西南高山峡谷区水土流失风险评估与管理策略
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Q948.112???

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国家重点研发计划项目(2022YFF1302905, 2022YFF1302900); 北京林业大学“5 · 5工程”科研创新团队项目(BLRC2023B09)


Assessment and management strategies for soil erosion risk in the Southwest Alpine Canyon Area of China
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National Key Research and Development Program Project(2022YFF1302905、2022YFF1302900) ; Research and Innovation Team Project of the "5·5 Engineering" at Beijing Forestry University (BLRC2023B09)

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    摘要:

    西南高山峡谷区因地势高陡、气候多变以及多种侵蚀营力驱动,导致水土流失分异明显、侵蚀类型复杂且矛盾突出,严重制约了当地生态环境的可持续发展。为科学评估水土流失风险并制定防治策略,研究从水土流失危险性、景观脆弱性、生态系统潜在损失的三维度构建水土流失风险评估指标体系,采用RUSLE模型耦合冻融侵蚀模型评估危险性,利用景观格局指数和InVEST模型计算脆弱性和潜在损失,系统评估了2000—2020年研究区水土流失风险的时空演变格局,并提出针对性管理措施。结果表明:(1)西南高山峡谷区水力侵蚀和冻融侵蚀面积占比分别为69.98%和30.02%,形成南水蚀、北冻蚀的空间分布格局。水力侵蚀以微度为主(69.38%),冻融侵蚀则以轻度(50.15%)和中度(33.69%)为主。(2)研究区水土流失风险总体较低,约87.42%的区域处于极低和低风险水平;空间分布呈西北-东南较高、西南-东北较低以及局部聚集、全局分散的特点。近二十年,水土流失风险整体呈增加态势,中及以上风险区面积增加了34.49%,但近十年加剧趋势有所减缓。(3)藏东川西南高山峡谷生态维护水源涵养区(Ⅱ区)水土流失风险水平上升最为明显,而滇北川西南高山峡谷蓄水保土区(Ⅲ区)的中高风险区转移率最高,均有超过50%的区域向更高风险级别转移,成为高风险转移的热点区域。研究表明,西南高山峡谷区水土流失风险类型多样,未来应加强低风险区生态稳定性以降低潜在的水土流失风险,同时针对高风险区制定并积极实施切实可行的恢复策略以修复受损生态系统,保障区域生态系统可持续性。

    Abstract:

    The Southwest Alpine Canyon Area of China exhibits pronounced soil erosion differentiation and complex erosion patterns due to steep terrain, variable climate, and multiple erosional drivers, posing significant challenges to local ecological sustainability. To scientifically assess soil erosion risks and formulate mitigation strategies, this study established a three-dimensional risk assessment framework integrating erosion hazard, landscape vulnerability, and potential ecosystem loss. The Revised Universal Soil Loss Equation (RUSLE) coupled with a freeze-thaw erosion model was employed to evaluate erosion hazard, while landscape pattern indices and the InVEST model were utilized to quantify vulnerability and potential loss. The spatiotemporal evolution of soil erosion risks from 2000 to 2020 was systematically analyzed, and targeted management measures were proposed. Key findings include: (1) Hydraulic and freeze-thaw erosion accounted for 69.98% and 30.02% of total erosion area, respectively, forming a distinct spatial pattern dominated by hydraulic erosion in the south and freeze-thaw erosion in the north. Hydraulic erosion primarily occurred at mild intensity (69.38%), whereas freeze-thaw erosion was predominantly light (50.15%) and moderate (33.69%).(2) Overall soil erosion risk remains relatively low, with 87.42% of the region classified as low and medium-low risk. Spatially, higher risks were concentrated in the northwest-southeast regions and exhibited localized aggregation with global dispersion. Over the past two decades, soil erosion risk showed an increasing trend, followed by a period of decline, but the overall trend was still upwards. The medium- or high-risk areas increased by 34.49%, but the rate of increase slowed down over the past decade. (3) The Eastern Tibet-Western Sichuan Alpine Canyon Ecological Conservation and Water Retention Zone (Zone Ⅱ) experienced the most pronounced risk escalation, while the Northern Yunnan-Western Sichuan Alpine Canyon Soil and Water Conservation Zone (Zone Ⅲ) showed the highest transition rate of medium-to-high risk areas, with over 50% of zones shifting to higher risk levels, marking these as critical hotspots. This study underscores the diversity of soil erosion risks in southwestern alpine canyons. Future efforts should prioritize ecological stability in low-risk zones to mitigate potential degradation while implementing region-specific restoration strategies in high-risk areas to rehabilitate degraded ecosystems and ensure regional ecological sustainability.

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兰梦瑶,关颖慧,周金星,王文刚,程陆陆,刘静.西南高山峡谷区水土流失风险评估与管理策略.生态学报,2025,45(20):9932~9949

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