拜泉县侵蚀沟形态特征及发育变化规律
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作者单位:

1.黑龙江大学现代农业与生态环境学院;2.黑龙江省水利科学研究院

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中图分类号:

S157.1????????????? ?????????????

基金项目:

国家重点研发计划项目子课题(2021YFD150080503):黑龙江省自然科学基金项目(LH2020D018)


Morphological Characteristics and Developmental Change Mechanism of Erosion Gully in Baiquan County
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Affiliation:

College of Advanve Agriculture and Ecological Environment,Heilongjiang University,Harbin

Fund Project:

National Key Research and Development Plan Special Sub-project(2021YFD150080503);Natural Science Foundation of Heilongjiang(LH2020D018)

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    摘要:

    [目的]为了解漫川漫岗黑土区侵蚀沟形态特征及不同时间尺度形态变化规律。[方法]本研究特选取拜泉县国富镇域内61条典型侵蚀沟为研究对象,采用无人机航拍技术生成数字高程模型,并通过人工目视解译提取沟长、断面宽深比等形态参数,结合历史航拍影像数据分析侵蚀沟发育变化规律及影响因素。[结果](1)03~21年间拜泉县研究区侵蚀沟发育剧烈,侵蚀沟类型变化较大,沟道变化显著。(2)拜泉县研究区侵蚀沟沟长及面积平均发育变化速率分别为9.64m/y、246.39m2/y,整体侵蚀沟形态复杂程度呈现先复杂后简单的变化趋势,且侵蚀沟沟岸扩张速度小于沟头前进速度,侵蚀沟表现为狭长不规则形。(3)研究区侵蚀沟各形态参数之间存在着一定的相关关系,顶宽与底宽、沟长与沟宽、周长与沟长、沟宽以及面积与沟长、沟宽之间均呈正相关关系,但沟长与沟宽在发育过程中未发现显著联系。[结论]研究结果可为东北漫川漫岗黑土区侵蚀沟发育演化研究提供科学依据和数据支撑。

    Abstract:

    [Objective] In order to understand the morphological characteristics of erosion gully and its morphological changes in different time scales in rolling hilly region of Northeast China. [Methods] In this study, 61 typical erosion gullies in Guofu Town, Baiquan County were selected as the research object, and the digital elevation model was generated by aerial photography of unmanned aerial vehicles. The morphological parameters such as ditch length and section width-depth ratio were extracted by manual visual interpretation, and the development and change law and influencing factors of erosion gullies were analyzed by combining historical aerial photography data.[Results] (1) During 2003-2021, the erosion gullies in Baiquan County research area developed rapidly, and the types of erosion gullies changed greatly, and the gully changes significantly. (2) The average development and change rates of the gully length and area in Baiquan County are 9.64 m/y and 246.39 m/y, respectively. The overall morphological complexity of the gully presents a trend of first complexity and then simplicity, and the spreading speed of the gully bank is lower than that of the gully head, and the gully is long, narrow and irregular. (3) There is a certain correlation between the morphological parameters of the erosion ditches in the study area, and there is a positive correlation between the top width and the bottom width, the length and width of ditches, the perimeter and the length and width of ditches, and the area and the length and width of ditches, but there is no significant correlation between the length and width of ditches in the development process.[Conclusion] The research results can provide scientific basis and data support for the research on the development and evolution of erosion gullies in rolling hilly region of Northeast China.

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  • 收稿日期:2023-12-02
  • 最后修改日期:2024-03-01
  • 录用日期:2024-03-04
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