Synthesis of ground motion history compatible with the response spectrum with densified controlling points
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摘要: 在传统地震动反应谱频域拟合方法的基础上,提出了拟合加密控制点目标反应谱的地震动合成方法,并在此基础上利用实际算例与传统方法进行了对比.本文方法在每次迭代调整过程中均考虑了对地震动加速度强度包络函数的模拟,并且对调整后的地震动进行了基线校正,从而确保最终合成的地震动时程既能以一定精度拟合加密目标反应谱,又能满足目标包络函数的要求,同时保证积分所得位移曲线不产生基线漂移.数值算例分析结果表明,本文方法与传统非加密控制点目标谱拟合方法相比,在地震动时程曲线合成、反应谱拟合精度以及收敛速度等方面均具有一定的优势.Abstract: Based on traditional frequency-domain response-spectrum-compatible method of ground motion, this paper proposes a synthesized method that can generate ground motion which is compatible with the target response spectrum with densified controlling points, and further compares the method with the classical one compatible with target response spectra of ground motion. This method takes into account the simulation of the acceleration envelope of the ground motion during each iteration adjustment for the initial non-stationary artificial ground motions generated by the trigonometric series superposition method, and the resulting ground-motion acceleration after the each iteration will undergo the baseline correction. Therefore, the synthesized ground motion generated by the proposed method can not only match the densified target spectrum with certain precision, but also satisfy the requirement of the envelope function of acceleration time history, and the integrated displacement curve does not present any baseline drift. Numerical results show that this method can not only match the target spectrum with relatively high convergence speed, but also fit the target envelope function with high precision. In addition, this method can realize baseline correction for the initial ground motion.
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自2014年3月以来,我们在云南省嵩明县小新街小江断裂附近(图 1a),利用电阻率层析成像技术进行与地震有关的电阻率图像动态变化的监测试验.布设了两条测线: 一条横跨小江断裂,长约700 m; 另一条几乎与小江断裂走向平行,长约1 150 m(图 1b).大约每两个月观测一次,观测中采用温纳-α装置.所使用的观测仪器为德国DMT公司的RESECS Ⅱ直流电法仪.观测场地的测试结果表明,该仪器对视电阻率的相对测量精度优于3%.
据中国地震台网测定,在试验观测时段中,云南省发生了4次MS≥4.5地震(表 1).我们的观测结果显示,无论是横跨还是平行于小江断裂走向的测线,在2014年8月和10月之前电阻率图像均未出现明显的异常变化(图 2a,b,c,d); 但在2015年1月(图 2f)都出现了明显的“区域性”降低; 约两个月之后,相继发生了沧源MS5.5和嵩明MS4.5地震(表 1); 震后约2.5个月(图 2g),电阻率图像几乎恢复至震前约4个月(图 2e)时的状态.一般情况下,气候(如降雨、干旱)和人类活动(如灌溉、抽取地下水)等对电阻率图像的影响不会超过100 m深度,这表明我们观测到的电阻率图像,特别是100 m深度以下部位的“区域性”电阻率异常降低可能与地震活动有关.由于地震前的电阻率异常空间分布与活动断层展布有关系,并且其幅度随震中距增加呈线性衰减(杜学彬,2010),因此本文认为: 2015年1月所观测到的电阻率“区域性”异常(电阻率减小)(图 2f)为嵩明MS4.5地震所致,同时表 1中前3次较大震级、较远距离的地震前未出现异常也是观测事实.
表 1 试验观测期间云南MS≥4.5地震的相关信息Table 1. Information related to the MS≥4.5 earthquakes during our experimental observation period序号 发震时间 地点 MS 震中位置 震源深度/km 震中距观测点的距离/km 年-月-日 北纬/° 东经/° 1 2014-08-03 昭通市鲁甸县 6.5 27.1 103.3 ~12 ~200 2 2014-10-07 普洱市景谷傣族彝族自治县 6.6 23.4 100.5 ~5 ~350 3 2015-03-01 临沧市沧源佤族自治县 5.5 23.5 98.9 ~11 ~480 4 2015-03-09 昆明市嵩明县 4.5 25.3 103.1 ~12 ~12 -
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1. 朱涛. 地震电阻率实验研究新进展及展望. 地球与行星物理论评. 2021(01): 61-75 . 百度学术
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