Investigation of Vegetation Changes in Different Mining Areas in Liaoning Province, China, Using Multisource Remote Sensing Data

: Mining can provide necessary mineral resources for humans. However, mining activities may cause damage to the surrounding ecology and environment. Vegetation change analysis is a key tool for evaluating damage to ecology and the environment. Liaoning is one of the major mining provinces in China, with rich mineral resources and long-term, high-intensity mining activities. Taking Liaoning Province as an example, vegetation change in six mining areas was investigated using multisource remote sensing data to evaluate ecological and environmental changes. Based on MODIS NDVI series data from 2000 to 2019, change trends of vegetation were evaluated using linear regression. According to the results, there are large highly degraded vegetation areas in the Anshan, Benxi, and Yingkou mining areas, which indicates that mining activities have seriously damaged the vegetation in these areas. In contrast, there are considerable areas with improved vegetation in the Anshan, Fushun, and Fuxin mining areas, which indicates that ecological reclamation has played a positive role in these areas. Based on Sentinel-2A data, leaf chlorophyll content was inferred by using the vegetation index MERIS Terrestrial Chlorophyll Index (MTCI) after measurement of leaf spectra and chlorophyll content were carried out on the ground to validate the performance of MTCI. According to the results, the leaf chlorophyll content in the mines is generally lower than in adjacent areas in these mining areas with individual differences. In the Yingkou mining area, the chlorophyll content in adjacent areas is close to the magnesite mines, which means the spillover effect of environmental pollution in mines should be considerable. In the Anshan, Benxi, and Diaobingshan mining areas, the environmental stress on adjacent areas is slight. All in all, iron and magnesite open-pit mines should be monitored closely for vegetation destruction and stress due to the high intensity of mining activities and serious pollution. In contrast, the disturbance to vegetation is limited in resource-exhausted open-pit coal mines and underground coal mines. It is suggested that land reclamation should be enhanced to improve the vegetation in active open-pit mining areas, such as the Anshan, Benxi, and Yingkou mining areas. Additionally, environmental protection measures should be enhanced to relieve vegetation stress in the Yingkou mining area.


Introduction
Vegetation is a topic of interest among scientists and researchers because it plays an important role in the interconnected systems of life on Earth. One important function of vegetation is soil stabilization and enrichment [1][2][3]. Vegetation degradation and desertification could contribute to broader environmental and ecological problems, such as loss of topsoil, increase in temperature, and diminished food resources for humans and wildlife [4,5].
Liaoning Province is located in the south of Northeast China. The climate of Liaoning Province is temperate and monsoonal with annual precipitation between 600 mm and 1100 mm. It is an important mining province in China. By of the end of 2015, 122 types of minerals had been discovered there, and there were 3096 mines with resource reserves. The reserves of iron and magnesite in Liaoning Province rank first in China. Within the province, 93% of iron ore is distributed in Anshan, Benxi, and Liaoyang, and magnesite is mainly in Yingkou and Haicheng. Coal mines were developed more than 100 years ago in the province. However, the coal resources in Fushun and Fuxin were exhausted in the beginning of the 21st century due to high intensity development. Two huge abandoned open pits are located in Fushun and Fuxin. Now, active coal mines are mainly distributed in Diaobingshan as underground mines. In this study, six major mining areas in Liaoning Province, Anshan, Benxi, Diaobingshan, Fushun, Fuxin, and Yingkou, were set as the study areas to investigate vegetation changes using remote sensing (Table 1, Figure 1).

Study Area
Liaoning Province is located in the south of Northeast China. The climate of Liaoning Province is temperate and monsoonal with annual precipitation between 600 mm and 1100 mm. It is an important mining province in China. By of the end of 2015, 122 types of minerals had been discovered there, and there were 3096 mines with resource reserves. The reserves of iron and magnesite in Liaoning Province rank first in China. Within the province, 93% of iron ore is distributed in Anshan, Benxi, and Liaoyang, and magnesite is mainly in Yingkou and Haicheng. Coal mines were developed more than 100 years ago in the province. However, the coal resources in Fushun and Fuxin were exhausted in the beginning of the 21st century due to high intensity development. Two huge abandoned open pits are located in Fushun and Fuxin. Now, active coal mines are mainly distributed in Diaobingshan as underground mines. In this study, six major mining areas in Liaoning Province, Anshan, Benxi, Diaobingshan, Fushun, Fuxin, and Yingkou, were set as the study areas to investigate vegetation changes using remote sensing (Table 1, Figure 1).   Sentinel-2A images contain 13 bands with spatial resolution ranging from 10 m to 60 m. The image data acquired on 2 and 10 August 2018, were downloaded (https:// earthexplorer.usgs.gov/, accessed on 15 March 2020) and then atmospherically corrected using SNAP software. The images were resampled to 10 m.

High-Resolution Data
GeoEye data were downloaded from Google Earth for validation (http://kh.google. com, accessed on 27 April 2020).

Other Data
The climate data (monthly averaged temperature and precipitation from 2000 to 2019) were from the corresponding nearest weather stations to these mining sites, provided by National Meteorological Information Center of China. The yearly total precipitation and yearly averaged temperature were derived from these monthly data. Ore production data were also collected for the driving force analysis (http://tjj.ln.gov.cn/tjsj/sjcx/ndsj/, accessed on 27 April 2020).

Composing the Method for Analysis of MODIS NDVI Yearly Data
Considering that the yearly NDVI is a reliable indicator reflecting the state of vegetation cover, the time series made up of the 16-day composite NDVI maps were combined to produce a NDVI map for each year through the maximum value composite (MVC) method [37]. The composition period of yearly NDVI varied covered the vegetation growing period from May to September [38][39][40]. The yearly maximum NDVI was calculated as follows: where MNDVI is the yearly maximum NDVI in one year, and i is the sequence number of the 10 NDVI maps from May to September in one year, from 1 to 10.

Changing Trend Analysis Based on Yearly NDVI
Based on the composed yearly MODIS NDVI data, the slope of the linear regression was used to simulate the trend of vegetation in the mining areas. The slope was calculated as follows: where j is the sequence number of the 20 years, from 1 to 20, and SLOPE refers to the slope of linear regression. For each pixel, the slope of the fitted line shows the trend of vegetation.
A positive slope indicates vegetation in good condition, whereas a negative slope indicates damaged vegetation. In this study, the NDVI series data were used to divide the degree of vegetation changes into seven levels according to the slope of the fitted line (Table 2) [41].

Chlorophyll Content Estimation Based on Sentinel Data and Difference Analysis
Based on Sentinel-2A images, some indices consisting of red-edge bands can be derived, from which the MERIS Terrestrial Chlorophyll Index (MTCI) could estimate leaf chlorophyll content with good performance [42]. Additionally, MTCI is simple to calculate, and its formula is as follows [43]: where R is the reflectance, and its subscript is the wavelength (nm). To validate the performance of MTCI, measurement of spectra and chlorophyll content were carried out on the ground. Boston ivy leaves in the Anshan and Diaobingshan mining area were selected as the leaf samples for the experiment. Leaf chlorophyll content was measured using SPAD-502 (Minolta Camera, Osaka, Japan). Five to seven points were measured evenly on each leaf, and the mean value SPAD was set as the chlorophyll content of the leaf. The SVC HR-1024 spectrometer (Spectra Vista Corporation, Poughkeepsie, NY, USA) was then used to collect the spectra data of the leaves. The spectral resolution of the SVC HR-1024 spectrometer was 3.5 nm in the range of 350 to 1000 nm, 9.5 nm in the range of 1000 to 1850 nm, and 6.5 nm in the range of 1850 to 2500 nm. The experimental light source was a halogen lamp with 60 • elevation angle and 50 cm distance from the target. After the spectral curves of 32 leaf samples were measured, MTCI and NDVI were calculated, respectively, to study their relationship with chlorophyll content. The MTCI was selected to estimate chlorophyll content of vegetation based on their statistical relationship. The existing relationship for global chlorophyll content estimation was used to estimate the leaf chlorophyll content [44]. The formula is as follows: where y is leaf chlorophyll content (µg/cm 2 ), and x is MTCI value in the image. To avoid the interference of non-vegetation pixels, the pixel of chlorophyll content would not be counted when the MTCI was lower than 1.41. To facilitate the analysis of spatial differences of chlorophyll content, each mining area was divided into mine and adjacent area. The chlorophyll content in mines (including stopes, waste dumps, and tailings ponds) was then compared with that in adjacent areas. The difference of chlorophyll content among the mines and adjacent areas was analyzed over the six mining areas.

Change in Trend of Vegetation from 2000 to 2019
The trend of vegetation indices in each mining area was generated through linear regression analysis based on the mean MNDVI in the whole area ( Figure 2, Table 3). The results showed that the fitted change slopes were 0.0021/y, 0.0016/y, 0.0031/y, 0.0024/y, 0.0029/y, and 0.0006/y for the Anshan, Benxi, Diaobingshan, Fushun, Fuxin, and Yingkou mining areas, respectively, over the past 20 years. In the Yingkou, Benxi, and Anshan mining areas, the slope was relatively low, indicating that the increasing trend of vegetation was slight. Furthermore, the coefficient of determination (0.066) was so low that it could not pass the significance test in the Yingkou, which means that the rate of vegetation change fluctuated greatly. However, the fitted slope and determination coefficient of the overall vegetation level in Liaoning Province were 0.0037 and 0.854, which were both larger than those of the six mining areas.

Change in Trend of Vegetation from 2000 to 2019
The trend of vegetation indices in each mining area was generated through linear regression analysis based on the mean MNDVI in the whole area ( Figure 2, Table 3). The results showed that the fitted change slopes were 0.0021/y, 0.0016/y, 0.0031/y, 0.0024/y, 0.0029/y, and 0.0006/y for the Anshan, Benxi, Diaobingshan, Fushun, Fuxin, and Yingkou mining areas, respectively, over the past 20 years. In the Yingkou, Benxi, and Anshan mining areas, the slope was relatively low, indicating that the increasing trend of vegetation was slight. Furthermore, the coefficient of determination (0.066) was so low that it could not pass the significance test in the Yingkou, which means that the rate of vegetation change fluctuated greatly. However, the fitted slope and determination coefficient of the overall vegetation level in Liaoning Province were 0.0037 and 0.854, which were both larger than those of the six mining areas.  The spatial distribution map of vegetation change showed that the greatly degraded areas were mainly located in stopes, waste dumps, and tailings ponds ( Figure 3). However, greatly improved areas were also mainly located in some waste dumps. The greatly degraded area was large in the Benxi, Yingkou, and Anshan mining areas, covering 22.083  The spatial distribution map of vegetation change showed that the greatly degraded areas were mainly located in stopes, waste dumps, and tailings ponds ( Figure 3). However, greatly improved areas were also mainly located in some waste dumps. The greatly degraded area was large in the Benxi, Yingkou, and Anshan mining areas, covering 22.083 km 2 , 23.203 km 2 , and 16.783 km 2 , respectively. In the Diaobingshan, Fuxin, and Fushun mining areas, the greatly degraded area was relatively small. The greatly improved area was large in the Anshan, Fushun, and Fuxin mining areas, covering 21.571 km 2 , 20.489 km 2 , and 16.098 km 2 , respectively. In the Benxi, Diaobingshan, and Yingkou mining areas, the greatly improved area was relatively small (Table 3).

Chlorophyll Content Distribution in Mining Areas
Based on the ground experiment, the relationship between MTCI, NDVI, and leaf chlorophyll content was derived. The correlation coefficient between MTCI and chlorophyll content is 0.956 (p < 0.01). However, the correlation coefficient between NDVI and chlorophyll content is −0.268, and it could not pass the significance test ( Figure 4). The performance of MTCI and NDVI was in accordance with the results of the literature [44]. Thus, MTCI could be set as an index for estimating chlorophyll content. The leaf chlorophyll content was then estimated by using MTCI according to Equation (4). The leaf chlorophyll content for each mining area is shown in Figure 5. km 2 , 23.203 km 2 , and 16.783 km 2 , respectively. In the Diaobingshan, Fuxin, and Fushun mining areas, the greatly degraded area was relatively small. The greatly improved area was large in the Anshan, Fushun, and Fuxin mining areas, covering 21.571 km 2 , 20.489 km 2 , and 16.098 km 2 , respectively. In the Benxi, Diaobingshan, and Yingkou mining areas, the greatly improved area was relatively small (Table 3).

Chlorophyll Content Distribution in Mining Areas
Based on the ground experiment, the relationship between MTCI, NDVI, and leaf chlorophyll content was derived. The correlation coefficient between MTCI and chlorophyll content is 0.956 (p < 0.01). However, the correlation coefficient between NDVI and chlorophyll content is −0.268, and it could not pass the significance test (Figure 4). The performance of MTCI and NDVI was in accordance with the results of the literature [44]. Thus, MTCI could be set as an index for estimating chlorophyll content. The leaf chlorophyll content was then estimated by using MTCI according to Equation (4). The leaf chlorophyll content for each mining area is shown in Figure 5.

Chlorophyll Content Distribution in Mining Areas
Based on the ground experiment, the relationship between MTCI, NDVI, and leaf chlorophyll content was derived. The correlation coefficient between MTCI and chlorophyll content is 0.956 (p < 0.01). However, the correlation coefficient between NDVI and chlorophyll content is −0.268, and it could not pass the significance test (Figure 4). The performance of MTCI and NDVI was in accordance with the results of the literature [44]. Thus, MTCI could be set as an index for estimating chlorophyll content. The leaf chlorophyll content was then estimated by using MTCI according to Equation (4). The leaf chlorophyll content for each mining area is shown in Figure 5.  In each mining area, the chlorophyll content in mines (including stope, waste dump, and tailings pond) was compared with that in adjacent areas. The statistical results showed that the chlorophyll value of the pixels in the mines was generally lower than that in adjacent areas, and the histogram of the pixels presented a "left bias" shape ( Figure 6). In contrast, the chlorophyll value in adjacent areas was generally higher, and the histogram of the pixels presented an approximate normal distribution. However, there were differences among these mining areas. In Fushun and Fuxin, the peak value of the histogram of mines shifted to right, and the histogram shape was more similar to adjacent areas. It indicated that the chlorophyll content of vegetation in mines was close to adjacent areas. Furthermore, the ratio of average chlorophyll content in mines to adjacent areas was selected to describe the differences (Figure 7). It was found that the ratio in Fushun, Fuxin, and Yingkou was greater than that in the other three mining areas. In Fushun and Fuxin, the ration was consistent with above histogram results. In Yingkou, the ratio was greater because the peak value of the histogram of the adjacent area shifted to the left, which meant that the average chlorophyll content in the adjacent area was relatively low in Yingkou. In each mining area, the chlorophyll content in mines (including stope, waste dump, and tailings pond) was compared with that in adjacent areas. The statistical results showed that the chlorophyll value of the pixels in the mines was generally lower than that in adjacent areas, and the histogram of the pixels presented a "left bias" shape ( Figure 6). In contrast, the chlorophyll value in adjacent areas was generally higher, and the histogram of the pixels presented an approximate normal distribution. However, there were differences among these mining areas. In Fushun and Fuxin, the peak value of the histogram of mines shifted to right, and the histogram shape was more similar to adjacent areas. It indicated that the chlorophyll content of vegetation in mines was close to adjacent areas. Furthermore, the ratio of average chlorophyll content in mines to adjacent areas was selected to describe the differences (Figure 7). It was found that the ratio in Fushun, Fuxin, and Yingkou was greater than that in the other three mining areas. In Fushun and Fuxin, the ration was consistent with above histogram results. In Yingkou, the ratio was greater because the peak value of the histogram of the adjacent area shifted to the left, which meant that the average chlorophyll content in the adjacent area was relatively low in Yingkou.

Natural Factors for Vegetation Change in These Mining Areas
The driving forces that lead to vegetation change include natural and human factors. Precipitation and temperature are considered as the main limiting natural factors for vegetation growth [45]. For Liaoning Province as a whole, the MNDVI change is highly correlated with precipitation (r = 0.420, p < 0.1) but weakly correlated with temperature (r = −0.014) ( Table 4). For the six mining areas, the correlation between vegetation change and

Natural Factors for Vegetation Change in These Mining Areas
The driving forces that lead to vegetation change include natural and human factors. Precipitation and temperature are considered as the main limiting natural factors for vegetation growth [45]. For Liaoning Province as a whole, the MNDVI change is highly correlated with precipitation (r = 0.420, p < 0.1) but weakly correlated with temperature (r = −0.014) ( Table 4). For the six mining areas, the correlation between vegetation change and

Natural Factors for Vegetation Change in These Mining Areas
The driving forces that lead to vegetation change include natural and human factors. Precipitation and temperature are considered as the main limiting natural factors for vegetation growth [45]. For Liaoning Province as a whole, the MNDVI change is highly correlated with precipitation (r = 0.420, p < 0.1) but weakly correlated with temperature (r = −0.014) ( Table 4). For the six mining areas, the correlation between vegetation change and precipitation is strong in the Fuxin (p < 0.01) and Diaobingshan (p < 0.05) mining areas. This indicates that vegetation is affected by precipitation in those two mining areas. In other words, mining activities have a weak effect on the vegetation there. In the Fuxin mining area, the coal resources are exhausted, and the mining activities are no longer intensive, so the vegetation is not affected by mining activities. In the Diaobingshan mining area, underground mining has a weak effect on vegetation. The correlation between vegetation change trend and precipitation was weak in the Anshan, Benxi, and Yingkou mining areas, which indicates that precipitation has a slight effect on the vegetation change in those three areas. Moreover, the relationship between vegetation and precipitation is consistent with a greatly degraded vegetation area (Tables 3 and 4). The smaller the area of degraded vegetation is, the stronger the relationship with precipitation.

Ecological Restoration for Vegetation Change in These Mining Areas
According to the results of vegetation change, the greatly improved vegetation area is 21.571, 20.489, and 16.098 km 2 in Anshan, Fushun, and Fuxin mining areas, respectively. It is mainly due to ecological restoration for these areas. Coal began to be mined approximately one hundred years ago in Fuxin and Fushun. At the end of the last century, coal resources were exhausted in these areas. As a result of long-term, high-intensity, and open-pit mining, huge pits and coal gangue dumps were formed in these areas. For example, the open pit is 4 km long and 2 km wide, and area of the coal gangue dump is 16 km 2 in Haizhou Surface Mine in Fuxin; and the open pit is 6.6 km long and 2.2 km wide, and area of the coal gangue dumps is 12.9 km 2 in Xilutian Mine in Fushun. Since the beginning of this century, large-scale reclamation activities have been carried out in these areas. After reclamation, the abandoned pits and dumps were covered by woods (such as Ulmus pumila, Robinia pseudoacacia, Amorpha fruticosa) and grass (such as Vitex Chinensis, Ostryopsis davidiana, Imperatacy lindrical, Themeda japonica, Arrndinella hirta).
Similar to coal mining in Fuxin and Fushun, iron ore mining has a long history with more than 100 years in Anshan. At present, there are approximately 8.8 km 2 pits and 38.9 km 2 tailings ponds and dumps around Anshan City. In the last 10 years, some efforts were made to cover these mining sites with vegetation. The Green Mine Programme (GMP), which aims to restore vegetation for mined mountains, was initiated in 2011 in Liaoning Province. From 2012 to 2015, 846 mines were managed with a total area of 48.33 km 2 . Due to these efforts, in this study, greatly improved vegetation was found in waste dumps ( Figure 8). In addition, the greatly improved vegetation area is 2.136, 0.824, and 0.741 km 2 in Yingkou, Diaobingshan, and Benxi mining areas, respectively. The mines are in service in these areas and less reclamation activities were carried out.

Destruction and Pollution of Vegetation by Mining Activities
Mining activities are the main cause of vegetation degradation in these mining areas.
In the stopes of open-pit mines, vegetation is destroyed by mining ore. In waste dumps, vegetation is occupied by waste and tailings. Among the six mining areas, Fushun and Fuxin are coal-exhausted. Due to low-intensity mining activities, the greatly degraded vegetation area is 7.126 km 2 in Fushun and 5.997 km 2 in Fuxin. Diaobingshan is a coal mining area with underground mining, and vegetation there is not obviously affected by mining activities aside from some coal gangues. Thus, the greatly degraded vegetation area is only 1.479 km 2 in Diaobingshan. On the contrary, mining activities are high-intensity in Anshan, Benxi, and Yingkou mining areas, where the annual output of iron ore is more than 1.7 × 10 8 t and magnesite ore is more than 1.3 × 10 7 t. Thus, the greatly degraded area is larger in these three mining areas, with 16.783 km 2 in Anshan, 22.083 km 2 in Benxi, and 23.203 km 2 in Yingkou.
Aside from direct effects of mining, vegetation around mines may be stressed by pollution that enters the environment from mining activities. There are some stress factors in active mining areas, such as dust pollution and water pollution (Figure 9). This phenomenon is obvious in the active, open-pit mining areas, such as Yingkou, Anshan, and Benxi. Deposited dust would cause soil hardening, pollution, and blockage of leaf stomata, and then the leaf chlorophyll content would be reduced for the reclaimed vegetation. Thus, the corresponding histogram of the pixels presented a "left bias" shape in mines in Anshan, Benxi, and Yingkou ( Figure 6). Furthermore, the impact would extend to adjacent areas with the spread of pollutants in some mining areas. For example, in Yingkou mining area, 1.4 × 10 5 t dust is emitted during the mining and sintering process each year, and it contains much magnesium carbonate and magnesium oxide [46]. The vegetation in the adjacent areas would be disturbed by the diffused dust. Compared with Anshan and Benxi, the average chlorophyll content in adjacent area was relatively low in Yingkou for this reason (Figures 6 and 7).

Destruction and Pollution of Vegetation by Mining Activities
Mining activities are the main cause of vegetation degradation in these mining areas. In the stopes of open-pit mines, vegetation is destroyed by mining ore. In waste dumps, vegetation is occupied by waste and tailings. Among the six mining areas, Fushun and Fuxin are coal-exhausted. Due to low-intensity mining activities, the greatly degraded vegetation area is 7.126 km 2 in Fushun and 5.997 km 2 in Fuxin. Diaobingshan is a coal mining area with underground mining, and vegetation there is not obviously affected by mining activities aside from some coal gangues. Thus, the greatly degraded vegetation area is only 1.479 km 2 in Diaobingshan. On the contrary, mining activities are high-intensity in Anshan, Benxi, and Yingkou mining areas, where the annual output of iron ore is more than 1.7 × 10 8 t and magnesite ore is more than 1.3 × 10 7 t. Thus, the greatly degraded area is larger in these three mining areas, with 16.783 km 2 in Anshan, 22.083 km 2 in Benxi, and 23.203 km 2 in Yingkou.
Aside from direct effects of mining, vegetation around mines may be stressed by pollution that enters the environment from mining activities. There are some stress factors in active mining areas, such as dust pollution and water pollution (Figure 9). This phenomenon is obvious in the active, open-pit mining areas, such as Yingkou, Anshan, and Benxi. Deposited dust would cause soil hardening, pollution, and blockage of leaf stomata, and then the leaf chlorophyll content would be reduced for the reclaimed vegetation. Thus, the corresponding histogram of the pixels presented a "left bias" shape in mines in Anshan, Benxi, and Yingkou ( Figure 6). Furthermore, the impact would extend to adjacent areas with the spread of pollutants in some mining areas. For example, in Yingkou mining area, 1.4 × 10 5 t dust is emitted during the mining and sintering process each year, and it contains much magnesium carbonate and magnesium oxide [46]. The vegetation in the Benxi, the average chlorophyll content in adjacent area was relatively low in Yingkou for this reason (Figures 6 and 7).

Conclusions
Mining activities can affect vegetation directly and indirectly. To quantitatively determine the effect, MODIS NDVI and Sentinel-2A data were used to monitor the vegetation change in six mining areas in Liaoning Province, North China. The conclusions are as follows.
(1) MODIS NDVI time series data were used to monitor the vegetation from 2000 to 2019 using a change trend analysis method. Over the full 20 years, the overall trend of vegetation in mining areas was positive, but it was lower than the average for all of Liaoning Province. Open-pit mining activities have a greater impact on vegetation than underground mining. Vegetation was highly degraded in the Yingkou, Benxi, and Anshan mining areas due to intensive mining activities there. Vegetation degradation was much

Conclusions
Mining activities can affect vegetation directly and indirectly. To quantitatively determine the effect, MODIS NDVI and Sentinel-2A data were used to monitor the vegetation change in six mining areas in Liaoning Province, North China. The conclusions are as follows.
(1) MODIS NDVI time series data were used to monitor the vegetation from 2000 to 2019 using a change trend analysis method. Over the full 20 years, the overall trend of vegetation in mining areas was positive, but it was lower than the average for all of Liaoning Province. Open-pit mining activities have a greater impact on vegetation than underground mining. Vegetation was highly degraded in the Yingkou, Benxi, and Anshan mining areas due to intensive mining activities there. Vegetation degradation was much less notable in the coal-exhausted Fushun and Fuxin mining areas and was not obvious in the Diaobingshan mining area because of underground mining.
(2) Sentinel-2A data were used to infer leaf chlorophyll content by using MTCI in the mining areas. The leaf chlorophyll content in the mines was generally lower than adjacent areas in the six mining areas, but there were individual differences among these mining areas. In the Yingkou mining area, the chlorophyll content in adjacent areas was close to the magnesite mines, which meant the spillover effect of environmental pollution in mines should be considerable. In the Anshan, Benxi, and Diaobingshan mining areas, the environmental stress on adjacent areas was slight. (