1982-2022年南方红壤区降雨侵蚀力时空格局演变及归因分析
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1.中国林业科学研究院热带林业研究所;2.国际竹藤中心

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基金项目:

国家重点研发计划课题(2022YFF1303004);国家自然科学基金项目(32301669)


Spatial-temporal pattern evolution and attribution analysis of rainfall erosivity in the red soil region of southern China from 1982 to 2022
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Affiliation:

1.中国林业科学研究院热带林业研究所;2.Research Institute of Tropical Forestry, Chinese Academy of Forestry

Fund Project:

National Key Research and Devel opment Program of China (2022YFF1303004); National Natural Science Foundation of China (32301669)

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    摘要:

    降雨侵蚀力是衡量降雨对土壤侵蚀潜力的重要指标,研究其长期演变规律对于区域水土保持规划及生态系统管理具有重要意义。基于南方红壤区279个气象站1982-2022年逐日降雨资料,采用Mann-Kendall非参数检验、Kriging插值、重力模型、地理探测器等方法分析了南方红壤区降雨侵蚀力的变化趋势、分布特征及影响因素,以期为南方红壤区土壤侵蚀预报及水土流失治理提供参考。结果表明:南方红壤区1982-2022年均降雨侵蚀力为8786.95 MJ·mm·hm-2·h-1·a-1,呈显著上升趋势。季节降雨侵蚀力分布不均,约有五成发生在夏季,受降雨侵蚀的风险最高;南方红壤区年降雨侵蚀力变化范围为3628.89~24654.70 MJ·mm·hm-2·h-1·a-1,总体呈现自北向南增加的趋势,大部分分区(83.7%)的年降雨侵蚀力呈现上升趋势;侵蚀性降雨量的q值为0.872,是南方红壤区降雨侵蚀力增加的主要驱动力,侵蚀性降雨日数、雨强和纬度是次要影响因素,q值分别为0.504、0.492和0.388。交互作用上,侵蚀性降雨量与侵蚀性雨强交互作用的q值最大为0.950。经纬度和海拔等地理因子根据区域的不同表现出不同的影响力,南方红壤区降雨侵蚀力的变化是多种因素共同作用的结果。由于地貌复杂、气候变化加剧和人类高强度活动,南方红壤区水土流失问题依然严峻,应根据各分区具体情况进一步加强相应的水土保持措施。

    Abstract:

    Rainfall erosivity serves as an important indicator of soil erosion potential due to rainfall. Analyzing the long-term evolution of rainfall erosivity is significant for regional soil and water conservation planning and ecosystem management. This study used the daily rainfall data from 279 meteorological stations in the southern red soil region from 1982 to 2022 to analyze rain fall erosivity. The rainfall erosivity at each station was calculated using the Zhang model. The spatial-temporal variation trend, distribution characteristics and climatic and geographic drivers of the rainfall erosivity were analyzed using the Mann-Kendall test, the Kriging interpolation, the gravity model and GeoDetector. The results show that the annual average rainfall erosivity in the southern red soil region was 8786.95 MJ·mm·hm-2·h-1·a-1 from 1982-2022, exhibiting a significant upward trend. Seasonal rainfall erosivity was unevenly distributed, with approximately 50% occurring in summer, leading to the highest soil erosion risk due to rainfall. The annual rainfall erosivity in the southern red soil region ranged from 3,628.89 to 24,654.70 MJ·mm·hm-2·h-1·a-1 and showed an overall spatial trend of increasing from north to south. Most subregions (83.7%) also had an increasing annual rainfall erosivity. Erosive rainfall had a q-value of 0.872 and was the main driving force of the increase in rainfall erosivity in the southern red soil region. The number of erosive rainfall days, rainfall intensity and latitude were the secondary influencing factors, with a q-value of 0.504, 0.492 and 0.388, respectively. The q-value for the interaction between erosive rainfall and intensity was the highest (0.950). Geographical factors, such as latitude, longitude and elevation, showed different influences across regions. The variations in rainfall erosivity resulted from the combined effect of various factors. Due to the complex topography, exacerbated climate change and intense human activities, soil and water erosion remained a significant issue in the southern red soil region. Therefore, it is imperative to enhance soil and water conservation measures based on specific regional conditions. The findings can provide a reference for soil erosion forecast and management in the southern red soil area.

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李嘉睿,李乐,郝泽周,高丙涛,叶天一,孙冰,陈雷,裴男才.1982-2022年南方红壤区降雨侵蚀力时空格局演变及归因分析.生态学报,,(). http://dx. doi. org/10.5846/stxb202407231738

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