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The Study of Tn-Situ Pore Pressure Monitoring of Seabed Soil Under Wave Loading

机译:波浪荷载作用下海底土壤TN原位孔隙压力监测研究

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In this study, the field monitoring of the pore water pressure of the seabed soil under the wave action is investigated. From the coastal geotechnical engineering viewpoint, the wave-induced pore water pressure of seabed under irregular wave action and wave height in-situ were discussed, and also comparison with the laboratory simulation test to understand the relationship properties. The monitoring of pore water pressure system is jointed with the run-up of wave monitoring pile system in Golden Coast of Tai-Nan. In order to obtain the profile of various pressures induced by wave loading, the monitoring depth set up from -0.5m to -3.5m in step of lm below seabed. Concerning above the monitoring of wave induced the pore water pressure within the seabed, the results of calculation of Yamamoto wave theory and the cyclic triaxial tests in laboratory could indicate that by using of the wave theory formulae derived under limitless depth seabed and pore water completely saturation, to evaluate the seabed of dynamic pore water pressure after the wave through the break zone. It found that the dynamic pore pressure induced by wave loading is underestimated tendency. But the decay curve of △u_(field)/ P compared with the monitoring data and theory calculation have same tendency. The ratio of △u_(field) P is decreased as depth dimensionless of z/L increasing. The monitoring results and analysis could be provided to the reference of the related seabed stability and coastal prevention disaster.
机译:在这项研究中,研究了波动下海底土壤孔隙水压力的现场监测。从沿海岩土工程观点来看,讨论了在不规则波动和波浪高度下海底的波诱导的孔隙水压,并与实验室模拟试验相比,了解关系特性。孔隙水压系统的监测与大南金海岸波监测桩系统的延伸。为了获得由波浪载荷引起的各种压力的轮廓,监测深度在海底下方LM的步骤中设置为-0.5m至-3.5m。关于上述波浪监测诱导海底内的孔隙水压力,山同波理论的计算结果和实验室的循环三轴试验可以表明,通过使用衍生的波理论公式源于无限的深度和孔隙水完全饱和,通过断开区域评估波浪后动态孔隙水压的海底。发现通过波浪载荷引起的动态孔隙压力被低估了趋势。但与监测数据和理论计算相比,△U_(场)/ p的衰减曲线具有相同的趋势。 △U_(田间)p的比率随着z / l增加的深度无量纲而降低。可以向相关海底稳定和沿海预防灾难的参考提供监测结果和分析。

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