aragog/data/1TPa-dK09-elec-free/entropy

The material properties shown here are computed in entropy space using the RTpress EOS developed by Wolf and Bower (2018). This high P–T EOS applies a generalized Rosenfeld–Tarazona model as a thermal perturbation to isothermal and adiabatic reference compression curves, resulting in a thermodynamically consistent formulation. RTpress remains accurate over a wide P-T range and depends on a limited number of physical parameters, which are calibrated from experimental or simulation data. In this case, we use their parameterization for MgSiO₃ melt, representing a rocky mantle composition up to 1TPa.本文所呈现的材料属性，系通过Wolf与Bower（2018）提出的RTpress状态方程（RTpress EOS）在熵空间中计算得到。该高压-高温（Pressure-Temperature，P-T）状态方程将广义Rosenfeld-Tarazona模型作为热微扰应用于等温与绝热参考压缩曲线，由此得到热力学自洽的数学表述。RTpress状态方程在宽广的压力-温度区间内均保持高精度，且仅依赖少量物理参数，这些参数可通过实验或模拟数据完成校准。本研究采用其针对硅酸镁熔体（MgSiO₃ melt）的参数化方案，该方案可表征最高达1太帕斯卡（1TPa）的岩石幔成分体系。