迟洋, 王清, 杨静. 2006: 吉林省乾安县"泥林"成因机制分析. 工程地质学报, 14(S1): 174-178.
    引用本文: 迟洋, 王清, 杨静. 2006: 吉林省乾安县"泥林"成因机制分析. 工程地质学报, 14(S1): 174-178.
    CHI Yang, WANG Qing, YANG Jing. 2006: FORMATION OF QIAN'AN "MUD FOREST" IN JILIN PROVINCE. JOURNAL OF ENGINEERING GEOLOGY, 14(S1): 174-178.
    Citation: CHI Yang, WANG Qing, YANG Jing. 2006: FORMATION OF QIAN'AN "MUD FOREST" IN JILIN PROVINCE. JOURNAL OF ENGINEERING GEOLOGY, 14(S1): 174-178.

    吉林省乾安县"泥林"成因机制分析

    FORMATION OF QIAN'AN "MUD FOREST" IN JILIN PROVINCE

    • 摘要: 吉林省乾安县泥林地质地貌特征极为特殊。它是在干燥气候环境中,黄土状土经过长期侵蚀、潜蚀而形成的群柱状地形,其地貌形态与岩溶地质景观石林极其相似,故称其为"泥林"。关于其成因机制目前说法不一,有研究表明泥林的形成主要是受地形地貌、地质构造、地下水作用以及风力作用的影响。经过研究认为除了上述的内外地质动力作用外,土体本身的粒度成分、物理化学性质等内在因素也在其形成过程中起到了决定性的作用。即泥林的形成不仅与内外动力地质作用有关,也与土体本身的成分有密切的关系。

       

      Abstract: The geomorphy character of Qian'an mud forest is very special. After ages of erosion, loessial soil changed into group of pillars in dry environment. Because it looks like hoodoo, which is a kind of karst topography, it is called "mud forest". There are several kinds of explains for its formation. The paper indicates that the prime reasons are geomorphy, geology tectonism, groundwater and wind erosion. Through the research we concladed that besides above geological dynamic actions, soils' grain size and physicochemical character are dominant factors in mud forest forming.

       

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