序降应力加速寿命试验(上)——试验分析篇

加速寿命试验是高可靠长寿命型产品的量化评估的重要途径,广泛应用于武器装备的定寿延寿课题中。为了进一步提高加速寿命试验的效率,提出一种新的试验方法——序降应力加速寿命试验。通过理论模型建立、试验数据分析和蒙特卡罗仿真对该方法的有效性进行分析。研究结果表明,在相同的试验环境下序降应力加速寿命试验方法不但能大幅度提高试验效率,同时还能提高试验分析精度。因此,在武器装备的定寿延寿课题中,序降应力加速寿命试验值得推广。

WEIBULL分布下的序降应力加速寿命试验

加速寿命试验(ALT)是用加大试验应力来缩短试验周期的一种基本寿命试验方法,其目的在于:以较低的试验代价(例如试验样本、试验周期等)获取具有足够精度的寿命信息.在现有方法的基础上,基于试验应力加载顺序的变化将可能使试验效率发生重大改善的设想,该文提出了一种新的试验方法——序降应力加速寿命试验,然后根据失效物理的退化模型,与其它几种试验方法比较了其有效性,并且给出了序降应力加速寿命试验在we ibu ll分布场合下的分布函数.

对数正态分布场合的序降应力加速寿命试验

加速寿命试验(ALT)是用加大试验应力来缩短试验周期的一种基本寿命试验方法,其目的在于:以较低的试验代价(例如试验样本、试验周期等)获取具有足够精度的寿命信息.序降应力加速寿命试验是一种更高效的加速寿命试验方法。该文利用积累失效模型,得出了序降应力加速寿命试验在对数正态分布场合的时间折算公式和分布函数。

Comparative Study of Changes in Stress-drop of the Jinggu MS6.6 and Ludian MS6.5 Earthquake Sequences

The earthquake stress-drop values of two sequences were accurately calculated after taking away the effects due to regional earthquake anelastic attenuation and station site response,using waveform data and seismic phase data of sequences of the Jinggu M_S6. 6,and Ludian M_S6. 5 earthquakes in Yunnan. These results show that the stress drop with magnitude increases within the scope of this study of magnitude. After eliminating the influence of the magnitude,the average value of stress-drop in the Jinggu sequence is higher than that of the Ludian sequence at the same magnitude range. This may be related to the stress state in different regions. In terms of the changes of time and space of stress-drop,before M_S5. 8 strong aftershock,the stress-drop is "slowing down-turning up-keeping a high value"after the mainshock,meanwhile,almost all of the abnormally high stress drop value is distributed around the M_S5. 8 strong aftershock, showing that the stress environment in the region was increasing after the mainshock. And after the M_S5. 9 strong aftershock,stress-drop rapidly declines to a relatively stable state,meanwhile,the high value of stress-drop is distributed around the strong aftershock,showing that the regional tectonic stress gets more fully release,its stress environment begins to rapidly decrease.For the Ludian sequence without a strong aftershock occurring,the average value of stress drop is lower than that of the Jinggu earthquake sequence at the same magnitude range,while at the same time,the stress-drop of the aftershock sequence almost hasn't changed much. In the time after the mainshock,combined with the release characteristics of the main energy,the stress in the region is excessively released,the subsequent stress in the region gradually returns to normal. This may be the reason why the activity of Ludianaftershocks significantly was weaker and subsequently there were no strong aftershocks occurred.

Research on Stress Drops and the Focal Mechanisms of the Xinyuan- Hejing ML6.8 Earthquake Sequences

Based on the digital waveform data recorded by Xinjiang Digital Seismic Network for the Xinyuan-Hejing M_L6.8 earthquake sequences of June 30,2012,this paper analyzes the stress drops of earthquake sequences and the correlation coefficients of focal mechanisms significant for strong aftershocks.Firstly,the source parameters of the Xinyuan-Hejing M_L6.8 earthquake sequences are obtained by applying the spectrum analysis and the Brunes source model.Then,the correlation coefficients of spectral amplitudes are calculated using the low-frequency spectral amplitude recorded by the same station for the different events.Finally,based on the results of the correlation coefficients of spectral amplitudes,the events with similar focal mechanisms are grouped using the clustering method.The results show that:(1)The stress drop values show a steady trend in the aftershock sequence calm period and the stress drop values show a rise-fall in strong aftershocks.(2)The moving average correlation coefficient of amplitude spectrum begins to spread after the main shock.It shows that the correlation decreases between the main shock and the aftershocks in mechanisms.(3)The results of focal mechanism groups show that the earthquake sequences are mainly strike slips.The stress distribution of the main pressure axis is nearly NS,which is the same as the structural stress field.(4)The magnitude and mechanism show that there is an agreement before the strong aftershock,which shows that the regional stress field is enhanced.