Guo Yan, Ji Wen-Jun, Wu Hong-Hai, Shi Zhou
Institute of Remote Sensing and Information Technology, Zhejiang University, Hangzhou 310058, China.
Guang Pu Xue Yu Guang Pu Fen Xi. 2013 Apr;33(4):1135-40.
Visible-near infrared (Vis-NIR) reflectance spectroscopy, which is rapid, cost-effective, in-situ, nondestructive and without hazardous chemicals, is increasingly being used for prediction and digital soil mapping of soil organic matter (SOM). This method is the inevitable demand for precision agriculture and soil remote sensing mapping. In the present study, the Vis-NIR (350-2 500 nm) diffuse reflectance spectral collected by ASD FieldSpec Pro FR spectrometer was truncated by removing the noisy edge values below 400 nm and above 2 450 nm and then was transformed into apparent absorbance spectral using log(1/ R). Based on the relationship analysis between absorbance spectral, spectral indices and SOM, partial least squares regression (PLSR) model was applied to predict SOM, and finally the spatial variability of SOM was characterized by geostatistics method. The results indicated that good model was modeling from the characteristic bands (CB, R2 = 0.91, RPD = 3.28) of correlation coefficient more than 0. 5, the spectral index (SI) of normalized difference index (NDI, R2 0.90, RPD = 3.08), CB integrating SI with which a correlation coefficient was more than 0.5 (R2 = 0.87, RPD = 2.67), and total bands (TA, 400-2 450 nm, R2 = 0.95, RPD = 4.36). While the digital mapping of SOM produced by kriging and cokriging interpolation methods implied a better prediction result, showing similar spatial distribution with the measured SOM, indicating that it is feasible and reliable to use these spectral indices to predict and map the spatial variability.
可见-近红外(Vis-NIR)反射光谱法快速、经济高效、原位、无损且无需使用有害化学物质,越来越多地用于土壤有机质(SOM)的预测和数字土壤制图。该方法是精准农业和土壤遥感制图的必然需求。在本研究中,用ASD FieldSpec Pro FR光谱仪采集的Vis-NIR(350-2500nm)漫反射光谱通过去除400nm以下和2450nm以上的噪声边缘值进行截断,然后使用log(1/R)转换为表观吸光度光谱。基于吸光度光谱、光谱指数与SOM之间的关系分析,应用偏最小二乘回归(PLSR)模型预测SOM,最后用地统计学方法表征SOM的空间变异性。结果表明,从相关系数大于0.5的特征波段(CB,R2 = 0.91,RPD = 3.28)、归一化差异指数(NDI,R2 = 0.90,RPD = 3.08)的光谱指数(SI)、相关系数大于0.5的CB与SI结合(R2 = 0.87,RPD = 2.67)以及全波段(TA,400-2450nm,R2 = 0.95,RPD = 4.36)建立了良好的模型。而通过克里金和协同克里金插值方法生成的SOM数字制图显示出更好的预测结果,与实测SOM具有相似的空间分布,表明使用这些光谱指数预测和绘制空间变异性是可行且可靠的。