Considering the joint effects of various factors such as temporal baseline, spatial baseline, thermal noise, the difference of Doppler centroid frequency and the error of data processing on the interference correlatio...Considering the joint effects of various factors such as temporal baseline, spatial baseline, thermal noise, the difference of Doppler centroid frequency and the error of data processing on the interference correlation, an optimum selection method of common master images for ground deformation monitoring based on the permanent scatterer and differential SAR interferometry (PS-DInSAR) technique is proposed, in which the joint correlation coeficient is used as the evaluation function. The principle and realization method of PS-DInSAR technology is introduced, the factors affecting the DInSAR correlation are analysed, and the joint correlation function model and its solution are presented. Finally an experiment for the optimum selection of common master images is performed by using 25 SAR images over Shanghai taken by the ERS-1/2 as test data. The results indicate that the optimum selection method for PS-DInSAR common master images is effective and reliable.展开更多
The paper presents the results of a ground penetrating radar (GPR) application for the detection of ground ice. We com- bined a reflection traveltime curves analysis with a frequency spectrogram analysis. We found s...The paper presents the results of a ground penetrating radar (GPR) application for the detection of ground ice. We com- bined a reflection traveltime curves analysis with a frequency spectrogram analysis. We found special anomalies at specific traces in the traveltime curves and ground boundaries analysis, and obtained a ground model for subsurface structure which allows the ground ice layer to be identified and delineated.展开更多
对于雷电流在地网上分布的研究大多是基于理论分析,为此,通过野外试验并结合ATP-EMTP仿真分析了雷击共用地网时雷电流的分布情况。研究结果表明:共用地网模型中连接地网的2条扁钢分流到远端地网电流5次回击幅值和电量平均值分别为-1.2 ...对于雷电流在地网上分布的研究大多是基于理论分析,为此,通过野外试验并结合ATP-EMTP仿真分析了雷击共用地网时雷电流的分布情况。研究结果表明:共用地网模型中连接地网的2条扁钢分流到远端地网电流5次回击幅值和电量平均值分别为-1.2 k A和-0.24 C,分别占注入触发闪电的7.8%和27.0%;波前时间平均值和波尾时间平均值分别为22.0μs和149.2μs,分别是注入触发闪电的44倍和16倍;触发闪电电流中的一次幅值为-19.3 k A的M分量分流到远端地网时波形和注入闪电电流相似,与回击分流到此的电流也较为相似。仿真与实测结果对比发现:回击过程分流的幅值和波前时间与实测结果相符合,但波尾时间模拟结果有明显的差异;M分量模拟结果与实测整体波形都比较符合,效果优于对回击过程的模拟。触发闪电电流注入后,共用地网远端M分量电流幅值衰减比例要远小于回击过程,而其波形与回击类似,M分量对远端地网分流和地电位升高的危害应值得关注。展开更多
地电位反击造成设备的损坏和人员生命安全是非常值得关注的问题。基于人工触发闪电,布置了共用地网的试验模型,通过引流杆注入真实雷电流,测量了共用接地情况下接地体的地电位升高电压,并对比分析了闪电回击和M分量放电过程引起地电位...地电位反击造成设备的损坏和人员生命安全是非常值得关注的问题。基于人工触发闪电,布置了共用地网的试验模型,通过引流杆注入真实雷电流,测量了共用接地情况下接地体的地电位升高电压,并对比分析了闪电回击和M分量放电过程引起地电位升高电压的波形特征。结果表明:获得触发闪电(T201514)7次回击和16次M分量上升沿10%~90%时间分别为0.4μs和279.7μs,半峰宽度的平均值分别为14.8μs和434.7μs。地电位升高电压波形的上升陡度和半峰宽度相对于回击都更大,将电压波形上升陡度和半峰宽度分别与电流波形的参数相比得到比值为14.0和2.7。M分量电压和电流波形相似,电压波形和电流波形对应参数的比值分别为0.8和1.1。触发闪电回击和M分量峰值的平均值分别为–19.1 k A和–1.3 k A,回击以及M分量的峰值和引起的地电位升高电压峰值有很好的线性拟合关系。将电压峰值和电流峰值相比得到等效接地电阻,雷电流的等效接地电阻明显小于回击。展开更多
文摘Considering the joint effects of various factors such as temporal baseline, spatial baseline, thermal noise, the difference of Doppler centroid frequency and the error of data processing on the interference correlation, an optimum selection method of common master images for ground deformation monitoring based on the permanent scatterer and differential SAR interferometry (PS-DInSAR) technique is proposed, in which the joint correlation coeficient is used as the evaluation function. The principle and realization method of PS-DInSAR technology is introduced, the factors affecting the DInSAR correlation are analysed, and the joint correlation function model and its solution are presented. Finally an experiment for the optimum selection of common master images is performed by using 25 SAR images over Shanghai taken by the ERS-1/2 as test data. The results indicate that the optimum selection method for PS-DInSAR common master images is effective and reliable.
文摘The paper presents the results of a ground penetrating radar (GPR) application for the detection of ground ice. We com- bined a reflection traveltime curves analysis with a frequency spectrogram analysis. We found special anomalies at specific traces in the traveltime curves and ground boundaries analysis, and obtained a ground model for subsurface structure which allows the ground ice layer to be identified and delineated.
文摘对于雷电流在地网上分布的研究大多是基于理论分析,为此,通过野外试验并结合ATP-EMTP仿真分析了雷击共用地网时雷电流的分布情况。研究结果表明:共用地网模型中连接地网的2条扁钢分流到远端地网电流5次回击幅值和电量平均值分别为-1.2 k A和-0.24 C,分别占注入触发闪电的7.8%和27.0%;波前时间平均值和波尾时间平均值分别为22.0μs和149.2μs,分别是注入触发闪电的44倍和16倍;触发闪电电流中的一次幅值为-19.3 k A的M分量分流到远端地网时波形和注入闪电电流相似,与回击分流到此的电流也较为相似。仿真与实测结果对比发现:回击过程分流的幅值和波前时间与实测结果相符合,但波尾时间模拟结果有明显的差异;M分量模拟结果与实测整体波形都比较符合,效果优于对回击过程的模拟。触发闪电电流注入后,共用地网远端M分量电流幅值衰减比例要远小于回击过程,而其波形与回击类似,M分量对远端地网分流和地电位升高的危害应值得关注。
文摘地电位反击造成设备的损坏和人员生命安全是非常值得关注的问题。基于人工触发闪电,布置了共用地网的试验模型,通过引流杆注入真实雷电流,测量了共用接地情况下接地体的地电位升高电压,并对比分析了闪电回击和M分量放电过程引起地电位升高电压的波形特征。结果表明:获得触发闪电(T201514)7次回击和16次M分量上升沿10%~90%时间分别为0.4μs和279.7μs,半峰宽度的平均值分别为14.8μs和434.7μs。地电位升高电压波形的上升陡度和半峰宽度相对于回击都更大,将电压波形上升陡度和半峰宽度分别与电流波形的参数相比得到比值为14.0和2.7。M分量电压和电流波形相似,电压波形和电流波形对应参数的比值分别为0.8和1.1。触发闪电回击和M分量峰值的平均值分别为–19.1 k A和–1.3 k A,回击以及M分量的峰值和引起的地电位升高电压峰值有很好的线性拟合关系。将电压峰值和电流峰值相比得到等效接地电阻,雷电流的等效接地电阻明显小于回击。