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基于中频增强现象估算水下薄球壳厚径比的方法
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作者 李威 石科良 《舰船科学技术》 2010年第5期24-26,72,共4页
利用谐波序列公式计算不同厚径比的弹性薄球壳回波形函数,从计算结果中可以发现很明显的中频增强现象。通过研究,利用修正射线理论计算得到的不同表面弹性波对回波的贡献,可以发现中频增强现象主要由亚音速反对称拉姆波a0-引起。同时,... 利用谐波序列公式计算不同厚径比的弹性薄球壳回波形函数,从计算结果中可以发现很明显的中频增强现象。通过研究,利用修正射线理论计算得到的不同表面弹性波对回波的贡献,可以发现中频增强现象主要由亚音速反对称拉姆波a0-引起。同时,数值计算结果显示球壳的径厚比a/h与最大增强时的频率xp近似成线形关系。利用这一特性,本文提出了一种估算薄球壳半径和厚度之比简单而实用的方法。 展开更多
关键词 中频增强 拉姆波 回波 弹性薄球壳
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Study on the Anomaly of Small Earthquake Activity Before Moderate-strong Earthquake in the Northeast Margin of the Qinghai-Xizang (Tibet) Block
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作者 Feng Jiangang Zhou Longquan +1 位作者 Yang Liming Dai Wei 《Earthquake Research in China》 2010年第1期13-21,共9页
26 earthquakes with MS ≥5. 0 have been recorded in the northeast margin of the Qinghai- Xizang (Tibet) block since 1980,22 of which were relatively independent of other moderate- strong earthquakes. Research on the i... 26 earthquakes with MS ≥5. 0 have been recorded in the northeast margin of the Qinghai- Xizang (Tibet) block since 1980,22 of which were relatively independent of other moderate- strong earthquakes. Research on the increase of small earthquake activity before the 22 moderate-strong earthquakes has indicated that small earthquake activity was enhanced before 17 of the moderate-strong earthquakes. Though the increased seismicity is a common phenomenon in the northeast margin of the Qinghai-Xizang ( Tibet ) block,we have difficulty in predicting the moderate-strong earthquakes by this phenomenon. In order to predict the moderate-strong earthquakes through the increased seismicity of small earthquakes,this paper attempts to propose a new method, which calculates small earthquake frequency through the change of distribution pattern of small earthquakes, based on the characteristics of small earthquake activity in the northeastern Qinghai-Xizang (Tibet) block,and then make primary applications. The result shows that we are able to obtain obvious anomalies in the frequency of small earthquakes before moderate strong earthquakes through the new method,with little spatial range effect on the amplitude of this small earthquake frequency anomaly. We can obtain mid to short-term anomaly indices for moderate-strong earthquakes in the northeast margin of the Qinghai-Xizang (Tibet) block. 展开更多
关键词 Moderate.strong earthquake Northeast margin of the Qinghai-Xizang (Tibet) block Small earthquake activity
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