中文摘要：

本文根据搭载于Cluster卫星的CIS/CODIF和RAPID仪器的观测数据，统计研究了等离子体片中的H＋、O＋离子在磁暴期间的时间变化特性，及其对太阳风条件的响应.观测结果表明：（1） 磁暴开始前，O＋离子（0-40 keV）数密度保持在较低水平.随着磁暴的发展，O＋数密度缓慢上升，其峰值出现在Dst极小值附近；H＋离子（0-40 keV）数密度在磁暴开始之前的较短时间迅速增加并达到峰值，在磁暴开始之后迅速降低，并在整个主相和恢复相期间保持在相对较低水平.更高能量的离子则在磁暴开始后迅速增多，并在低能O＋离子达到峰值之前达到峰值.因此我们推测磁暴初期从等离子体片注入环电流的主要是H＋离子，主相后期O＋离子可能扮演更为重要的角色.（2）在地磁活动时期，太阳风密度和动压强与等离子体片中的H＋、O＋数密度存在一定相关性.等离子体片中的H＋离子对北向IMF Bz较为敏感，而IMF Bz南向条件下更有利于太阳风参数对等离子体片中O＋数密度的影响.在地磁活动平静期，太阳风条件对等离子体片中的离子没有明显影响.

英文摘要：

Observations obtained from CIS/CODIF and RAPID instrument onboard Cluster are used to investigate the temporal behavior of H＋ and O＋ ions in the storm time plasmasheet and the relationship between plasmasheet ions and solar wind conditions. It is found that： （1） The number density of O＋ ions （0~40 keV） is quite low before SSC, and increases slowly as Dst decreases, reaching its peak value at the vicinity of Dst minimum. The density of H＋ ions enhances greatly shortly before SSC, and decreases sharply after SSC. It keeps at a relatively low level during the whole main phase and recovery phase. Fluxes of energetic H＋ and O＋ ions enhance greatly after SSC and reach their maximum values before their low energy counterparts. It implies that ions injected into ring current at early storm time are mainly H＋ ions and only at later times O＋ ions could significantly affect the ring current. （2） During geomagnetic active times, solar wind pressure, density and electric field are positively correlated with simultaneous H＋ and O＋ number density in the plasma sheet. The dependence of H＋ number density on solar wind parameters is stronger under northward IMF （Interplanetary Magnetic Field）, while O＋ number density favors southward IMF. During geomagnetic quiet times, there is no clear evidence for a correlation between solar wind conditions and ions in the plasmasheet.