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A series solution for surface motion amplification due to underground group cavities:Incident P waves 被引量:3
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作者 LIANG Jian-wen(梁建文) ZHANG Hao(张浩) Vincent W Lee 《Acta Seismologica Sinica(English Edition)》 CSCD 2004年第3期296-307,共12页
A series solution for surface motion amplification due to underground group cavities for incident plane P waves is derived by Fourier-Bessel series expansion method. It is shown that underground group cavities signifi... A series solution for surface motion amplification due to underground group cavities for incident plane P waves is derived by Fourier-Bessel series expansion method. It is shown that underground group cavities significantly am-plify the surface ground motion nearby. It is suggested that the effect of subways on ground motion should be con-sidered when the subways are planned and designed. 展开更多
关键词 underground group cavities surface motion plane P wave SCATTERING series solution CLC number: P315.3 Document code: A
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BERNOULLI CONVOLUTIONS ASSOCIATED WITH CERTAIN NON-PISOT NUMBERS
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作者 FengDejun WangYang 《Analysis in Theory and Applications》 2003年第4期312-331,共20页
The Bernoulli convolution ν λ measure is shown to be absolutely continuous with L 2 density for almost all 12<λ<1,and singular if λ -1 is a Pisot number. It is an open question whether the Pisot typ... The Bernoulli convolution ν λ measure is shown to be absolutely continuous with L 2 density for almost all 12<λ<1,and singular if λ -1 is a Pisot number. It is an open question whether the Pisot type Bernoulli convolutions are the only singular ones. In this paper,we construct a family of non-Pisot type Bernoulli convolutions ν λ such that their density functions,if they exist,are not L 2. We also construct other Bernolulli convolutions whose density functions,if they exist,behave rather badly. 展开更多
关键词 Bernolulli convolutions Random power series Self-similar measures Pisot numbers Salem numbers
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Study of evolution forecast of the area of the Huanghe River mouth
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作者 Guo Yongsheng, Xu Xuegong, Fan Zhaomu, Wu Peihong and Zhu Xiaoge Department of Geography, Shandong Normal University, Jinan 250014, China Department of Geography, Peking University, Beijing 100871, China Remote Sensing Geology Department, Oil Exploration and Exploitation Scientific Research Institute, Beijing 100083, China 《Acta Oceanologica Sinica》 SCIE CAS CSCD 1993年第2期249-259,共11页
From 1979 to 1989, the current Qingshuigou course of the Huanghe River formed a sub - delta which resembles a beak extending into the Laizhou Bay. It covers 618 km2 in area. To meet the needs of developing and constru... From 1979 to 1989, the current Qingshuigou course of the Huanghe River formed a sub - delta which resembles a beak extending into the Laizhou Bay. It covers 618 km2 in area. To meet the needs of developing and constructing the Huanghe River Delta and under the presupposition of keeping the current course for 15-20 a, we forecast mainly by using the OM (1, 1) model that the front border of the sub-delta will be close to 119°30'E and its area will become 923 km2by the end of the year 2000. The Huanghe River will make land 760 km2 in area. 展开更多
关键词 Huanghe River mouth Markov chain forecasting method of grey number series
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