Simulating models for Phaeozem hyperspectral reflectance

It is difficult to analyse soil properties quantitatively with multispectral remote sensing data. An alternative solution is to determine the main spectral characteristic control points of soil hyperspectral reflectance curves by sensitivity analysis methods. Hyperspectral reflectance is simulated u...

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Published inInternational journal of remote sensing Vol. 32; no. 13; pp. 3819 - 3834
Main Authors Liu, Huanjun, Zhang, Xinle, Yu, Wantai, Zhang, Bai, Song, Kaishan, Blackwell, J
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LanguageEnglish
Published Abingdon Taylor & Francis 01.01.2011
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Abstract It is difficult to analyse soil properties quantitatively with multispectral remote sensing data. An alternative solution is to determine the main spectral characteristic control points of soil hyperspectral reflectance curves by sensitivity analysis methods. Hyperspectral reflectance is simulated using the control points based on multispectral reflectance collected from satellites in this study. The laboratory hyperspectral reflectance and its continuum-removed curve of Phaeozem and the parent material (PM) of samples collected from Heilongjiang Province, China were analysed, and the spectral characteristic control points determined. Hyperspectral simulating linear and quadratic models based on laboratory reflectance were then built. Results show that montmorillonite and illite are the dominant minerals in Phaeozem PM. Organic matter content determines the spectral characteristics of Phaeozem and makes it suitable for reflectance simulation in the spectrum range of 1000 nm and less; the higher the organic matter content the greater the spectral absorption area. There are two absorption valleys at 500 and 660 nm, which determine the spectral characteristic control points of Phaeozem between 450 and 930 nm, namely 450, 500, 590, 660 and 930 nm. Both the linear and quadratic simulation models built with the characteristic control points accurately describe Phaeozem reflectance, which proves that the characteristic control points are selected reasonably and representatively. The hyperspectral simulation method based on multispectral reflectance closely represents the characteristics of Phaeozem hyperspectral reflectance, partly removes noise and improves the precision of predicting organic matter content. Therefore the method is feasible and useful for data compression of Phaeozem hyperspectral reflectance, soil and vegetation indices building, and quantitative remote sensing in the Phaeozem Zone, northeast China.
AbstractList It is difficult to analyse soil properties quantitatively with multispectral remote sensing data. An alternative solution is to determine the main spectral characteristic control points of soil hyperspectral reflectance curves by sensitivity analysis methods. Hyperspectral reflectance is simulated using the control points based on multispectral reflectance collected from satellites in this study. The laboratory hyperspectral reflectance and its continuum-removed curve of Phaeozem and the parent material (PM) of samples collected from Heilongjiang Province, China were analysed, and the spectral characteristic control points determined. Hyperspectral simulating linear and quadratic models based on laboratory reflectance were then built. Results show that montmorillonite and illite are the dominant minerals in Phaeozem PM. Organic matter content determines the spectral characteristics of Phaeozem and makes it suitable for reflectance simulation in the spectrum range of 1000 nm and less; the higher the organic matter content the greater the spectral absorption area. There are two absorption valleys at 500 and 660 nm, which determine the spectral characteristic control points of Phaeozem between 450 and 930 nm, namely 450, 500, 590, 660 and 930 nm. Both the linear and quadratic simulation models built with the characteristic control points accurately describe Phaeozem reflectance, which proves that the characteristic control points are selected reasonably and representatively. The hyperspectral simulation method based on multispectral reflectance closely represents the characteristics of Phaeozem hyperspectral reflectance, partly removes noise and improves the precision of predicting organic matter content. Therefore the method is feasible and useful for data compression of Phaeozem hyperspectral reflectance, soil and vegetation indices building, and quantitative remote sensing in the Phaeozem Zone, northeast China.
Author Liu, Huanjun
Yu, Wantai
Blackwell, J
Zhang, Xinle
Song, Kaishan
Zhang, Bai
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CitedBy_id crossref_primary_10_1016_j_geoderma_2019_113896
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crossref_primary_10_3390_agriculture14060873
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Issue 13
Keywords data
sensitivity analysis
Parent
simulation
multispectral remote sensing
Laboratory
Phaeozems
Modeling
Spectral data
Continuum
solution
Simulation model
soils
satellites
Laboratory study
Multispectral detection
Property of soil
Curve
samples
Analysis method
materials
Hyperspectral characteristic
Control point
Reflectance
Northeast
Language English
License CC BY 4.0
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Snippet It is difficult to analyse soil properties quantitatively with multispectral remote sensing data. An alternative solution is to determine the main spectral...
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SubjectTerms absorption
Animal, plant and microbial ecology
Applied geophysics
Biological and medical sciences
China
Computer simulation
Earth sciences
Earth, ocean, space
Exact sciences and technology
Fundamental and applied biological sciences. Psychology
General aspects. Techniques
illite
Internal geophysics
Mathematical models
organic matter
Reflectance
Reflectivity
Remote sensing
satellites
simulation models
Soil (material)
soil properties
Spectra
spectral analysis
Teledetection and vegetation maps
vegetation
Title Simulating models for Phaeozem hyperspectral reflectance
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