sufaces: Application to the surface composition of two Centaurs. Icarus, 160 (2): 313-324. doi: 10.1006/icar.2002.6970

Reinart, A., Reinhold, M., 2008. Mapping surface temperature in large lakes with MODIS data. Remote Sensing of Environment, 112 (2): 603-611. doi: 10.1016/j.rse.2007.05.015

Salisbury, J. W., Wald, A., 1992. The role of volume scattering in reducing spectral contrast of reststrahlen bands in spectra of powdered minerals. Icarus, 96 (1): 121-128. doi: 10.1016/0019-1035(92)90009-V

Salisbury, J. W., Walter, L. S., 1989. Thermal infrared (2.5-13.5μm) spectroscopic remote sensing of igneous rock types on particulate planetary surfaces. Journal of Geophysical Research, 94 (B7): 9192-9202. doi: 10.1029/JB094iB07p09192

Shepard, M. K., Helfenstein, P., 2007. A test of the Hapke photometric model. Journal of Geophysical Research, 112 (E03001): 1-17.

Simonelli, D. P., Veverka, J., Thomas, P. C., et al., 1996. Ida lightcurves: Consistency with Galileo shape and photometric models. Icarus, 120 (1): 38-47. doi: 10.1006/icar.1996.0035

Spitzer, W. G., Kleinman, D. A., 1961. Infrared lattice bands in quartz. Phsical Review, 121 (5): 1324-1335. doi: 10.1103/PhysRev.121.1324

Vaughan, R. G., Calvin, W. M., Taranik, J. V., 2003. SE-BASS hyperspectral thermal infrared data: Surface emissivity measurement and mineral mapping. Remote Sensing of Environment, 85 (1): 48-63. doi: 10.1016/S0034-4257(02)00186-4

Vaughan, R. G., Hook, S. J., Calvin, W. M., et al., 2005. Surface mineral mapping at streamboat springs, Neveda, USA with multi-wavelength thermal infrared images. Remote Sensing of Environment, 99 (1-2): 140-158. doi: 10.1016/j.rse.2005.04.030

Wald, A. E., Salisbury, J. W., 1995. Thermal infrared directional emissivity of powdered quartz. Journal of Geophysical Research, 100 (B12): 24665-24675. doi: 10.1029/95JB02400

刘连文, 郑洪波, 翦知湣, 2005. 南海沉积物漫反射光谱反映的220ka以来东亚夏季风变迁. 地球科学———中国地质大学学报, 30 (5): 543-549. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200505004.htm

刘志飞, Christophe, C., Alain, T., 2005. 傅里叶变换红外光谱(FTIR) 方法在南海定量矿物学研究中的应用: 以MD01-2393孔为例. 地球科学———中国地质大学学报, 30 (1): 25-29. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200501002.htm

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