河北坝上康保地区土地沙化变化特征及其驱动因素

    Change characteristics and driving factors of land desertification in Kangbao area of Bashang, Hebei Province

    • 摘要:
      研究目的 康保地区位于北京西北方向、河北坝上农牧交错带,土地沙化现象较明显,制约了首都生态屏障保护建设。在此地区开展土地沙漠化研究对保障首都生态安全具有重要意义。
      研究方法 通过遥感解译和地面调查相结合的方法分析了康保地区土地沙化的程度及其变化,识别土地沙化的主要驱动因素和物质来源。
      研究结果 2021年,康保地区约95%的土地出现不同程度的沙化,重度和极重度土地沙化面积占比分别为1.34%和6.23%,主要分布于康保北部、东部和西南部,与2016年相比,土地沙化程度总体呈减轻趋势,重度和极重度土地沙化面积分别减少326.31 km2和35.79 km2,与1984年相比,土地沙化程度极大改善,重度和极重度土地沙化面积分别减少759.61 km2和158.46 km2
      结论 康保地区土地沙化受气候、地质环境和人类活动共同驱动,植树种草、土地利用方式改变等人类活动是近年来康保地区土地沙化减缓的主要原因,表层沉积物主要来源于二叠纪花岗岩类侵入体的风化或水蚀搬运。土地沙化是康保地区生态安全的主要制约因素,土地沙化整体呈持续改善的趋势,自然条件为土地沙化提供了地质环境背景,人类活动(垦牧、地下水开采、植树种草、土地利用类型改变等)是近年来土地沙化变化的主要驱动因素。

       

      Abstract:
      This paper is the result of urban geological survey engineering.
      Objective Kangbao area is located northwest of Beijing, within the agro−pastoral ecotone of the Bashang Plateau in Hebei Province, adjacent to the Hunshandake Sandy Land. Land desertification is relatively prominent in this region, which to a certain extent restricts the construction and protection of the ecological barrier of the national capital. Therefore, conducting research on land desertification in this area is of great significance for safeguarding the ecological security of the national capital.
      Methods This study analyzed the degree and changes of land desertification in Kangbao County through a combination of remote sensing interpretation and field surveys, and identified the main driving factors and material sources of land desertification.
      Results In 2021, approximately 95% of the land area in Kangbao area experienced varying degrees of desertification, with severe and extremely severe desertification accounting for 1.34% and 6.23% respectively. These severely desertified areas are mainly distributed in the northern, eastern, and southwestern parts of Kangbao area. Compared with 2016, the overall degree of land desertification showed a mitigating trend: the area of severe desertification decreased by 326.31 km2, and the area of extremely severe desertification reduced by 35.79 km2. In comparison with 1984, the degree of land desertification has been significantly improved: the area of severe desertification decreased by 759.61 km2, and the area of extremely severe desertification declined by 158.46 km2. Land desertification in Kangbao area is jointly driven by climate, geological environment, and human activities. Human activities such as afforestation and grass planting, as well as changes in land use patterns, are the main reasons for the mitigation of land desertification in recent years. The surface sediments are mainly derived from the weathering, or water erosion and transportation, of Permian granitic intrusions.
      Conclusions Land desertification is a major factor affecting the ecological security of Kangbao area. The overall trend of land desertification is continuously improving. Natural conditions provide the geological and environmental background for desertification, while human activities (such as reclamation and grazing, groundwater exploitation, afforestation and grass planting, and changes in land use types) are the main driving factors for the changes in land desertification in recent years.

       

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