CN108020322B - Quantitative detection method of airborne thermal infrared hyperspectral remote sensing in coal field fire area - Google Patents

Quantitative detection method of airborne thermal infrared hyperspectral remote sensing in coal field fire area Download PDF

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CN108020322B
CN108020322B CN201610986998.6A CN201610986998A CN108020322B CN 108020322 B CN108020322 B CN 108020322B CN 201610986998 A CN201610986998 A CN 201610986998A CN 108020322 B CN108020322 B CN 108020322B
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杨国防
赵英俊
张鑫
田新光
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Beijing Research Institute of Uranium Geology
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Abstract

本发明属于遥感探测技术领域,具体涉及一种煤田火区的机载热红外高光谱遥感定量探测方法;本发明的目的是,针对现有技术不足,提供一种解决煤田火区复杂危险环境下无法快速准确地定位煤火燃烧位置和燃烧范围的难题的煤田火区的机载热红外高光谱遥感定量探测方法;包括以下步骤:步骤一:数据获取;步骤二:几何校正和图像均色镶嵌;步骤三:煤火探测波段选择;步骤四:地表温度反演模型;步骤五:热异常信息提取;步骤六:基于发射率特征精确提取煤田火区范围;实现了煤田火区的定量化探测,探测煤火区范围准确,采用的方法步骤简洁,完全可用于高光谱热红外遥感技术的煤田火区探测当中,为煤田火区灭火工程提供实时性支撑数据。

Figure 201610986998

The invention belongs to the technical field of remote sensing detection, and in particular relates to an airborne thermal infrared hyperspectral remote sensing quantitative detection method in a coal field fire area; the purpose of the invention is to provide a solution to the problem of the complex and dangerous environment of the coal field fire area in view of the deficiencies of the prior art. Airborne thermal infrared hyperspectral remote sensing quantitative detection method for coal field fire areas where it is difficult to quickly and accurately locate the burning position and combustion range of coal fires; including the following steps: step 1: data acquisition; step 2: geometric correction and image homogeneous color mosaic ; Step 3: Coal fire detection band selection; Step 4: Surface temperature inversion model; Step 5: Extraction of thermal anomaly information; Step 6: Accurately extract the coal field fire area based on the emissivity feature; Realize the quantitative detection of coal field fire area , the detection range of coal fire area is accurate, and the method and steps used are simple, which can be used in the detection of coal field fire area by hyperspectral thermal infrared remote sensing technology, and provide real-time support data for coal field fire area fire extinguishing project.

Figure 201610986998

Description

Airborne thermal infrared hyperspectral remote sensing quantitative detection method for coal field fire area
Technical Field
The invention belongs to the technical field of remote sensing detection, and particularly relates to an airborne thermal infrared hyperspectral remote sensing quantitative detection method for a coal field fire area.
Background
In China, the reserves of coal resources are the first in the world, but the spontaneous combustion phenomenon of coal fire is very serious, which not only causes huge waste of the coal resources, but also causes great pollution to the environment. The students at home and abroad utilize the remote sensing technology to carry out coal field fire area identification and monitoring, mainly rely on multispectral and medium-low resolution remote sensing images, can only provide information such as fire source position and fire area approximate range qualitatively or semi-quantitatively, and are difficult to meet the requirements of increasing monitoring precision and accuracy of the coal field fire area. The conventional remote sensing coal fire detection method adopts a proper threshold value to perform density segmentation on the temperature inverted according to thermal infrared data so as to achieve the aim of roughly detecting coal fire, and the range of the coal field fire area detected by the method usually comprises non-coal fire temperature abnormal interference ground objects such as water bodies, hot plants and the like, so that the range of the coal field fire area is difficult to accurately extract. How to accurately and effectively extract the coal fire area range by adopting a remote sensing technology is an urgent problem to be solved in coal field fire area treatment.
The appearance of hyperspectral thermal infrared remote sensing provides a solution to the above problems. The hyperspectral thermal infrared remote sensing has three-dimensional information of space, radiation and spectrum, large data volume and rich information. The included feature information of the ground object radiation is more fine. How to utilize the abundant ground feature radiation information to finely distinguish ground feature heat anomaly and finely and quantitatively detect coal fire of a coal field is few in domestic research.
Under the background condition, the invention provides an aviation hyperspectral thermal infrared remote sensing coal fire quantitative detection method. The hyperspectral instrument adopts a TASI airborne hyperspectral sensor developed in Canada, and the spectral range is as follows: 8.0-11.5 mu m, the number of the spectral channels theoretically has infinite separability, the data of the embodiment of the invention has 32 spectral channels, and the dynamic range is 16 bits. The method fully utilizes the technical advantage of multiple hyperspectral thermal radiation channels, realizes efficient and rapid quantitative detection of the fire area of the coal field, and provides real-time basis for work deployment and fire area management and evaluation of fire extinguishing engineering of the coal field.
Disclosure of Invention
The invention aims to provide an onboard thermal infrared hyperspectral remote sensing quantitative detection method for a coal field fire area, which solves the problem that the combustion position and the combustion range of coal fire cannot be quickly and accurately positioned in a complex dangerous environment of the coal field fire area
The technical scheme of the invention is as follows:
an airborne thermal infrared hyperspectral remote sensing quantitative detection method for a coal field fire area comprises the following steps:
the method comprises the following steps: data acquisition
Carrying out laboratory spectrum calibration and radiometric calibration on the sensor by adopting a known laser generator and a black body, setting a low-temperature black body reference source at 0 ℃, setting a high-temperature black body reference source at 100 ℃, and selecting an area with an obvious ground linear target to carry out geometric parameter correction flight on the sensor to obtain correction data; acquiring hyperspectral data according to a designed flight path, and simultaneously, performing ground synchronous temperature measurement by adopting a high-sensitivity infrared radiant spot thermometer to serve as calibration data of the hyperspectral data;
step two: geometric correction and image color-equalizing mosaic;
inputting POS positioning data, original IMU data, DEM data and ground GPS base station data into an ITRES system data processing module, and performing system geometric error correction on aviation hyperspectral thermal infrared data; on the basis, more than 30 control points are selected from the high-precision topographic map for geometric correction, and the irregular geometric error of the flight band caused by topographic relief is eliminated;
determining a reference flight band image as a reference of an output mosaic image, and adjusting the flight band image with chromatic aberration to the reference image by adopting a chromatic order adjusting method as shown in a formula (1) according to the statistical radiation difference of the overlapping area of the adjacent flight band images so as to keep the tone of the adjacent images consistent; finally, a data overlapping area pixel value histogram statistical method is adopted for color homogenizing treatment, and adjacent flight band radiation difference is thoroughly eliminated;
Figure DEST_PATH_GDA0001244508040000021
wherein X is the flight band data to be adjusted; r is a radiation adjustment coefficient and is determined according to difference statistics of adjacent image values; n is the original data radiation quantization value, m is the radiation quantization value after data adjustment, and usually m is equal to n;
step three: coal fire detection band selection
Noise statistic analysis is carried out on the hyperspectral thermal infrared data, the wave bands with large strip noise, low signal-to-noise ratio and small difference of surface feature radiation brightness are deleted, the background and the thermal abnormal radiation brightness value with obvious difference and large difference of medium, low and high temperature abnormal radiation brightness values are selected as data participating in surface temperature inversion;
step four: surface temperature inversion model
Primarily estimating the earth surface temperature by adopting an emissivity normalization method, acquiring a regression correction parameter between the estimated earth surface temperature and ground synchronous temperature measurement data by utilizing a least square linear regression method, and performing optimized correction on the estimated temperature by utilizing the correction parameter to improve the temperature inversion precision;
(1) supposing that the obtained hyperspectral thermal infrared data has a maximum emissivity value epsilon in a certain wave bandmaxHere, the preliminary estimated temperature for each wavelength is determined from equation (2) according to Planck's law, without taking into account the ambient radiation:
Figure DEST_PATH_GDA0001244508040000031
where L (λ) is the radiance value obtained by the sensor, c1,c2Is Planck constant; epsilonmaxAssigning a value according to the maximum emissivity of the ground object in the image;
(2) taking the maximum value of the temperature of each wavelength as a target estimated temperature:
TM=max(Tλ) (3)
(3) based on a least square linear regression fitting method, correcting the preliminarily estimated temperature data by using the fitting coefficient of the preliminarily estimated temperature and the ground synchronous measured temperature to eliminate the influence of environmental radiation;
step five: thermal anomaly information extraction
Performing histogram probability statistical analysis according to the inverted temperature image information, and searching a knee point position where the high-frequency temperature is excessive to the low-frequency temperature as a lower limit of a thermal abnormal temperature threshold;
step six: accurate extraction of coal field fire zone range based on emissivity characteristics
The thermal infrared radiation received by the sensor comprises ground object self radiation, atmospheric uplink radiation and reflected radiation of the ground object to the surrounding environment, and under the condition of thermal equilibrium, the ambient radiation reflected by the ground object is mainly atmospheric downlink radiation; based on the lambert of the earth surface, according to kirchhoff's law, the sum of the reflectivity and the emissivity of the earth surface is 1, and the radiation brightness received by the sensor in the thermal infrared hyperspectral band range can be expressed as:
Figure DEST_PATH_GDA0001244508040000041
τλis the atmospheric transmission rate, epsilon, between the sensor and the targetλEmissivity of ground object, Bλ(Tc) At a temperature of TcThe black body radiation of (2) can be obtained according to a Planck black body radiation formula;
Figure DEST_PATH_GDA0001244508040000042
respectively, the downlink radiation and the uplink radiation of the atmosphere; in No. atWhen synchronous sounding data is provided, analog calculation is performed by using Modtran4
Figure DEST_PATH_GDA0001244508040000043
τλ
Converting the formula (4) to obtain emissivity epsilonλThe calculation formula of (2):
Figure DEST_PATH_GDA0001244508040000044
Bλ(Tc),
Figure DEST_PATH_GDA0001244508040000045
τλare integral average values within the bandwidth of the corresponding channel of the sensor; it is noted that the fire area range of the coal field is accurately extracted based on the emissivity characteristics, and all band data of the thermal infrared hyperspectrum participate in the operation, which is different from the coal fire detection band selected in the third step;
analyzing the difference between the interference factors and the ground object emissivity of the coal fire area: the emissivity wave band difference is enhanced by adopting a ratio method, and the difference between a target coal field fire area and interference factors is highlighted; using a threshold segmentation method in bpSeparating the thermal plant from the thermal anomaly in the image to generate a plant thermal anomaly range region of interest; re-selecting threshold value at bwSeparating the water body from the thermal anomaly in the image to generate a water body thermal anomaly range region of interest; finally, combining the thermal plant and the water body thermal abnormal range to generate a thermal plant and water body non-coal fire interference thermal abnormal range region of interest; and taking the generated non-coal-fire-interference heat abnormal range interested region as a mask file to remove the heat abnormal range extracted in the step five, thereby achieving the purpose of accurately extracting the coal field fire region.
The invention has the beneficial effects that:
1. the invention successfully realizes the quantitative detection of the fire area of the coal field;
2. the method has the advantages that the coal fire area detection range is accurate, and the steps of the method are simple and efficient;
3. the method can be used for detecting the fire area of the coal field by the hyperspectral thermal infrared remote sensing technology, and provides real-time support data for fire extinguishing engineering of the fire area of the coal field.
Drawings
FIG. 1 is a flow chart of an airborne thermal infrared hyperspectral remote sensing quantitative detection method for a coal field fire area;
FIG. 2 is a radiation profile of a terrain at different temperatures;
FIG. 3 is a statistical histogram of temperature and frequency in a fire zone
Detailed Description
The invention will be further described with reference to the following figures and examples:
an airborne thermal infrared hyperspectral remote sensing quantitative detection method for a coal field fire area comprises the following steps:
the method comprises the following steps: data acquisition
Carrying out laboratory spectrum calibration and radiometric calibration on the sensor by adopting a known laser generator and a black body, setting a low-temperature black body reference source at 0 ℃, setting a high-temperature black body reference source at 100 ℃, and selecting an area with an obvious ground linear target to carry out geometric parameter correction flight on the sensor to obtain correction data; acquiring hyperspectral data according to a designed flight path, and simultaneously, performing ground synchronous temperature measurement by adopting a high-sensitivity infrared radiant spot thermometer to serve as calibration data of the hyperspectral data;
step two: geometric correction and image color-equalizing mosaic;
inputting POS positioning data, original IMU data, DEM data and ground GPS base station data into an ITRES system data processing module, and performing system geometric error correction on aviation hyperspectral thermal infrared data; on the basis, more than 30 control points are selected from the high-precision topographic map for geometric correction, and the irregular geometric error of the flight band caused by topographic relief is eliminated;
determining a reference flight band image as a reference of an output mosaic image, and adjusting the flight band image with chromatic aberration to the reference image by adopting a chromatic order adjusting method as shown in a formula (1) according to the statistical radiation difference of the overlapping area of the adjacent flight band images so as to keep the tone of the adjacent images consistent; finally, a data overlapping area pixel value histogram statistical method is adopted for color homogenizing treatment, and adjacent flight band radiation difference is thoroughly eliminated;
Figure DEST_PATH_GDA0001244508040000051
wherein X is the flight band data to be adjusted; r is a radiation adjustment coefficient and is determined according to difference statistics of adjacent image values; n is the original data radiation quantization value, m is the radiation quantization value after data adjustment, and usually m is equal to n;
step three: coal fire detection band selection
Noise statistic analysis is carried out on the hyperspectral thermal infrared data, the wave bands with large strip noise, low signal-to-noise ratio and small difference of surface feature radiation brightness are deleted, the background and the thermal abnormal radiation brightness value with obvious difference and large difference of medium, low and high temperature abnormal radiation brightness values are selected as data participating in surface temperature inversion;
step four: surface temperature inversion model
Primarily estimating the earth surface temperature by adopting an emissivity normalization method, acquiring a regression correction parameter between the estimated earth surface temperature and ground synchronous temperature measurement data by utilizing a least square linear regression method, and performing optimized correction on the estimated temperature by utilizing the correction parameter to improve the temperature inversion precision;
(1) supposing that the obtained hyperspectral thermal infrared data has a maximum emissivity value epsilon in a certain wave bandmaxHere, the preliminary estimated temperature for each wavelength is determined from equation (2) according to Planck's law, without taking into account the ambient radiation:
Figure DEST_PATH_GDA0001244508040000061
where L (λ) is the radiance value obtained by the sensor, c1,c2Is Planck constant; epsilonmaxAssigning a value according to the maximum emissivity of the ground object in the image;
(2) taking the maximum value of the temperature of each wavelength as a target estimated temperature:
TM=max(Tλ) (3)
(3) based on a least square linear regression fitting method, correcting the preliminarily estimated temperature data by using the fitting coefficient of the preliminarily estimated temperature and the ground synchronous measured temperature to eliminate the influence of environmental radiation;
step five: thermal anomaly information extraction
Performing histogram probability statistical analysis according to the inverted temperature image information, and searching a knee point position where the high-frequency temperature is excessive to the low-frequency temperature as a lower limit of a thermal abnormal temperature threshold;
step six: accurate extraction of coal field fire zone range based on emissivity characteristics
The thermal infrared radiation received by the sensor comprises ground object self radiation, atmospheric uplink radiation and reflected radiation of the ground object to the surrounding environment, and under the condition of thermal equilibrium, the ambient radiation reflected by the ground object is mainly atmospheric downlink radiation; based on the lambert of the earth surface, according to kirchhoff's law, the sum of the reflectivity and the emissivity of the earth surface is 1, and the radiation brightness received by the sensor in the thermal infrared hyperspectral band range can be expressed as:
Figure DEST_PATH_GDA0001244508040000071
τλis the atmospheric transmission rate, epsilon, between the sensor and the targetλEmissivity of ground object, Bλ(Tc) At a temperature of TcThe black body radiation of (2) can be obtained according to a Planck black body radiation formula;
Figure DEST_PATH_GDA0001244508040000072
respectively, the downlink radiation and the uplink radiation of the atmosphere; under the condition of not having synchronous sounding data, the Modtran4 is utilized to simulate calculation
Figure DEST_PATH_GDA0001244508040000073
τλ
Converting the formula (4) to obtain emissivity epsilonλThe calculation formula of (2):
Figure DEST_PATH_GDA0001244508040000074
Bλ(Tc),
Figure DEST_PATH_GDA0001244508040000075
τλare integral average values within the bandwidth of the corresponding channel of the sensor; it is noted that the fire area range of the coal field is accurately extracted based on the emissivity characteristics, and all band data of the thermal infrared hyperspectrum participate in the operation, which is different from the coal fire detection band selected in the third step;
analyzing the difference between the interference factors and the ground object emissivity of the coal fire area: the emissivity wave band difference is enhanced by adopting a ratio method, and the difference between a target coal field fire area and interference factors is highlighted; using a threshold segmentation method in bpSeparating the thermal plant from the thermal anomaly in the image to generate a plant thermal anomaly range region of interest; re-selecting threshold value at bwSeparating the water body from the thermal anomaly in the image to generate a water body thermal anomaly range region of interest; finally, combining the thermal plant and the water body thermal abnormal range to generate a thermal plant and water body non-coal fire interference thermal abnormal range region of interest; and taking the generated non-coal-fire-interference heat abnormal range interested region as a mask file to remove the heat abnormal range extracted in the step five, thereby achieving the purpose of accurately extracting the coal field fire region.
Examples
The flow of the airborne thermal infrared hyperspectral remote sensing quantitative detection method for the coal field fire area is shown in figure 1, and the method comprises the following steps:
the method comprises the following steps: data acquisition
The known laser generator and the black body are adopted to carry out laboratory spectrum calibration and radiometric calibration on the sensor, the reference source of the low-temperature black body is set to be 0 ℃, the reference source of the high-temperature black body is set to be 100 ℃, and the identifiability of low-temperature and high-temperature ground objects is ensured. And selecting an area with an obvious ground linear target to carry out sensor geometric parameter correction flight, and acquiring correction data. And acquiring hyperspectral data according to the designed flight path, and simultaneously, performing ground synchronous temperature measurement by adopting a high-sensitivity infrared radiant spot thermometer to serve as calibration data of the hyperspectral data.
Step two: geometric correction and image color-mean-mosaic.
And inputting the POS positioning data, the original IMU data, the DEM data and the ground GPS base station data into an ITRES system data processing module, and performing system geometric error correction on the aviation hyperspectral thermal infrared data. On the basis, a sufficient number of control points are selected from the high-precision topographic map to carry out geometric correction, and the irregular geometric error of the flight band caused by topographic relief is eliminated.
Determining a reference aerial image as the reference of the output mosaic image, and adjusting the aerial image with chromatic aberration to the reference image by adopting a chromatic order adjustment method (formula 1) according to the statistical radiation difference of the overlapping area of the adjacent aerial images so as to keep the tone of the adjacent images consistent. And finally, carrying out color homogenizing treatment by adopting a data overlapping area pixel value histogram statistical method, and thoroughly eliminating adjacent flight band radiation difference.
Figure DEST_PATH_GDA0001244508040000081
X is the flight band data to be adjusted; r is a radiation adjustment coefficient and is determined according to difference statistics of adjacent image values; n is the original data radiation quantization value, m is the data adjusted radiation quantization value, and m is n.
Step three: coal fire detection band selection
Noise statistic analysis is carried out on thermal infrared hyperspectral data, strip noise with equal intervals of 29-32 wave bands of data in an embodiment is large, the signal to noise ratio is low, and the difference of radiation brightness of ground objects at different temperatures is small. The high-temperature abnormality at the temperature of more than 200 ℃ is overlapped and crossed with the high-temperature abnormal radiation brightness at the temperature of 155-195 ℃ in a wave band of 17-28 ℃; in the 1-16 wave band, the background and the heat abnormal radiation brightness value have obvious difference, and the difference of the medium, low and high temperature abnormal radiation brightness values is large, so that the difference is easy to distinguish (figure 2). The wave bands of 1 to 16 are the optimal wave bands for detecting abnormal coal fire information.
Step four: surface temperature inversion model
(1) Supposing that the obtained hyperspectral thermal infrared data has maximum emissivity in a certain wave bandValue epsilonmaxHere, the preliminary estimated temperature for each wavelength is determined from equation (2) according to Planck's law, without taking into account the ambient radiation:
Figure DEST_PATH_GDA0001244508040000091
where L (λ) is the radiance value obtained by the sensor, c1,c2Is Planck constant. EpsilonmaxAnd assigning a value according to the maximum emissivity of the ground object in the image.
(2) Taking the maximum value of the temperature of each wavelength as a target estimated temperature:
TM=max(Tλ) (3)
(3) and correcting the preliminarily estimated temperature data by using the fitting coefficient of the preliminarily estimated temperature and the ground synchronous measured temperature based on the least square linear regression fitting method, so as to eliminate the influence of environmental radiation.
Step five: thermal anomaly information extraction
Histogram probability statistical analysis is carried out on the inversion temperature data of the thermal infrared image, and the position of an inflection point (figure 3) at which the high-frequency temperature is excessive to the low-frequency temperature is searched and used as the lower limit of the thermal abnormal temperature threshold value, so that the thermal abnormal ground object is separated from the background.
Step six: accurate extraction of coal field fire zone range based on emissivity characteristics
Different ground objects have different properties such as composition, surface structure and the like, and have different emissivity. The interference factors in the thermal anomaly of the difference of the ground object emissivity are utilized.
The thermal infrared radiation received by the sensor comprises ground object self radiation, atmospheric uplink radiation and reflected radiation of the ground object to the surrounding environment, and under the thermal equilibrium condition, the ambient radiation reflected by the ground object is mainly the atmospheric downlink radiation. Based on the lambert of the earth surface, according to kirchhoff's law, the sum of the reflectivity and the emissivity of the earth surface is 1, and the radiation brightness received by the sensor in the thermal infrared hyperspectral band range can be expressed as:
Figure DEST_PATH_GDA0001244508040000092
τλis the atmospheric transmission rate, epsilon, between the sensor and the targetλEmissivity of ground object, Bλ(Tc) At a temperature of TcThe black body radiation of (2) can be obtained according to a Planck black body radiation formula;
Figure DEST_PATH_GDA0001244508040000101
respectively, the down radiation and the up radiation of the atmosphere. Under the condition of not having synchronous sounding data, the Modtran4 is utilized to simulate calculation
Figure DEST_PATH_GDA0001244508040000102
τλ
Converting the formula (4) to obtain emissivity epsilonλThe calculation formula of (2):
Figure DEST_PATH_GDA0001244508040000103
Bλ(Tc),
Figure DEST_PATH_GDA0001244508040000104
τλare the integrated average values over the bandwidth of the corresponding channel of the sensor. It should be noted that the fire area range of the coal field is accurately extracted based on the emissivity characteristics, and all band data of the thermal infrared hyperspectrum participate in the operation, which is different from the coal fire detection band selected in the third step.
Analyzing the difference between interference factors (water body and factory building) and the emissivity of ground objects in the coal fire area: the emissivity of the embodiment data adopted by the invention is obviously lower in the emissivity of water body in the 23-25 wave band and obviously lower in the emissivity of hot plant in the 9-12 wave band. The differences are small in value, and the invention adopts a ratio method to enhance the differences of the emissivity wave bands (6 and 7 formulas) and highlights the differences between the target coal field fire area and the interference factors. Using a threshold segmentation method in bpAnd separating the hot plant from the thermal anomaly in the image to generate a plant thermal anomaly range region of interest. Re-selection ofTaking the threshold value as bwAnd separating the water body from the thermal anomaly in the image to generate a water body thermal anomaly range region of interest. And finally, combining the thermal plant and the water body thermal abnormal range to generate an interested region of the thermal plant and the water body non-coal fire interference thermal abnormal range. And taking the generated non-coal-fire-interference heat abnormal range interested region as a mask file to remove the heat abnormal range extracted in the step five, thereby achieving the purpose of accurately extracting the coal field fire region.
bp=e10*b9(6)
bw=e10*b24(7)
b9Emissivity data for the 9 th band, b24The emissivity data of the 24 th wave band.

Claims (1)

1.一种煤田火区的机载热红外高光谱遥感定量探测方法,其特征在于:包括以下步骤:1. a kind of airborne thermal infrared hyperspectral remote sensing quantitative detection method in coal field fire area, is characterized in that: may further comprise the steps: 步骤一:数据获取Step 1: Data acquisition 采用已知激光发生器和黑体对传感器进行实验室光谱定标和辐射定标,低温黑体参考源设定0℃,高温黑体参考源设定100℃,选择地面线性目标明显的区域进行传感器几何参数校正飞行,获取校正数据;按照设计的飞行航线进行高光谱热红外数据获取,同时,采用高灵敏度的红外辐射点温计进行地面同步温度测量,作为高光谱热红外数据的定标数据;Use a known laser generator and a blackbody to perform laboratory spectral calibration and radiometric calibration on the sensor. The low temperature blackbody reference source is set to 0°C, the high temperature blackbody reference source is set to 100°C, and the area with obvious ground linear targets is selected for sensor geometry parameters. Calibrate the flight and obtain the calibration data; obtain the hyperspectral thermal infrared data according to the designed flight route, and at the same time, use a high-sensitivity infrared radiation point thermometer to measure the ground synchronous temperature as the calibration data of the hyperspectral thermal infrared data; 步骤二:几何校正和图像均色镶嵌Step 2: Geometric Correction and Image Homogenization Mosaic 将POS定位数据、原始IMU数据、DEM数据和地面GPS基站数据输入ITRES系统数据处理模块,对航空高光谱热红外数据进行系统几何差误校正;在此基础上,从高精度地形图上选取大于30个的控制点进行几何精校正,消除地形起伏引起的航带无规律性几何误差;Input the POS positioning data, original IMU data, DEM data and ground GPS base station data into the data processing module of the ITRES system to perform systematic geometric error correction on the aviation hyperspectral thermal infrared data; The geometric precision correction of each control point is carried out to eliminate the irregular geometric error of the navigation belt caused by the terrain fluctuation; 确定一幅参考航带影像作为输出镶嵌图像的基准,根据相邻航带影像重叠区的统计辐射差异,采用色差调整方法如公式(1)所示,将具有色差的航带影像调整到参考影像上去,使相邻图像的色差保持一致;最后,采用数据重叠区像元值直方图统计方法进行匀色处理,彻底消除相邻航带辐射差异;Determine a reference airway image as the benchmark of the output mosaic image, and adjust the airway image with color difference to the reference image by using the chromatic aberration adjustment method as shown in formula (1) according to the statistical radiation difference in the overlapping area of the adjacent airway images. Then, the color difference of adjacent images is kept consistent; finally, the statistical method of pixel value histogram in the data overlap area is used to perform color equalization processing to completely eliminate the radiation difference between adjacent airways;
Figure FDA0002301735100000011
Figure FDA0002301735100000011
其中,X为待调整的航带数据;R为辐射调整系数,根据相邻影像值差异统计确定;n为原数据辐射量化值,m为数据调整后辐射量化值,取m=n;Among them, X is the flight band data to be adjusted; R is the radiation adjustment coefficient, which is statistically determined according to the difference of adjacent image values; n is the radiation quantization value of the original data, m is the radiation quantization value after data adjustment, and takes m=n; 步骤三:煤火探测波段选择Step 3: Coal fire detection band selection 对高光谱热红外数据进行噪声统计分析,删除条形噪声大、信噪比低、地物辐射亮度差异小的波段,选择背景与热异常辐射亮度值存在明显差异,且中、低、高温异常辐射亮度值差异较大,作为参加地表温度反演的数据;Perform noise statistical analysis on hyperspectral thermal infrared data, delete bands with large bar noise, low signal-to-noise ratio, and small differences in radiance of ground objects, select background and thermal anomaly radiance values that have significant differences, and medium, low, and high temperature anomalies The radiance values vary greatly, and are used as the data for participating in the surface temperature inversion; 步骤四:地表温度反演模型Step 4: Surface temperature inversion model 采用发射率归一化方法初步估算地表温度,利用最小二乘线性回归方法获取初步估算地表温度与地面同步测温数据间的拟合系数,利用拟合系数对目标估算温度进行优化校正,提高温度反演精度;The emissivity normalization method is used to preliminarily estimate the surface temperature, and the least squares linear regression method is used to obtain the fitting coefficient between the preliminarily estimated surface temperature and the ground synchronous temperature measurement data. Inversion accuracy; (1)假设获取的高光谱热红外数据在某个波段存在发射率最大值εmax,在此不考虑环境辐射,根据Planck定律由公式(2)求得各波长的初步估算地表温度:(1) Assuming that the obtained hyperspectral thermal infrared data has the maximum emissivity ε max in a certain band, the ambient radiation is not considered here, and the preliminary estimated surface temperature of each wavelength is obtained by formula (2) according to Planck's law:
Figure FDA0002301735100000021
Figure FDA0002301735100000021
式中,L(λ)为传感器获取的辐射亮度值,c1,c2为普朗克常量;εmax由影像中地物的最大发射率赋值;In the formula, L(λ) is the radiance value obtained by the sensor, c 1 , c 2 are Planck constants; ε max is assigned by the maximum emissivity of the ground objects in the image; (2)取各波长温度最大值作为目标估算温度:(2) Take the maximum temperature of each wavelength as the target estimated temperature: TM=max(Tλ) (3)T M =max(T λ ) (3) (3)基于最小二乘线性回归拟合的方法,利用初步估算地表温度和地面同步测量温度的拟合系数再对目标估算温度数据进行校正,消除环境辐射的影响;(3) Based on the method of least squares linear regression fitting, use the fitting coefficient of the preliminary estimated surface temperature and the ground synchronously measured temperature to correct the target estimated temperature data to eliminate the influence of environmental radiation; 步骤五:热异常信息提取Step 5: Thermal anomaly information extraction 根据反演的温度图像信息进行直方图概率统计分析,寻找高频温度向低频温度过度的拐点位置,作为热异常温度阈值下限;According to the inversion temperature image information, the histogram probability statistical analysis is carried out, and the inflection point position where the high-frequency temperature transitions to the low-frequency temperature is found as the lower limit of the thermal anomaly temperature threshold; 步骤六:基于发射率特征精确提取煤田火区范围Step 6: Accurately extract the coal field fire area based on emissivity features 传感器接收到的热红外辐射包括地物自身辐射、大气上行辐射和地物对周围环境的反射辐射,在热平衡条件下,地物反射的周围环境辐射主要是大气下行辐射;基于地表朗伯体的条件下,根据基尔霍夫定律可知,地表的反射率与发射率之和为1,热红外高光谱波段范围内传感器接收到的辐射亮度表示为:The thermal infrared radiation received by the sensor includes the radiation of the ground object itself, the upward radiation of the atmosphere and the reflected radiation of the ground object to the surrounding environment. Under the condition of thermal equilibrium, the ambient radiation reflected by the ground object is mainly the downward radiation of the atmosphere; Under the conditions, according to Kirchhoff's law, the sum of the reflectivity and emissivity of the surface is 1, and the radiance received by the sensor in the thermal infrared hyperspectral band range is expressed as:
Figure FDA0002301735100000031
Figure FDA0002301735100000031
τλ为传感器与目标之间的大气透过率,ελ为地物发射率,Bλ(Tc)为温度为Tc的黑体辐射,根据普朗克黑体辐射公式求得;
Figure FDA0002301735100000032
分别为大气的下行辐射和上行辐射;在不具备同步探空数据的情况下,利用Modtran4模拟计算
Figure FDA0002301735100000033
τλ
τ λ is the atmospheric transmittance between the sensor and the target, ε λ is the ground object emissivity, and B λ (Tc) is the black body radiation with a temperature of Tc, which is obtained according to the Planck black body radiation formula;
Figure FDA0002301735100000032
are the downward radiation and the upward radiation of the atmosphere, respectively; in the absence of synchronous sounding data, Modtran4 is used to simulate the calculation
Figure FDA0002301735100000033
τ λ ;
将(4)式变换得到发射率ελ的计算公式:Transform (4) to obtain the calculation formula of emissivity ελ:
Figure FDA0002301735100000034
Figure FDA0002301735100000034
Bλ(Tc),
Figure FDA0002301735100000035
τλ均为传感器相应通道带宽内的积分平均值;需要注意的是,基于发射率特征精确提取煤田火区范围,热红外高光谱全部波段数据参与运算,与步骤三中选择的煤火探测波段不同;
B λ (Tc),
Figure FDA0002301735100000035
τ λ is the integral average value within the corresponding channel bandwidth of the sensor; it should be noted that, based on the emissivity feature to accurately extract the coal field fire area, all the thermal infrared hyperspectral band data participate in the calculation, which is different from the coal fire detection band selected in step 3. different;
分析干扰因素与煤火区地物发射率的差异:采用比值法增强发射率波段差异,突出目标煤田火区与干扰因素之间的差异;利用阈值分割的方法在bp图像中将热厂房从热异常中分离出来,生成热厂房热异常范围感兴趣区;再选取阈值在bw图像中将水体从热异常中分离出来,生成水体热异常范围感兴趣区;最后将热厂房和水体热异常范围进行合并,生成热厂房、水体非煤火干扰热异常范围感兴趣区;将生成的非煤火干扰热异常范围感兴趣区作为掩膜文件从步骤五中提取的热异常范围中去除,达到准确提取煤田火区的目的。Analyze the difference between the interference factors and the emissivity of the ground objects in the coal fire area: use the ratio method to enhance the emissivity band difference, highlight the difference between the target coal field fire area and the interference factors; use the threshold segmentation method to separate the thermal powerhouse from the thermal powerhouse in the bp image. Then, the threshold value is selected to separate the water body from the thermal anomaly in the bw image to generate the area of interest for the thermal anomaly range of the water body; finally, the thermal anomaly range of the thermal powerhouse and the water body is analyzed Merge, generate the area of interest in the thermal anomaly range of thermal powerhouses and water bodies that are not interfered by coal fire; use the generated area of interest in the non-coal fire interference thermal anomaly range as a mask file to remove from the thermal anomaly range extracted in step 5 to achieve accurate extraction The purpose of the coal field fire zone.
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