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作 者:FENG Jianqing ZOU Yongliao BIAN Wei ZHENG Yongchun LI Chunlai
机构地区:[1]National Astronomical Observatories, Chinese Academy of Sciences, Beo'ing 100012, China [2]Graduate University of the Chinese Academy of Sciences, Beijing 100049, China
出 处:《Chinese Journal Of Geochemistry》2010年第2期204-211,共8页中国地球化学学报
基 金:supported by the National High Technology Research and De-velopment Program of China (863 Program) (Grant No. 2008AA12A213);It was also granted by the Na-tional Natural Science Foundation of China (No. 40904051)
摘 要:Brightness temperature is a main index to reflect the energy of microwave radiation of an object. Using lunar brightness temperature data, physical properties of lunar regolith, such as thickness, heat flow and dielectric permittivity, could be interpreted. There are two methods to study brightness temperature distribution of the moon: the first is used to measure lunar brightness temperature by radio observation or spaceborne microwave radiometers, and the second is used to simulate calculation by the physical model. On the basis of the measurements of lunar brightness temperature in the history, this study analyzed the main physical model of lunar brightness temperature, also including its theory and influence factors. The authors concluded that surface and subsurface temperatures of the moon, dielectric properties and layered structure of lunar regolith were the main factors affecting the global brightness temperature of the moon. These factors should be quantified in detail in the future research.Brightness temperature is a main index to reflect the energy of microwave radiation of an object. Using lunar brightness temperature data, physical properties of lunar regolith, such as thickness, heat flow and dielectric permittivity, could be interpreted. There are two methods to study brightness temperature distribution of the moon: the first is used to measure lunar brightness temperature by radio observation or spaceborne microwave radiometers, and the second is used to simulate calculation by the physical model On the basis of the measurements of lunar brightness temperature in the history, this study analyzed the main physical model of lunar brightness temperature, also including its theory and influence factors. The authors concluded that surface and subsurface temperatures of the moon, dielectric properties and layered structure of lunar regolith were the main factors affecting the global brightness temperature of the moon. These factors should be quantified in detail in the future research.
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