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林业科学 ›› 2011, Vol. 47 ›› Issue (6): 9-16.doi: 10.11707/j.1001-7488.20110602

• 论文 • 上一篇    下一篇

荒漠化土地土壤有机质含量的实测光谱估测

高志海1, 白黎娜1, 王琫瑜1, 李增元1, 李晓松2, 王玉魁3,4   

  1. 1. 中国林业科学研究院资源信息研究所 国家林业局林业遥感与信息技术重点实验室 北京 100091;2. 中国科学院遥感应用研究所 北京 100101;3. 北京林业大学水土保持学院 北京 100083;4. 国家林业局泡桐研究开发中心 郑州 450003
  • 收稿日期:2009-12-16 修回日期:2011-04-26 出版日期:2011-06-25 发布日期:2011-06-25
  • 通讯作者: 王玉魁

Estimation of Soil Organic Matter Content in Desertified Lands Using Measured Soil Spectral Data

Gao Zhihai1, Bai Lina1, Wang Bengyu1, Li Zengyuan1, Li Xiaosong2, Wang Yukui3,4   

  1. 1. Key Laboratory of Forestry Remote Sensing and Information Techniques of State Forestry Administration Institute of Forest Resource Information Techniques, Chinese Academy of Forestry Beijing 100091;2. Institute of Remote Sensing Applications, Chinese Academy of Sciences Beijing 100101;3. Water & Soil Conservation College, Beijing Forestry University Beijing 100083;4. Paulownia Research and Development Center of State Forestry Administration Zhengzhou 450003
  • Received:2009-12-16 Revised:2011-04-26 Online:2011-06-25 Published:2011-06-25

摘要:

在对2个荒漠化典型区土壤采样、化验分析和光谱测量的基础上,分析荒漠化土地土壤的反射光谱特征及土壤有机质的光谱敏感范围,构建多种土壤有机质含量高光谱估测模型。结果表明: 荒漠化土地土壤具独特的波浪型光谱曲线,其主要特点是在可见光和近红外的500~900 nm光谱范围存在一个明显的弓形突起区,其对提取土壤有机质信息有实际意义; 相关分析发现,在中心波长分别为600和830 nm的可见光和近红外光光谱范围分别存在1个有机质光谱敏感区; 土壤有机质含量高光谱估测模型验证结果表明,利用波长588 nm处的反射光谱对数lgR588和反射光谱倒数1/R588以及波长835 nm处的反射光谱倒数的导数(1/R835)'和反射光谱对数的导数(lgR835)'分别建立的模型,可以较好地估测荒漠化土地土壤有机质含量。

关键词: 荒漠化土地, 土壤有机质, 土壤光谱, 估测模型

Abstract:

The topsoil spectral characteristics and spectral segments sensitivity to soil organic matter (SOM) were studied on the basis of laboratory analysis and spectral measurement of soil samples collected from 2 typical areas of desertification, and then models for estimating SOM of topsoil layer were established. The results showed that the soils of desertified lands had the unique wave-shaped spectral curves, with an obvious bow-shaped protuberance area in 500-900 nm wavelength range, which could be used to extract SOM information from soil spectrum. It was found by the correlation analysis that there were two spectral segments sensitive to SOM, centered at 600 and 830 nm wavelengths respectively. The result of model validation indicated that the models, taking the logarithm reflectance and reciprocal reflectance at 588 nm (lgR588, 1/R588) and the first derivative reflectance of reciprocal reflectance and logarithm reflectance at 835 nm (1/R835)', (lgR835)' as independent variable respectively, could be used to accurately estimate the SOM content in desertified lands.

Key words: desertified lands, soil organic matter, soil spectrum, estimate model

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