CN112378864A - Airborne hyperspectral soil information retrieval method - Google Patents

Airborne hyperspectral soil information retrieval method Download PDF

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CN112378864A
CN112378864A CN202011165167.5A CN202011165167A CN112378864A CN 112378864 A CN112378864 A CN 112378864A CN 202011165167 A CN202011165167 A CN 202011165167A CN 112378864 A CN112378864 A CN 112378864A
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soil
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秦凯
赵宁博
杨越超
李明
朱玲
崔鑫
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Beijing Research Institute of Uranium Geology
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Abstract

The invention belongs to the technical field of geological exploration, and particularly relates to an airborne hyperspectral soil information retrieval method, which comprises the following steps: (1) carrying out geometric correction, radiation correction and atmospheric correction on the airborne spectrum original data to generate airborne hyperspectral reflectivity image data; (2) generating a soil sampling point image spectrum library on the airborne hyperspectral reflectivity image data; (3) screening out an image spectrum set which is closest to a ground measurement spectrum of the sampling point from a soil sampling point image spectrum library; (4) constructing a hyperspectral loam localization information matrix, and calculating a soil information regression equation; (5) carrying out spectrum angle classification on the airborne high spectral reflectivity image data by adopting the screened soil sampling point image spectrum set; generating masked image reflectance data; (6) and calculating the image reflectivity data after the mask according to a regression equation of the soil information to obtain a soil information inversion result.

Description

Airborne hyperspectral soil information retrieval method
Technical Field
The invention belongs to the technical field of geological exploration, and particularly relates to an airborne hyperspectral soil information retrieval method.
Background
A large amount of hyperspectral data has become available for observing earth systems from multi-platform sensors, ranging from ground spectrometers on the earth, unmanned aerial vehicle hyperspectral measurement systems to aerial and satellite remote sensing systems on the earth, ranging from a few meters to a few hundred meters. The airborne hyperspectral data are important data sources, and the regional soil geochemical mapping performed by the airborne hyperspectral data has important research significance on soil investigation, soil texture analysis and agriculture. Due to the fact that the scale of the current airborne hyperspectral data is inconsistent with the scale of the ground measured spectrum data and the influence of interference factors such as moisture, atmosphere and the like, the hyperspectral geochemistry mapping accuracy of the regional scale is not high.
Therefore, an airborne hyperspectral soil information inversion method needs to be designed for research, and a hyperspectral soil information quantitative analysis model is realized.
Disclosure of Invention
Aiming at the defects of the prior art, the invention provides an airborne hyperspectral soil information retrieval method, which is used for solving the technical problem that the hyperspectral geochemistry mapping precision of the regional scale is not high due to the inconsistent scale of airborne hyperspectral data and ground measured spectrum data and the influence of interference factors such as moisture, atmosphere and the like in the prior art.
The technical scheme of the invention is as follows:
an airborne hyperspectral soil information retrieval method comprises the following steps:
the method comprises the following steps: geometric correction, radiation correction and atmospheric correction are carried out on the airborne spectrum original data, water vapor absorption wave bands are removed, all the aerial bands are inlaid, and airborne hyperspectral reflectivity image data are generated;
step two: collecting an average reflectivity spectrum of an image area in a certain range on airborne high-spectral reflectivity image data by taking the coordinates of each soil ground sampling point as a center, and generating a soil sampling point image spectrum library according to the serial number sequence of the ground sampling points;
step three: performing cluster analysis on the soil sampling point image spectrum library in the second step, and screening out an image spectrum set closest to the ground measurement spectrum of the sampling point;
step four: constructing a hyperspectral loam information matrix by the soil sampling point spectrum set and the geochemical analysis results of corresponding sampling points, and calculating a regression equation of soil information by adopting a partial least square method;
step five: carrying out spectrum angle classification on the airborne high spectral reflectivity image data obtained in the first step by adopting the soil sampling point image spectrum set screened out in the third step; according to the classification result, only image pixels representing soil in the image are reserved by using a masking method, and masked image reflectivity data are generated;
step six: and calculating the image reflectivity data after the mask according to the regression equation of the soil information in the step four to obtain the soil information inversion result.
In the second step, the average reflectivity spectrum of the image area in a certain range is collected, and the collection method comprises the following steps: selecting M x M as the number of pixels of the collected image, wherein the initial values of M are respectively 3, 5, 7 and 9; and respectively calculating the spectrum angle errors of the image area average reflectivity spectrum with different M values and the corresponding point ground measurement spectrum, and selecting the average reflectivity spectrum with the minimum spectrum angle error.
The third step further comprises the following substeps:
step 3.1: setting a soil sampling point image spectrum set number K;
step 3.2: randomly selecting k image spectrums from a soil sampling point image spectrum library as a mass center;
step 3.3: calculating the distance between each image spectrum in the image spectrum library and each centroid, and taking the distance between each image spectrum and each centroid as a division principle, namely: when the image spectrum is close to a certain centroid, the set to which the centroid belongs is divided;
step 3.4: after all image spectrums are grouped into sets, k sets exist in total; then re-computing the centroid of each set;
step 3.5: if the distance between the newly calculated centroid and the original centroid is smaller than a certain set threshold value, clustering reaches an expected result, and the algorithm is terminated; otherwise, repeating the step 3.3-3.5;
step 3.6: and carrying out spectrum angle operation on the centroid of each set and the ground measurement spectrum of the sampling point, wherein the image spectrum set with the minimum centroid of the spectrum angle is the soil sampling point spectrum set.
In the step 3.3: for each image spectrum in the image spectrum library, calculating the distance between each image spectrum and each centroid, wherein the formula for calculating the distance is shown as the following formula (1):
Figure BDA0002745546070000031
wherein, ciAs a set of image spectra (c)1,c2,...,ck) (ii) a x is the reflectance value of the image spectrum; implicit layer features, K is the number of sets of clusters; mu.siThe centroid spectral reflectance for the ith set.
In step 3.4, the centroid of each set is recalculated, and the formula is calculated, as shown in the following formula (2):
Figure BDA0002745546070000032
wherein, ciAs a set of image spectra (c)1,c2,...,ck): x is the reflectance value of the image spectrum; mu.siThe centroid spectral reflectance for the ith set.
The invention has the beneficial effects that:
according to the airborne hyperspectral soil information retrieval method, a great deal of experimental research is carried out on nutrient elements (nitrogen, phosphorus and potassium) and heavy metal elements (copper, lead, zinc, chromium and the like) of soil and beneficial elements (selenium), the distribution and the content of the elements can be effectively extracted, the applicability is strong, and the method has reference significance for quantitative analysis work of other elements.
Detailed Description
The airborne hyperspectral soil information inversion method designed by the invention is further described by combining the specific embodiment and the technical scheme, and comprises the following steps:
the method comprises the following steps: acquiring airborne spectrum original data of a research area, performing geometric correction, radiation correction and atmospheric correction on the airborne spectrum original data, removing water vapor absorption wave bands, completing embedding of all air bands, and generating airborne hyperspectral reflectivity image data;
step two: collecting an average reflectivity spectrum of an image area in a certain range on airborne high-spectral reflectivity image data by taking the coordinates of each soil ground sampling point as a center, and generating a soil sampling point image spectrum library according to the serial number sequence of the ground sampling points;
in the second step, the average reflectivity spectrum of the image area in a certain range is collected, and the collection method comprises the following steps: selecting M x M as the number of pixels of the collected image, wherein the initial values of M are respectively 3, 5, 7 and 9; and respectively calculating the spectrum angle errors of the image area average reflectivity spectrum with different M values and the corresponding point ground measurement spectrum, and selecting the average reflectivity spectrum with the minimum spectrum angle error.
Step three: performing cluster analysis on the soil sampling point image spectrum library in the second step, and screening out an image spectrum set closest to the ground measurement spectrum of the sampling point;
the third step further comprises the following substeps:
step 3.1: setting a soil sampling point image spectrum set number K;
step 3.2: randomly selecting k image spectrums from a soil sampling point image spectrum library as a mass center;
step 3.3: calculating the distance between each image spectrum in the image spectrum library and each centroid, and taking the distance between each image spectrum and each centroid as a division principle, namely: when the image spectrum is close to a certain centroid, the set to which the centroid belongs is divided;
in the step 3.3: for each image spectrum in the image spectrum library, calculating the distance between each image spectrum and each centroid according to the following formula (1):
Figure BDA0002745546070000041
wherein, ciAs a set of image spectra (c)1,c2,...,ck) (ii) a x is the reflectance value of the image spectrum; implicit layer features, K is the number of sets of clusters; mu.siThe centroid spectral reflectance for the ith set.
Step 3.4: after all image spectrums are grouped into sets, k sets exist in total; then, the centroid of each set is recalculated, and the calculation formula is as shown in the following formula (2):
Figure BDA0002745546070000051
wherein, ciAs a set of image spectra (c)1,c2,...,ck) (ii) a x is the reflectance value of the image spectrum; mu.siThe centroid spectral reflectance for the ith set.
Step 3.5: if the distance between the newly calculated centroid and the original centroid is smaller than a certain set threshold value, clustering reaches an expected result, and the algorithm is terminated; otherwise, repeating the step 3.3-3.5;
step 3.6: and carrying out spectrum angle operation on the centroid of each set and the ground measurement spectrum of the sampling point, wherein the image spectrum set with the minimum centroid of the spectrum angle is the soil sampling point spectrum set.
Step four: constructing a hyperspectral loam information matrix by the soil sampling point spectrum set and the geochemical analysis results of corresponding sampling points, and calculating a regression equation of soil information by adopting a partial least square method;
step five: carrying out spectrum angle classification on the airborne high spectral reflectivity image data of the research area in the first step by adopting the soil sampling point image spectrum set screened out in the third step; according to the classification result, only image pixels representing soil in the image are reserved by using a masking method, and masked image reflectivity data are generated;
step six: and according to the regression equation of partial least square calculation of the soil information, calculating the image reflectivity data after the mask according to the regression equation of the soil information in the step four, and obtaining the soil information inversion result.
The specific embodiment example:
according to the method, the airborne hyperspectral data SASI is selected to perform content inversion on the total nitrogen of the soil, and other elements can refer to the method.
(1) And selecting a Qixing agricultural field area of black soil of Sanjiang in northeast China for testing, acquiring airborne SASI (geosynthetic inertial navigation System) hyperspectral data of the bare soil, and performing geometric correction, radiation correction and atmospheric correction on the data. The water vapor absorption wave band is removed, the reflectivity image data of the research area is generated, the area is 1500 square kilometers, the spectral interval is 950nm-2450nm, and the total number of 85 effective wave bands are obtained. The spatial resolution is 2.5 m.
(2) The coordinates of the 200 sample points on the surface and the geochemical analysis data are collected. Collecting an average reflectivity spectrum of a 3 x 3 image area on airborne SASI (sampled satellite System) hyperspectral reflectivity image data by taking the coordinates of each soil ground sampling point as a center, and generating a soil sampling point image spectrum library according to the numbering sequence of the ground sampling points;
(3) performing cluster analysis on the soil sampling point image spectrum library, and screening out an image spectrum set closest to a ground measurement spectrum of the sampling point: firstly, setting a soil sampling point image spectrum set number 3; secondly, randomly selecting 3 image spectrums from a soil sampling point image spectrum library as a mass center; then calculating the distance between each image spectrum in the image spectrum library and each centroid, dividing 3 image spectrum sets, and then recalculating the centroid of each set; and finally, setting the maximum iteration frequency to be 50 times, carrying out spectrum angle operation on the mass center of each set and the ground measurement spectrum of the sampling point, and selecting the image spectrum set with the minimum mass center of the spectrum angle as the soil sampling point spectrum set, wherein the number of the sampling points of the set is 163.
(4) Constructing a hyperspectral soil geology information matrix by using the selected soil sampling point spectrum set and the geochemical analysis results of the corresponding sampling points, and calculating a regression equation of soil total nitrogen by adopting a partial least square method:
Y=7.86534*X1-7.645558*X2-10.13127*X3+40.17681*X4-0.02235985*X5-31.57936*X6-4.228151*X7+2.09692
wherein Y is the total nitrogen content; x1Image reflectance value at a center wavelength of 1332.5 nm; x2An image reflectance value of center wavelength 1512.5 nm; x3Image reflectance value at a center wavelength of 1662.5 nm; x4An image reflectance value of center wavelength 1722.5 nm; x5An image reflectance value of center wavelength 2067.5 nm; x4An image reflectance value of center wavelength 2217.5 nm; x4The image reflectance value is at a center wavelength of 2307.5 nm.
(5) And (4) adopting the screened soil sampling point image spectrum set as a sample, and carrying out spectrum angle classification on the airborne high-spectrum reflectivity image data of the research area. And according to the classification result, only image pixels representing soil in the image are reserved by using a masking method, and the masked image reflectivity data is generated.
(6) And (4) according to the regression equation calculated by partial least squares of total nitrogen calculated in the step (4), performing band operation on the masked image reflectivity data to obtain the soil total nitrogen content inversion result.
While the embodiments of the present invention have been described in detail, the present invention is not limited to the above-described examples, and various changes can be made without departing from the spirit of the present invention within the knowledge of those skilled in the art.

Claims (5)

1. An airborne hyperspectral soil information retrieval method is characterized by comprising the following steps: the method comprises the following steps:
the method comprises the following steps: geometric correction, radiation correction and atmospheric correction are carried out on the airborne spectrum original data, water vapor absorption wave bands are removed, all the aerial bands are inlaid, and airborne hyperspectral reflectivity image data are generated;
step two: collecting an average reflectivity spectrum of an image area in a certain range on airborne high-spectral reflectivity image data by taking the coordinates of each soil ground sampling point as a center, and generating a soil sampling point image spectrum library according to the serial number sequence of the ground sampling points;
step three: performing cluster analysis on the soil sampling point image spectrum library in the second step, and screening out an image spectrum set closest to the ground measurement spectrum of the sampling point;
step four: constructing a hyperspectral loam information matrix by the soil sampling point spectrum set and the geochemical analysis results of corresponding sampling points, and calculating a regression equation of soil information by adopting a partial least square method;
step five: carrying out spectrum angle classification on the airborne high spectral reflectivity image data obtained in the first step by adopting the soil sampling point image spectrum set screened out in the third step; according to the classification result, only image pixels representing soil in the image are reserved by using a masking method, and masked image reflectivity data are generated;
step six: and calculating the image reflectivity data after the mask according to the regression equation of the soil information in the step four to obtain the soil information inversion result.
2. The airborne hyperspectral soil information inversion method according to claim 1, characterized by comprising the following steps: in the second step, the average reflectivity spectrum of the image area in a certain range is collected, and the collection method comprises the following steps: selecting M x M as the number of pixels of the collected image, wherein the initial values of M are respectively 3, 5, 7 and 9; and respectively calculating the spectrum angle errors of the image area average reflectivity spectrum with different M values and the corresponding point ground measurement spectrum, and selecting the average reflectivity spectrum with the minimum spectrum angle error.
3. The airborne hyperspectral soil information inversion method according to claim 1, characterized by comprising the following steps: the third step further comprises the following substeps:
step 3.1: setting a soil sampling point image spectrum set number K;
step 3.2: randomly selecting k image spectrums from a soil sampling point image spectrum library as a mass center;
step 3.3: calculating the distance between each image spectrum in the image spectrum library and each centroid, and taking the distance between each image spectrum and each centroid as a division principle, namely: when the image spectrum is close to a certain centroid, the set to which the centroid belongs is divided;
step 3.4: after all image spectrums are grouped into sets, k sets exist in total; then re-computing the centroid of each set;
step 3.5: if the distance between the newly calculated centroid and the original centroid is smaller than a certain set threshold value, clustering reaches an expected result, and the algorithm is terminated; otherwise, repeating the step 3.3-3.5;
step 3.6: and carrying out spectrum angle operation on the centroid of each set and the ground measurement spectrum of the sampling point, wherein the image spectrum set with the minimum centroid of the spectrum angle is the soil sampling point spectrum set.
4. The airborne hyperspectral soil information inversion method according to claim 3, characterized by comprising the following steps: in the step 3.3: for each image spectrum in the image spectrum library, calculating the distance between each image spectrum and each centroid, wherein the formula for calculating the distance is shown as the following formula (1):
Figure FDA0002745546060000021
wherein, ciAs a set of image spectra (c)1,c2,...,ck) (ii) a x is the reflectance value of the image spectrum; implicit layer features, K is the number of sets of clusters; mu.siThe centroid spectral reflectance for the ith set.
5. The airborne hyperspectral soil information inversion method according to claim 4, characterized by comprising the following steps: in said step 3.4, the centroid of each set is recalculated, and the formula is calculated, as shown in the following formula (2):
Figure FDA0002745546060000031
wherein, ciAs a set of image spectra (c)1,c2,...,ck) (ii) a x is the reflectance value of the image spectrum; mu.siThe centroid spectral reflectance for the ith set.
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