为解决地震微区划问题的饱和水土地震特性评价

B. A. Trifonov, V. Sevostyanov, S. Milanovskiy, V. V. Nesynov
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引用次数: 0

摘要

参与地震微区划的专家对于在评价预期地震效应时是否考虑饱和水细土的反应存在不同的意见。在使用地震刚度(MSS)方法时,许多研究者认为不宜对地下水位(GWL)进行校正。在本文中,我们分析了我们自己的实地研究结果和参与SMZ方法论发展的其他研究人员的研究结果。特别注意了GWL对横向s波计算MSS时S.V. Medvedev方程中地震烈度增量(ΔIGWL)的影响。本文的研究结果表明,在地震烈度增量计算中,ΔIGWL的修正是不可忽视的。作者认为,在水饱和细土中进行强运动的登记时,继续进行实地试验是有利的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Evaluation of seismic properties of water-saturated soils for solving problems in seismic microzoning
The experts involved in seismic microzoning (SMZ) have different opinions on whether to take into account the response of water-saturated fine soils upon the assessment of expected seismic effect. When using the method of seismic stiffness (MSS), a number of researchers consider inexpedient to apply the correction for the groundwater level (GWL). In the present paper, we analyze both the results of our own field studies and those of other researchers involved in the development of SMZ methodology. Particular attention is paid to the GWL influence on the increment of seismic intensity (ΔIGWL ) in the S.V. Medvedev’s equation upon MSS calculations by transverse s-waves. The research results provided in this paper prove that the correction for ΔIGWL should not be ignored in calculations of the seismic intensity increment. The authors appear it expedient to continue field tests in the registration of strong movements in water-saturated fine soils.
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