为实现双通道无线电能传输(wireless power transfer,WPT)系统功率均衡和抗偏移能力提升,文中在传统的双层正交双D线圈结构的基础上,提出一种具有全向抗偏移能力的双通道磁耦合器。该耦合器在由X轴和Y轴构成的平面内任意方向平移时均具...为实现双通道无线电能传输(wireless power transfer,WPT)系统功率均衡和抗偏移能力提升,文中在传统的双层正交双D线圈结构的基础上,提出一种具有全向抗偏移能力的双通道磁耦合器。该耦合器在由X轴和Y轴构成的平面内任意方向平移时均具有强抗偏移能力。其发射侧和接收侧分别由两组解耦线圈组成,在一定偏移范围内,两组线圈间的互感对称,可实现双通道WPT系统的功率均衡。文中首先分析采用谐振补偿、失谐补偿和混合拓扑的双通道WPT系统对该类磁耦合器的共性要求;然后提出磁耦合器的设计方法并完成案例设计;继而利用有限元法仿真分析设计案例对各项指标的满足情况;最后研制磁耦合器样机并开展实验验证。结果表明,除极端偏移位置外,在X轴和Y轴方向100 mm偏移范围内,该磁耦合器的传输效率均保持在91.12%以上,且两通道输出功率之比均大于0.87,具有良好的功率均衡效果。展开更多
The bridgmanite(Bgm)to silicate post-perovskite(PPv)phase transition is believed to be the main cause for the distinct seismic features observed in the D''layer,the lowermost region of the Earth’s mantle.Howe...The bridgmanite(Bgm)to silicate post-perovskite(PPv)phase transition is believed to be the main cause for the distinct seismic features observed in the D''layer,the lowermost region of the Earth’s mantle.However,the transition depth and elasticity of the PPv phase have been highly debated,as the chemical complexity within the D''layer can largely affect the Bgm-PPv transition pressure and the associated velocity contrast.Experimental measurements of sound velocities for PPv with different chemical compositions under relevant lowermost-mantle conditions are essential but remain limited.In this study,we have reliably measured both compressional wave velocity(VP),shear wave velocity(VS),and density,for two Fe-bearing PPv compositions[(Mg0.85Fe0.15)SiO3and(Mg0.75Fe0.25)SiO3]at lowermost mantle pressures using Impulsive Stimulated Light Scattering(ISS),Brillouin Light Scattering(BLS),and X-ray Diffraction(XRD)in diamond anvil cells.Our results indicate that the velocities of Fe-bearing PPv at 120 GPa can be described by the following relationships:VS(km/s)=7.65-2.8XFe and VP(km/s)=14.11-3.8XFe,where XFe represents mole fraction of the Fe content.The variations in the Fe content of PPv may provide one of the explanations for the seismic lateral variations observed at the Earth’s core mantle boundary.By comparing our results with the high-pressure velocities of Bgm,our velocity model suggests significant discontinuities across the Bgm-PPv transition,characterized by a reduction in both VP and VΦ,and an increase in VS.These findings highlight the importance of considering the influence of chemical composition,particularly Fe content which could vary significantly at the D''region,on the seismic properties of the PPv phase.The observed velocity contrasts across the Bgm-PPv transition may contribute to the complex seismic signatures observed in the D''layer,underscoring the potential role of this phase transition in interpreting the seismic features of the lowermost mantle region.展开更多
摘要为实现双通道无线电能传输(wireless power transfer,WPT)系统功率均衡和抗偏移能力提升,文中在传统的双层正交双D线圈结构的基础上,提出一种具有全向抗偏移能力的双通道磁耦合器。该耦合器在由X轴和Y轴构成的平面内任意方向平移时均具有强抗偏移能力。其发射侧和接收侧分别由两组解耦线圈组成,在一定偏移范围内,两组线圈间的互感对称,可实现双通道WPT系统的功率均衡。文中首先分析采用谐振补偿、失谐补偿和混合拓扑的双通道WPT系统对该类磁耦合器的共性要求;然后提出磁耦合器的设计方法并完成案例设计;继而利用有限元法仿真分析设计案例对各项指标的满足情况;最后研制磁耦合器样机并开展实验验证。结果表明,除极端偏移位置外,在X轴和Y轴方向100 mm偏移范围内,该磁耦合器的传输效率均保持在91.12%以上,且两通道输出功率之比均大于0.87,具有良好的功率均衡效果。
基金the U.S.National Science Foundation Geophysics Program(EAR-2001381)the resources of the Advanced Photon Source,a U.S.Department of Energy(DOE)Office of Science User Facility operated for the DOE Office of Science by Argonne National Laboratory under Contract No.DE-AC02-06CH11357.
摘要The bridgmanite(Bgm)to silicate post-perovskite(PPv)phase transition is believed to be the main cause for the distinct seismic features observed in the D''layer,the lowermost region of the Earth’s mantle.However,the transition depth and elasticity of the PPv phase have been highly debated,as the chemical complexity within the D''layer can largely affect the Bgm-PPv transition pressure and the associated velocity contrast.Experimental measurements of sound velocities for PPv with different chemical compositions under relevant lowermost-mantle conditions are essential but remain limited.In this study,we have reliably measured both compressional wave velocity(VP),shear wave velocity(VS),and density,for two Fe-bearing PPv compositions[(Mg0.85Fe0.15)SiO3and(Mg0.75Fe0.25)SiO3]at lowermost mantle pressures using Impulsive Stimulated Light Scattering(ISS),Brillouin Light Scattering(BLS),and X-ray Diffraction(XRD)in diamond anvil cells.Our results indicate that the velocities of Fe-bearing PPv at 120 GPa can be described by the following relationships:VS(km/s)=7.65-2.8XFe and VP(km/s)=14.11-3.8XFe,where XFe represents mole fraction of the Fe content.The variations in the Fe content of PPv may provide one of the explanations for the seismic lateral variations observed at the Earth’s core mantle boundary.By comparing our results with the high-pressure velocities of Bgm,our velocity model suggests significant discontinuities across the Bgm-PPv transition,characterized by a reduction in both VP and VΦ,and an increase in VS.These findings highlight the importance of considering the influence of chemical composition,particularly Fe content which could vary significantly at the D''region,on the seismic properties of the PPv phase.The observed velocity contrasts across the Bgm-PPv transition may contribute to the complex seismic signatures observed in the D''layer,underscoring the potential role of this phase transition in interpreting the seismic features of the lowermost mantle region.