摘要
提出了一种提取热红外图像发射率信息的比值加权法.研究表明,本区石灰岩光谱由CO3弯曲振动控制,发射谷在11.3μm附近(6通道),石英砂岩的光谱在8.6~9.0μm(2通道)和9.8~10.6μm(5通道)为低发射率,而杂砂岩由于含有硅酸盐矿物和一些碳酸盐矿物,在9.8~10.6μm(5通道)和10.6~11.4μm(6通道)呈相对低发射率.结果显示比值加权法对于航空热红外多波段扫描仪TIMS数据地物发射率信息提取是有效的.
The ratioweighted method for extracting emissivity information was described. The study shows that the limestone spectra in the study area are dominated by CO3 bending vibration reststrahlen band near 11.3μm(in CH6),the spectrum of quartz sandstone has low emissivity at 8.6~9.0μm (CH2) and 9.8~10.6μm (CH5), while the greywacke has low relative emissivity at 9.8~10.6μm (CH5) and 10.6~11.4μm (CH6) due to the silicate mineral and some content of carbonate mineral. The results indicate that the ratioweighted method can be used for extracting emissivity information of ground objects from the airborne TIMS data.
出处
《红外与毫米波学报》
SCIE
EI
CAS
CSCD
北大核心
1998年第3期166-170,共5页
Journal of Infrared and Millimeter Waves