Study of spatial distribution of elements in the system “water – bottom sediments” of the Uzynbulak creek of the Semipalatinsk test site

N. Mukhamediyarov, S. Makarychev, V. V. Kolbin, M. Dyussembayeva, Erbol Z. Shakenov, G. M. Yessilkanov, Aray E. Temirzhanova, A. Tashekova, M. A. Umarov
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Abstract

The results of studying the features of the spatial distribution of macro- and microelements in the “water – bottom sediments” system in the channel of the Uzynbulak creek (“Degelen” site of the Semipalatinsk test site, Kazakhstan) are presented. The studies were carried out in the summer of 2015. As a result of the study of the chemical composition in surface waters and bottom sediments of the Uzynbulak creek, the content of Li, Be, Na, Mg, K, Ca, V, Ni, Mo, Fe, Sr, Al, Zn, Ba, La, Ce, U was revealed. The nature of the origin and the main factors determining the increased content of a number of the studied elements have been determined. The main mechanisms of the formation of the elemental composition in surface waters, the degree of spreading of elements exceeding the MPC (maximum permissible concentration) beyond the “Degelen” site are considered.
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塞米巴拉金斯克试验场乌津布拉克河“水底沉积物”系统中元素的空间分布研究
本文介绍了对Uzynbulak河(哈萨克斯坦塞米巴拉金斯克试验场“Degelen”试验场)河道“水底沉积物”系统中宏、微量元素空间分布特征的研究结果。这些研究于2015年夏天进行。通过对Uzynbulak河地表水和底泥化学成分的研究,揭示了该河流中Li、Be、Na、Mg、K、Ca、V、Ni、Mo、Fe、Sr、Al、Zn、Ba、La、Ce、U等元素的含量。已经确定了起源的性质和决定一些所研究元素含量增加的主要因素。考虑了地表水中元素组成形成的主要机制,以及元素在“Degelen”位点以外超过MPC(最大允许浓度)的扩散程度。
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