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地核物质的状态方程和参数
引用本文:刘植凤,杜国强,李艳.地核物质的状态方程和参数[J].云南大学学报(自然科学版),2008,30(3):265-268.
作者姓名:刘植凤  杜国强  李艳
作者单位:石家庄经济学院,地球动力研究所,河北,石家庄,050031
基金项目:河北省教育厅资助重点项目 , 石家庄经济学院校科研和教改项目
摘    要: 解释了3种地核物质状态方程的异同,验证了Vinet et al. EOS(equation of state)比Shanker et al.EOS更接近Stacy EOS的结论,后者与高压极限的热动力学一致、而且与来源于地震波的数据完全匹配;同时与地震波测量数据进行了对照;给出了内核边界压力下物质摩尔体积随温度的变化函数,预言了密度亏损的温度变化.这对于揭示地球深部物质特性、研究地核内的轻物质组分以及深部动力学原理具有重要意义.

关 键 词:地核  不可压缩系数  热压  PREM模型
文章编号:0258-7971(2008)03-0265-04
修稿时间:2007年10月17

The equation of state of the iron in the Earth's core
LIU Zhi-feng,DU Guo-qiang,LI Yan.The equation of state of the iron in the Earth's core[J].Journal of Yunnan University(Natural Sciences),2008,30(3):265-268.
Authors:LIU Zhi-feng  DU Guo-qiang  LI Yan
Institution:Institute of Geophysics, Shijiazhuang Economic University, Shijiazhuang 050031, China
Abstract:The difference of three equations of state was studied.It is concluded that Vinet et al.equation of state (EOS) is more compatible with the seismological data than Shanker et al.EOS.Vinet et al.EOS is resemble with the Stacy EOS which consisted with the thermodynamics of high pressure limit and completely compatible with the data derived from seismology.A plot of volume vs.temperature is presented for hcp iron under ICB pressure.The variation of core density deficit with temperature is predicted.The conclusion is important to infer the property of iron in the inner core and deduce the composition of the Earth’s core.
Keywords:the Earth’s core  bulk modulus  thermal pressure  PREM model
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