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ZrF对LiF-BeF熔盐中UO沉淀的抑制作用。

Inhibition effect of ZrF on UO precipitation in the LiF-BeF molten salt.

作者信息

Peng Hao, Song Yulong, Ji Nan, Xie Leidong, Huang Wei, Gong Yu

机构信息

Shanghai Institute of Applied Physics, Chinese Academy of Sciences Shanghai 201800 PR China

University of Chinese Academy of Sciences Beijing 100049 PR China.

出版信息

RSC Adv. 2021 May 24;11(31):18708-18716. doi: 10.1039/d1ra02332b.

Abstract

The dissolution-precipitation behavior of zirconium dioxide (ZrO) in molten lithium fluoride-beryllium fluoride (LiF-BeF, (2 : 1 mol, FLiBe)) eutectic salt at 873 K was studied. The results of the dissolution experiment showed that the saturated solubility of ZrO in the FLiBe melt was 3.84 × 10 mol kg with equilibrium time of 6 h, and its corresponding apparent solubility product (') was 3.40 × 10 mol kg. The interaction between Zr(iv) and O was studied by titrating lithium oxide (LiO) into the FLiBe melt containing zirconium tetrafluoride (ZrF), and the concentration of residual Zr(iv) in the melt gradually decreased due to precipitate formation. The precipitate corresponded to ZrO, as confirmed by the stoichiometric ratio and X-ray diffraction analysis. The ' was 3.54 × 10 mol kg, which was highly consistent with that from the dissolution experiment. The obtained ' of ZrO was in the same order of magnitude as that of uranium dioxide (UO), indicating that a considerable amount of ZrF could inhibit the UO formation when oxide contamination occurred in the melt containing ZrF and uranium tetrafluoride (UF). Further oxide titration in the LiF-BeF-ZrF (5 mol%)-UF (1.2 mol%) system showed that ZrO was formed first with O addition less than 1 mol kg, and the precipitation of UO began only after the O addition reached 1 mol kg and the precipitation of ZrO decreased the ZrF concentration to 0.72 mol kg (3 mol%). Lastly, UO and ZrO coprecipitated with further O addition of more than 1 mol kg. The preferential formation of ZrO effectively avoided the combination of UF and O. This study provides a solution for the control of UO precipitation in molten salt reactors.

摘要

研究了二氧化锆(ZrO)在873K的熔融氟化锂-氟化铍(LiF-BeF,(2:1摩尔,FLiBe))共晶盐中的溶解-沉淀行为。溶解实验结果表明,ZrO在FLiBe熔体中的饱和溶解度为3.84×10⁻⁵摩尔/千克,平衡时间为6小时,其相应的表观溶度积(Ksp)为3.40×10⁻¹⁰摩尔²/千克²。通过将氧化锂(Li₂O)滴定到含有四氟化锆(ZrF₄)的FLiBe熔体中,研究了Zr(Ⅳ)与O之间的相互作用,由于沉淀形成,熔体中残余Zr(Ⅳ)的浓度逐渐降低。经化学计量比和X射线衍射分析证实,沉淀物对应于ZrO。其Ksp为3.54×10⁻¹⁰摩尔²/千克²,与溶解实验结果高度一致。所得到的ZrO的Ksp与二氧化铀(UO₂)的Ksp处于同一数量级,这表明当含有ZrF₄和四氟化铀(UF₄)的熔体中发生氧化物污染时,大量的ZrF₄可以抑制UO₂的形成。在LiF-BeF-ZrF₄(5摩尔%)-UF₄(1.2摩尔%)体系中进一步进行氧化物滴定表明,当添加的O小于1摩尔/千克时,首先形成ZrO,只有当添加的O达到1摩尔/千克且ZrO的沉淀使ZrF₄浓度降至0.72摩尔/千克(3摩尔%)时,UO₂的沉淀才开始。最后,当添加的O超过1摩尔/千克时,UO₂和ZrO会共沉淀。ZrO的优先形成有效地避免了UF₄与O的结合。本研究为控制熔盐反应堆中UO₂沉淀提供了一种解决方案。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ca46/9033476/fc7e4e275c6d/d1ra02332b-f1.jpg

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