航空航天方法在土壤研究中的应用

Z. Aliyev
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摘要

航空航天技术在土壤科学中的应用极大地推动了土壤测绘和土壤覆盖监测的发展。早在20世纪30年代,利用遥感图像绘制详细的土壤图和评估作物状况的机会就很大。研究土壤覆盖的远程方法是基于这样一个事实,即土壤中二次变化的起源和程度不同,以不同的方式反射、吸收和发射来自不同光谱区域的电磁波。因此,每个土壤物体都有自己的光谱亮度图像,这些图像是在航空和太空图像上拍摄的。地面光谱反射率已经得到了充分的研究,在这方面,应该参考I.I.Karmanov的基本工作,他用SF-10分光光度计测量了400–750 nm范围内的光谱反射系数,超过了4000 s。土壤样品和其他作者[1-6]。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Using Aerospace Methods in Soil Research
The use of aerospace techniques in soil science gave a significant impetus to the development of soil mapping and monitoring of soil cover. Back in the 30s of the twentieth century, there were significant opportunities for the use of remote images in the preparation of detailed soil maps and for assessing the state of crops. Remote methods for studying the soil cover are based on the fact that different in origin and degrees of secondary changes in the soil in different ways reflect, absorb and emit electromagnetic waves from different zones of the spectrum. As a result, each soil object has its own spectral-brightness image captured on aerial and space images. The ground-based spectral reflectivity has been adequately studied, and in this connection one should refer to the fundamental works of I. I. Karmanov, who measured spectral reflection coefficients in the range 400–750 nm with a spectrophotometer SF-10 more than 4 thousand s. soil samples and other authors [1-6].
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