Collaborative Research: A New Mechanism for Metal Isotope Fractionation Induced by Natural Solid-State Ion Conduction

合作研究:天然固态离子传导诱导金属同位素分馏的新机制

基本信息

  • 批准号:
    2025319
  • 负责人:
  • 金额:
    $ 30.23万
  • 依托单位:
  • 依托单位国家:
    美国
  • 项目类别:
    Continuing Grant
  • 财政年份:
    2020
  • 资助国家:
    美国
  • 起止时间:
    2020-08-01 至 2024-07-31
  • 项目状态:
    已结题

项目摘要

Naturally occurring metallic silver is sometimes found with a wire-, string- or rope-like morphology, commonly called “wire silver”. Until recently, very little was known about the structural characteristics of wire silver and even less about how it forms. Surprisingly, this morphology can be created in the laboratory under simple conditions very different from those found in nature, yet their structural characteristics are very similar to natural samples. From the study of natural and synthetic specimens, it has been found that wire silver formation occurs by a solid-state process called “ion conduction”, where metal ions can move directly through a crystal structure, and in this case, silver(I) ions move through the mineral argentite. Even more surprising, this ion transport during wire growth causes an enrichment of the heavy stable isotope 109Ag in the wire. This is opposite of that predicted by mechanisms of isotope enrichment known to occur in nature. Thus, further study of wire silver growth may elucidate a previously unrecognized mechanism for isotope separation in nature. Understanding this mechanism and the degree of possible isotope enrichment is significant for our basic understanding of physical and chemical phenomena. These in turn have direct application to the study of geochemical and geological processes such as metal transport and the isotopic signatures found in ore deposits. Broader impacts include possible technological applications where the isotope chemistry of materials can affect their physical properties. This study involves scientists from multiple academic departments and different disciplines, and will include student training and participation at multiple levels, from undergraduates through doctoral candidates. This project integrates experimental mineralogy, analytical geochemistry and computational methods in the study of wire silver formation under highly controlled conditions as a means to elucidate the fundamental mechanism of the observed isotope effect. Isotope fractionation is hypothesized to result from the process of predissociation during superionic conduction, occurring preferentially for 109Ag+ ions as they move through the silver sulfide structure. The study will also test whether this isotope effect extends to other transition metals such as copper, zinc and nickel. Understanding the mechanisms, magnitude and direction of isotope fractionation is essential for the use and accurate interpretation of isotope data in geological studies, and allows for the engineered development of materials with “tuned” isotope chemistries. Finally, this unexploited physical phenomenon might be leveraged to improve the characteristics of technological devices that utilize fast ion conduction.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
自然生成的金属银有时呈线状、线状或绳状形态,通常被称为“线银”。直到最近,人们对线银的结构特征知之甚少,更不知道它是如何形成的。令人惊讶的是,这种形态可以在实验室中在与自然中发现的非常不同的简单条件下创造出来,但它们的结构特征与自然样品非常相似。从对天然和合成样品的研究中发现,金属丝银的形成是通过一种称为离子传导的固态过程进行的,在这种情况下,金属离子可以直接通过晶体结构移动,在这种情况下,银(I)离子通过矿物银辉石移动。更令人惊讶的是,金属丝生长过程中的离子传输导致金属丝中重的稳定同位素109Ag的浓缩。这与已知在自然界中发生的同位素浓缩机制所预测的相反。因此,对丝银生长的进一步研究可能会阐明自然界中一种以前不被认识的同位素分离机制。了解这种机制和可能的同位素富集度,对于我们对物理和化学现象的基本理解具有重要意义。这些反过来又直接应用于研究地球化学和地质过程,如金属迁移和在矿床中发现的同位素特征。更广泛的影响包括可能的技术应用,在这些应用中,材料的同位素化学可以影响其物理性质。这项研究涉及来自多个学术部门和不同学科的科学家,并将包括从本科生到博士生的多个层次的学生培训和参与。该项目将实验矿物学、分析地球化学和计算方法结合在一起,研究高度受控条件下线银的形成,以阐明所观察到的同位素效应的基本机制。同位素分馏被认为是在快离子传导过程中预解离过程的结果,当109Ag+离子通过硫化银结构时优先发生。这项研究还将测试这种同位素效应是否延伸到铜、锌和镍等其他过渡金属。了解同位素分馏的机制、大小和方向对于在地质学研究中使用和准确解释同位素数据至关重要,并使“调整”的同位素化学物质的工程化开发成为可能。最后,这种未被利用的物理现象可能被用来改进利用快速离子传导的技术设备的特征。该奖项反映了NSF的法定使命,并通过使用基金会的智力优势和更广泛的影响审查标准进行评估,被认为值得支持。

项目成果

期刊论文数量(1)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Development and validation of ReaxFF forcefield for solid-state ion conduction in Ag/S-based systems.
用于 Ag/S 系统中固态离子传导的 ReaxFF 力场的开发和验证。
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John Rakovan其他文献

Energy-resolved neutron imaging and diffraction including grain orientation mapping using event camera technology
使用事件相机技术的能量分辨中子成像和衍射,包括晶粒取向映射
  • DOI:
    10.1038/s41598-025-96790-1
  • 发表时间:
    2025-04-15
  • 期刊:
  • 影响因子:
    3.900
  • 作者:
    Tsviki Y. Hirsh;Andrew F. T. Leong;Adrian S. Losko;Alexander Wolfertz;Daniel J. Savage;Tim T. Jäger;John Rakovan;James J. Wall;Alexander M. Long;Sven C. Vogel
  • 通讯作者:
    Sven C. Vogel
Geochemical and textural characterization of phosphate accessory phases in the vein assemblage and metasomatically altered Llallagua tin porphyry
  • DOI:
    10.1007/s00710-017-0510-6
  • 发表时间:
    2017-03-31
  • 期刊:
  • 影响因子:
    1.100
  • 作者:
    Wladyslaw B. Betkowski;John Rakovan;Daniel E. Harlov
  • 通讯作者:
    Daniel E. Harlov

John Rakovan的其他文献

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{{ truncateString('John Rakovan', 18)}}的其他基金

Development of a Tender-Energy Microspectroscopy and Imaging User Facility for Earth Sciences at NSLS and NSLS-II
NSLS 和 NSLS-II 地球科学招标能源显微光谱和成像用户设施的开发
  • 批准号:
    1128753
  • 财政年份:
    2013
  • 资助金额:
    $ 30.23万
  • 项目类别:
    Standard Grant
Coprecipitation of Pb and As in apatite and applications to environmental remediation
磷灰石中 Pb 和 As 的共沉淀及其在环境修复中的应用
  • 批准号:
    0952298
  • 财政年份:
    2010
  • 资助金额:
    $ 30.23万
  • 项目类别:
    Continuing Grant
Collaborative Research: Crystal Chemistry of U, Th and Other Radionuclides in Apatite: Environmental and Geochemical Implications
合作研究:磷灰石中 U、Th 和其他放射性核素的晶体化学:环境和地球化学影响
  • 批准号:
    0409435
  • 财政年份:
    2004
  • 资助金额:
    $ 30.23万
  • 项目类别:
    Standard Grant
Collaborative Research: The Palygorskite-Sepiolite to Smectite Transformation and the Influence on Reactive Surface Sites
合作研究:坡缕石-海泡石向蒙皂石的转变及其对反应表面位点的影响
  • 批准号:
    0001251
  • 财政年份:
    2000
  • 资助金额:
    $ 30.23万
  • 项目类别:
    Standard Grant
Probing the Structure and Energetics of Reactive Sites at the Mineral-Water Interface: Implications for Element Partitioning and Geochronology
探测矿泉水界面反应位点的结构和能量:对元素划分和地质年代学的影响
  • 批准号:
    9814691
  • 财政年份:
    1999
  • 资助金额:
    $ 30.23万
  • 项目类别:
    Standard Grant

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合作研究:REU 地点:地球与行星科学和天体物理学 REU 与纽约市立大学合作,位于美国自然历史博物馆
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