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Spatio-temporal change in land uses of the black soil area in northeast China over the past half century |
XIAO Hong-Ye1,2,3( ), LIU Guo-Dong1,2,3, YANG Ze1,2,3, FANG Na-Na1,2,3, DAI Hui-Min1,2,3, LIU Kai1,2,3, HAN Xiao-Meng1,2,3, ZHU Heng1( ) |
1. Shenyang Center of China Geological Survey, Shenyang 110034, China 2. Key Laboratory of Black Soil Evolution and Ecological Effect, Ministry of Natural Resources, Shenyang 110034, China 3. Key Laboratory of Black Soil Evolution and Ecological Effect, Liaoning Province, Shenyang 110034, China |
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Abstract As one of four major black soil areas in the world, the black soil area in northeast China boasts fertile and rare black soil resources, and its protection and utilization have always attracted much attention. The changes in land uses/cover affect the structure, function, and health of the ecosystem and thus are greatly significant for the sustainable utilization of land resources. Based on the data on the land uses/cover in 1970, 1995, 2010, and 2020, this study analyzed the spatio-temporal characteristics of the change in the land uses of the black soil area in northeast China over the past half century using the methods, such as transfer matrix, comprehensive dynamic degree, and spatial change model. The results are as follows. ①The areas of construction land, cultivated land, and grassland in the black soil area of northeast China generally increased over the past half century, whereas the areas of wetland, woodland, and unused land generally decreased. The changes in land types mainly occurred in the Sanjiang Plain, the northwestern Songnen Plain, and the Xiliaohe Plain. ②The change in each land type was dominated by the alternating quantity, with a large amount of spatial position shift occurring. ③The degree of land utilization slightly increased yearly but is still lower than the national level, suggesting considerable potential for land development and utilization. Therefore, further studies should focus on the spatio-temporal characteristics and mechanisms of the change in the land uses of the black soil area in northeast China, as well as their impacts on the habitats, ecological service functions, and balance of carbon budget, to fully utilize and protect the black soil area and optimize the national spatial layout.
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Received: 27 January 2022
Published: 03 January 2023
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Corresponding Authors:
ZHU Heng
E-mail: kaolakaola1987@163.com;zhuheng129@126.com
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土地利用类型 | 土地利用属性 | 耕地 | 水田、旱地 | 林地 | 有林地、灌木林、疏林地和其他林地 | 草地 | 高覆盖度草地、中覆盖度草地和低覆盖度草地 | 湿地 | 河渠、湖泊、水库坑塘、滩涂、滩地和沼泽地 | 建设用地 | 城镇用地、农村居民点和其他建设用地 | 未利用地 | 沙地、戈壁、盐碱地、永久性冰川雪地、裸土地、裸岩石质地和其他未利用土地 |
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Land use type classification table
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地类 | A1 | A2 | … | Aj | … | An | 期初面积 | 减少面积 | A1 | P11 | P12 | … | P1j | … | P1n | P1+ | P1+-P11 | A2 | P21 | P22 | … | P2j | … | P2n | P2+ | P2+-P22 | … | … | … | … | … | … | … | … | … | Ai | Pi1 | Pi2 | … | Pij | … | Pin | Pi+ | Pi+-Pii | … | … | … | … | … | … | … | … | … | An | Pn1 | Pn2 | … | Pnj | … | Pnn | Pn+ | Pn+-Pnn | 期末面积 | P+1 | P+2 | … | P+j | … | P+n | 1 | - | 增加面积 | P+1-P11 | P+2-P22 | … | P+j-Pjj | … | P+n-Pnn | - | - |
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Land use transfer matrix
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Line chart of land use area changes for various types from 1970 to 2020
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The spatial transfer of land use for various types from 1970 to 2020
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土地类型 | 耕地 | 林地 | 草地 | 湿地 | 建设用地 | 未利用地 | 期初 | 减少 | 耕地 | 2196.40 | 80.39 | 89.28 | 44.30 | 58.09 | 6.71 | 2475.17 | 278.77 | 林地 | 306.96 | 4212.16 | 389.52 | 56.19 | 7.73 | 5.38 | 4977.93 | 765.78 | 草地 | 301.58 | 207.69 | 1139.65 | 86.16 | 15.6 | 57.03 | 1807.71 | 668.06 | 湿地 | 243.91 | 122.88 | 286.02 | 468.81 | 4.67 | 10.97 | 1137.25 | 668.44 | 建设用地 | 30.22 | 1.95 | 4.48 | 1.83 | 151.54 | 0.9 | 190.91 | 39.37 | 未利用地 | 10.73 | 6.18 | 68.49 | 11.28 | 2.31 | 133.27 | 232.25 | 98.98 | 期末 | 3089.8 | 4631.26 | 1977.43 | 668.56 | 239.93 | 214.25 | 10821.23 | 2519.40 | 新增 | 893.4 | 419.1 | 837.78 | 199.75 | 88.39 | 80.99 | 2519.4 | |
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The transfer matrix of land use area in black soil area from 1970 to 2020104hm2
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土地类型 | 耕地 | 林地 | 草地 | 湿地 | 建设用地 | 未利用地 | 期初 | 减少 | 耕地 | 20.30 | 0.74 | 0.83 | 0.41 | 0.54 | 0.06 | 22.87 | 2.58 | 林地 | 2.84 | 38.92 | 3.6 | 0.52 | 0.07 | 0.05 | 46.00 | 7.08 | 草地 | 2.79 | 1.92 | 10.53 | 0.80 | 0.14 | 0.53 | 16.71 | 6.17 | 湿地 | 2.25 | 1.14 | 2.64 | 4.33 | 0.04 | 0.10 | 10.51 | 6.18 | 建设用地 | 0.28 | 0.02 | 0.04 | 0.02 | 1.4 | 0.01 | 1.76 | 0.36 | 未利用地 | 0.10 | 0.06 | 0.63 | 0.10 | 0.02 | 1.23 | 2.15 | 0.91 | 期末 | 28.55 | 42.80 | 18.27 | 6.18 | 2.22 | 1.98 | 100.00 | 23.28 | 新增 | 8.26 | 3.87 | 7.74 | 1.85 | 0.82 | 0.75 | 23.28 | |
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Matrix of land use transfer rate in black soil area from 1970 to 2020%
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Variation of each land type
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The area change rate of each land type in the black soil area from 1970 to 2020
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Curve diagram of comprehensive dynamic degree of land use
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土地利用类型 | 未利用土地 | 林地、草地、湿地 | 耕地 | 建设用地 | 分级指数 | 1 | 2 | 3 | 4 |
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Land use degree classification assignment table
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Comprehensive index of land use degree in different years
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Land use transfer network for different time periods in the black soil area of Northeast China in the past half century
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The change of the gravity center for each land type in 50 years
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ZHANG Chun-Lai, YANG Hui, Huang Fen, CAO Jian-Hua. Distribution and influencing factors of selenium content in soil in karst areas in Mashan County, Guangxi, China[J]. Geophysical and Geochemical Exploration, 2021, 45(6): 1497-1503. |
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