Liu Huan-Jun, Zhang Xin-Le, Zheng Shu-Feng, Tang Na, Hu Yan-Liang
Key Laboratory of Resources Remote Sensing & Digital Agriculture, Ministry of Agriculture, Beijing 100081, China.
Guang Pu Xue Yu Guang Pu Fen Xi. 2010 Dec;30(12):3355-8.
To develop soil organic matter (OM) quick measuring methods, deepen the application of remote sensing in agriculture, improve agricultural production and management way, and promote the development of quantitative remote sensing studies relating to terrestrial ecosystem, field hyperspectral reflectance in the visible/near infrared bands of black soil in Hailun city, northeast China, was collected and analyzed with spectral analysis methods to discover the spectral characteristics of field reflectance and its influencing factors, and the spectral indices were derived, then black soil organic matter predicting model based on the correlation between OM content and spectral indices was built. Root mean squared error (RMSE) was introduced to validate the predictability and precision of the models, and coefficient of the determination (R2) was used to evaluate stability of the models. The results are as follows: the main spectral region of remarkable differences between field black soil reflectance curves is less than 1 250 nm, especially less than 1 000 nm; OM is the main factor determining the curve shape of field black soil reflectance, anc there are single or double spectral wave troughs for different soil samples because of varying OM content at the spectral region less 1 100 nm; correlation between OM and differential coefficient of logarithmic reflectance reciprocal (DCLRR) is much more significant than that between OM and other reflectance or its transforms, and the maximum coefficient of correlation is at 1 260 nm; the predicting model for black soil OM content is built with DCLRR at 1 260 nm as independent varialble and OM as dependent variable, and the coefficients of determination R2 of the model is 0.71, RMSE is 0.42, so the model is quite good in stability and predictability, and can be used in fast testing of organic matter in black soil.
为研发土壤有机质(OM)快速测量方法,深化遥感技术在农业中的应用,改进农业生产与管理方式,推动陆地生态系统定量遥感研究发展,采集了中国东北海伦市黑土在可见光/近红外波段的田间高光谱反射率,并采用光谱分析方法进行分析,以发现田间反射率的光谱特征及其影响因素,进而导出光谱指数,然后基于OM含量与光谱指数之间的相关性建立了黑土有机质预测模型。引入均方根误差(RMSE)来验证模型的可预测性和精度,并用决定系数(R2)来评估模型的稳定性。结果如下:田间黑土反射率曲线显著差异的主要光谱区域小于1250nm,尤其是小于1000nm;OM是决定田间黑土反射率曲线形状的主要因素,在小于1100nm的光谱区域,不同土壤样品因OM含量不同而存在单或双光谱波谷;OM与对数反射率倒数微分系数(DCLRR)之间的相关性比OM与其他反射率或其变换之间的相关性显著得多,最大相关系数出现在1260nm处;以1260nm处的DCLRR为自变量、OM为因变量建立了黑土OM含量预测模型,该模型的决定系数R2为0.71,RMSE为0.42,因此该模型在稳定性和可预测性方面表现良好,可用于黑土有机质的快速检测。