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首页> 外文期刊>Journal of Mineralogical and Petrological Sciences >Density of jadeite melts under high pressure and high temperature conditions
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Density of jadeite melts under high pressure and high temperature conditions

机译:高压高温条件下翡翠熔体的密度

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The density of the jadeite (NaAlSi_2O_6) melt has been measured up to 6.5 GPa and 2273 K using the X-ray absorption technique at beamline 13-BM-D of the Advanced Photon Source. A fit of the pressure-density-temperature data to the high temperature Birch-Murnaghan equation of state yielded the following thermo-elastic parameters: density, p_0 = 2.36 g/cm~3, isothermal bulk modulus, K_(T0) = 21.5 ± 0.8 GPa, its pressure derivative, K_o′ = 8.9 ± 1.2, and the temperature derivative (∂K_T/∂T)_P = -0.0021 ± 0.0011 GPa/K at a reference temperature T_0 = 1473 K. The densification of jadeite melt at low pressures is primarily dominated by topological changes in the structure, including a decrease in T-O-T angle and breaking and reforming of the T-O bond (T = Si~(4+), Al~(3+)). Compressibilities of jadeite, albite, diopside, phonolite and peridotite melts display a systematic trend: the K_0-K_0′ plot of these silicate melts exhibits an inverse linear relation.
机译:在高级光子源的光束线13-BM-D处,使用X射线吸收技术测量了高达6.5 GPa和2273 K的翡翠(NaAlSi_2O_6)熔体的密度。将压力-密度-温度数据与高温Birch-Murnaghan状态方程拟合可得到以下热弹性参数:密度,p_0 = 2.36 g / cm〜3,等温体积模量,K_(T0)= 21.5±在参考温度T_0 = 1473 K时,其压力导数为0.8 GPa,K_o'= 8.9±1.2,温度导数(∂K_T/∂T)_P = -0.0021±0.0011 GPa / K。压力主要由结构的拓扑变化决定,包括TOT角的减小以及TO键的断裂和重整(T = Si〜(4 +),Al〜(3+))。硬玉,钠长石,透辉石,方沸石和橄榄岩熔体的可压缩性显示出系统的趋势:这些硅酸盐熔体的K_0-K_0'图显示出反线性关系。

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