Three Typical Hydrological-Hydrochemical Situations Near the Danube River Mouth Based on the Marine Hydrophysical Institute Research Expeditions in 1997-2013

IF 0.7 Q4 OCEANOGRAPHY Physical Oceanography Pub Date : 2019-07-01 DOI:10.22449/0233-7584-2019-4-367-383
S. Kondratev
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引用次数: 3

Abstract

Purpose. The paper is aimed at studying the present state of water ecology of the Black Sea northwestern shelf (NWS). Since the early 60-ies of the last century, ecology in this region deteriorated seriously due to intensive anthropogenic load that resulted in eutrophication of waters and regular fish mortality in the warm period of a year. Methods and Results. In 1997-2013 Marine Hydrophysical Institute realized 7 hydrological and hydrochemical expeditions near the Danube mouth. The dissolved oxygen and nutrients (nitrate, nitrite, phosphate and silicic acid) contents were analyzed in the water samples collected at the bottom (0.5-1 m above the bottom) and surface (0-1 m) horizons. Conclusions. Revealed are three hydrological-hydrochemical situations typical of the region: distribution of the transformed Danube flow far to the east, pressing of the Danube flow to the west coast of the Black Sea and alongshore upwelling. Silica and nitrate are rapidly and almost completely extracted from the seawater (the latter one – even in early winter) during photosynthesis in the surface waters on the NWS. The processes of particulate organic matter mineralization in the bottom waters of the NWS are assumed to be an additional source of silicic acid and nitrates. As for silicic acid, the process takes place during a warm season, and for nitrates – even in early winter. The alongshore upwelling in summer can lead to oxygen deficiency in the coastal waters and that, in its turn, can result in fish mortality on the shelf. The waters of the northwestern shelf open part which, in autumn 2010, pressed the Danube transformed freshwater flow to the Black Sea west coast, contained very small concentrations of biogenic elements (low content of silicic acid should be particularly noted). The study confirms the fact that the hazardous process of change in the phytoplankton species composition still continues, thus, altering the whole food chain in the Black Sea.
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基于1997-2013年海洋水文研究所考察的多瑙河河口三种典型水文水化学情况
目的。本文旨在研究黑海西北陆架(NWS)水生态的现状。自上世纪60年代初以来,由于强烈的人为负荷,该地区生态恶化严重,导致水体富营养化,鱼类在一年中温暖期出现规律性死亡。方法与结果。1997-2013年,海洋水文物理研究所在多瑙河口附近进行了7次水文和水化学考察。分析了底部(离底0.5-1 m)和表层(0-1 m)水样中溶解氧和营养物质(硝酸盐、亚硝酸盐、磷酸盐和硅酸)的含量。结论。揭示了该地区典型的三种水文-水化学状况:多瑙河流的转变向东分布、多瑙河流向黑海西海岸的挤压和沿岸上升流。二氧化硅和硝酸盐在NWS地表水的光合作用中迅速而几乎完全地从海水中提取出来(后者-即使在初冬)。NWS海底颗粒有机质矿化过程被认为是硅酸和硝酸盐的另一个来源。至于硅酸,这个过程发生在温暖的季节,而硝酸盐,甚至在初冬也会发生。夏季的沿岸上升流会导致沿海水域缺氧,进而导致大陆架上的鱼类死亡。2010年秋天,西北大陆架开放部分的水域挤压多瑙河,将淡水流转化为黑海西海岸,其中生物元素的浓度非常低(硅酸的含量很低,应该特别注意)。这项研究证实了这样一个事实,即浮游植物物种组成的危险变化过程仍在继续,从而改变了黑海的整个食物链。
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来源期刊
Physical Oceanography
Physical Oceanography OCEANOGRAPHY-
CiteScore
1.80
自引率
25.00%
发文量
8
审稿时长
24 weeks
期刊最新文献
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