课题基金 / 基金详情

Time-Resolved Structural Analysis of Heavy Metal Cation Exchange Reactions in Anionic Clay and Manganese Oxide Nanoparticles

Time-Resolved Structural Analysis of Heavy Metal Cation Exchange Reactions in Anionic Clay and Manganese Oxide Nanoparticles
阴离子粘土和氧化锰纳米颗粒中重金属阳离子交换反应的时间分辨结构分析
批准号:
0125908
负责人:
Peter Heaney
金额:
$22.6万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2002
资助国家:
美国
项目状态:
已结题
起止时间:
2002-01-01 至 2005-12-31

项目摘要

项目成果

Peter Heaney的其他基金

相似基金

相关文献

中文摘要
翻译
点击翻译按钮获取中文摘要
英文摘要
HeaneyEAR-0125908Anionic clays and manganese oxides occur abundantly as nanocrystalline coatings on soil and sediment particles in surficial environments. They exhibit a remarkable facility for exchanging ions dissolved in aqueous fluids and act as major traps for anions and cations. The investigators of this proposal will apply a novel crystallographic approach to resolve mechanisms of cation exchange in layered double hydroxide and Mn oxide materials. Powdered samples will be monitored by synchrotron X-ray diffraction during the process of cation exchange. These experiments will yield the first time-resolved analyses of the structural distortions that occur to accommodate substitutions by transition metals in low-temperature minerals. Additionally, in concert with high-temperature infrared spectroscopy, synchrotron XRD analyses will be performed as samples are heated, allowing the structural manifestations of thermal decomposition to be correlated with cation exchange capacity.These studies will allow the investigators to capture intermediate transition steps that are overlooked by a more conventional static analysis of final run products. As the structural perturbations that are associated with chemical substitutions tend to stabilize the exchanged phases, these studies will indicate which factors limit the degree of exchange for selected cations. Consequently, these experiments will suggest approaches to the design of new remediation materials with amplified exchange characteristics.
期刊论文(0)
专著(0)
科研奖励(0)
会议论文
Structural controls on Fe oxide formation: A crystallographic analysis of the growth of hematite versus goethite
In situ synchrotron X-ray diffraction of Fe oxide transformations in aqueous solutions
Mechanisms of Mineral Dissolution: Time-Resolved Synchrotron X-ray Diffraction of Fe-and Mn-oxides with Dissolved Organic Ligands
Time-Resolved Diffraction Studies of Soil-Forming Mineral Reactions
海外基金