...
首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >The phase diagram of the Fe-P binary system at 3 GPa and implications for phosphorus in the lunar core
【24h】

The phase diagram of the Fe-P binary system at 3 GPa and implications for phosphorus in the lunar core

机译:3 GPA的Fe-P二元系统的相图以及月球核心的磷对磷的影响

获取原文
获取原文并翻译 | 示例
           

摘要

Phosphorus is a potential candidate in the metallic core of the Moon. The phase diagram of the Fe-P binary system was investigated at the pressure of 3 GPa and temperatures of up to 1600 degrees C. Up to 3.0 wt% and 10.4 wt% phosphorus can dissolve in the solid iron and liquid Fe-P phases at 1100 degrees C and 3 GPa, respectively. The eutectic temperature on the iron-rich side was determined as 1085 degrees C at 3 GPa. The solubility of phosphorus in the iron decreases from similar to 1.4 wt% at 1100 degrees C to similar to 0.7 wt% at 1500 degrees C and 3 GPa. Structure of the solid iron in the quenched sample is the body-center cubic, corresponding to alpha-Fe phase. Extending the phosphorus solubility in the solid iron to the present lunar core conditions yields a maximum phosphorus concentration in a fully crystallized iron core of 0.85 +/- 0.15 wt%. If there are Ni and C in the core, the value would be depressed to 0.4 +/- 0.1 wt%. In addition, based on a simple siderophile mass balance between the bulk Moon (BM) and bulk silicate Moon (BSM) and a modeled phosphorus partition coefficient, D-P-Moon(core/mantle) (40-200) for the lunar magma ocean, a bulk silicate Earth-like P content (82 +/- 8 ppm) in the initial Moon yields a lunar core with <0.3 wt% P. Some other potential light elements such as S and C could reduce the P content in the lunar core. Furthermore, the partition coefficient of phosphorus in the iron and liquid melt (D-p(SM/)LM) was found to be 0.10 +/- 0.03 at 3 GPa. Taking the sulfur into account, the D s p m / Lm increase to 0.18 +/- 0.02 at 5 GPa in the S-rich liquid metal (similar to 8 wt%). In the case of a solid lunar inner core and S-bearing liquid outer core, their P contents were assessed to be less than 0.09 +/- 0.01 wt% and 0.51 +/- 0.01 wt%, respectively, when the lunar core's storage of P is <0.3 wt%. The moderate phosphorus solubility in the solid iron, combined with the assumption of abundant phosphorus in the bulk Moon, indicates tha
机译:磷是月球金属核心的潜在候选者。在3GPa的压力下研究了Fe-P二元系统的相图,高达1600℃的温度高达3.0wt%和10.4wt%的磷,可以溶于固体铁和液体Fe-P阶段分别为1100℃和3 GPA。铁含有铁侧的共晶温度在3GPa下定为1085℃。磷在铁中的溶解度从1100℃的1100℃与1.4wt%相似,在1500℃和3gPa下类似于0.7wt%。淬火样品中的固体铁的结构是体中心立方,对应于α-Fe相。在固体铁中延伸磷溶解度至本发明的月球核心条件,在完全结晶的铁芯中产生的最大磷浓度为0.85 +/- 0.15wt%。如果核心中存在NI和C,则该值将被压低为0.4 +/- 0.1wt%。此外,基于散装月球(BM)和散硅(BSM)之间的简单散发性质量平衡和月球岩浆海洋的模型磷分配系数,DP-Moon(核心/地幔)(40-200),初始月亮的散装硅酸盐地球样P含量(82 +/- 8ppm)产生了带有<0.3wt%的月球核心。一些其他潜在的光元件,如S和C可以减少月球内核中的P含量。此外,在3GPa下发现铁和液体熔体中的磷(D-P(SM /)LM)的分配系数为0.10 +/- 0.03。考虑到硫磺,在富含S的含水金属(类似于8wt%)中,D S P m / Lm在5GPa下增加至0.18 +/- 0.02。在固体月球内核和S轴承液外核的情况下,当农历核心的存储时,分别评估其P含量分别小于0.09 +/- 0.01wt%和0.51 +/- 0.01wt%。 p <0.3wt%。固体铁中适度的磷溶解度,结合散装月亮中丰富的磷的假设,表明了

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