Prevalence of rare earth elements in natural waters of Khanty-Mansiysk

Tatiana I. Romanova, Mihail G. Korotkov, Yuri V. Korzhov
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Abstract

Relevance. New data on the content of lanthanides in the water–rock system are important for understanding the behavior of rare-earth elements in the environment, open up the possibility of using them as indicators of geochemical processes and anthropogenic factor, taking into account the specialities of their migration and fractionation. Aim. Assessment of the quantitative content and distribution of rare-earth elements (La, Ce, Pr, Nd, Pm, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu) in the surface and underground waters of Khanty-Mansiysk to identify the main patterns of their behavior. Objects. Surface and underground waters of the natural reserve Samarovsky Chugas, as well as ground deposits and products of secondary mineral formation. Methods. The bulk analysis of water is performed by a standard set of spectral and electrochemical methods. The rare-earth content was determined by inductively coupled plasma mass spectrometry. Chemical composition of ground deposits and secondary mineral formation products – by neutron activation analysis. Results. The paper demonstrates rare-earth elements behavior in aqueous medium, ground deposits and products of secondary mineral formation. Different approaches to rare-earth elements rationing in waters and solid sediments showed comparability of lanthanide distribution spectra to each other and made it possible to identify some features of the rare-earth elements distribution pattern in different environments. In the waters, there are positive anomalies of europium and gadolinium and negative anomaly of cesium. Gadolinium anomalies were detected in ground deposits, and europium in secondary mineral formation products. The high migration activity of the entire considered series of rare-earth elements in the solution coming from the holding deposits was established. During following geochemical processes, mainly middle lanthanides (Sm, Eu, Gd, and Tb) fall out of the solution in the form of secondary mineral formation products. 
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汉特-曼西斯克天然水域中稀土元素的含量
相关性。有关水-岩石系统中镧系元素含量的新数据对于了解稀土元素在环境中的行为非常重要,并为将其用作地球化学过程和人为因素的指标提供了可能性,同时考虑到其迁移和分馏的特殊性。目标评估汉特-曼西斯克市地表水和地下水中稀土元素(La、Ce、Pr、Nd、Pm、Sm、Eu、Gd、Tb、Dy、Ho、Er、Tm、Yb、Lu)的定量含量和分布情况,以确定其行为的主要模式。研究对象萨马洛夫斯基丘加斯自然保护区的地表水和地下水,以及地面沉积物和二次矿物形成的产物。分析方法水体分析采用一套标准的光谱和电化学方法。稀土含量采用电感耦合等离子体质谱法测定。地面沉积物和二次矿物形成产物的化学成分--采用中子活化分析法。结果。论文展示了稀土元素在水介质、地面沉积物和二次矿物形成产物中的行为。水和固体沉积物中稀土元素配比的不同方法表明,镧系元素的分布光谱相互之间具有可比性,因此可以确定不同环境中稀土元素分布模式的一些特征。在水体中,铕和钆呈正异常,铯呈负异常。在地面沉积物中检测到钆异常,在二次矿物形成产物中检测到铕异常。在来自矿床的溶液中,所考虑的所有稀土元素都具有很高的迁移活性。在接下来的地球化学过程中,主要是中镧系元素(Sm、Eu、Gd 和 Tb)以二次成矿产物的形式从溶液中脱落。
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