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81.
Mental tusk classification is one of the most important problems in Brain-computer interface. This paper studies the classification of five-class mental tusks. The nonlinear parameter of mean period obtained from frequency domain information was used as features for classification implemented by using the method of SVM (support vector machines). The averaged classification accuracy of 85. 6% over 7 subjects was achieved for 2-second EEG segments. And the results for EEG segments of 0.5s and 5.0s compared favorably to those of Garrett's. The results indicate that the parameter of mean period represents mental tusks well for classification, Furthermore, the method of mean period is less computationally demanding, which indicates its potential use for online BCI systems. 相似文献
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83.
为解决水下隧道和隧洞工程盾构施工关键掘进参数在复合地层中难以控制的问题,以广东陆丰核电站1、2号机组排水隧洞工程盾构施工为背景,将平均影响值(Mean Impact Value,MIV)算法引入BP神经网络模型,筛选出对施工效果影响显著的关键掘进参数,在此基础上,基于AIC准则对其进行最优分布拟合,提出以50%和90%置信水平下的置信区间,分别作为掘进参数的控制区间和预警区间的掘进参数优化设计方案,并基于Python脚本语言自带的开源Scikit-Learn、SciPy模块库开发了相应的程序。分析结果表明,刀盘扭矩、总推力等参数对隧洞拱顶沉降起重要的控制作用,所开发程序具有良好的统计分析、快速指导施工的功能,可以为同类型盾构在相似复合地层下掘进参数的选取、优化和隧洞拱顶沉降量的控制提供参考。 相似文献
84.
450MHz无线列调电台会因外界环境温度变化RSSI输出电平发生温度漂移,造成接收门限的温度漂移。为此研究用软件方法解决该问题。 相似文献
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86.
在常温与高温下,对1Cr18Ni9Ti不锈钢进行单轴应力控制下的棘轮循环试验,分析峰值应力、平均应力、低应力循环历史及温度对饱和棘轮应变的影响.基于峰值应力与饱和棘轮应变的单调抛物率关系及棘轮门槛应力值与温度的线性关系,利用单试样法建立了1Cr18Ni9Ti不锈钢常温和高温下的饱和棘轮演化模型。 相似文献
87.
轮轨接触应力的有限元分析 总被引:4,自引:0,他引:4
利用ANSYS有限元分析软件对轮轨接触进行了弹性静力分析,模拟了轮轨真实的几何形状和边界条件,分别研究了轴重、轮径、横移量对接触应力的影响,并对各种参数的变化规律进行了分析,得出了轮轨间接触应力的分布规律。 相似文献
88.
金建明 《西南交通大学学报》1998,33(2):122-126
利用动力响应状态特征量为状态指标来判定简支梁在移动质量荷载下的状态是否变化。以矩形截面简支梁为例,考察出现局部损伤的情况,通过对大量计算结果的分析处理,选取对应移动质量荷载的敏感状态特征量--加速度均方根值,提出了简支梁损伤判别的动力响应法-加速度均方根值法。 相似文献
89.
Least mean square (LMS) decision feedback equalizer (DFE) is preferred as an effective solution to coping with inter-symbol interference (ISI) for ATSC digital television (DTV) receivers. In DTV transmission environment, echo delay often covers several hundreds symbols, which leads to very large-scale equalizer. One consequence of the large-scale equalizer is the very slow convergence, which combined with error propagation, inherent drawback of DFE, seriously deteriorates the performance of the receivers, especially in severe channels. More working modes and corresponding robust control mechanism were given to help the equalizer converge to the stable state smoothly. Simulation results show that the improved equalizer can perform better, especially in the severe channels. 相似文献
90.
The response of the Black Sea mean level to atmospheric pressure (AP) and wind forcing is investigated using 5 years of TOPEX/POSEIDON (T/P hereafter) data. A coherence analysis is first applied to mean sea level and pressure to examine the validity of the inverse barometer (IB) approximation over this area. As expected, it reveals very significant deviations from an IB response attributed to the narrowness of the Bosphorus Strait and its limiting role in water exchanges. A comparison is drawn with the Mediterranean Sea case. A single basin version of the Candela analytical model [Candela, J., 1991. The Gibraltar Strait and its role in the dynamics of the Mediterranean Sea. Dyn. Atmos. Oceans 15, 267–300], which takes linear friction at the strait into account, is then used. The model explains a significant part of the T/P mean sea level variance (about 30%, while the IB correction only explains 5% of its variance) and provides a means to correct the altimeter data for the pressure effect much better than the standard IB effect. The response of the mean sea level to wind forcing is then analysed. Coherence analysis between sea level and along-strait wind stress (WS) reveals a significant coherence at periods ranging from 40 to 100 days, with an almost steady phase of 270°. This result is confirmed with a multiple coherence analysis (mean sea level vs. WS and AP). A plausible mechanism is a piling-up of water at the northern or southern end of the strait due to along-strait wind forcing. The associated along-strait pressure gradient would modify the barotropic flow in the strait and then the mean sea level. Using an extension of the Candela model, we show that this mechanism is consistent with T/P mean sea level observations. 相似文献