2012-2020年乌格利奇水库水体及底泥毒理学研究

I. Tomilina, R. Lozhkina, L. Grebenyuk
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引用次数: 0

摘要

根据水和底部沉积物的生物测定结果,对乌格利奇水库某些地区的毒理学状况进行了长期评估。2012-2020年研究期间,水库各断面水毒性均有降低的趋势。2019年亲缘斑颈蛇生殖指标达到最大值。底部沉积物的毒性在水库上游有轻微降低的趋势,在中下游没有变化。在2012-2013年对乌格利奇水库的致畸学研究中发现,观察期内口部结构发生病理改变的手蛾幼虫比例平均为14.5%,高于既定对照(6.7-7.0%)和背景值(0-8.0%)。水和沉积物污染的分析数据证实了生物测定的结果。在库区之间,水的污染系数在个别元素和总量上都没有显著差异。总污染系数和平均污染系数在中部达到最大值,其中Cu和Zn浓度较高。尽管水库底部沉积物中Cr、Ni、Cu、Zn、Cd和Pb的浓度呈下降趋势,但Cd、Cr、Ni和Zn的浓度超过了上伏尔加河流域设定的背景浓度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
TOXICOLOGICAL STUDIES OF WATER AND BOTTOM SEDIMENTS OF THE UGLICH RESERVOIR DURING THE PERIOD 2012–2020 years
A long-term assessment of the toxicological condition of certain areas of the Uglich reservoir is given based on the results of bioassay of water and bottom sediments. During the research period 2012–2020, there was a tendency of the toxicity reduction of water in all sections of the reservoir. The maximum values of reproductive indicators of Ceriodaphnia affinis were registered in 2019. The toxicity of bottom sediments had a slight tendency to decrease in the upper section of the reservoir and did not change in the middle and lower sections. During the teratological study of the Uglich reservoir in 2012–2013 years it was found that the proportion of chironomid larvae with pathomorphological changes in the structures of the mouth parts during the observation period was on average 14.5%, which is higher than the established control (6.7–7.0%) and background values (0–8.0%). The results of the bioassay are confirmed by analytical data on water and sediment pollution. Significant differences in the pollution coefficient of water between the reservoir areas, both in individual elements and in total, have not been recorded. The highest values of the total and average pollution coefficient were reached in the middle section, where higher concentrations of Cu and Zn were determined. Despite the tendency of decreasing concentrations of Cr, Ni, Cu, Zn, Cd and Pb in the bottom sediments of the reservoir, the levels of Cd, Cr, Ni and Zn exceeded their background concentrations established for the Upper Volga basin.
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