无线传感器网络中的错误测量数据会导致网络服务质量下降和能量浪费.提出了一种通过融合邻居节点的测量数据来实现故障检测的策略.主要做了以下3项工作:(1)提出了一种新颖的对邻居节点测量数据进行加权的方法;(2)提出了一种衡量测量数...无线传感器网络中的错误测量数据会导致网络服务质量下降和能量浪费.提出了一种通过融合邻居节点的测量数据来实现故障检测的策略.主要做了以下3项工作:(1)提出了一种新颖的对邻居节点测量数据进行加权的方法;(2)提出了一种衡量测量数据之间差距的方法;(3)提出了基于加权中值的故障诊断策略WMFDS(weighted median fault detection scheme),它同时适用于二进制决策和实数测量值.理论分析及仿真结果表明,即使节点发生故障的概率很高,提出的诊断策略也能得到很高的检测精度和较小的误判率,这表明在无线传感器网络故障检测中应用该方法具有很好的性能.展开更多
总结了关联维数和K o lm ogorov熵的计算方法,给出详细的计算步骤,并通过对某型发动机在不同状态下关联维数和K o lm ogorov熵的计算和混沌特性分析,提出一种将关联维数和K o lm ogorov熵结合使用的新的故障诊断手段。实验结果表明:由...总结了关联维数和K o lm ogorov熵的计算方法,给出详细的计算步骤,并通过对某型发动机在不同状态下关联维数和K o lm ogorov熵的计算和混沌特性分析,提出一种将关联维数和K o lm ogorov熵结合使用的新的故障诊断手段。实验结果表明:由于不同故障的动力学产生机制不同,通常也具有不同的关联维数和K o l-m ogorov熵,故关联维数和K o lm ogorov熵可用于故障的特征提取。展开更多
The N-S trending Xiaojiang fault zone and the NW-SE trending Qujiang-Shiping fault zone are adjacent active fault systems and seismogenic zones associated with strong and major earthquakes in Yunnan, China. To underst...The N-S trending Xiaojiang fault zone and the NW-SE trending Qujiang-Shiping fault zone are adjacent active fault systems and seismogenic zones associated with strong and major earthquakes in Yunnan, China. To understand the interaction of the two fault systems, and its probable influence on earthquake occurrences, this paper conducts a synthetic study based on data of active tectonics, historical earthquakes, relocated small earthquakes, GPS station velocities and focal mechanism resolutions. The study makes several conclusions. （1） The active southward motion of the western side of the Xiaojiang fault zone （i.e. the side of the Sichuan-Yunnan block） has a persistent and intensive effect on the Qujiang-Shiping fault zone. The later fault zone has absorbed and transformed the southward motion of the western side of the former fault zone through dextral strike-slip/sheafing as well as transverse shortening/thrusting. （2） Along the Xiaojiang fault zone, the present sinistral strike-slip/sheafing rate decreases from 10 and 8 mm/a on the northern, central and central-southern segments to 4 mm/a on the southern segment. The decreased rate has been adjusted in the area along and surrounding the Qujiang-Shiping fault zone through reverse-dextral faulting and distributed sheafing and shortening. （3） The tectonic-dynamic relation between the Xiaojiang fault zone and the Qujiang-Shiping fault zone is also manifested by a close correlation of earthquake occurrences on the two fault zones. From 1500 to 1850 a sequence of strong and major earthquakes occurred along the Xiaojiang fault zone and its northern neighbor, the Zemuhe fault zone, which was characterized by gradually accelerating strain release, gradually shortening intervals between M≥7 events, and major releases occurring in the mid to later stages of the sequence. As a response to this sequence, after an 88-year delay, another sequence of 383 years （from 1588 to 1970） of strong and major earthquakes occurred on the Qujiang-Shiping fault zone, 展开更多
基金Supported by the National Natural Science Foundation of China under Grant No.60633060(国家自然科学基金)the National High-Tech Research and Development Plan of China under Grant No.2006AA01Z223(国家高技术研究发展计划(863))the National Grand Fundamental Research973Program of China under Grant No.2005CB321604(国家重点基础研究发展规划(973))
文摘无线传感器网络中的错误测量数据会导致网络服务质量下降和能量浪费.提出了一种通过融合邻居节点的测量数据来实现故障检测的策略.主要做了以下3项工作:(1)提出了一种新颖的对邻居节点测量数据进行加权的方法;(2)提出了一种衡量测量数据之间差距的方法;(3)提出了基于加权中值的故障诊断策略WMFDS(weighted median fault detection scheme),它同时适用于二进制决策和实数测量值.理论分析及仿真结果表明,即使节点发生故障的概率很高,提出的诊断策略也能得到很高的检测精度和较小的误判率,这表明在无线传感器网络故障检测中应用该方法具有很好的性能.
文摘总结了关联维数和K o lm ogorov熵的计算方法,给出详细的计算步骤,并通过对某型发动机在不同状态下关联维数和K o lm ogorov熵的计算和混沌特性分析,提出一种将关联维数和K o lm ogorov熵结合使用的新的故障诊断手段。实验结果表明:由于不同故障的动力学产生机制不同,通常也具有不同的关联维数和K o l-m ogorov熵,故关联维数和K o lm ogorov熵可用于故障的特征提取。
基金supported by the Special Funds for Research of Earthquake Science (Grant No. 200708035)the Special Project M7 of China Earthquake Administration
文摘The N-S trending Xiaojiang fault zone and the NW-SE trending Qujiang-Shiping fault zone are adjacent active fault systems and seismogenic zones associated with strong and major earthquakes in Yunnan, China. To understand the interaction of the two fault systems, and its probable influence on earthquake occurrences, this paper conducts a synthetic study based on data of active tectonics, historical earthquakes, relocated small earthquakes, GPS station velocities and focal mechanism resolutions. The study makes several conclusions. （1） The active southward motion of the western side of the Xiaojiang fault zone （i.e. the side of the Sichuan-Yunnan block） has a persistent and intensive effect on the Qujiang-Shiping fault zone. The later fault zone has absorbed and transformed the southward motion of the western side of the former fault zone through dextral strike-slip/sheafing as well as transverse shortening/thrusting. （2） Along the Xiaojiang fault zone, the present sinistral strike-slip/sheafing rate decreases from 10 and 8 mm/a on the northern, central and central-southern segments to 4 mm/a on the southern segment. The decreased rate has been adjusted in the area along and surrounding the Qujiang-Shiping fault zone through reverse-dextral faulting and distributed sheafing and shortening. （3） The tectonic-dynamic relation between the Xiaojiang fault zone and the Qujiang-Shiping fault zone is also manifested by a close correlation of earthquake occurrences on the two fault zones. From 1500 to 1850 a sequence of strong and major earthquakes occurred along the Xiaojiang fault zone and its northern neighbor, the Zemuhe fault zone, which was characterized by gradually accelerating strain release, gradually shortening intervals between M≥7 events, and major releases occurring in the mid to later stages of the sequence. As a response to this sequence, after an 88-year delay, another sequence of 383 years （from 1588 to 1970） of strong and major earthquakes occurred on the Qujiang-Shiping fault zone,
