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１９９６年１月３日和８日，江西省彭泽县长江马湖堤相继发生两起特大崩岸事件。长江水利委员会组成专家组在现场进行了详细考察，并进行了地球物理勘探，查明崩岸的原因主要是不利的地质结构、长江对岸坡的长期冲蚀淘刷、深泓迫近江堤、堤内鱼塘积水、长江水位降落较快以及堤基加载和砂土震动液化等因素综合作用造成的。此外，对新堤的地质条件也作出了初步评价。
On January 3 and 8, 1996, two major landslide accidents occurred along Mahu Di, the Changjiang River in Pengze County, Jiangxi Province. Yangtze River Water Resources Commission formed a group of experts to conduct a detailed inspection at the scene and conducted a geophysical survey to identify the main reason for bank collapse adverse geological structure, the Yangtze River erosion of the long-term erosion scour, deep Wang approached the river embankment, dike Fish pond water, the Yangtze River water level rapid decline and embankment load and sand vibration liquefaction and other factors caused by the combined effect. In addition, the geological conditions of the new embankment also made a preliminary assessment.