Solid solution of CaSiO3 and MgSiO3 perovskites in the lower mantle: The role of ferrous iron

被引:2
|
作者
Zhang, Feiwu [1 ]
Xiao, Tingting [1 ,2 ]
Muir, Joshua M. R. [1 ]
机构
[1] Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550081, Peoples R China
[2] Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Peoples R China
基金
中国国家自然科学基金;
关键词
CaSiO3; MgSiO3; iron; miscibility; the lower mantle; Physics and Chemistry of Earth's Deep Mantle and Core; TOTAL-ENERGY CALCULATIONS; PHASE-TRANSFORMATIONS; HIGH-PRESSURE; DEEP MANTLE; CAMGSI2O6; TEMPERATURE; BRIDGMANITE; PERIDOTITE; MINERALOGY; STABILITY;
D O I
10.2138/am-2022-8356
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The solid solution between CaSiO3 and MgSiO3 perovskites is an important control on the properties of the lower mantle but the effect of one of the most important impurity elements (iron) on this solution is largely unknown. Using density functional theory (DFT), ferrous iron's influence on the reciprocal solubility of MgSiO3 and CaSiO3 perovskite (forming a single Ca-Mg mixed perovskite phase) was calculated under pressures and temperatures of 25-125 GPa and 0-3000 K, respectively. Except at iron-rich conditions, ferrous iron preferentially partitions into the mixed perovskite phase over bridgmanite. This is a small effect (partitioning coefficient K-D similar to 0.25-1), however, when compared to the partitioning of ferrous iron to ferropericlase, which rules out perovskite phase mixing as a mechanism for creating iron-rich regions in the mantle. Iron increases the miscibility of Ca and Mg perovskite phases and reduces the temperature at which the two perovskite phases mix but this effect is highly nonlinear. We find that for a pyrolytic mantle [Ca% = 12.5 where Ca% = Ca/(Ca+Mg)] a perovskite ferrous iron concentration of similar to 13% leads to the lowest mixing temperature and the highest miscibility. With this composition, 1% ferrous iron in a pyrolytic composition would lead to mixing at similar to 120 GPa along the geothermal gradient, and 6.25% ferrous iron leads to mixing at similar to 115 GPa and 13% similar to 110 GPa. At high iron concentrations, Fe starts to impair miscibility, with 25% ferrous iron leading to mixing at similar to 120 GPa. Thus, in normal pyrolytic mantle, iron could induce a small amount of Ca-pv and Mg-pv mixing near the D" layer but it generally partitions to ferropericlase instead and does not impact mixing. Extremely iron rich parts of the lower mantle such as ULVZs or the CMB (potentially) are also not a likely source of phase mixed perovskites due to the nonlinear effect of ferrous iron on phase mixing.
引用
收藏
页码:439 / 446
页数:8
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