کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4677138 1634788 2013 12 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Assessing uncertainty in geochemical models for core formation in Earth
ترجمه فارسی عنوان
ارزیابی عدم قطعیت در مدل های ژئوشیمیایی برای تشکیل هسته در زمین
کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات علوم زمین و سیاره ای (عمومی)
چکیده انگلیسی

Unraveling the conditions at which Earth's metallic iron core formed yields important information about Earth's early accretion and differentiation history. Multi-variable statistical modeling of siderophile element partitioning between core-forming metallic liquids and silicate melts form the basis for physical models of core formation. While it seems clear that core segregation in a deep peridotitic magma ocean is generally consistent with many mantle siderophile element abundances, there is considerable disparity among extant physical models in terms of the key parameters of pressure, temperature and oxygen fugacity at which the core formed. Moreover, there is ongoing debate over whether simple single-stage equilibrium or more complex multi-stage accretion models are required by the partitioning data. Here we consider how variations in the statistical regression of partitioning data affect the outcomes of physical models for core formation. Taking extant experimental data sets for four well-studied siderophile elements (Ni, Co, W and V) as examples, we find that the regression model exerts a fundamental control on physical model outcomes. Further, the experimental data are currently too imprecise to discriminate among various single-stage and continuous core formation scenarios. Progress in the development of physical models requires better isolation of the independent variables that affect partition coefficients and verification of activity models at high pressure and temperature in order to reduce the global uncertainty in multi-variable statistical models.


► Siderophile element modeling constrains core formation conditions in Earth.
► Siderophile element partitioning data are modeled using multi-variable regression.
► Core formation model outcomes show a large dependency on regression method.
► Regression models are too imprecise to select among competing core formation models.
► Improvements in isolating independent variable dependencies are required.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Earth and Planetary Science Letters - Volume 365, 1 March 2013, Pages 165–176
نویسندگان
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