CN1595109A - High spectrum minerals maximum correlation identification method based on spectrum hybrid composition - Google Patents
High spectrum minerals maximum correlation identification method based on spectrum hybrid composition Download PDFInfo
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Abstract
It is a highlight spectrum mineral maximum relative identification method based on the light spectrum mixture which comprises the following steps: to get the highlight spectrum image data of certain area; to choose possible distribution mineral spectrum in the area in the spectrum base as reference light spectrum; to calculate the correlation coefficient between each image element and selected mineral spectrum in the spectrum base; to identify one maximum or multiple picture elements with the selected mineral light spectrum in the base; to judge whether there exists the selected mineral in one or multiple picture elements or whether the mineral is in dominancy. It uses the common factors and fundamental relationship between the mixture and single mineral spectrum and calculates the Spearmam R or Kendall tau correlation coefficients with no consideration of the variable order and then identifies whether the area exists certain mineral or whether it is in dominancy.
Description
Technical field
The present invention relates to a kind of method of discerning mineral, specifically, relate to a kind of high spectrum mineral that mixing is formed based on spectrum and utilize its related coefficient, the method for identification mineral.
Background technology
Mineral species identification is one of high spectral technique the most successful field of using.The single diagnostic absorption of rock forming mineral feature can be utilized absorption bands position (λ), the absorption degree of depth (H), absorption width (W), absorption area (A), absorb intactly sign of symmetry (d), the number (n) that absorbs and parameters sortnig work one.Single diagnostic according to the end member mineral absorbs waveform, extracts from high-spectral data and strengthens these parameter informations, can be directly used in identification rock ore deposit type.High spectrum characteristics is the spectral band that is to utilize limited segmentation, remove to reproduce the wave spectrum curve of pixel homologue, thereby utilize video wave spectrum and mineral reference spectra to mate the identification mineral, can improve the uncertainty influence (as spectral drift, variation etc.) of single waveform so to a certain extent, improve the precision of identification.By radiation transfer theory, can set up the physical spectrum model according to the difference of different atural objects or the response of different pixel spectral reflectivity and carry out mineral species identification.Utilize model not only can carry out the identification of atural object, also can quantize material simultaneously and form, but comparatively harsh to the requirement of parameter.
For the distribution of face of land atural object or for the atural object of present pixel scale size, it is non-existent that pure relatively end member is formed, form but organically combine, to make the spectrum signature of atural object combine the spectral effects of different component and more complicated and changeable by the end member composition that difference has an inner link.Above-mentioned carries out Spectral matching and decomposition algorithm based on the overall optical spectrum signature, as spectrum angle technology, linear hybrid spectral resolution etc., has certain effect under certain condition.But aborning, pure pixel does not exist substantially, and uncertain factor is more in coupling and the decomposition.Simultaneously because the influence of the variation of actual object spectrum, the noise that obtains data, rebuilding spectrum error, accurate matching ratio difficulty causes identification of rock ore deposit and obscuring and error analytically.
Nature mixed spectra feature complexity.But, for any mixing, often occupy the but main status of tool in the reflection of its attribute of the composition of leading position or end member, especially some evident characteristic are formed or end member has more advantage.
Summary of the invention
Purpose of the present invention is exactly the identification problem that solves mixed pixel in the reality, according to the factor analysis principle in the statistics, from the discussion of the relation of personality and common, analyze and mix the different correlativitys of forming end members and potpourri, reach occuping the identification of dominance atural object in the atural object especially potpourri.
Can be understood as the two for mixed spectra and simple ore thing spectrum is that two groups of discrete data organically constitute respectively, relation between the two data also may exist potential causality (Causality) and rank character (Hierarchy) except relation mathematics, the surface; No matter be that causality or rank character can be by exploring the analysis that concerns between these two groups of discrete datas, seek common factor potential between rock/aggregate (mixing) and the simple ore thing and essential getting in touch, and reach extraction monomineralic identification and information.
The very big relative identifying method of mineral of the present invention comprises the steps:
(1) obtains the high spectrum image data in somewhere;
(2) the mineral spectrum that selection and this zone may distribute in library of spectra is as reference spectrum;
(3) calculate each pixel spectrum and in library of spectra the related coefficient between the reference spectra of selected mineral;
(4) determine with library of spectra in one or more pixel of related coefficient maximum of selected mineral spectrum;
(5) judge whether exist selected mineral or this selected mineral to occupy the dominance status in this one or more pixel;
(6) utilize different color ranges to represent the relative trend that mineral distribute.
The very big relative identifying method of mineral of the present invention, wherein utilize following formula in step (3):
R
Xi, R
YiBe respectively the order of set of variables X and Y, R
x, R
yBe respectively the equal order of X and Y; X and Y are respectively reference spectra and pixel spectrum; Calculate Spearman (Spearman R) related coefficient.
The very big relative identifying method of mineral of the present invention, wherein in step (3), utilize formula:
P is the X pairing sum consistent with Y, and Q is the inconsistent pairing sum of X and Y; Tx is and variable X matched group equal numbers that Ty is and variable Y matched group equal numbers; X and Y are respectively reference spectra and pixel spectrum;
Calculate Ken Deer (Kendall tau) coefficient.
The invention has the advantages that and utilize common factor and essential connection potential between potpourri and the monomineralic spectrum, under the condition of the association of not considering to sort between the variable, by calculating Spearman (Spearman R) or Ken Deer (Kendall tau) related coefficient, thereby determine whether selected area exists certain mineral or this mineral whether to occupy the dominance status.
Other details of the very big relative identifying method of mix forming based on spectrum of high spectrum mineral and characteristics can be cheer and bright by reading the embodiment that hereinafter encyclopaedizes in conjunction with the accompanying drawings.
Description of drawings
Fig. 1 the present invention is based on mix to form, by calculating the relevant identification figure of the talcum that Spearman (Spearman R) and Ken Deer (Kendall tau) related coefficient obtain;
Fig. 2 the present invention is based on to mix composition, by calculating the kaolinic relevant identification figure that Spearman (Spearman R) and Ken Deer (Kendall tau) related coefficient obtain;
Fig. 3 the present invention is based on mix to form, by calculating the relevant identification figure of the white mica that Spearman (Spearman R) and Ken Deer (Kendall tau) related coefficient obtain;
Fig. 4 the present invention is based on mix to form, by calculating the relevant identification figure of the kalzit that Spearman (Spearman R) and Ken Deer (Kendall tau) related coefficient obtain;
Fig. 5 the present invention is based on mix to form, by calculating the relevant identification figure of the chlorite that Spearman (Spearman R) and Ken Deer (Kendall tau) related coefficient obtain;
Fig. 6 the present invention is based on to mix composition, by calculating the epidotic relevant identification figure that Spearman (Spearman R) and Ken Deer (Kendall tau) related coefficient obtain;
Fig. 7 is the image wave spectrum of the talcum according to the present invention and the check analysis of standard spectrum;
Fig. 8 is the check analysis of kaolinic image wave spectrum and standard spectrum according to the present invention;
Fig. 9 is the image wave spectrum of the white mica according to the present invention and the check analysis of standard spectrum;
Figure 10 is the image wave spectrum of the kalzit according to the present invention and the check analysis of standard spectrum;
Figure 11 is the image wave spectrum of the chlorite according to the present invention and the check analysis of standard spectrum;
Figure 12 is the check analysis of epidotic image wave spectrum and standard spectrum according to the present invention.
Embodiment
As mentioned above, can be understood as the two for mixed spectra and simple ore thing spectrum is that two groups of discrete data organically constitute respectively, relation between the two data also may exist potential causality (Causality) and rank character (Hierarchy) except relation mathematics, the surface; No matter be that causality or rank character can be by exploring the analysis that concerns between these two groups of discrete datas, seek common factor potential between rock/aggregate (mixing) and the simple ore thing and essential getting in touch, and reach extraction monomineralic identification and information.The present invention has adopted Spearman (Spearman R) and Ken Deer (Kendall tau), and the said two devices relation is inquired into.
Because, Spearman R becomes normal distribution with the variable that Kendall tau coefficient does not need to be studied, so this just in time satisfies the non-normality of spectroscopic data, the related coefficient of calculating theoretically and actual angle of mixing the distribution trend of leading atural object attribute in the potpourri is described better.Learn in the application on the ground of reality, often do not need to provide especially the residing particular location of end member, but identify the basic trend of its distribution, can be familiar with end member like this at the occurrence status in space with understand physics and the chemical action process of end member mineral, obtain the information of learning accordingly in the space quantitative change.
Under the condition of the association of not considering to sort between the variable, Spearman R related coefficient illustrates related degree with variance explanation ratio.In the wave spectrum of rock ore deposit, its data constitute the description to rock ore deposit spectral properties in proper order.In Spearman R hypothesis, the variable of being studied has performance (the Siegel andCastellan of ordering; 1988).Therefore, rock/mixing and mineral/end member can constitute two orderly series and study.To carrying out correlation analysis and conspicuousness test of hypothesis between ordered data, thereby reach approval to the two common factor, with the degree size of this approval perception as the foundation that end member is cut apart.Satisfying under the condition of conspicuousness hypothesis, the high correlativity that heals (approval perception degree) embodies the two common feature the more, and potpourri is that the degree of the reference end member that relied on is bigger, thereby is partitioned into pure end member according to certain principle.The down comprehensive of natural cause and in the pixel yardstick (several meters to tens meters) that remote sensing is at present studied, nature is difficult to exist purer end member.Can think that when the common paricular value that the two acquires a certain degree this mixed pixel has the end member of maximum correlation for the two.Really, may not be a kind of in this mixed pixel for the end member of identification, but the end member material of being discerned is at least formed and have been dominated this mixed pixel spectral signature.
Method of the present invention comprises the steps:
(1) obtains the high spectrum image data in somewhere;
(2) the mineral spectrum that selection and this zone may distribute in library of spectra is as reference spectrum;
(3) calculate each pixel and in library of spectra the related coefficient between the selected mineral spectrum;
(4) determine with library of spectra in one or more pixel of related coefficient maximum of selected mineral spectrum;
(5) judge whether exist selected mineral or this selected mineral to occupy the dominance status in this one or more pixel.
The very big relative identifying method of mineral of the present invention, wherein utilize following formula in step (3):
R
Xi, R
YiBe respectively the order of set of variables X and Y, R
x, R
yBe respectively the equal order of X and Y; X and Y are respectively reference spectra and pixel spectrum; Calculate Spearman (Spearman R) related coefficient.
The very big relative identifying method of mineral of the present invention, wherein in step (3), utilize formula:
P is the X pairing sum consistent with Y, and Q is the inconsistent pairing sum of X and Y; Tx is and variable X matched group equal numbers that Ty is and variable Y matched group equal numbers; X and Y are respectively reference spectra and pixel spectrum;
Calculate Ken Deer (Kendall tau) coefficient.
Wherein, Kendall tau is the same with Spearman R in itself.From the statistics angle both be equal.But the equation difference of logic that is constituted and calculating.What is more important, Kendall tau has different explanations with Spearman R intension: Spearman R can think the to sort common Pearson time effect related coefficient of variable; And Kendall tau is a probability, is that two variable real data are in the probability of same sequence and other is comprehensive with the probability difference that is in different order.Therefore Spearman R and Kendall tau numerical values recited are inconsistent.The numerical relation of the two is expressed (Siegel and Castellan with available as lower inequality; 1988):
-1≤3×Kendall?tau-2×Spearman?R≤1
Seek to mix and end member spectrum between inner link the time, not only the contact of same sequence is important between data, the difference of order is also extremely important between data simultaneously.
Accompanying drawing 1-6 is respectively the present invention is based on and mixes composition, by calculating serpentine, smalite, white mica, kalzit, chlorite and the epidotic relevant identification figure that Spearman (Spearman R) and Ken Deer (Kendall tau) related coefficient obtain; They are to select the HyMap data of East Tianshan of Xinjiang knoll copper nickel bed to carry out example.This mineral deposit is made up of the ore body and the mineralization body of different sizes, originates in the ultrabasic rock and controlled by certain petrofacies.The ore rock alteration is strong, often has talcumization, sheridaniteization, antigoriteization.Especially the rock crown alteration of ore body is stronger, and rock is alteration slabbing, powder shape often.The clay grounting that tool is stronger, kaolinization.These alterations distribute and have weathering of tangible face type and line style weathering branch band feature.According to the relation in metallogenic theory and alteration and ore deposit, select epidote, chlorite, serpentine, kalzit, smalite and white mica to discern as reference spectrum.The left side is Spearman (Spearman R) coefficient in each accompanying drawing, and the right is Ken Deer (Kendall tau) coefficient.The black distributive province represents that there are the mineral that detect in this place among the figure, and perhaps these mineral occupy the dominance status.
Fig. 7-the 12nd, the check analysis of serpentine, smalite, white mica, kalzit, chlorite and epidotic image wave spectrum and standard spectrum according to the present invention.Extract the pairing video spectrum of color range and the standard mineral spectrum correspondence analysis of different levels from high spectrum video, the spectrum of the part that related coefficient is bigger (dotted portion among the figure) is very consistent with the standard wave spectrum of end member (dot-and-dash line part among the figure).Along with the reduction of related coefficient, its pixel wave spectrum (solid line part among the figure) also increases with the otherness of standard wave spectrum thereupon, and especially the secondary features of some features obviously disappears.This shows that there are more weak inner link in the less pixel of related coefficient and this end member mineral, or basic onrelevant.This pixel is that the possibility of these end member mineral is also very little, or is not these end member mineral.
Table 1 and table 2 are respectively the correlation parameter of Spearman and the distribution of Kendall coefficient
The most boundaries of Spearman R coefficient of rank correlation are between 0.6～0.9, and Kendall tau coefficient circle is between 0.4～0.7.From table 1 and table 2 as can be known, significance test p＜0.06, the overwhelming majority is near 0.001.Therefore, the related coefficient of being calculated meets significance test, has big correlativity.
Table 1 Spearman coefficient of rank correlation distributes
Mineral coefficient minimum value maximal value mean variance
Kalzit R 0.447213 0.934594 0.81256 0.032227
p 0 0.013219 0 0.000014
Chlorite R 0.484761 0.871858 0.789467 0.019424
p 0 0.00663 0 0.000012
Epidote R 0.349761 0.870397 0.698577 0.042139
p 0 0.058138 0.000045 0.000139
Smalite R 0.542158 0.938154 0.776793 0.031374
p 0 0.001969 0.000002 0.000008
White mica R 0.459399 0.935929 0.753615 0.036218
p 0 0.010653 0.000007 0.000032
Antigorite R 0.437152 0.835818 0.739126 0.025418
p 0 0.015709 0.000006 0.000029
Table 2 Kendall coefficient of concordance distributes
Mineral coefficient minimum value maximal value mean variance
R 0.317607 0.783908 0.618844 0.037760
Kalzit p 0 0.013705 0.000004 0.000019
R 0.301149 0.696552 0.521554 0.038770
Chlorite p 0 0.019430 0.000094 0.000118
R 0.251152 0.713464 0.544243 0.041325
Epidote p 0 0.051277 0.000057 0.000151
R 0.393103 0.797701 0.597479 0.032225
Smalite p 0 0.002282 0.000008 0.000022
R 0.31954 0.802299 0.538260 0.034176
White mica p 0 0.013142 0.000063 0.000140
R 0.264368 0.641379 0.497374 0.031543
Antigorite p 0.000001 0.040197 0.000174 0.000206
Claims (3)
1. the very big relative identifying method of high spectrum mineral that mixing is formed based on spectrum comprises the steps:
(1) obtains the high spectrum image data in somewhere;
(2) the mineral spectrum that selection and this zone may distribute in library of spectra is as reference spectrum;
(3) calculate each pixel spectrum and in library of spectra the related coefficient between the selected mineral spectrum;
(4) determine with library of spectra in one or more pixel of related coefficient maximum of selected mineral spectrum;
(5) judge whether exist selected mineral or this selected mineral to occupy the dominance status in this one or more pixel.
2. the very big relative identifying method of high spectrum mineral according to claim 1 is characterized in that utilizing following formula in above-mentioned steps (3):
R
Xi, R
YiBe respectively the order of set of variables X and Y, R
x, R
xBe respectively the equal order of X and Y; X and Y are respectively reference spectra and pixel spectrum; Calculate Spearman (Spearman R) related coefficient.
3,, it is characterized in that in above-mentioned steps (3), utilizing formula according to the very big relative identifying method of the described high spectrum mineral of claim 1:
P is the X pairing sum consistent with Y, and Q is the inconsistent pairing sum of X and Y; Tx is and variable X matched group equal numbers that Ty is and variable Y matched group equal numbers; X and Y are respectively reference spectra and pixel spectrum; Calculate Ken Deer (Kendall tau) coefficient.
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| CN1315094C (en) * | 2005-04-14 | 2007-05-09 | 中国国土资源航空物探遥感中心 | Imaging spectrum data processing system and imaging spectrum data processing method |
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