...
首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >The iron-nickel-phosphorus system: Effects on the distribution of trace elements during the evolution of iron meteorites
【24h】

The iron-nickel-phosphorus system: Effects on the distribution of trace elements during the evolution of iron meteorites

机译:铁-镍-磷系统:对铁陨石演化过程中微量元素分布的影响

获取原文
获取原文并翻译 | 示例

摘要

To better understand the partitioning behavior of elements during the formation and evolution of iron meteorites, two sets of experiments were conducted at 1 atm in the Fe-Ni-P system. The first set examined the effect of P on solid metal/liquid metal partitioning behavior of 22 elements, while the other set explored the effect of the crystal structures of body-centered cubic (alpha)- and face-centered cubic (gamma)-solid Fe alloys on partitioning behavior. Overall, the effect of P on the partition coefficients for the majority of the elements was minimal. As, Au, Ga, Ge, Ir, Os, Pt, Re, and Sb showed slightly increasing partition coefficients with increasing P-content of the metallic liquid. Co, Cu, Pd, and Sn showed constant partition coefficients. Rh, Ru, W, and Mo showed phosphorophile (P-loving) tendencies. Parameterization models were applied to solid metal/ liquid metal results for 12 elements. As, Au, Pt, and Re failed to match previous parameterization models, requiring the determination of separate parameters for the Fe-Ni-S and Fe-Ni-P systems. Experiments with coexisting alpha and gamma Fe alloy solids produced partitioning ratios close to unity, indicating that an alpha versus gamma Fe alloy crystal structure has only a minor influence on the partitioning behaviors of the trace element studied. A simple relationship between an element's natural crystal structure and its alpha/gamma partitioning ratio was not observed. If an iron meteorite crystallizes from a single metallic liquid that contains both S and P, the effect of P on the distribution of elements between the crystallizing solids and the residual liquid will be minor in comparison to the effect of S. This indicates that to a first order, fractional crystallization models of the Fe-Ni-S-P system that do not take into account P are appropriate for interpreting the evolution of iron meteorites if the effects of S are appropriately included in the effort. Published by Elsevier Ltd.
机译:为了更好地了解铁陨石形成和演化过程中元素的分配行为,在Fe-Ni-P系统中的1个大气压下进行了两组实验。第一组研究了P对22种元素在固态金属/液态金属分配行为上的影响,而另一组研究了体心立方(α)和面心立方(γ)固体的晶体结构的影响铁合金对分配行为的影响。总体而言,P对大多数元素的分配系数的影响很小。随着Au,Ga,Ge,Ir,Os,Pt,Re和Sb的分配系数随着金属液体中P含量的增加而略有增加。 Co,Cu,Pd和Sn显示出恒定的分配系数。 Rh,Ru,W和Mo表现出亲磷性(偏爱P)。将参数化模型应用于12种元素的固态金属/液态金属结果。由于Au,Pt和Re无法匹配以前的参数化模型,因此需要确定Fe-Ni-S和Fe-Ni-P系统的单独参数。共存α和γFe合金固体的实验产生的分配比接近于1,表明α与γFe合金的晶体结构对所研究的痕量元素的分配行为只有很小的影响。没有观察到元素的天然晶体结构与其α/γ分配比之间的简单关系。如果铁陨石从同时含有S和P的单一金属液体中结晶,则与S的影响相比,P对元素在结晶性固体和残余液体之间分布的影响将很小。如果适当地包括了S的影响,则不考虑P的Fe-Ni-SP系统的一阶分步结晶模型适用于解释铁陨石的演化。由Elsevier Ltd.发布

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