The North Crimean Canal is a watercourse originating from the Kakhovka Reservoir and flowing into the Crimean Peninsula.The canal is an important source of drinking water supply and is also used to irrigate agricultur...The North Crimean Canal is a watercourse originating from the Kakhovka Reservoir and flowing into the Crimean Peninsula.The canal is an important source of drinking water supply and is also used to irrigate agricultural lands and fillfish farms.Due to its location,in recent years its functioning has not been stable,and the processes occurring along the canal have been poorly studied.In this study,we determined the content(with a safety assessment),features of spatial and seasonal distribution,and potential sources of hydrocarbons in the water of the North Crimean Canal,Crimea.During the study period(from March to November 2023)in the primary canal,the content of aliphatic hydrocarbons did not exceed sanitary standards(0.05 mg·L^(-1)).Their increased concentrations in the secondary canals could be associated with the input of organic substances into the canal water as it moves across the Crimean Peninsula.The composition of n-alkanes had temporal and spatial variability.In the period from spring to autumn,the content of autochthonous compounds decreased sharply.The share of allochthonous compounds increased as a consequence of the natural processes.The analysis of biogeochemical markers showed that autochthonous compounds produced by phytoplankton predominated in the spring–summer period.Subsequently,they had less importance,and the main share was accounted for allochthonous n-alkanes.展开更多
1 Introduction A presence of resting stages in various aquatic organisms is a long-known phenomenon as a mechanism of species adaptation to exist in unstable aquatic habitats,surviving adverse conditions in the"s...1 Introduction A presence of resting stages in various aquatic organisms is a long-known phenomenon as a mechanism of species adaptation to exist in unstable aquatic habitats,surviving adverse conditions in the"sleeping"state(Radzikowski,2013).Bank of resting stages of planktonic organisms is an important component of the plankton community,without which we cannot understand community dynamics(Brendonck and De Meester,2003).展开更多
A pool of dormant stages of planktonic organisms in saline lakes is a substantial component in the plankton communities;we need to take it into account to understand plankton dynamics.Hypersaline water bodies in Crime...A pool of dormant stages of planktonic organisms in saline lakes is a substantial component in the plankton communities;we need to take it into account to understand plankton dynamics.Hypersaline water bodies in Crimea,the largest peninsula in the Black Sea,constitute a very characteristic and peculiar habitat type in the region.We examined the presence of crustacean resting stages in sediments of dried up sites of the Crimean hypersaline lakes.Sediment samples were taken in 9 different lakes.Experiments performed on the hatching of these resting stages showed the presence of Moina salina(Cladocera),parthenogenetic Artemia and Artemia urmiana(Anostraca),Eucypris mareotica( inflata)(Ostracoda),and Cletocamptus retrogressus(Harpacticoida).Comparing the experimental results obtained with clean dried brine shrimp cysts and those kept in sediment samples,it was noted that clean cysts hatched much faster than those from sediments did.Some components in bottom sediments slow down and desynchronize hatching from resting eggs in different groups of crustaceans.The sediments of different lakes inhibited the nauplii output from Artemia and ostracod resting eggs to different degrees.More data are needed before we can discuss the reasons of this inhibition.The nonsynchronous output of active stages from the bottom resting ones may be an adaptation that allows crustacean species to exist in extreme and unpredictably changing environments,avoiding the risk that all may emerge at once under unsuitable conditions.展开更多
1 Introduction The salt lakes of the Crimea contain the practically inexhaustible sources of salts of sodium,magnesium,bromine and other chemical elements(Ponizovskii,1965),being the potential powerful raw materials b...1 Introduction The salt lakes of the Crimea contain the practically inexhaustible sources of salts of sodium,magnesium,bromine and other chemical elements(Ponizovskii,1965),being the potential powerful raw materials base for the展开更多
1 Introduction It is known that more than 300 lakes and lagoons are present in the Crimean Peninsula,which are divided depending on position to 7 groups:Perekop,Tarkhankut,Evpatoriyskaya,Khersonesskaya,lake on the mou...1 Introduction It is known that more than 300 lakes and lagoons are present in the Crimean Peninsula,which are divided depending on position to 7 groups:Perekop,Tarkhankut,Evpatoriyskaya,Khersonesskaya,lake on the mountainpastures,Kerch and Genicheskaya.Almost the all lakes,with the exception of the small freshwater lakes,which situated on mountain pastures of the Main ridge of展开更多
^99Sr concentrations, resulting from the Chernobyl NPP accident, were determined in the salt lakes of the Crimea （Lakes Kiyatskoe, Kirleutskoe, Kizil-Yar, Bakalskoe and Donuzlav）, together with the redistribution be...^99Sr concentrations, resulting from the Chernobyl NPP accident, were determined in the salt lakes of the Crimea （Lakes Kiyatskoe, Kirleutskoe, Kizil-Yar, Bakalskoe and Donuzlav）, together with the redistribution between the components of the ecosystems. The content of mercury in the waters of the studied reservoirs was also established. Vertical distributions of natural radionuclide activities （^238U, ^232Th, ^226Ra, ^210pb, ^40K） and anthropogenic ^137Cs concentrations （as radiotracers） were determined in the bottom sediments of the Koyashskoe salt lake （located in the south-eastern Crimea） to evaluate the long- term dynamics and biogeochemical processes. Radiochemical and chemical analysis was undertaken and radiotracer and statistical methods were applied to the analytical data. The highest concentrations of ^99Sr in the water of Lake Kiyatskoe （350.5 and 98.0 Bq/m^3） and Lake Kirleutskoe （121.3 Bq/m^3） were due to the discharge of the Dnieper water from the North-Crimean Canal. The high content of mercury in Lake Kiyatskoe （363.2 ng/L） and in seawater near Lake Kizil-Yar （364 ng/L） exceeded the maximum permissible concentration （3.5 times the maximum）. Natural radionuclides provide the main contribution to the total radioactivity （artificial and natural combined） in the bottom sediments of Lake Koyashskoe. The significant concentration of ^210pb in the upper layer of bottom sediments of the lake indicates an active inflow of its parent radionuclide-gaseous ^222Rn from the lower layers of the bottom sediment. The average sedimentation rates in Lake Koyashskoe, determined using ^210pb and ^137Cs data, were 0.117 and 0.109 cm per year, respectively.展开更多
The comparative study of technogenic ^(90)Sr behavior features in Crimea lakes’ ecosystems with different levels of salinity was carried out in 2016-2021.Two sources of ^(90)Sr input were identified for all the studi...The comparative study of technogenic ^(90)Sr behavior features in Crimea lakes’ ecosystems with different levels of salinity was carried out in 2016-2021.Two sources of ^(90)Sr input were identified for all the studied lakes:the primary source concerned with atmospheric fallout immediately after the Chernobyl NPP accident and the secondary long-term input of this radionuclide by waterway.The half-life of the ^(90)Sr concentration in the water of the hypers aline Lake Sasyk-Sivash was estimated to vary from 0.8 to 1.1 years after the closure of the North Crimean Canal(NCC).Biogeochemical processes in the lake under the absence of the secondary source of the radionuclide input were shown to decrease in the ^(90)Sr residence time in the water column by 131 times.For brackish water bodies,a significant factor influencing the radionuclide concentration in ecosystems of lakes was the pH of their water,while for hypers aline lakes the level of water salinity was the main factor determining ^(90)Sr behavior.The concentration of ^(90)Sr in bottom sediments of studied lakes depended mainly on this radionuclide concentration in a water environment.Calculated ^(90)Sr distribution factors(Kd) for studied lakes’ bottom sediments varied in a range of n·10^(0)÷n·10^(2) for hypersaline lakes and of n·10^(1)÷n·10^(2) for lakes with brackish waters.Due to the closure of the NCC,the ^(90)Sr redistribution took place in lake ecosystems only under the geochemical processes within the water bodies themselves.The results obtained in this work are of particular importance as a starting point or a basis for further radioecological studies of the Crimean inland waters after the reopening of the NCC and the Dnieper waters re-entering the territory of Crimea in 2022after the 8 years of their absence.展开更多
Based on numerous geological data obtained by the authors for several decades, the stratification of Permian and Carboniferous ancient and exotic blocks of Crimean Mountains is performed. The sequence of geological ev...Based on numerous geological data obtained by the authors for several decades, the stratification of Permian and Carboniferous ancient and exotic blocks of Crimean Mountains is performed. The sequence of geological events that cause their origin is revealed. Carnian-Norian, Rhaetian-Hettangian and Early-Pliensbachian phases of collapse, sliding and burial of Paleozoic blocks are specified. Final stage (block re-deposition) is confined to the Toarcian and Aalenian ages. The data obtained allow re-interpreting the origin of ancient exotic blocks of the Crimea.展开更多
The Russian Federation unilaterally invaded the Republic of Ukraine＇s Crimean Peninsula, then commenced to occupy more of Eastern Ukraine on the transparent pretext of protecting Russian speakers in 2014, using mask...The Russian Federation unilaterally invaded the Republic of Ukraine＇s Crimean Peninsula, then commenced to occupy more of Eastern Ukraine on the transparent pretext of protecting Russian speakers in 2014, using masked ＂zombie＂ fighters but denied that they were uniformed Russian soldiers, violating several agreements from 1954 to 1994 and legitimate international expectations before and afterwards. Elections were held, seriatim, one alter another, contrived supposedly to reflect the wishes of ethnic Russians in cities along Ukraine＇s eastern border, results of which triggered declarations by separatists of ＂independence＂ followed by formation of ＂people＇s republics＂ as city states. What this signifies is a clash of cultural expectations： of core values, both in the hearts and minds of all parties involved, and in the methods chosen by Russian Federation and Ukrainian independence movement leaders compared with Western governments. If Russia is revoking its transfer of the Crimea to Ukraine on an assertion that such transfer 60 years back was improvident then the Western Alliance should respond by revoking the Potsdam Declaration and other agreements investing Russia with control of Krnigsberg （renamed Kaliningrad） including the Treaty of Paris, and possibly revoking commitments made improvidently at the Teheran and Yalta summit conferences, transferring what was Eastern Poland west of the Curzon Line to the Soviet Union and eventually to Ukraine. If the West will tolerate a Russian siege of Crimea, it should forthwith impose an Allied siege of Kaliningrad and occupy that oblast immediately, retuming Krnigsberg to sovereignty under Lithuanian or Polish and EU control with annexation as a NATO base. What the West with NATO must do is to fight encirclement with encirclement including military, information, economic, trade encirclement as part of what is termed ＂hybrid warfare＂. Stopping military advancement eastward into Europe is only one prong of the problem. Another is Greece, a country that has formed the foundation of the defense of Europe to its own economic detriment. Ukraine as a hot spot is the consequence of China＇s ambition to partner with Ukraine in construction of a post-Panamax deep water cargo port on the Crimean peninsula, prompting Russian Federation opposition （Chinese Billionaire, 2013）. This paper proposes that China transfer its deep water port to Greece fund it through a new East Europe Infrastructure Investment Bank （EEIIB）, achieve the same USD Trillion annual trade influx into the European Union, relieve Greece＇s agony without austerity by inaugurating a Chinese ＂Marshall Plan＂ to become the ＂Chen Yi Plan＂, relieve Greece＇s economic agony without imposing austerity by relocating China＇s planned deep water post-Panamax mega-port from Yevpatoria in Crimean Peninsula to a suitable Greek port, thereby making Greece sustainably rich much as the Marshall Plan did for post-war Germany.展开更多
基金This work has been supported by the Russian Science FoundationProject No.23-26-00128,“The role of the North Crimean Canal irrigation system in the processes of transfer of long-lived radionuclides of the Chernobyl origin,heavy metals,as well as hydrocarbons with the Dnieper water to the irrigated farmlands of Crimea”。
文摘The North Crimean Canal is a watercourse originating from the Kakhovka Reservoir and flowing into the Crimean Peninsula.The canal is an important source of drinking water supply and is also used to irrigate agricultural lands and fillfish farms.Due to its location,in recent years its functioning has not been stable,and the processes occurring along the canal have been poorly studied.In this study,we determined the content(with a safety assessment),features of spatial and seasonal distribution,and potential sources of hydrocarbons in the water of the North Crimean Canal,Crimea.During the study period(from March to November 2023)in the primary canal,the content of aliphatic hydrocarbons did not exceed sanitary standards(0.05 mg·L^(-1)).Their increased concentrations in the secondary canals could be associated with the input of organic substances into the canal water as it moves across the Crimean Peninsula.The composition of n-alkanes had temporal and spatial variability.In the period from spring to autumn,the content of autochthonous compounds decreased sharply.The share of allochthonous compounds increased as a consequence of the natural processes.The analysis of biogeochemical markers showed that autochthonous compounds produced by phytoplankton predominated in the spring–summer period.Subsequently,they had less importance,and the main share was accounted for allochthonous n-alkanes.
文摘1 Introduction A presence of resting stages in various aquatic organisms is a long-known phenomenon as a mechanism of species adaptation to exist in unstable aquatic habitats,surviving adverse conditions in the"sleeping"state(Radzikowski,2013).Bank of resting stages of planktonic organisms is an important component of the plankton community,without which we cannot understand community dynamics(Brendonck and De Meester,2003).
文摘A pool of dormant stages of planktonic organisms in saline lakes is a substantial component in the plankton communities;we need to take it into account to understand plankton dynamics.Hypersaline water bodies in Crimea,the largest peninsula in the Black Sea,constitute a very characteristic and peculiar habitat type in the region.We examined the presence of crustacean resting stages in sediments of dried up sites of the Crimean hypersaline lakes.Sediment samples were taken in 9 different lakes.Experiments performed on the hatching of these resting stages showed the presence of Moina salina(Cladocera),parthenogenetic Artemia and Artemia urmiana(Anostraca),Eucypris mareotica( inflata)(Ostracoda),and Cletocamptus retrogressus(Harpacticoida).Comparing the experimental results obtained with clean dried brine shrimp cysts and those kept in sediment samples,it was noted that clean cysts hatched much faster than those from sediments did.Some components in bottom sediments slow down and desynchronize hatching from resting eggs in different groups of crustaceans.The sediments of different lakes inhibited the nauplii output from Artemia and ostracod resting eggs to different degrees.More data are needed before we can discuss the reasons of this inhibition.The nonsynchronous output of active stages from the bottom resting ones may be an adaptation that allows crustacean species to exist in extreme and unpredictably changing environments,avoiding the risk that all may emerge at once under unsuitable conditions.
文摘1 Introduction The salt lakes of the Crimea contain the practically inexhaustible sources of salts of sodium,magnesium,bromine and other chemical elements(Ponizovskii,1965),being the potential powerful raw materials base for the
文摘1 Introduction It is known that more than 300 lakes and lagoons are present in the Crimean Peninsula,which are divided depending on position to 7 groups:Perekop,Tarkhankut,Evpatoriyskaya,Khersonesskaya,lake on the mountainpastures,Kerch and Genicheskaya.Almost the all lakes,with the exception of the small freshwater lakes,which situated on mountain pastures of the Main ridge of
文摘^99Sr concentrations, resulting from the Chernobyl NPP accident, were determined in the salt lakes of the Crimea （Lakes Kiyatskoe, Kirleutskoe, Kizil-Yar, Bakalskoe and Donuzlav）, together with the redistribution between the components of the ecosystems. The content of mercury in the waters of the studied reservoirs was also established. Vertical distributions of natural radionuclide activities （^238U, ^232Th, ^226Ra, ^210pb, ^40K） and anthropogenic ^137Cs concentrations （as radiotracers） were determined in the bottom sediments of the Koyashskoe salt lake （located in the south-eastern Crimea） to evaluate the long- term dynamics and biogeochemical processes. Radiochemical and chemical analysis was undertaken and radiotracer and statistical methods were applied to the analytical data. The highest concentrations of ^99Sr in the water of Lake Kiyatskoe （350.5 and 98.0 Bq/m^3） and Lake Kirleutskoe （121.3 Bq/m^3） were due to the discharge of the Dnieper water from the North-Crimean Canal. The high content of mercury in Lake Kiyatskoe （363.2 ng/L） and in seawater near Lake Kizil-Yar （364 ng/L） exceeded the maximum permissible concentration （3.5 times the maximum）. Natural radionuclides provide the main contribution to the total radioactivity （artificial and natural combined） in the bottom sediments of Lake Koyashskoe. The significant concentration of ^210pb in the upper layer of bottom sediments of the lake indicates an active inflow of its parent radionuclide-gaseous ^222Rn from the lower layers of the bottom sediment. The average sedimentation rates in Lake Koyashskoe, determined using ^210pb and ^137Cs data, were 0.117 and 0.109 cm per year, respectively.
基金Scientific research on salt and brackish water lakes was supported by the Russian Science Foundation,with grant No.18-16-00001Development of biological and geochemical foundations for the development of aquaculture in hypersaline lakes and lagoons of Crimea,2021-2022Comparative studies on the Black Sea were carried out within the framework of the State Assignment for the IBSS,Molismological and biogeochemical foundations of the homeostasis of marine ecosystems,with State registration number of the state assignment 121031500515-8。
文摘The comparative study of technogenic ^(90)Sr behavior features in Crimea lakes’ ecosystems with different levels of salinity was carried out in 2016-2021.Two sources of ^(90)Sr input were identified for all the studied lakes:the primary source concerned with atmospheric fallout immediately after the Chernobyl NPP accident and the secondary long-term input of this radionuclide by waterway.The half-life of the ^(90)Sr concentration in the water of the hypers aline Lake Sasyk-Sivash was estimated to vary from 0.8 to 1.1 years after the closure of the North Crimean Canal(NCC).Biogeochemical processes in the lake under the absence of the secondary source of the radionuclide input were shown to decrease in the ^(90)Sr residence time in the water column by 131 times.For brackish water bodies,a significant factor influencing the radionuclide concentration in ecosystems of lakes was the pH of their water,while for hypers aline lakes the level of water salinity was the main factor determining ^(90)Sr behavior.The concentration of ^(90)Sr in bottom sediments of studied lakes depended mainly on this radionuclide concentration in a water environment.Calculated ^(90)Sr distribution factors(Kd) for studied lakes’ bottom sediments varied in a range of n·10^(0)÷n·10^(2) for hypersaline lakes and of n·10^(1)÷n·10^(2) for lakes with brackish waters.Due to the closure of the NCC,the ^(90)Sr redistribution took place in lake ecosystems only under the geochemical processes within the water bodies themselves.The results obtained in this work are of particular importance as a starting point or a basis for further radioecological studies of the Crimean inland waters after the reopening of the NCC and the Dnieper waters re-entering the territory of Crimea in 2022after the 8 years of their absence.
文摘Based on numerous geological data obtained by the authors for several decades, the stratification of Permian and Carboniferous ancient and exotic blocks of Crimean Mountains is performed. The sequence of geological events that cause their origin is revealed. Carnian-Norian, Rhaetian-Hettangian and Early-Pliensbachian phases of collapse, sliding and burial of Paleozoic blocks are specified. Final stage (block re-deposition) is confined to the Toarcian and Aalenian ages. The data obtained allow re-interpreting the origin of ancient exotic blocks of the Crimea.
文摘The Russian Federation unilaterally invaded the Republic of Ukraine＇s Crimean Peninsula, then commenced to occupy more of Eastern Ukraine on the transparent pretext of protecting Russian speakers in 2014, using masked ＂zombie＂ fighters but denied that they were uniformed Russian soldiers, violating several agreements from 1954 to 1994 and legitimate international expectations before and afterwards. Elections were held, seriatim, one alter another, contrived supposedly to reflect the wishes of ethnic Russians in cities along Ukraine＇s eastern border, results of which triggered declarations by separatists of ＂independence＂ followed by formation of ＂people＇s republics＂ as city states. What this signifies is a clash of cultural expectations： of core values, both in the hearts and minds of all parties involved, and in the methods chosen by Russian Federation and Ukrainian independence movement leaders compared with Western governments. If Russia is revoking its transfer of the Crimea to Ukraine on an assertion that such transfer 60 years back was improvident then the Western Alliance should respond by revoking the Potsdam Declaration and other agreements investing Russia with control of Krnigsberg （renamed Kaliningrad） including the Treaty of Paris, and possibly revoking commitments made improvidently at the Teheran and Yalta summit conferences, transferring what was Eastern Poland west of the Curzon Line to the Soviet Union and eventually to Ukraine. If the West will tolerate a Russian siege of Crimea, it should forthwith impose an Allied siege of Kaliningrad and occupy that oblast immediately, retuming Krnigsberg to sovereignty under Lithuanian or Polish and EU control with annexation as a NATO base. What the West with NATO must do is to fight encirclement with encirclement including military, information, economic, trade encirclement as part of what is termed ＂hybrid warfare＂. Stopping military advancement eastward into Europe is only one prong of the problem. Another is Greece, a country that has formed the foundation of the defense of Europe to its own economic detriment. Ukraine as a hot spot is the consequence of China＇s ambition to partner with Ukraine in construction of a post-Panamax deep water cargo port on the Crimean peninsula, prompting Russian Federation opposition （Chinese Billionaire, 2013）. This paper proposes that China transfer its deep water port to Greece fund it through a new East Europe Infrastructure Investment Bank （EEIIB）, achieve the same USD Trillion annual trade influx into the European Union, relieve Greece＇s agony without austerity by inaugurating a Chinese ＂Marshall Plan＂ to become the ＂Chen Yi Plan＂, relieve Greece＇s economic agony without imposing austerity by relocating China＇s planned deep water post-Panamax mega-port from Yevpatoria in Crimean Peninsula to a suitable Greek port, thereby making Greece sustainably rich much as the Marshall Plan did for post-war Germany.
