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How cores grow by pebble accretion

机译:鹅卵石堆积如何增加岩心

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With this corrigendum we correct the erroneous vaporiza- tion curve (previously indicated as liquidus) in Fig. 6 and further clarify the discussion regarding the state of the core under the expected pressure/temperature conditions. The phase transition points in the SiO 2 quotidian equation of state (QEOS) from Vazan et al. (2013) used to construct the vaporization curve were shifted to lower P-T values by inaccurate scaling of the zero- energy and bulk density parameters in their equation of state calculation. The effects of this error on our results are lim- ited to the graph and discussion of the core-surface conditions presented in Sect. 4.2 because we did not use this equation of state in our simulations and only used it to determine the SiO 2 phase at the core surface. In Fig. 1 we show the corrected figure, which replaces Fig. 6 of the paper. Figure 2, for reference, shows the corrected and erroneous QEOS curves as well as the vapor pressure and solidus.
机译:利用这一勘误,我们纠正了图6中的错误蒸发曲线(以前表示为液相线),并进一步阐明了在预期压力/温度条件下关于堆芯状态的讨论。 Vazan等人的SiO 2 quotidian状态方程(QEOS)中的相变点。由于状态方程式中零能和体积密度参数的不正确缩放,用于构建汽化曲线的等人(2013年)被转移到较低的P-T值。该误差对我们结果的影响仅限于该图和本节中介绍的岩心表面条件的讨论。 4.2,因为我们在仿真中没有使用这个状态方程,而只是用它来确定核心表面的SiO 2相。在图1中,我们显示了校正后的图,它代替了本文的图6。供参考的图2显示了校正和错误的QEOS曲线以及蒸气压和固相线。

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