The inhabitants of the spring ice,under-ice water,and sediments of the white sea in the estuarine zone of the Severnaya Dvina River     

A. F. Sazhin  F. V. Sapozhnikov  T. N. Rat’kova  N. D. Romanova  V. P. Shevchenko  A. S. Filippov 《Oceanology》2011,51(2):295-305

The data on the supra-ice snow, ice, under-ice water, and benthic algal flora obtained in 2007–2008 by sampling in the estuary of the Severnaya Dvina River are analyzed. The river ice and under-ice water in the estuarine zone and in the channel part of the Severnaya Dvina differed greatly in the algal flora’s composition. The fresh water species never exceeded 8.6%, while the ice algae composed 90–96% of the total ice inhabitants’ biomass. In the under-ice water, this value did not exceed 58–64%. The bacteria in the ice composed not more than 2.5–10% of the total biomass, while, in the under-ice water, 36–49%. The shares of ciliates (0.04%) and nematodes (0.005–1.6%) in the total biomass were negligible. In the estuarine zone, the ice was inhabited mainly by nematodes (78% of the total biomass), while, in the river, their share decreased to 9%. The contribution of bacteria was 15% in Dvina Bay and increased to 61% in the river. The importance of algae in the snow was minor: 7% of the total biomass in the marine zone and 30% in the river region. High species diversity of the algal flora in the sandy and sandy-silty littoral grounds was revealed. The values of the total biomass of the bottom algal flora (0.38 g C/m²) were only two to three times lower than the values revealed in similar habitats in the summer. The epipelithic forms (0.15 g C/m²) dominated, being represented by 46 species of algae (49%). The shares of epipsammonic (0.12 g C/m²) and planktonic (0.11 g C/m²) species were almost equal to each other: 25 and 22 species, respectively (27 and 24%).  相似文献   

Studies of the White Sea System from onboard the R/V Ekolog in July 2010     

V. P. Shevchenko  R. A. Ananyev  A. I. Gusakova  N. N. Dmitrevskii  M. D. Kravchishina  A. V. Mishin  N. V. Politova  M. S. Potakhin  A. V. Tolstikov  A. S. Filippov  A. L. Chul’tsova 《Oceanology》2011,51(6):1074-1077

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Estimation of Extreme Sea Level in the Akkuyu Nuclear Power Plant Area     

Kabatchenko  I. M.  Kulikov  E. A.  Litvinenko  G. I.  Filippov  Yu. G. 《Russian Meteorology and Hydrology》2020,45(1):39-44

Russian Meteorology and Hydrology - Possible extreme fluctuations of sea level in the area of the Akkuyu nuclear power plant induced by tsunami, wind, waves, and tides are discussed. The...  相似文献   

Specific features of the distribution of trace and rare earth elements in recent bottom sediments in the lower course of the Severnaya Dvina River and White Sea     

A. V. Maslov  V. P. Shevchenko  V. N. Podkovyrov  Yu. L. Ronkin  O. P. Lepikhina  A. N. Novigatsky  A. S. Filippov  N. V. Shevchenko 《Lithology and Mineral Resources》2014,49(6):433-460

The paper discusses results of the lithogeochemical examination of recent bottom sediments in the lower course of the Severnaya Dvina River and White Sea. It has been established that the average concentration of several trace elements (Hf, Sc, Co, Y, Ni, V, Cr, Zr, Ba, and others) therein correlates with the content of the silt-pelite fraction. Maximal concentrations of the majority of above elements are confined to the silty-clayey sediments at the Basin/Dvina Bay boundary. They localized near the coastal zone only for some clastophile (Zr, Cr, and others). Typical values of the hydrolyzate module, chemical index of alteration, and Al₂O₃/SiO₂ ratio in the aleuropelitic and pelitic sediments of the Severnaya Dvina River delta, Dvina Bay, and the Dvina Bay Basin boundary suggest that these sediments are confined to sufficiently cold climate settings. Data points of sediment composition in discriminant paleotectonic diagrams are scattered over a large field probably due to high contents of the weakly weathered plagioclases, micas, and amphiboles, as well as the hydrogenic process promoting the accumulation of Fe and Mn. The PAAS-normalized spectra of rare earth elements (REE) in bottom sediments of the Pinega and Severnaya Dvina rivers, marginal filter of the latter river, Dvina Bay, and the Dvina Bay Basin boundary are similar to the REE distribution in clayey rocks of the ancient platform cover (except for a slight positive Eu anomaly). The REE systematics and distribution pattern of compositional data points of recent bottom sediments in the Gd_N/Yb_N-Eu/Eu* and Eu/Eu*-Cr/Th diagrams and values of several indicator ratios of trace elements suggest that the studied rocks were formed by the mixing of clastic materials from geochemically contrast provenances: northwestern provenance (Kola-Karelia geoblock), which is mostly composed of the Archean and Early Proterozoic crystalline complexes, and the southeastern provenance (northwestern periphery of the Mezen syncline), which is almost totally composed of Phanerozoic sedimentary rocks. The latter provenance likely played a crucial role in the geochemical signature of recent bottom sediments over a significant area of the White Sea.  相似文献   

Minor elements in quartz from hydrothermal-metamorphic veins in the Nether Polar Ural Province     

S. K. Kuznetsov  E. N. Svetova  S. N. Shanina  V. N. Filippov 《Geochemistry International》2012,50(11):911-925

Vein quartz from the Nether Polar Ural Province was examined by atomic emission spectrometry, gas chromatography, electron paramagnetic resonance, and electron microscopy. According to atomic emission spectrometric analysis, the total concentration of Al, Fe, Mg, Ti, Ca, Na, K, and other minor elements in the quartz varies from 8 to 47 ppm. The lowest concentrations of minor elements were detected in the granulated quartz. Giant-crystalline milk-white quartz is noted for higher concentrations of minor elements, including Na, K, and Ca, because it contains gas-liquid inclusions. The fine-grained quartz contains very small mineral inclusions and is thus noted for elevated concentrations of Ca, Fe, K, Mg, and Ti. Gas chromatographic data on the gas phase separated from the quartz at its heating indicate that this phase contains H₂O, CO₂, and other components. The H₂O concentration reaches 429 ??g/g, while the CO₂ content is commonly no higher than 20 ??g/g. Gas separation is at a maximum at temperatures of 100?C600°C, when gasliquid inclusions decrepitate, as is typical, first of all, of the giant-crystalline milk-white quartz. Gas separation continues at higher temperatures (below 1000°C) but is much less intense. The electron microscopic examination of quartz grains after their acid treatment indicates that the surface of these grains is covered by caverns of various morphology and size, which were produced by the partial dissolution of the quartz and the opening of its gas-liquid and mineral inclusions occurring near the surface; the inclusions were not, however, completely removed. The crystal structure of the quartz contains minor Al, Ge, Na, Li, Ti, and Fe. The lowest concentrations of Al and Ge paramagnetic centers are typical of the granulated (recrystallized) and fine-grained quartz. The giant-crystalline quartz, including its transparent varieties, and individual quartz crystals, first of all their smoky-citrine varieties, contain higher concentrations of minor elements. In the Nether Polar Ural Province, granulated quartz is potentially promising for producing especially pure quartz concentrates. The quality of the translucent coarse-to giant-crystalline quartz, which predominates in the resources and reserves, is deteriorated by gas-liquid inclusions in it and requires deep processing of the raw minerals.  相似文献   

Composition and provenances of mesozoic sandstones in Sikhote Alin     

A. N. Filippov 《Lithology and Mineral Resources》2012,47(1):70-88

The composition of sandstones constituting different structural stages of the Jurassic accretionary wedge in the Samarka (upper and middle? structural levels in the Lyamfana Creek and Katen River basins, respectively) and Nadan’khada-Bikin (lower level in the Ulitka River basin) terranes of the Sikhote Alin region reflects changes in provenances and tectonic settings of the near-continental sedimentation basin in different periods of the wedge formation. In the terminal Middle Jurassic (Lyamfana Creek), the region was dominated by the subduction regime with sedimentary material transported from the eroded part of the continental-margin magmatic arc. During the Kimmeridgian-Tithonian (Katen River), erosion of granitoid batholiths of the arc exposed blocks of the crystalline basement along strike-slip faults. In the Tithonian-Berriasian period (Ulitka River), the role of these blocks increased, suggesting intensification of oblique subduction or development of transform faults during the accretion.  相似文献   

Oxygen isotope composition of water and snow-ice cover of isolated lakes at various stages of separation from the White Sea     

A. P. Lisitzin  Yu. K. Vasil’chuk  V. P. Shevchenko  N. A. Budantseva  E. D. Krasnova  A. N. Pantyulin  A. S. Filippov  Ju. N. Chizhova 《Doklady Earth Sciences》2013,449(2):406-412

This study aimed to analyze the oxygen isotope composition of water, ice, and snow in water bodies isolated from the White Sea and to identify the structural peculiarities of these pools during the winter period. The studies were performed during early spring in Kandalaksha Bay of the White Sea, in Velikaya Salma Strait and in Rugoserskaya Inlet. The studied water bodies differ in their degree of isolation from the sea. In particular, Ermolinskaya Inlet has normal water exchange with the sea; the Lake on Zelenyi Cape represents the first stage of isolation; i. e., it has permanent water exchange with the sea by the tide. Kislo-Sladkoe Lake receives sea water from time to time. Trekhtsvetnoe Lake is totally isolated from the sea and is a typical meromictic lake. Finally, Nizhnee Ershovskoe Lake exhibits some features of a saline water body. The oxygen isotope profile of the water column in Trekhtsvetnoe Lake allows defining three layers; this lake may be called typically meromictic. The oxygen isotope profile of the water column in Kislo-Sladkoe Lake is even from the surface to the bottom. The variability of δ¹⁸O is minor in Lake on Zelenyi Cape. A surface layer (0–1 m) exists in Nizhnee Ershovskoe Lake, and the oxygen isotope variability is well pronounced. Deeper, where the freshwater dominates, the values of ?18Îvary insignificantly disregarding the water depth and temperature. This fresh water lake is not affected by the seawater and is not stratified according to the isotope profile. It is found that applying the values of ?18Î and profiles of temperature and salinity may appear as an effective method in defining the water sources feeding the water bodies isolated from the sea environment.  相似文献   

Complex studies of the White Sea during the expedition onboard the R/V Ekolog in July 2012     

A. A. Klyuvitkin  M. D. Kravchishina  A. S. Filippov  A. V. Tolstikov  L. E. Reykhard  A. D. Mutovkin  A. L. Chul’tsova 《Oceanology》2013,53(6):765-767

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Jet phenomena above null points of the coronal magnetic field     

B. Filippov  S. Koutchmy  L. Golub 《Geomagnetism and Aeronomy》2009,49(8):1109-1112

Short-lived plasma jets of various scales, from giant X-ray jets more than 300 Mm in extent to numerous small jets with sizes typical of macrospicules, are the phenomena observed in the solar corona in extreme ultraviolet and X-ray emission. Small jets are particularly prominent in polar coronal holes. They are close neighbors of tiny bright loops and coincide in time with their sudden brightening and increase in size. The geometric shape of the jets and their location suggest that they arise near singular null points of the coronal magnetic field. These points appear in coronal holes due to the emergence of small bipolar or unipolar magnetic structures within large-scale unipolar cells. Polar jets show a distinct vertical plasma motion in a coronal hole that introduces significant momentum and mass into the solar wind flow. Investigating the dynamics of polar jets can elucidate certain details in the problem of fast solar wind acceleration.  相似文献   

Longitudinal statistics of plasma bubbles: Possible tropospheric influence     

L. N. Sidorova  S. V. Filippov 《Geomagnetism and Aeronomy》2016,56(4):482-492

The assumption about the possible influence of a tropospheric source on the nature of the longitudinal statistics variation (relative frequency of observation) of plasma bubbles determined by the He⁺ density in the upper ionosphere altitudes is tested. To do this, the statistics are comparatively analyzed with a number of characteristics of the ionosphere and thermosphere, the longitudinal changes of which can be related to the DE3 tidal wave generated in the troposphere. Evidence of the possible influence of the troposphere on the longitudinal statistics of plasma bubbles has been obtained. Based on qualitative analysis, it was found that the thermospheric winds modulated by the DE3 tidal wave can link these statistics with processes in the troposphere.  相似文献