针对一起35 k V干式电抗器单相接地故障,分别进行直流电阻预试、高频震荡脉冲匝间绝缘测试及返厂解剖,发现第5层包封区域存在严重匝间短路。电抗器匝间短路会导致导线熔断,使得常规预试项目存在局限性。对故障35 k V干式电抗器进行COMSO...针对一起35 k V干式电抗器单相接地故障,分别进行直流电阻预试、高频震荡脉冲匝间绝缘测试及返厂解剖,发现第5层包封区域存在严重匝间短路。电抗器匝间短路会导致导线熔断,使得常规预试项目存在局限性。对故障35 k V干式电抗器进行COMSOL有限元热场仿真,电抗器的温度分布结果表明,电抗器在运行时的最热点位于第6层包封,温升约为73.8 K,此外第5、7、14、15层包封的温升也明显高于其他包封,容易使绝缘劣化导致设备故障。通过对故障电抗器的试验进行分析及热场仿真,可以为设备的设计、制造及日常检修、维护提供参考依据。展开更多
Heat flow is inevitably accompanied by temperature change,thus,the water temperature coseismic response during earthquake activity should also obey the laws of thermodynamics.Taking the M S8.0 Wenchuan,Sichuan,China e...Heat flow is inevitably accompanied by temperature change,thus,the water temperature coseismic response during earthquake activity should also obey the laws of thermodynamics.Taking the M S8.0 Wenchuan,Sichuan,China earthquake and the M9.0Tohoku,Japan earthquake as an example,and based on the data of water temperature coseismic responses observed in well ZK26 in Haikou,Hainan Province,China,we investigate the relationship between well water temperature change and heat transfer in the coseismic response process and the relevant thermodynamic mechanism by using the numerical simulation method for thermodynamic equations.Then,through forward modeling,we obtain several simulation curves of water temperature change in response to earthquakes along the well depth at different times.The simulated curves of water temperature change approximately fit the observed curves.Consequently,based on the variation of temperature,we find that the modes of well water temperature coseismic response( ascending,descending or stable) are related to factors such as the location of sensors,distribution and location of heat sources,the span between sensors and heat sources.展开更多
文摘针对一起35 k V干式电抗器单相接地故障,分别进行直流电阻预试、高频震荡脉冲匝间绝缘测试及返厂解剖,发现第5层包封区域存在严重匝间短路。电抗器匝间短路会导致导线熔断,使得常规预试项目存在局限性。对故障35 k V干式电抗器进行COMSOL有限元热场仿真,电抗器的温度分布结果表明,电抗器在运行时的最热点位于第6层包封,温升约为73.8 K,此外第5、7、14、15层包封的温升也明显高于其他包封,容易使绝缘劣化导致设备故障。通过对故障电抗器的试验进行分析及热场仿真,可以为设备的设计、制造及日常检修、维护提供参考依据。
基金sponsored by the Spark Program of 2011,China Earthquake Administration(XH1020)the Basic Research Program of the Hainan Province(ZDXM20110107)
文摘Heat flow is inevitably accompanied by temperature change,thus,the water temperature coseismic response during earthquake activity should also obey the laws of thermodynamics.Taking the M S8.0 Wenchuan,Sichuan,China earthquake and the M9.0Tohoku,Japan earthquake as an example,and based on the data of water temperature coseismic responses observed in well ZK26 in Haikou,Hainan Province,China,we investigate the relationship between well water temperature change and heat transfer in the coseismic response process and the relevant thermodynamic mechanism by using the numerical simulation method for thermodynamic equations.Then,through forward modeling,we obtain several simulation curves of water temperature change in response to earthquakes along the well depth at different times.The simulated curves of water temperature change approximately fit the observed curves.Consequently,based on the variation of temperature,we find that the modes of well water temperature coseismic response( ascending,descending or stable) are related to factors such as the location of sensors,distribution and location of heat sources,the span between sensors and heat sources.
