Key Laboratory for Geographical Process Analysis & Simulation of Hubei Province, Central China Normal University, Wuhan 430079, China.
The College of Urban & Environmental Sciences, Central China Normal University, Wuhan 430079, China.
Int J Environ Res Public Health. 2022 Jan 29;19(3):1571. doi: 10.3390/ijerph19031571.
Accelerated land use and land cover changes affect regional landscape patterns and change the ecological environment, including soil conservation capabilities. This is not conducive to the sustainable development of human society. In this research, we explored the land use change pattern and landscape change pattern in western Hubei from 2000 to 2020. Using the Chinese soil loss equation and stepwise regression, we measure how landscape patterns affect soil erosion under land use and cover changes in western Hubei Province. The results show that average soil erosion in the mountainous areas of western Hubei tended to increase from 2000 to 2010 and decrease from 2010 to 2020; soil erosion was higher in the western than in the eastern part of the study area. The land in areas with high-intensity and low-intensity soil erosion was mainly waterfront/grassland and cropland/forestland, respectively, and the area of moderate to severe soil erosion was greatest when the slope was 10-20°. When the slope exceeded 20°, the soil erosion area of each grade tended to decrease; thus, 20° is the critical slope for soil erosion in the study area. The landscape pattern in mountainous areas changed dramatically from 2000 to 2020. At the landscape level, landscape fragmentation increased and connectivity decreased, but the area of landscape diversity was stable. Soil erosion in western Hubei was positively correlated with the contiguity index, aggregation index and largest patch index but negatively correlated with the Shannon evenness index. The higher the landscape fragmentation and the greater the accumulation of single land-use types, the more severe the soil erosion is, while the higher the landscape connectivity and the richer the landscape diversity, the less severe the soil erosion is. The results can inform regional landscape management and soil conservation research.
土地利用和土地覆被变化的加速影响区域景观格局,并改变生态环境,包括土壤保持能力。这不利于人类社会的可持续发展。在本研究中,我们探讨了 2000 年至 2020 年期间鄂西地区的土地利用变化格局和景观变化格局。利用中国土壤流失方程和逐步回归方法,我们测量了景观格局在鄂西地区土地利用和覆被变化下对土壤侵蚀的影响。结果表明,鄂西山区的平均土壤侵蚀量在 2000 年至 2010 年期间呈上升趋势,在 2010 年至 2020 年期间呈下降趋势;西部地区的土壤侵蚀量高于东部地区。高强度和低强度土壤侵蚀的土地主要是滨水/草地和耕地/林地,而中等至严重土壤侵蚀的面积在坡度为 10-20°时最大。当坡度超过 20°时,各等级的土壤侵蚀面积趋于减少;因此,20°是研究区土壤侵蚀的临界坡度。从 2000 年到 2020 年,山区的景观格局发生了巨大变化。在景观水平上,景观破碎度增加,连通性降低,但景观多样性面积保持稳定。鄂西地区的土壤侵蚀与连接度指数、聚集度指数和最大斑块指数呈正相关,与 Shannon 均匀度指数呈负相关。景观破碎度越高,单一土地利用类型的积累越多,土壤侵蚀越严重,而景观连通度越高,景观多样性越丰富,土壤侵蚀越不严重。研究结果可为区域景观管理和土壤保持研究提供信息。