SEA-PORT CONSTRUCTION IMPACT ON LIMAN NATURE ALONG THE BLACK SEA COASTAL ENVIRONMENT

Author(s):  
Р. Перерайс ◽  
R. Pererays

Construction of sea-ports in limanic aquathory along the Northern Black Sea coast have prefer impact on the coastal environment. Especially deep impact have liman bottom artificial deepening, liman slopes artificial reconstruction, navigate canals, jetties of different sizes, ground dumps etc. Typical examples are Odessa, Ill'ichevsk, Yuzhniy commercial sea-ports in northern sector of the Black Sea. On shores nearest Port Yuzhniy jetties was firstly employed new construction against sea wave erosion. This new artificial shore terrace, that consist of natural matherials, expressed as shore protection, purification of sea water, needless ground depot, new shore territory and squire for recreants simultaneous.

2019 ◽  
Vol 25 ◽  
pp. 63-78
Author(s):  
Andrey G. Kostianoy ◽  
Sergey A. Lebedev ◽  
Dmitry M. Soloviev ◽  
Yalcin Tepe

Heavy rains have become a serious problem for the coastal zone of the Krasnodar Territory of the Russian Federation and the Black Sea coast of Turkey. They lead to a significant increase in water levels in rivers, flooding of villages and even large cities, damage to urban and tourist infrastructure, roads and railways, bridges, beaches, flushing of garbage and sewage into rivers. This leads to environmental problems and even loss of life. River runoff forms river plumes in the coastal zone of the sea, which, depending on wind speed and direction, speed and direction of coastal currents, river runoff and density difference with sea water, can have various forms and spread in different directions from the mouth of the river, as well as participate in mesoscale and sub-mesoscale circulation of coastal waters. River plumes significantly affect the quality of sea water and the sanitary and epidemiological situation on the beaches of the resort area of Krasnodar Territory and Turkey. The situation is aggravated by the fact that sewage systems are in poor condition in cities or are completely absent in most of small villages along rivers and the coastal zone. After heavy rains, wastewater very often reaches the sea and poses a serious threat to human health. The purpose of this study is to use satellite remote sensing to demonstrate the behavior of river plumes along the Black Sea Turkish coast.


2021 ◽  
Vol 250 ◽  
pp. 05001
Author(s):  
Mzia Diasamidze ◽  
Ana Shotadze

The aim of this research is to study the main ecological parameters of the Black Sea in an experimental way as well as to evaluate the results and to draw conclusions. We aim at determining the cause of pollution of the sea area represented by the emissions from ships’ engines and pollution by surface waters. Our empirical part that included the field expeditions, sampling was carried out with the involvement of students within the framework of the internal grant research project “Monitoring of the Black Sea Ecological Status - Sea Water Quality Survey”. We studied the level of pollution of two rivers flowing into the Black Sea, Bartskhana and Kubistskali, and made relevant conclusions about the types of pollution, proper measurements and causal relationship of the causes of sea water pollution with the vessels entering the port of Batumi.


2019 ◽  
pp. 135-149
Author(s):  
L. M. Poletayeva ◽  
O. Yu. Sapko ◽  
T. A. Safranov

Among all the natural resources available in Odesa Region vacationists prefer beaches and associated entertainments. Quality and general ecological condition of the beaches in addition to the potential and actual beach capacity are key factors for tourist flow to Odesa Region and its socio-economic development. In order to substantiate the recreational and tourist development of the territory an economic and logistic evaluation of its resource base should be carried out. This will make it possible to determine an input tourist flow which dictates the volumes of required tourist infrastructure and material and technical facilities. The purpose of this study is to evaluate recreational potential of Odesa Region’s beach zones. To achieve this, all main natural and anthropogenic factors determining the recreational potential of the coastal zone were analyzed. The study is also based on scientific researches in the field of recreational and tourist activities made by well-known experts, on the existing regulatory frameworks and results of the authors' own research works. For the first time, recreational capacity and logistic potential of Odesa Region’s beach zones were estimated. Based on this estimation multiple conclusions about the most promising areas for future development of the recreation sector were made. It was determined that favorable climatic conditions, considerable length of beaches and other natural and recreational resources allow us to speak about good prospects of the Odesa Region’s coastal zone for various forms of recreation including thalassotherapy. In fact, thalassotherapy opportunity (first of all, beach recreation) is a very important factor of attractiveness for vacationists visiting the Odesa Region’s coastal zone. According to our research, Bilhorod-Dnistrovskyi, Tatarbunarskyi and Lymanskyi districts are the most promising ones for recreational development. The total capacity of the beaches here even exceeds the districts' own population. Conducted recreational zoning of the Odesa’s Black Sea coast established that, based on the natural recreational factors, out of 9 recreational microdistricts only 3 of them may be classified as favorable, with 5 being relatively favorable and 1 – completely unfavorable. But, from the perspective of sea water quality, some microdistricts (Luzanivskyi and Arkadiyskyi) do not meet sanitary standards during the period of intense precipitation. It was found that there is a need for expansion of beach areas as well as a need for regulation and redistribution of the recreational and tourist flow. In order to increase recreational attractiveness of Odesa Region, regional and city administrations should pay more attention to the ecological conditions of beach areas of the Black Sea coast. The obtained results may be used by the Department of Culture and Tourism of the Odesa Regional State Administration, divisions of the Ministry of Ecology and Natural Resources of Ukraine in order to assess the recreational potential of the Odesa Region’s beach areas.


2019 ◽  
Vol 4 (1) ◽  
pp. 3-11
Author(s):  
B. N. Belyaev ◽  
N. M. Beregovaya

The results of long-term studies of conditions of cultivation of red Black Sea algae Gelidium spinosum (S. G. Gmelin) P. C. Silva (Rhodophyta) in Silva P. C., Basson P. W. & Moe R. L. 1996: 141 in the systems of engineering type aimed at increasing R-phycoerythrin concentration are given. The systems were developed on the basis of studying the influence of temperature, light and regimes of the nutrient medium flow saturated with carbon dioxide on the biomass growth and were protected by several patents. Anti-fouling methods were also taken into consideration while developing the systems. The relevance of the work is determined by the value of G. spinosum, which is a natural pigment and food dye, a powerful antioxidant used in immune diagnosis, microscopy and cytometry, the cost of which is estimated at $3250–14000 per 1 gram. The aim of the work was to optimize Black Sea G. spinosum cultivation conditions in the coastal systems of engineering type for increasing the yield of the R-phycoerythrin per unit of the area of cultivators. As the material we used G. spinosum from fouling of the rocks and shore protection structures in the vicinity of Sevastopol, which was cultivated in the laboratory setup at the temperature in the range of 15–27 °C, light intensity 10–25 klx in the regime of 18 h day : 6 h night, variations of flow of the nutrient medium using the Black Sea water with addition of salt, salts of nitrogen, phosphorus, iron, magnesium and manganese. At the last stage of the work the yield was (96.2 ± 8.8) g·m−2·day−1 of G. spinosum wet weight. At the lowest harvest of 87.4 g·m−2, with a minimum of dry matter of 36 % and the content of phycoerythrin to 12 mg·g−1, the pigment yield of R-phycoerythrin will be 378.6 mg·m−2·day−1. In the future, the coastal system of the cultivators with the depth of 0.5 m and mirror surface area of 1 ha (when working only 300 days a year) will produce not less than 1100 kg of R-phycoerythrin.


Author(s):  
S. Z. Baykara ◽  
E. H. Figen ◽  
A. Kale ◽  
T. N. Veziroglu

Hydrogen sulphide, an acid gas, is generally considered an environmental pollutant. As an industrial byproduct, it is produced mostly during fuel processing. Hydrogen sulphide occurs naturally in many gas wells and also in gas hydrates and gas-saturated sediments especially at the bottom of the Black Sea where 90% of the sea water is anaerobic.The anoxic conditions exist in the deepest parts of the basin since nearly 7300 years, caused by the density stratification following the significant influx of the Mediterranean water through the Bosphorous nearly 9000 years ago. Here, H2S is believed to be produced by sulphur reducing bacteria at an approximate rate of 10 000 tons per day, and it poses a serious threat since it keeps reducing the life in the Black Sea. An oxygen–hydrogen sulphide interface is established at 150–200 m below the surface after which H2S concentration starts increasing regularly until 1000 m, and finally reaches a nearly constant value of 9.5 mg/l around 1500 m depth.Hydrogen sulphide potentially has economic value if both sulphur and hydrogen can be recovered. Several methods are studied for H2S decomposition, including thermal, thermochemical, electrochemical, photochemical and plasmochemical methods.In the present work, H2S potential in the Black Sea is investigated as a source of hydrogen, an evaluation of the developing prominent techniques for hydrogen production from H2S is made, and an engineering assessment is carried out regarding hydrogen production from H2S in the Black Sea using a process design based on the catalytic solar thermolysis approach. Possibility of a modular plant is considered for production at larger scale.


Author(s):  
Г. Выхованец ◽  
G. Vyhovanec

Typical coastal elements of limans and lagoons are barriers, that separate limanic aquatories from a Seas. On limanic shores structure of the Black Sea sand barriers represented three longitudinal landscape “zones”: sea beach (“frontal”), dune-aeolian and limanic (“back of the barrier”). They closely interactive between themselves under influence of lithodynamical exchanges of sediment. General tendency of the barriers dynamics is displacement to Land direction.


Author(s):  
Elena Kovaleva ◽  
Elena Kovaleva ◽  
Alexander Izhitskiy ◽  
Alexander Izhitskiy ◽  
Alexander Egorov ◽  
...  

Studying of methane formation and distribution in natural waters is important for understanding of biogeochemical processes of carbon cycle, searching for oil and gas sections and evaluation of CH4 emissions for investigations of greenhouse effect. The Black Sea is the largest methane water body on our planet. However, relatively low values of methane concentration (closed to equilibrium with the atmospheric air) are typical of the upper aerobic layer. At the same time, the distribution pattern of CH4 in surface waters of coastal areas is complicated by the influence of coastal biological productivity, continental runoff, bottom sources, hydrodynamic processes and anthropogenic effect. The investigation is focused on the spatial variability of dissolved methane in the surface layer of the sea in coastal regions affected by the continental runoff and anthropogenic pressure. Unique in situ data on methane concentrations were collected along the ship track on 2 sections between Sochi and Gelendzhik (2013, 2014) and 2 sections between Gelendzhik and Feodosia (2015). Overall 170 samples were obtained. Gas-chromatographic analysis of the samples revealed increase of CH4 saturation in the southeastern part of the Crimean shelf and the Kerch Strait area. Such a pattern was apparently caused by the influence of the Azov Sea water spread westward along the Crimean shore from the strait. This work was supported by the Russian Science Foundation, Project 14-50-00095 and the Russian Foundation for Basic Research, Project 16-35-00156 mol_a.


Author(s):  
Olga Mashukova ◽  
Olga Mashukova ◽  
Yuriy Tokarev ◽  
Yuriy Tokarev ◽  
Nadejda Kopytina ◽  
...  

We studied for the first time luminescence characteristics of the some micromycetes, isolated from the bottom sediments of the Black sea from the 27 m depth. Luminescence parameters were registered at laboratory complex “Svet” using mechanical and chemical stimulations. Fungi cultures of genera Acremonium, Aspergillus, Penicillium were isolated on ChDA medium which served as control. Culture of Penicillium commune gave no light emission with any kind of stimulation. Culture of Acremonium sp. has shown luminescence in the blue – green field of spectrum. Using chemical stimulation by fresh water we registered signals with luminescence energy (to 3.24 ± 0.11)•108 quantum•cm2 and duration up to 4.42 s, which 3 times exceeded analogous magnitudes in a group, stimulated by sea water (p < 0.05). Under chemical stimulation by ethyl alcohol fungi culture luminescence was not observed. Culture of Aspergillus fumigatus possessed the most expressed properties of luminescence. Stimulation by fresh water culture emission with energy of (3.35 ± 0.11)•108 quantum•cm2 and duration up to 4.96 s. Action of ethyl alcohol to culture also stimulated signals, but intensity of light emission was 3–4 times lower than under mechanical stimulation. For sure the given studies will permit not only to evaluate contribution of marine fungi into general bioluminescence of the sea, but as well to determine places of accumulation of opportunistic species in the sea.


Author(s):  
Natalia Andrulionis ◽  
Natalia Andrulionis ◽  
Ivan Zavialov ◽  
Ivan Zavialov ◽  
Elena Kovaleva ◽  
...  

This article presents a new method of laboratory density determination and construction equations of state for marine waters with various ionic compositions and salinities was developed. The validation of the method was performed using the Ocean Standard Seawater and the UNESCO thermodynamic equation of state (EOS-80). Density measurements of water samples from the Aral Sea, the Black Sea and the Issyk-Kul Lake were performed using a high-precision laboratory density meter. The obtained results were compared with the density values calculated for the considered water samples by the EOS-80 equation. It was shown that difference in ionic composition between Standard Seawater and the considered water bodies results in significant inaccuracies in determination of water density using the EOS-80 equation. Basing on the laboratory measurements of density under various salinity and temperature values we constructed a new equation of state for the Aral Sea and the Black Sea water samples and estimated errors for their coefficients.


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