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THE PHENOMENON OF THE SOIL PLUG USUALLY RISING INSIDE THE SUCTION FOUNDATIONS DURING SUCTION PENETRATION WAS QUANTITATIVELY DESCRIBED AND PREDICTED. THE FORMATION PROCESS OF THE SOIL PLUG WAS SIMULATED AND CALCULATED BY DEM ( DISCRETE ELEMENT METHOD) MODEL. THE SEEPAGE FLOW, THE SELF-WEIGHT OF SOIL, THE FRICTION ON THE CHAMBER WALL AS WELL AS THE SUCTION INSIDE THE CHAMBER ARE CONSIDERED AS THE MAIN EXTERNAL FORCES IN THE PROCESS. THE RESULTS ARE COMPARED WITH A SET OF LABORATORY MODEL TESTS PERFORMED BY USING THREE SOIL TYPES (SAND, SILTY CLAY AND CLAY) IN THE BOHAI SEA AREA. THE HEIGHTS OF SOIL PLUG FROM NUMERICAL ESTIMATIONS ARE LOWER THAN THOSE FROM MODEL TEST RESULTS, MAINLY BECAUSE THE SUCTION PRESSURE AND FRICTION RESISTANCE ARE APPLIED IN AN IDEAL WAY UNDER THE NUMERICAL SIMULATION.
THE PHENOMENON OF THE SOIL PLUG USUALLY RISING INSIDE THE SUCTION FOUNDATIONS DURING SUCTION PENETRATION WAS QUANTITATIVELY DESCRIBED AND PREDICTED. THE FORMATION PROCESS OF THE SOIL PLUG WAS SIMULATED AND CALCULATED BY DEM (DISCRETE ELEMENT METHOD) MODEL. THE SEEPAGE FLOW, THE SELF-WEIGHT OF SOIL, THE FRICTION ON THE CHAMBER WALL AS WELL AS THE SUCTION INSIDE THE CHAMBER ARE CONSIDERED AS THE MAIN EXTERNAL FORCES IN THE PROCESS. THE RESULTS ARE COMPARED WITH A SET OF LABORATORY MODEL TESTS PERFORMED BY USING THREE SOIL TYPES (SAND, SILTY CLAY AND CLAY) IN THE BOHAI SEA AREA. THE HEIGHTS OF SOIL PLUG FROM NUMERICAL ESTIMATIONS ARE LOWER THAN THOSE FROM MODEL TEST RESULTS, MAINLY BECAUSE THE SUCTION PRESSURE AND FRICTION RESISTANCE ARE APPLIED IN AN IDEAL WAY UNDER THE NUMERICAL SIMULATION.