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Time-Domain Analysis of Tamper Displacement during Dynamic Compaction Based on Automatic Control

机译:基于自动控制的动态压实过程中篡改位移的时域分析

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Crater depth is a vital issue in dynamic compaction (DC) because it is a controlling parameter in DC and a characterization index of soil properties. A continuous mathematical model capturing the time-domain process of tamper displacement is presented in this paper. The model is simple and the parameters involved are easy to obtain. It was found that the accumulated crater depth increases but its increment in the crater depth decreases with multiple impacts. Three groups of large-scale DC tests with 10,000 kN?m were conducted to evaluate the performance of the proposed model. The results showed that the proposed model captures the typical trends in the tamper displacement of single and multiple impacts. In addition, a concept of the crater depth ratio is proposed based on the proposed model, and the concept is used to evaluate the efficiency of DC and to predict the optimum tamping number of DCs.
机译:火山口深度是动态压实(DC)中的一个重要问题,因为它是DC中的控制参数和土壤性质的表征指标。 本文介绍了捕获篡改位移时域流程的连续数学模型。 该模型很简单,涉及的参数易于获得。 发现累积的火山口深度增加,但在火山口深度的增量随着多次影响而降低。 进行了三组大型DC测试,进行了10,000 kn?M,以评估所提出的模型的性能。 结果表明,该模型捕获了单一和多次冲击的篡改位移中的典型趋势。 另外,基于所提出的模型提出了一种陨石坑深度比的概念,并且该概念用于评估DC的效率并预测DCS的最佳夯实数量。

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