2013
DOI: 10.1007/s12517-013-1015-1
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A study on the hyperspectral signatures of sandy soils with varying texture and water content

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Cited by 11 publications
(3 citation statements)
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“…According to Lambert’s absorption law, the spectral properties vary with the composition or structure of the material, and the spectra from different groups vary in regard to the position and intensity of the absorption peaks [ 36 ]. It is also affected by the nonuniform distribution of soil surface texture, density, and internal composition, making it difficult to eliminate all redundant information, such as overlap, from the spectral data [ 37 , 38 , 39 ]. Thus, to reduce spectral noise, baseline drift, and interference from other backgrounds, as well as to distinguish overlapping peaks for the purpose of qualitative or quantitative analysis of complex mixtures, five different preprocessing methods were used in this study to analyze the spectral information [ 40 ].…”
Section: Methodsmentioning
confidence: 99%
“…According to Lambert’s absorption law, the spectral properties vary with the composition or structure of the material, and the spectra from different groups vary in regard to the position and intensity of the absorption peaks [ 36 ]. It is also affected by the nonuniform distribution of soil surface texture, density, and internal composition, making it difficult to eliminate all redundant information, such as overlap, from the spectral data [ 37 , 38 , 39 ]. Thus, to reduce spectral noise, baseline drift, and interference from other backgrounds, as well as to distinguish overlapping peaks for the purpose of qualitative or quantitative analysis of complex mixtures, five different preprocessing methods were used in this study to analyze the spectral information [ 40 ].…”
Section: Methodsmentioning
confidence: 99%
“…With the extensive application of spectral technology in the detection of soil nutrient content, there has been a significant improvement made to the level of automation and efficiency for soil dynamic monitoring, which enables the real-time variable rate fertilization. In practice, however, soil spectral signal can be affected by a range of external environmental parameters, such as soil moisture content [12], soil salt content [13], soil particle size [14], soil texture [15], and outdoor temperature, and especially soil moisture content. It was revealed by a study that soil hyperspectral detection can be severely disrupted by soil moisture content in the water absorption bands (1400, 1900, and 2200 nm) [16], thus resulting in a poor applicability of the prediction model [17].…”
Section: Introductionmentioning
confidence: 99%
“…With the rise of remote sensing technology, the application of hyperspectral remote sensing techniques to monitor soil salinity not only saves time and effort, but also exhibits the characteristics of rapid deployment, macroscopic and dynamic features, and a superior performance that cannot be achieved by other means. In recent years, numerous scholars have studied soil salinity estimation for different soil types based on visible-near-infrared (NIR) spectroscopy [13][14][15][16][17][18][19][20][21]. The background, environment, measuring instruments, etc.…”
Section: Introductionmentioning
confidence: 99%