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LANTHANIDE OXALATES AS A POSSIBLE FORM OF INTERMEDIATE SEPARATION FOR LONG-LIVED FISSION-PRODUCT NUCLIDES

机译:草酸镧作为长寿裂变产物核素中间分离的一种可能形式

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The chemical composition of fission-product nuclides after their removal from a reactor after one year operation attracts attention by prevalence of rare earth elements (La, Ce, Pr, Nd, Pm, Y) together with alkaline (Cs) and alkaline-earth (Sr, Ba) elements. Their contribution to the total radioactivity increases with time and reaches up to 96% in 5 years. All lanthanides form some types of insoluble compounds, and oxalates are one of them. The solubility products of both normal (simple) oxalates and double REE oxalates with added alkaline cations are considered as a basis for possible intermediate operation of lanthanide group precipitation. Ba and Sr could be coprecipitated together with them, especially within a universal Ca-oxalate matrix. Long-lived actinides (Pu, Am, Np, Cm) form sparingly insoluble oxalates too, and they are discussed as probable participants of suggested technology.
机译:裂变产物核素在运行一年后从反应堆中移出后的化学组成引起稀土元素(La,Ce,Pr,Nd,Pm,Y)以及碱金属(Cs)和碱土( Sr,Ba)元素。它们对总放射性的贡献随时间增加,并在5年内达到96%。所有镧系元素均形成某些类型的不溶性化合物,草酸盐是其中之一。普通(简单)草酸盐和双REE草酸盐与添加的碱性阳离子的溶解度产物均被视为镧系元素沉淀可能的中间操作的基础。 Ba和Sr可以与它们一起沉淀,尤其是在通用草酸钙基质中。长寿命的act系元素(Pu,Am,Np,Cm)也会形成难溶的草酸盐,它们被认为是建议技术的参与者。

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