尹晓慧, 许国辉, 王欣, 卫聪聪. 2008: 黄河水下三角洲差异侵蚀微地貌成因探讨. 工程地质学报, 16(S1): 38-43.
    引用本文: 尹晓慧, 许国辉, 王欣, 卫聪聪. 2008: 黄河水下三角洲差异侵蚀微地貌成因探讨. 工程地质学报, 16(S1): 38-43.
    YIN Xiaohui, XU Guohui, WANG Xin, WEI Congcong. 2008: THE ORIGIN DISCUSSION OF DIFFERENTIAL EROSION MICROTOPOGRAPHY ON THE YELLOW RIVER SUBAQUEOUS DELTA. JOURNAL OF ENGINEERING GEOLOGY, 16(S1): 38-43.
    Citation: YIN Xiaohui, XU Guohui, WANG Xin, WEI Congcong. 2008: THE ORIGIN DISCUSSION OF DIFFERENTIAL EROSION MICROTOPOGRAPHY ON THE YELLOW RIVER SUBAQUEOUS DELTA. JOURNAL OF ENGINEERING GEOLOGY, 16(S1): 38-43.

    黄河水下三角洲差异侵蚀微地貌成因探讨

    THE ORIGIN DISCUSSION OF DIFFERENTIAL EROSION MICROTOPOGRAPHY ON THE YELLOW RIVER SUBAQUEOUS DELTA

    • 摘要: 土体在动力荷载作用下,当动荷载与土体静强度的比值即循环应力比超过某一临界循环应力比时,土体才会发生累积变形和强度弱化。对黄河三角洲的调查分析可知,黄河水下三角洲浅表土体强度存在空间非均匀性,于是波浪动荷载对底床作用的循环应力比就不同。黄河水下三角洲底床经受大风暴浪作用时,浅表强度弱区的土体会由于循环应力比超过临界循环应力比而使强度进一步弱化,高强度区的土体可以处于稳定状态。通过水槽实验发现,底床强度弱区的土体在波浪剪切力作用下,会发生整体滑动现象,造成床面的剧烈侵蚀。对于黄河水下三角洲出现的局部差异侵蚀地貌,应是浅表强度弱区土体会在风暴浪作用下进一步弱化后,底床土体由于波浪剪切力作用发生整体滑动而被底流带走而形成。

       

      Abstract: The cycle stress ratio is the ratio of dynamic strength and soil static strength, as it passes the critical cycle stress ratio,accumulated deformation takes on and soil strength declines.According to researches about the Yellow River Delta, on the Yellow River Subaqueous Delta, the soil strength distribution is not homogeneous, so the critical cycle stress ratio of superficial soil is different. In the action of the storm wave load, the low strength soil, which passes critical cycle stress ratio, would be weaker and the high strength soil could keep stable. The flume experiment shows that the low strength soil in the action of wave shearing force would slide, as the result, strong erosion happens on the bottom. In conclusion, low strength soil is weaker in the action of storm waves, slide in the action of wave shear force and is took away by the bottom current. Then,Local defferential erosion Geomorphology appears on the Yellow River Subaqueous Delta.

       

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