土壤表面水分中波红外偏振光谱特征

IF 0.6 4区 物理与天体物理 Q4 OPTICS
Zhang Qia
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引用次数: 0

摘要

采用光谱偏振法在中波红外范围内对不同含水量土壤表面进行了测量。结果表明:含水土壤表面的热辐射几乎是无极化的,土壤表面的极化特征主要是由太阳光的反射引起的。特别是在强日照光谱范围内,极化程度随着土壤湿度的增加而单调增加。这种定量关系为中w波段红外偏振光遥感监测土壤水分提供了依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Polarization spectral characteristics of soil surface moisture in the mid-wave infrared range
The surfaces of soil with different moisture contents had been surveyed by the spectral polarimetry in the midw ave infrared range.The results indicate that the thermal radiation from the w ater-bearing soil surface is almost unpolarized,and the polarization characteristic of the soil surface is mainly caused by the reflection of solar light.Especially in the strong sunshine spectral range,the degree of polarization increases monotonically w ith the increase of soil moisture.This quantitative relationship provides basis for soil moisture monitoring by the remote sensing of the polarization of light in the mid-w ave infrared range.
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CiteScore
1.20
自引率
14.30%
发文量
4258
审稿时长
2.9 months
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