首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Unified analyses for P-V-T equation of state of MgO: A solution for pressure-scale problems in high P-T experiments
【24h】

Unified analyses for P-V-T equation of state of MgO: A solution for pressure-scale problems in high P-T experiments

机译:MgO的P-V-T状态方程的统一分析:高P-T实验中压力尺度问题的解决方案

获取原文
获取原文并翻译 | 示例
       

摘要

In order to determine an accurate and reliable high-pressure and high-temperature equation of state (EOS) of MgO, unified analyses were carried out for various pressure-scale-free experimental data sets measured at 1 atm to 196 GPa and 300-3700 K, which are zero-pressure thermal expansion data, zero-pressure and high-temperature adiabatic bulk modulus (Ks) data, room temperature and high-pressure Ks data, and shock compression data. After testing several EOS models based on the Mie-Grüneisen-Debye description for the thermal pressures with the Vinet and the third-order Birch-Murnaghan equations for the 300-K isothermal compression, we determined the K'o and γ(V) using a new functional form -y = -y0{1 + a[(V/V_0)~b — 1]) to express the volume dependence of the Grüneisen parameter. Through least squares analyses with prerequisite zero-pressure and room temperature properties of Vo, K_(s0), α_0, and C_(PO), we simultaneously optimized a set of parameters of K'_(T0), 'Yo, a, and b required to represent the P-V-T EOS. Determined new EOS models of MgO successfully reproduced all the analyzed P-V-T-Ks data up to 196 GPa and 3700 K within the uncertainties,and the total residuals between calculated and observed pressures were found to be 0.8 GPa in root mean squares. These EOS models, even though very simple, are able to reproduce available data quite accurately in the wide pressure-temperature range and completely independent from other pressure scales. We propose these models for primary pressure calibration standards applicable to quantitative high-pressure and high-temperature experiments.
机译:为了确定准确可靠的MgO高温高压状态方程(EOS),对在1 atm至196 GPa和300-3700下测得的各种无压力标度的实验数据集进行了统一分析。 K是零压力热膨胀数据,零压力和高温绝热体积模量(Ks)数据,室温和高压Ks数据以及冲击压缩数据。在根据Mie-Grüneisen-Debye描述使用Vinet和300-K等温压缩的三阶Birch-Murnaghan方程测试了几种基于Eie模型的热应力模型后,我们使用以下公式确定了K'o和γ(V)一种新的函数形式-y = -y0 {1 + a [(V / V_0)〜b_1])来表示Grüneisen参数的体积依赖性。通过使用Vo,K_(s0),α_0和C_(PO)的必要零压力和室温特性进行最小二乘法分析,我们同时优化了K'_(T0),'Yo,a和b代表PVT EOS。确定的新的MgO EOS模型成功地在不确定性范围内重现了所有分析的P-V-T-Ks数据,最高可达196 GPa和3700 K,并且计算出的压力与实测压力之间的总残差均方根为0.8 GPa。这些EOS模型即使非常简单,也能够在宽的压力温度范围内相当精确地再现可用数据,并且完全独立于其他压力刻度。我们为适用于定量高压和高温实验的主要压力校准标准件提出了这些模型。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号