Comparative analysis of the structure of planktonic algae of the Volga and Kama rivers before their confluence in the Kuibyshev reservoir (the Republic of Tatarstan, RF)

Q3 Agricultural and Biological Sciences
L. Khaliullina
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Abstract

The article presents the results of comparative analysis of the structure of planktonic algae in the Volga and Kama rivers, as well as the assessment of the trophic state of these water bodies, which form the Kuibyshev reservoir at their confluence. The hydrochemical regime of the Kuibyshev reservoir is nonhomogeneous and is determined by the chemical properties of the Volga and Kama, differing in the ratio of ions and mineralization. The ionic compositionin Kama is often dominated by sulfates. Its mineralization ranges from 168 to 674 mg L-1, depending on the season and dryness of the year. The Volga contains calcium hydrocarbonate and display a lower degree of mineralization (120-130 mg L-1). Different composition of the incoming water, runoff rate, the degree of volume drawdown, intra-basin processes and groundwater inflows exhibit a direct impact on the conditions for the existence of planktonic algae. During the growing season of 2012, 123 algae taxa were identified among the phytoplankton of the Volga and Kama rivers (the areas before their confluence in the Kuibyshev reservoir). In terms of species diversity, diatoms and green algae were prevalent. The Volga exhibits higher species diversity (107 species), while the phytoplankton in Kama displays less diverse (77 species). In the seasonal dynamics of phytoplankton in both areas, two peaks of abundance and biomass are observed, i.e., at the middle and at the end of summer. The studied areas of Volga River are characterized by a phytoplankton complex of blue-green, diatoms and green algae, while diatom phytoplankton predominates in Kama River. In the summer-autumn period, the "blooming" of water in both rivers is connected with massive development of blue-green algae of the genera Aphanizomenon, Microcystis, Anabaena and Oscillatoria. During most of the growing season, the waters of Volga and Kama rivers belong to the mesasaprobic type and correspond to the moderately-polluted zone. Moreover, the waters of Kama River are characterized by higher saprobity indices. The trophic status of studied rivers mostly corresponds to eutrophic type, and in the periods of maximum development of planktonic algae - to hypereutrophic type.
伏尔加河和卡马河汇入古比雪夫水库前浮游藻类结构的比较分析(鞑靼斯坦共和国,俄罗斯)
本文介绍了对伏尔加河和卡马河浮游藻类结构的比较分析结果,以及对这些水体营养状态的评估,这些水体在它们的交汇处形成了库比雪夫水库。Kuibishev储层的水化学状况是不均匀的,由Volga和Kama的化学性质决定,离子和矿化率不同。Kama的离子组成通常以硫酸盐为主。其矿化度范围为168至674 mg L-1,具体取决于季节和一年中的干燥程度。伏尔加河含有碳酸氢钙,矿化度较低(120-130 mg L-1)。进水的不同组成、径流量、水量下降程度、流域内过程和地下水流入量对浮游藻类的存在条件有直接影响。在2012年的生长季节,在伏尔加河和卡马河的浮游植物中发现了123个藻类分类群(在它们汇入库比雪夫水库之前的区域)。就物种多样性而言,硅藻和绿藻占主导地位。伏尔加河的物种多样性较高(107种),而卡马的浮游植物多样性较低(77种)。在这两个地区浮游植物的季节动态中,观察到丰度和生物量的两个峰值,即在夏中和夏末。伏尔加河研究区的特点是由蓝绿色、硅藻和绿藻组成的浮游植物复合体,而硅藻浮游植物在卡马河占主导地位。在夏秋季节,两河水体的“开花”与Aphanizomenon属、微囊藻属、Anabaena属和Oscillania属蓝绿藻的大量发育有关。在生长季节的大部分时间里,伏尔加河和卡马河的水域属于中亚热带,属于中度污染区。此外,Kama河的水域具有较高的皂化指数。所研究河流的营养状况大多对应于富营养型,并且在浮游藻类发育最大的时期,为超富营养型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
caspian journal of environmental sciences
caspian journal of environmental sciences Environmental Science-Environmental Science (all)
CiteScore
2.30
自引率
0.00%
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0
审稿时长
5 weeks
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