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Journal of Arid Land  2025, Vol. 17 Issue (2): 224-244    DOI: 10.1007/s40333-025-0073-z     CSTR: 32276.14.JAL.0250073z
Research article     
Spatiotemporal evolution of ecological environment quality and its drivers in the Helan Mountain, China
HE Yuanrong1,2, CHEN Yuhang1,*(), ZHONG Liang1, LAI Yangfeng1, KANG Yuting1, LUO Ming1, ZHU Yunfei3, ZHANG Ming3
1Digital Fujian Institute of Big Data for Natural Disaster Monitoring, Xiamen University of Technology, Xiamen 361000, China
2Hunan Key Laboratory of Remote Sensing Monitoring of Ecological Environment in Dongting Lake Area, Changsha 410004, China
3Zhundong Oil Production Plant, Xinjiang Oilfield Company, Changji 831511, China
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Abstract  

Understanding the ecological evolution is of great significance in addressing the impacts of climate change and human activities. However, the ecological evolution and its drivers remain inadequately explored in arid and semi-arid areas. This study took the Helan Mountain, a typical arid and semi-arid area in China, as the study area. By adopting an Enhanced Remote Sensing Ecological Index (ERSEI) that integrates the habitat quality (HQ) index with the Remote Sensing Ecological Index (RSEI), we quantified the ecological environment quality of the Helan Mountain during 2010-2022 and analyzed the driving factors behind the changes. Principal Component Analysis (PCA) was used to validate the composite ERSEI, enabling the extraction of key features and the reduction of redundant information. The results showed that the contributions of first principal component (PC1) for ERSEI and RSEI were 80.23% and 78.72%, respectively, indicating that the ERSEI can provide higher precision and more details than the RSEI in assessing ecological environment quality. Temporally, the ERSEI in the Helan Mountain exhibited an initial decline followed by an increase from 2010 to 2022, with the average value of ERSEI ranging between 0.298 and 0.346. Spatially, the ERSEI showed a trend of being higher in the southwest and lower in the northeast, with high-quality ecological environments mainly concentrated in the western foothills at higher altitudes. The centroid of ERSEI shifted northeastward toward Helan County from 2010 to 2022. Temperature and digital elevation model (DEM) emerged as the primary drivers of ERSEI changes. This study highlights the necessity of using comprehensive monitoring tools to guide policy-making and conservation strategies, ensuring the resilience of fragile ecosystems in the face of ongoing climatic and anthropogenic pressures. The findings offer valuable insights for the sustainable management and conservation in arid and semi-arid ecosystems.



Key wordsecological environment quality      Enhanced Remote Sensing Ecological Index (ERSEI)      Principal Component Analysis (PCA)      Moran's I      centroid migration analysis      geographic detector (Geodetector)      Helan Mountain     
Received: 08 August 2024      Published: 28 February 2025
Corresponding Authors: *CHEN Yuhang (E-mail: 2222031097@stu.xmut.edu.cn)
Cite this article:

HE Yuanrong, CHEN Yuhang, ZHONG Liang, LAI Yangfeng, KANG Yuting, LUO Ming, ZHU Yunfei, ZHANG Ming. Spatiotemporal evolution of ecological environment quality and its drivers in the Helan Mountain, China. Journal of Arid Land, 2025, 17(2): 224-244.

URL:

http://jal.xjegi.com/10.1007/s40333-025-0073-z     OR     http://jal.xjegi.com/Y2025/V17/I2/224

Fig. 1 Overview of the Helan Mountain based on the digital elevation model (DEM)
Data Resolution (m) Time period Unit Data source
Landsat 5 TM images 30 2010 - EarthExplorer (https://earthexplorer.usgs.gov/)
Landsat 8 OLI images 30 2014-2022 - GSCloud (https://www.gscloud.cn/)
Precipitation 1000 2010-2022 mm Resources and Environmental Science Data Center (http://www.resdc.cn)
Temperature 1000 2010-2022 Resources and Environmental Science Data Center (http://www.resdc.cn)
DEM 15 2022 m GSCloud (https://www.gscloud.cn/)
Slope 15 2022 ° GSCloud (https://www.gscloud.cn/)
NPP 30 2022 g C/(m2•a) GSCloud (https://www.gscloud.cn/)
Population density 1000 2010-2022 persons/km2 GSCloud (https://www.gscloud.cn/)
LULC 1000 2010-2022 - Resources and Environmental Science Data Center (http://www.resdc.cn)
Table 1 Detailed description of data used in the study
Fig. 2 Technical workflow of this study. GEE, Google Earth Engine; LULC, land use and land cover; NDVI, Normalized Difference Vegetation Index; WET, Wetness Component; NDBSI, Normalized Difference Built-up and Soil Index; LST, Land Surface Temperature; HQ, habitat quality; PCA, Principal Component Analysis; ERSEI, Enhanced Remote Sensing Ecological Index; RSEI, Remote Sensing Ecological Index; Geodetector, geographic detector.
Threat factor Maximum impact distance (km) Weight Decay type
Farmland 0.5 0.2 Linear
Construction land 5.0 0.5 Index
Table 2 Threat factors and their weights in the study area
LULC type Habitat suitability Sensitivity
Farmland Construction land
Farmland 0.3 0.0 0.5
Woodland 1.0 0.4 0.6
Grassland 0.7 0.3 0.4
Shrubland 0.8 0.3 0.4
Wetland 1.0 0.4 0.5
Water body 0.9 0.6 0.7
Construction land 0.0 0.0 0.0
Unused land 0.0 0.0 0.0
Table 3 Habitat suitability of each LULC type and its sensitivity to different coercion factor
Description Interaction effect
q(F1∩F2)<min(q(F1), q(F2)) Nonlinear attenuation
min(q(F1), q(F2))<q(F1∩F2)<max(q(F1), q(F2)) Single-factor nonlinear attenuation
q(F1∩F2)>max(q(F1), q(F2)) Two-factor enhancement
q(F1∩F2)=q(F1)+q(F2) Independent
q(F1∩F2)>q(F1)+q(F2) Nonlinear enhancement
Table 4 Description of interaction effects caused by the interaction between driving factors
Fig. 3 Spatial distributions of LULC type (a-f), RSEI (g-l), and ERSEI (m-r) in region A, region B, and region C in the Helan Mountain in 2010 and 2022
Index Target PC1 PC2 PC3 PC4 PC5
RSEI NDVI 0.5472 -0.2350 0.5989 -0.5355 -
WET 0.4684 0.7028 -0.4334 -0.3144 -
LST -0.5086 0.6241 0.5731 -0.1527 -
NDBSI -0.4716 -0.2477 -0.3537 -0.7689 -
Eigenvalue 0.1848 0.0204 0.0107 0.0023 -
Contribution (%) 78.72 12.34 7.90 1.05 -
ERSEI NDVI 0.5277 -0.1432 -0.2462 -0.6146 -0.5124
WET 0.4471 -0.2667 0.6561 0.4461 -0.3153
LST -0.5077 -0.0488 0.6372 -0.5595 -0.1443
NDBSI -0.4335 0.1993 -0.2223 0.3253 -0.7856
HQ 0.2756 0.9307 0.2311 -0.0657 -0.0086
Eigenvalue 0.1740 0.0404 0.0177 0.0101 0.0020
Contribution (%) 80.23 8.88 5.24 5.02 1.03
Table 5 Principal Component Analysis results of ERSEI and RSEI
Fig. 4 Spatial variations in NDVI (a1-a4), LST (b1-b4), WET (c1-c4), NDBSI (d1-d4), and HQ (e1-e4) in the the Helan Mountain during 2010-2022
Fig. 5 Temporal variations in the mean NDVI, WET, NDBSI, LST and HQ in the Helan Mountain during 2010-2022
Fig. 6 Spatial distributions of ERSEI in the Helan Mountain in 2010 (a), 2014 (b), 2018 (c), and 2022 (d), as well as trend in ERSEI during 2010-2022
Fig. 7 Area and proportion of different grades of ecological environment quality during 2010-2022
Fig. 8 Global Moran's I scatter plots for ERSEI in the Helan Mountain in 2010 (a), 2014 (b), 2018 (c), and 2022 (d)
Fig. 9 Elliptical distributions and their corresponding centroids for ERSEI in the Helan Mountain in different years from 2010 to 2020 (a) and a closer view of the centroid migration trajectory of ERSEI (b)
Year Latitude Longitude Angle Oblateness
2010 38°50′53″N 106°00′32″E 40°00′00″ 0.65
2014 38°51′14″N 106°01′19″E 40°34′48″ 0.66
2018 38°51′25″N 106°01′41″E 40°58′48″ 0.66
2022 38°51′32″N 106°01′30″E 41°03′00″ 0.66
Table 6 Centroid migration analysis of the ERSEI in the study area during 2010-2022
Driving factor 2010 2014 2018 2022 2010-2022
q-value P-value q-value P-value q-value P-value q-value P-value Average q-value rank
NPP 0.300 >0.05 0.580 >0.05 0.422 >0.05 0.420 >0.05 0.431 4
Temperature 0.662 <0.01 0.599 <0.01 0.579 <0.01 0.571 <0.01 0.603 1
Population density 0.063 >0.05 0.049 >0.05 0.030 >0.05 0.034 >0.05 0.043 7
Precipitation 0.649 <0.01 0.606 <0.01 0.541 <0.01 0.557 <0.01 0.588 3
DEM 0.657 <0.01 0.590 <0.01 0.559 <0.01 0.554 <0.01 0.590 2
Slope 0.217 >0.05 0.197 >0.05 0.191 >0.05 0.210 >0.05 0.204 5
Aspect 0.103 >0.05 0.118 >0.05 0.139 >0.05 0.136 >0.05 0.124 6
Table 7 Impacts of various driving factors on ERSEI from 2010 to 2022
Fig. 10 Results of interaction detection showing the combined effects of any two driving factors on ERSEI changes in the Helan Mountain for 2010 (a), 2014 (b), 2018 (c), and 2022 (d)
Index Ecological restoration sites
Very poor Poor Fair Good Excellent
ERSEI 101 49 10 6 3
IRSEI 87 50 20 8 4
Table 8 Ecological environment quality of 169 ecological restoration sites scaled by ERSEI and IRSEI
Fig. 11 Distribution of 169 key ecological restoration sites (a), Rujigou mine area based on GF-1 remote sensing image in 2013 (b), and Rujigou mine area based on GF-2 remote sensing image in 2021 (c). The distribution data of 169 key ecological restoration sites and high-resolution remote sensing imagery were provided by the Department of Natural Resources of Ningxia Hui Autonomous Region.
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