Yu Huanhuan, Chen Peng, Sun Yingyue
College of Geographic Science and Tourism, Jilin Normal University, Siping, 136000, Jlin, China.
Sci Rep. 2024 Sep 20;14(1):21955. doi: 10.1038/s41598-024-72782-5.
Lishu County, which is located in the black soil region of Northeast China, represents a key site for the analysis of soil erosion intensity. This study offers a scientific foundation for the development of targeted soil and water conservation strategies within the region. The Revised Universal Soil Loss Equation (RUSLE) was employed to compute the soil erosion modulus in Lishu County, with the objective of conducting a quantitative analysis of the temporal and spatial distribution patterns of soil erosion. Additionally, the changing characteristics of soil erosion were examined from the perspectives of land use types and slope variations. The Generalized Connectivity Causality Model (GCCM) was utilized to identify the causal relationship between soil erosion and land use types through the reconstruction of state space and cross-mapping predictions. (1) Soil erosion in Lishu County between 2000 and 2020 predominantly exhibited mild to moderate levels, characterized by patchy and sporadic erosion, with relatively severe occurrences in the northern and central regions. (2) Soil erosion was correlated with land use and slope variations, with more than 90% of erosion incidents transpiring in cultivated land areas. The 3°-5° slope range in Lishu County emerged as a focal point for erosion, necessitating targeted prevention and control measures. (3) The GCCM model illustrated a discernible causal relationship between soil erosion and land use, revealing mutual influences between the two factors. Between 2000 and 2020, both the area and intensity of soil erosion in Lishu County exhibited an initial increase, followed by a subsequent decrease. This suggests an overall trend of amelioration in soil erosion conditions. However, notable spatial disparities persist in the erosion distribution across the region.
梨树县位于中国东北黑土区,是分析土壤侵蚀强度的关键地点。本研究为该地区制定针对性的水土保持策略提供了科学依据。采用修正通用土壤流失方程(RUSLE)计算梨树县的土壤侵蚀模数,旨在对土壤侵蚀的时空分布格局进行定量分析。此外,还从土地利用类型和坡度变化的角度研究了土壤侵蚀的变化特征。利用广义连通性因果模型(GCCM),通过状态空间重构和交叉映射预测,识别土壤侵蚀与土地利用类型之间的因果关系。(1)2000—2020年梨树县土壤侵蚀以轻度至中度为主,呈斑块状、零星分布,北部和中部地区侵蚀相对严重。(2)土壤侵蚀与土地利用和坡度变化相关,90%以上的侵蚀事件发生在耕地。梨树县3°—5°坡度范围是侵蚀重点区域,需采取针对性防治措施。(3)GCCM模型表明土壤侵蚀与土地利用之间存在明显因果关系,二者相互影响。2000—2020年,梨树县土壤侵蚀面积和强度均呈先增加后降低趋势,表明土壤侵蚀状况总体呈改善趋势。但区域侵蚀分布仍存在明显空间差异。