通过监测辽宁锦州地区不同干旱胁迫条件下春玉米拔节-吐丝期冠层高光谱分布,研究其可见光、红边区和近红外光的光谱分布特征,分析不同波长光谱反射率与各深度土壤湿度的相关关系,结果表明:拔节-吐丝期,0～20 cm层土壤湿度与350～710 nm区间光谱反射率存在显著的负相关关系,各层土壤湿度(0～60 cm)与710～1 300nm区间光谱反射呈正相关关系,其中40 cm深度土壤湿度与光谱反射率正相关性较好;红边区(680～760nm)光谱反射率较好的反映了植株的生长状况,该区间单位波长光谱反射率变化由增加-减小,为相对较稳定的光谱区间.各层土壤湿度与红边参数的多项式回归趋势相似,表层0和20 cm土壤湿度与红边参数关系曲线呈先增加后减小趋势,40和60 cm土壤湿度则先减小后增加.%The spectral absorption and attenuation coefficients of 16 phytoplankton species were measured in the laboratory using acs instrument Ancillary measurements included particle size distribution and chlorophyll a concentration (Chi a). The results indicated that both algal cell size and Chi a were the two major factors dominating the magnitudes of the spectral absorption and attenuation coefficients. The spectral behaviors of attenuation spectra were dominated by algal cell size, the relationship of them didn't follow the monotonic function. Both the ratio of absorption in blue and red waveband and the spectral slope of absorption coefficient were influenced by the product of algal cell density and squares of cell size rather than algal cell size alone. The relationship between algal cell size and both absorption and attenuation spectra would be interpreted by Mie theory for homogenous sphere, which imply that the heterogeneity and non-spherical shape in algal cell morphology and internal structure have little effect on the inherent association among them.
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