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    周宇欣, 姜群鸥, 刘兰华, 何财松, 周扬, 格桑卓玛. 藏东南地区水土流失及其生态风险评估[J]. 北京林业大学学报, 2023, 45(7): 88-98. DOI: 10.12171/j.1000-1522.20220404
    引用本文: 周宇欣, 姜群鸥, 刘兰华, 何财松, 周扬, 格桑卓玛. 藏东南地区水土流失及其生态风险评估[J]. 北京林业大学学报, 2023, 45(7): 88-98. DOI: 10.12171/j.1000-1522.20220404
    Zhou Yuxin, Jiang Qunou, Liu Lanhua, He Caisong, Zhou Yang, Kassandro Mar. Soil and water loss and ecological risk assessment in southeastern Tibet of southwestern China[J]. Journal of Beijing Forestry University, 2023, 45(7): 88-98. DOI: 10.12171/j.1000-1522.20220404
    Citation: Zhou Yuxin, Jiang Qunou, Liu Lanhua, He Caisong, Zhou Yang, Kassandro Mar. Soil and water loss and ecological risk assessment in southeastern Tibet of southwestern China[J]. Journal of Beijing Forestry University, 2023, 45(7): 88-98. DOI: 10.12171/j.1000-1522.20220404

    藏东南地区水土流失及其生态风险评估

    Soil and water loss and ecological risk assessment in southeastern Tibet of southwestern China

    • 摘要:
        目的  分析藏东南地区水土流失时空演变特征,进行水土流失生态风险综合评估,以期为藏东南地区水土流失防控工作提供理论依据和科学指导。
        方法  采用USLE模型对研究区2014、2017和2020年土壤侵蚀模数和水土流失敏感性指数进行估算;然后基于降水、土壤、植被覆盖、敏感性指数等指标,对藏东南地区水土流失生态风险进行综合评估。
        结果  (1)藏东南地区整体土壤侵蚀模数相对较低,土壤侵蚀等级主要以微度侵蚀和轻度侵蚀为主,二者面积约占研究区面积的95%;在时间尺度上,微度侵蚀区域呈现逐渐发展为轻度侵蚀区的趋势。(2)2014—2020年,区域水土流失敏感性指数最高值在3.0左右波动,2017年有所上升,2020年又小幅回落,整体上数值变化不大;高值区主要分布在高山冰雪覆盖地带,低值区主要分布在高植被覆盖区域。(3)区域水土流失生态风险指数在1.2 ~ 4.2之间,高风险区主要分布在研究区西南部亚热带雨林区域,低值主要分布在研究区东北部高原草甸区域。水土流失风险等级整体上处于波动变化,但需要注意的是高度危险区域面积占比呈逐渐扩大趋势。
        结论  藏东南地区水土流失情况整体处于较低水平,西南和东北两个区域水土保持效果较好,然而,研究区西南部区域水土流失生态风险指数处于较高水平,故这些区域仍需要做好水土保持防护工作,保障区域生态环境安全。研究区西北至东南区域水土保持效果相对较差,需要加强水土流失治理工作,进行植被恢复或采取水土保持工程措施。

       

      Abstract:
        Objective  This paper aims to analyze the spatial and temporal characteristics of soil and water loss in southeast area of Tibet of southwestern China, and to conduct a comprehensive assessment of soil and water loss ecological risk, with a view to providing a theoretical basis and scientific guidance for the prevention and control of soil and water loss in southeast area of Tibet.
        Method  The USLE model was used to estimate the soil erosion modulus and erosion sensitivity index for year 2014, 2017 and 2020 in the study area; then a comprehensive assessment of the ecological risk of soil erosion in southeast area of Tibet was conducted based on precipitation, soil, vegetation cover, sensitivity index and other indicators.
        Result  (1) The overall soil erosion in southeast area of Tibet was relatively low, and the soil erosion grades were mainly composed of very slight erosion and light erosion, which accounted for about 95% of the study area, the very slight erosion area showed the trend of developing into the light erosion area gradually. (2) From 2014 to 2020, the highest value of the sensitivity index of regional soil and water loss fluctuated around 3.0, which increased in 2017 and decreased slightly in 2020, with little change in the overall value. The high value areas were mainly distributed in the Alpine ice-snow covered areas, the low value areas were mainly distributed in the high vegetation coverage areas. (3) The ecological risk index of soil and water loss in southeast area of Tibet ranged from 1.2 to 4.2. The high risk area was mainly distributed in the subtropical rainforest area in the southwest of the study area, and the low risk area was mainly distributed in the northeast plateau meadow area. The risk grade of soil and water loss fluctuated on the whole, but it should be noted that the proportion of high risk area increased gradually.
        Conclusion  The soil and water loss in southeast area of Tibet is at a low level, and the effect of soil and water conservation in southwest and northeast area of Tibet is good. However, the ecological risk index of soil and water loss in southwest of the research area is at a high level, therefore, these areas still need to do a good job of soil and water conservation protection, to ensure the safety of regional ecological environment. The effect of soil and water conservation in the northwest to southeast region of the study area is relatively poor, so it is necessary to strengthen the control of soil and water loss, such as carrying out vegetation restoration or taking engineering measures.

       

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