本文通过再现相平衡实验数据和检查热力学活度模型两种手段,对榴辉岩中几种常用的温压计进行了检验,发现榴辉岩中某些常用温压计存在以下问题:(1)在 Eliis and Green(1979)、Powell(1985)、Krogh(1988)和 Ravna(2000)四种石榴石-单斜辉...本文通过再现相平衡实验数据和检查热力学活度模型两种手段,对榴辉岩中几种常用的温压计进行了检验,发现榴辉岩中某些常用温压计存在以下问题:(1)在 Eliis and Green(1979)、Powell(1985)、Krogh(1988)和 Ravna(2000)四种石榴石-单斜辉石温度计中只有 Ravna(2000)的版本能较好的再现相平衡实验数据。(2)将石榴石-单斜辉石温度计应用于含 X_(Jd)>0.55绿辉石的榴辉岩中会出现很大的误差。(3)Green and Hellman(1982)的石榴石-多硅白云母温度计计算的高压含多硅白云母榴辉岩变质温度普遍偏高,但是计算超高压榴辉岩的结果能较好的与 Ravna(2000)的石榴石-单斜辉石温度计计算结果保持一致。(4)Waters and Martin(1993)的石榴石-单斜辉石-多硅白云母压力计、Ravna and Terry(2004)的石榴石-单斜辉石-多硅白云母-蓝晶石-柯石英/石英温压计的精度都受到了 Holland(1990)的单斜辉石活度模型的限制,它们不能适用于绿辉石 X_(Jd)>0.55的榴辉岩,而 Waters and Manin(1996)对 Waters and Martin(1993)的版本做了一个经验校正,弥补了单斜辉石活度模型的缺陷,因此可以适用于绿辉石 X_(Jd)>0.55的榴辉岩。(5)Nakamura and Banno(1997)的石榴石-绿辉石-蓝晶石-柯石英温压计因运用了不恰当的石榴石和铁钙辉石的活度模型,从而使得计算结果与岩相学观察结果不一致。因此,我们建议:对于绿辉石 X_(Jd)<0.55的多硅白云母榴辉岩,可以运用 Waters and Martin(1993)压力计和 Ravna(2000)的温度计联合求解温压;对于含高硬玉组分(X_(Jd)>0.55)绿辉石的超高压多硅白云母榴辉岩,可选用 Waters and Martin(1996)压力计和 Green andHellman(1982)的温度计联合求解温压;对于含有石榴石+绿辉石+蓝晶石+柯石英矿物组合的榴辉岩,在 X_(Jd)<0.55的情况下。可选用 Ravna and Terry(2004)的温压计求解温压。在应用这些温压计时,应注意各温压计的适用温压范围和成分范围,尤其是石榴石 X_(Jd)、Mg~#和绿辉石 X_(Jd)的范围。另外,由于矿物中 Fe^(3+)的含量对温度计算结果影响很大,所以还必须合理地校正所选矿物的 Fe^(3+)。展开更多
Based on the Cu-Zr-Ti ternary phase diagram,four sets of Cu-Zr-Ti multilayered films with various compositions of Cu20Zr36Ti44,Cu36Zr31Ti33,Cu49Zr24Ti27,and Cu67Zr16Ti17 were prepared and then the ion beam mixing was ...Based on the Cu-Zr-Ti ternary phase diagram,four sets of Cu-Zr-Ti multilayered films with various compositions of Cu20Zr36Ti44,Cu36Zr31Ti33,Cu49Zr24Ti27,and Cu67Zr16Ti17 were prepared and then the ion beam mixing was carried out.It turned out that the increase of Cu content doesn't always have a positive effect on the glass forming ability.The glass forming ability of Cu49Zr24Ti27 was degraded due to the appearance of a Cs Cl-type B2 structure Cu Zr phase in the eutectic region.The experimental observations justify the existence of the Cu Zr phase under the non-equilibrium condition.Possible formation mechanisms for the crystalline phase were also discussed in terms of the atomic collision theory.展开更多
We introduce a pre-hydrodynamic correction to the commonly used Glauber model to bring the random scattering information to the initial condition of the hydrodynamic description for the heavy ion collisions.The result...We introduce a pre-hydrodynamic correction to the commonly used Glauber model to bring the random scattering information to the initial condition of the hydrodynamic description for the heavy ion collisions.The results of this correction obviously shrink the value of the elliptic flow in the medium momentum region and move the corresponding momentum of the maximum v 2 forwards to smaller p T value.These fit the experimental data quite well.This correction implies that the quark-gluon plasma(QGP) has reached the thermal equilibrium when the hydrodynamic expansion starts.Such a conclusion of quick-equilibrium confirms the conclusion that QGP is a strongly interacting system.展开更多
文摘本文通过再现相平衡实验数据和检查热力学活度模型两种手段,对榴辉岩中几种常用的温压计进行了检验,发现榴辉岩中某些常用温压计存在以下问题:(1)在 Eliis and Green(1979)、Powell(1985)、Krogh(1988)和 Ravna(2000)四种石榴石-单斜辉石温度计中只有 Ravna(2000)的版本能较好的再现相平衡实验数据。(2)将石榴石-单斜辉石温度计应用于含 X_(Jd)>0.55绿辉石的榴辉岩中会出现很大的误差。(3)Green and Hellman(1982)的石榴石-多硅白云母温度计计算的高压含多硅白云母榴辉岩变质温度普遍偏高,但是计算超高压榴辉岩的结果能较好的与 Ravna(2000)的石榴石-单斜辉石温度计计算结果保持一致。(4)Waters and Martin(1993)的石榴石-单斜辉石-多硅白云母压力计、Ravna and Terry(2004)的石榴石-单斜辉石-多硅白云母-蓝晶石-柯石英/石英温压计的精度都受到了 Holland(1990)的单斜辉石活度模型的限制,它们不能适用于绿辉石 X_(Jd)>0.55的榴辉岩,而 Waters and Manin(1996)对 Waters and Martin(1993)的版本做了一个经验校正,弥补了单斜辉石活度模型的缺陷,因此可以适用于绿辉石 X_(Jd)>0.55的榴辉岩。(5)Nakamura and Banno(1997)的石榴石-绿辉石-蓝晶石-柯石英温压计因运用了不恰当的石榴石和铁钙辉石的活度模型,从而使得计算结果与岩相学观察结果不一致。因此,我们建议:对于绿辉石 X_(Jd)<0.55的多硅白云母榴辉岩,可以运用 Waters and Martin(1993)压力计和 Ravna(2000)的温度计联合求解温压;对于含高硬玉组分(X_(Jd)>0.55)绿辉石的超高压多硅白云母榴辉岩,可选用 Waters and Martin(1996)压力计和 Green andHellman(1982)的温度计联合求解温压;对于含有石榴石+绿辉石+蓝晶石+柯石英矿物组合的榴辉岩,在 X_(Jd)<0.55的情况下。可选用 Ravna and Terry(2004)的温压计求解温压。在应用这些温压计时,应注意各温压计的适用温压范围和成分范围,尤其是石榴石 X_(Jd)、Mg~#和绿辉石 X_(Jd)的范围。另外,由于矿物中 Fe^(3+)的含量对温度计算结果影响很大,所以还必须合理地校正所选矿物的 Fe^(3+)。
基金The National Natural Science Foundation of China(Grant No.51131003)The National Basic Research Program of China("973"Project)(Grant Nos.2011CB606301,2012CB825700)The Administration of Tsinghua University
文摘Based on the Cu-Zr-Ti ternary phase diagram,four sets of Cu-Zr-Ti multilayered films with various compositions of Cu20Zr36Ti44,Cu36Zr31Ti33,Cu49Zr24Ti27,and Cu67Zr16Ti17 were prepared and then the ion beam mixing was carried out.It turned out that the increase of Cu content doesn't always have a positive effect on the glass forming ability.The glass forming ability of Cu49Zr24Ti27 was degraded due to the appearance of a Cs Cl-type B2 structure Cu Zr phase in the eutectic region.The experimental observations justify the existence of the Cu Zr phase under the non-equilibrium condition.Possible formation mechanisms for the crystalline phase were also discussed in terms of the atomic collision theory.
基金supported by the National Natural Science Foundation of China (Grant Nos. 10775069,10935001 and 11075075)the Research Fund for the Doctoral Program of Higher Education (Grant No.200802840009)the Priority Academic Program Development of Jiangsu Higher Education Institution
文摘We introduce a pre-hydrodynamic correction to the commonly used Glauber model to bring the random scattering information to the initial condition of the hydrodynamic description for the heavy ion collisions.The results of this correction obviously shrink the value of the elliptic flow in the medium momentum region and move the corresponding momentum of the maximum v 2 forwards to smaller p T value.These fit the experimental data quite well.This correction implies that the quark-gluon plasma(QGP) has reached the thermal equilibrium when the hydrodynamic expansion starts.Such a conclusion of quick-equilibrium confirms the conclusion that QGP is a strongly interacting system.
