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Том 54, № 7 (2018)

Article

On Traces of Strong Late Medieval Earthquakes at the Uzbek Madrasah–Mosque Complex, Staryi Krym, Crimea

Korzhenkov A., Lomakin D., Ovsyuchenko A., Lar’kov A., Marakhanov A., Rogozhin E.

Аннотация

The results of archeoseismological investigations of medieval architectural monuments—the Uzbek Mosque and Indzhi-Bey-Khatun Madrasah (Uzbek Madrasah–Mosque Complex)—in the town of Staryi Krym (eastern Crimean Peninsula) are presented. The character of revealed destructions and collapses unambiguously indicates their seismic origin. Local seismic intensity was apparently VIII ≤ I ≤ IX on the MSK-64 scale. Using this data, we reveal traces of at least two significant seismic events. According to the results of our archeological study, the first occurred at the beginning of the 15th century: this was likely the Yalta earthquake of 1423, with the maximum integrated seismic effect then being directed along the submeridional axis. The second strong earthquake occurred later. The preserved illustrations and photographs suggest destructions took place in the late 18th–19th century, between 1797 and 1888–1889(?). The maximum integrated seismic effect of this later earthquake was directed along the WNW–ESE axis. The Yalta earthquakes of 1927 did not significantly damage either the mosque or the madrasah.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):627-645
pages 627-645 views

Aquifer Dynamics and Atmospheric Electricity

Shuleikin V.

Аннотация

Measurements of variations in the atmospheric electric field (AEF), soil and atmospheric radon concentration, and hydrogeological parameters have made it possible to establish links between the listed processes. A rise in aquifer levels increases the outflow of soil radon, which decreases the AEF; a decrease in levels leads to the opposite effect. The rise can be caused by the infiltration of precipitation, hydraulic fracturing, and lowering of atmospheric pressure; the fall can be caused by the pumping of artesian waters or by an increase in atmospheric pressure.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):646-653
pages 646-653 views

Results of Measurements of Radon Volume Activity in Azerbaijan

Aliyev C., Feyzullayev A., Baghirli R., Mahmudova F.

Аннотация

The procedures and results of measuring radon volume activity (concentration) in Azerbaijan (in residential and industrial premises, soil air, thermal waters, and mud volcanoes) are described. It was established that indoor radon concentrations vary in a wide range: from 20 to 1110 Bq/m3; about 7% of the total amount of measurements exceed the maximum permissible limits in Azerbaijan (200 Bq/m3). Based on these data, maps of the distribution of indoor radon volume activity in Azerbaijan are constructed for the first time. The enhanced radon concentrations are confined to fold-mountain massifs of Greater and Lesser Caucasus and Talysh. Results of measurements of radon concentrations in indoor air are very consistent with the data of radon content in soil air. The content of radon in thermal waters is not high generally, except for the waters of one carbon source in the Talysh region, where its concentration is above the maximum permissible level accepted for drinking water. Enhanced values of radon volume activity in mud volcanoes (especially in gases released from the gryphons) have also been revealed. Based on the complex processing of the data, a conclusion is drawn about the natural origin of enhanced values of radon volume activity in this part of the examined residential premises in Azerbaijan.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):654-660
pages 654-660 views

Prevention of Shield-Induced Desynchronosis in Invertebrates by a Variable Magnetic Field of Extremely Low Frequency

Temuryants N., Tumanyants K., Kostyuk A., Yarmolyuk N., Tumanyants E.

Аннотация

We have found that planarians Dugesia tigrina and snails Helix albescens develop desynchronosis under conditions of moderate ferromagnetic shielding at which both variable and constant components of the geomagnetic field are inhibited. Desynchronosis is diagnosed by changes in the infradian rhythms of the movements of the planarians and the nociception parameters of the snails. We observe the following changes: a decrease in the number of periods or their changes and phase shifts, which are especially pronounced in the shortest periods. In the case of an additional effect on animals of an alternating magnetic field of 8 Hz frequency by the induction of 50 nT under shielding conditions, we observe no change in the rhythmic processes of the infradian range in invertebrates. Thus, we conclude that a variable magnetic field of 8 Hz prevents the development of shield-induced desynchronosis.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):661-666
pages 661-666 views

Processes of Formation of Beryllium Hydroxide Aerosols and Assessment of Ecological Risks Arising during Their Emissions to the Environment

Obvintsev Y., Gubanova D., Minashkin V.

Аннотация

The processes leading to the formation of toxic beryllium-containing aerosol particles at the stages of beryllium hydroxide production using a new innovative technology of ore processing at the Ermakovskoe deposit are considered. In order to create a conceptual structure of experimental samples of the units for control emissions and discharges of pollutants in the production of beryllium hydroxide, the processes of aerosol formation at various technological stages of beryllium production have been studied. A diffusion model is proposed for droplet evaporation during the leaching and hydrolysis of beryllium concentrates, which makes it possible to determine the rate of evaporation, temperature, size, and lifetime of a droplet depending on the environmental conditions. The results of model calculations (for the diffusion model) of the dispersed composition of beryllium-containing aerosol particles are presented. The most hazardous stages of emissions and discharges of beryllium-containing aerosols in the production of beryllium hydroxide according to a new technology have been identified; the ecological risks arising during emissions of aerosol particles into the atmosphere are assessed.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):667-677
pages 667-677 views

Geophysical Processes, Solar Energy, and Biosphere as System Factors of the Evolution of the Earth

Savchenko I., Belozerov N., Girenko I.

Аннотация

The concept of the role of the biosphere in the evolution of the Earth is proposed and confirmed by calculations. According to this concept, in the prebiosphere period, a shell structure was formed, the global convection occurred in the form of tectonics of small plates, and the absence of continents excluded the involvement of water in the oxidation of igneous rocks. In the biosphere period, photosynthetic organisms began to supply free oxygen and organic matter (OM) to the environment. Oxygen began to take part in the geochemical processes of ore conversion, the formation of the nitrogen–oxygen composition of the atmosphere, and the generation of granitoids from volcanic rock. Global systems for the generation of granitoids of the continental crust and hydrocarbons (HCs), which are formed during subduction–collision absorption of the oceanic crust, have been identified for the first time. On the transit route to the Benioff zone, granites are melted out from oxygen-enriched halmyrolysis products and the thermal metamorphism of OM yields solid allotropic carbon compounds, oil, and combustible and other gases and is accompanied by the release of OM decomposition energy. This is one of the ways to convert biosphere solar energy into the endodynamic processes of the evolution of the Earth. The average annual precipitation of the primary OM in the ocean is 785.5 Mt, and 1.7 km3 of the continental crust are generated. Over the biosphere period, the World Ocean became shallower by 904.5 million km2. Geodynamic and geophysical processes, primarily global convection, in conjunction with biosphere factors, have resulted in the current state of the Earth’s shells and the existence of HCs and continental-crust generation systems in them.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):678-687
pages 678-687 views

Transport of Air Masses and Pollutants to the Russian Arctic Islands (19862016): Long-Term, Interannual, and Seasonal Variations

Vinogradova A., Ivanova Y.

Аннотация

The Arctic is the most important, as well as the most vulnerable, region in the Northern Hemisphere with respect to climate changes. It is natural that climate changes observed on the globe in recent decades affect the environment in northern regions and processes determining climate. An analysis of time variations in these processes is important in understanding observed phenomena and in estimating their possible consequences. In this work, 30-year data series on the frequency of air-mass transport from Europe, Asia, and North America to the Arctic archipelagos of Franz Josef Land and Severnaya Zemlya and Wrangel Island have been analyzed, and statistical regularities observed in atmospheric-circulation processes in different seasons have been studied using atmospheric-circulation indices. The atmospheric concentrations of anthropogenic heavy metals (HMs) and their fluxes onto the surface of the Russian Arctic islands have been analyzed. The frequency of air-mass transport to the Russian Arctic from the continents has decreased over the last 30 years. Therefore, the composition of the atmosphere and precipitation over the Arctic becomes more and more maritime, which may affect variations in the properties of surface natural objects such as soil, water, vegetation, etc. Interannual variations in atmospheric-circulation processes are wide, which results in wide interannual variations in the atmospheric concentrations of anthropogenic HMs and their fluxes onto the surface. This also explains interannual variations in the content of HMs accumulated in the snow cover every year during the snowy season. Within some months and years, the maximum concentrations of nickel and copper in the air and snow cover of the Arctic islands may reach their concentration levels observed in less remote regions on the mainland. On the other hand, there are years, when no anthropogenic pollutants are transported to the Russian Arctic islands during the summer months. The main reason for seasonal variations in the concentrations of anthropogenic pollutants in the Arctic regions is in seasonal variations in the rate of precipitation of HMs onto the surface during their long-range transport.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):688-699
pages 688-699 views

Distribution of Manmade Low-Frequency Magnetic Noise in a Big Industrial City

Tyagunov D.

Аннотация

This paper deals with measurements of technogenic magnetic noise in the frequency range of 0.01–200 Hz carried out in the daytime within the central part of Yekaterinburg, the city’s bypass road, and the Yekaterinburg ring road. The equipment, measurement technique, and methods of data processing are described. On the basis of the results, the magnetic induction module was determined and a schematic map of the distribution of anthropogenic magnetic noise over the area of Yekaterinburg and in its surroundings was constructed. It is shown that magnetic noise is concentrated in the central regions of the city, and its amplitude can reach ~1500 nT. Within the regions near the ring road, magnetic noise decreases to 150 nT. Examples of records of anthropogenic magnetic noise created by power lines and electric trains of the underground are also given. They show that the amplitude of magnetic noise produced by these sources is much higher than the average intensity of magnetic noise in the central part of the city. We reveal that the amplitude of the vertical component of the magnetic noise, as a rule, is larger in comparison with the horizontal components.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):700-704
pages 700-704 views

Variations in the K-Index of Geomagnetic Activity in the Moscow Region

Riabova S., Spivak A.

Аннотация

We present the results of a statistical analysis of geomagnetic activity measured at the Mikhnevo Geophysical Observatory of the Institute of Geosphere Dynamics of the Russian Academy of Sciences (54.960° N; 37.774° E) located in Moscow region (central part of the Eastern European Platform) and its relation to the solar activity. We use the station geomagnetic K-index as a characteristic of the geomagnetic activity. We apply the results of instrumental observations of the geomagnetic field carried out at the Mikhnevo Geophysical Observatory from 2009 to 2015 to calculate the K-index using the method of adaptive smoothing. The geophysical situation of the Moscow region is characterized by a significant number of days with a disturbed state of the geomagnetic field (in the period analyzed here, magnetic storms were recorded in 181 cases and a disturbed geomagnetic situation was identified in 333 cases). At the same time, there is a tendency for an increase in geomagnetic activity with time: from 2009 to 2015, the number of days with disturbed geomagnetic conditions increased almost eight times. The recurrence of geomagnetic disturbances is characterized by clearly pronounced periodicity with characteristic periods of about 2 weeks, 27 and 60 days, half a year, and 1 year. The total duration of geomagnetic disturbances, which is characterized by K ≥ 4, varies significantly with time. The evaluation of the correlation between the total monthly number of geomagnetic disturbances characterized by a value of K ≥ 3 and the parameter determining the intensity of solar radio emissions (flux density) at a frequency of 2800 MHz (with a wavelength of 10.7 cm) (F 10.7) provide evidence about the significant correlation between the number of geomagnetic disturbances and solar activity.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):705-710
pages 705-710 views

Application of a New Method of Spectral Analysis for Detecting Synchronous Processes in Heliobiology

Ozheredov V., Breus T.

Аннотация

Until now, the sum of periodic variations was the main carrier of information in biological and heliogeophysical signals. However, not all of the time series of interest contain dominant periodic components. The relaxation analysis used in this paper makes it possible to generalize the “spectral” formalism to signals that cannot be represented as a sum of a limited number of quasiperiodic components. An algorithm for filtering noise and long-period trends is developed based on the separation of the original signal into rapidly and slowly relaxing components. The main theorem that guarantees the operability of the algorithm is proven. A method for constructing an orthonormal basis whose components have a strictly defined relaxation time is described. The result of the signal expansion over this basis is called the relaxation spectrum. It can be used to divide the time series into signal-to-noise or oscillation-trend if there are no adequate Fourier or stochastic models. The hypothesis that geomagnetic rhythms with periods of about 7 and 9 days have the most significant influence on physiological indicators of biological objects (including those of the population as a whole), as was stated earlier by the heliobiologists, is confirmed based on an automatic algorithm for extracting reliable spectral peaks of population and heliogeomagnetic time series and detecting similar peaks using the Sørensen measure.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):711-722
pages 711-722 views

Factors of Solar Activity Enhance Locomotor and Exploratory Behavior in Rats

Mukhin V., Pavlov K., Abdurasulova I., Klimenko V.

Аннотация

According to the literature, solar activity affects the functioning of the human brain. However, its effect has not been studied on experimental animals. The purpose of this study was to investigate whether factors of solar activity influence the behavior of rats. From October 26 to December 24, 2011, the behavior of individual rats or small groups of them (N = 19) was recorded in an open field test and operant food-uptake behavior test. Parameters of solar activity were obtained from public databases on the Internet. Results of the correlation analysis have demonstrated that the number of sectors travelled by the rats in the open field test, number of holes they investigated, and number of food pellets they earned while learning a food-uptake task were positively associated with solar activity on the day of the study and in the days before and after that. Such associations were revealed for the number of sunspots, the intensity of solar radiation in the radio range, and number of solar flares in the X-ray and Hα ranges. Factor analysis made it possible to distinguish two factors positively associated with the behavior of rats. One of them closely correlated with the solar radio flux and can therefore be presumably attributed to its electromagnetic component. The other is closely related to the 3-h planetary index of oscillations of the Earth’s magnetic field K, and this indicates its corpuscular nature. These results correspond to the literature data on the association between the parameters of solar and geomagnetic activity and the characteristics of electrical activity of the brain of humans and animals. The behavior of rats is associated most closely with the number of sunspots on the day of the study, the parameter of which significantly correlates with both factors of solar activity. Therefore, this index can be used to consider the influence of solar activity on the behavior of rats in experimental practice.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):723-729
pages 723-729 views

Historical Database of Geomagnetic and Auroral Activity for the Study of Solar–Terrestrial Relationships

Ptitsyna N., Sokolov S., Soldatov V., Tyasto M.

Аннотация

In situ data on geomagnetic and auroral activity obtained in recent years has contributed to a greater understanding of solar–terrestrial processes. However, because space exploration began only in the middle of the 20th century, in situ data are insufficient to analyze geomagnetic variations and solar-activity variations on a time scale from decades to centuries. The Russian network of magnetic and meteorological observatories provides one of the longest data series. For example, the magnetograms from St. Petersburg (SPE), Pavlovsk (SLU), and Voeikovo (LNN) stations provide long series of continuous records of variations of declination (D) and horizontal (H) and vertical (Z) components of the geomagnetic field. The aim of this paper is to make this data publicly available. For this purpose, a specialized database has been developed for the study of various aspects of solar–terrestrial relationships, including heliobiomagnetology. The database contains (1) digital images of analog magnetograms from SPE (1869–1877) and SLU (1878–1921, images for 1921–1941 are still being scanned), (2) hourly values of declination D and horizontal H and vertical Z components of the geomagnetic field obtained at SPE and SLU stations for 1869–1914, (3) data on geomagnetic storms from the SLU station for 1878–1941 and from the LNN station for 1947–1954, and (4) data on aurora borealis observed at 141 stations of the Russian Meteorological Network for 1837–1909. The database is designed to provide online access to the Russian collection of historical data on geomagnetic and auroral activity. On this basis, it is possible to carry out research on various aspects of space weather and climate and use it, among other things, to solve problems of heliomagnetobiology. Users are provided with easy access to individual magnetograms at different zoom levels. Online access will allow a wide range of researchers to use these databases to solve problems related to historical space weather data.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):730-737
pages 730-737 views

Acoustic and Electric Precursors of Strong Thunderstorm Events under Megalopolis Conditions

Spivak A., Rybnov Y., Soloviev S., Kharlamov V.

Аннотация

Analysis of the results of instrumental observations of the electric field and micro-variations in the atmospheric pressure in the surface atmosphere during strong thunderstorms in Moscow in the period 2014−2016 is carried out. It is shown that the arrival of a thunderstorm front has been preceded by long-period (~10 min) variations in the electric field strength, internal gravity waves, and increased magnitudes of impedance acoustic correlation. After the arrival of a cold atmospheric front, as well as in the periods of thunderstorm events, high-frequency (~1 min) variations in the electric field and increased turbidity of the atmosphere are observed. Wind motions in the atmosphere are almost absent in the atmosphere, but internal gravity waves are observed at the final stage of the phenomena. The period of variations in the electric field increases up to ~15 min.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):738-744
pages 738-744 views

Ring-Shaped Seismicity Structures in the Cascadia Subduction Zone: Possible Upcoming Large Earthquakes

Kopnichev Y., Sokolova I.

Аннотация

Seismicity characteristics in the Cascadia subduction zone located west of North America are considered. It has been established that, since 1964, shallow (h = 0–33 km) ring-shaped seismicity structures with threshold magnitudes Mt of 4.4 and 4.6, respectively, have been formed prior to two large earthquakes (on August 17, 1991, Mw = 7.1 and April 25, 1992, Mw = 7.2). Note that, unlike many other subduction zones, deep ring-shaped structures (h = 34–70 km) have not been observed here. At the same time, deep seismicity strips are sometimes formed in this zone. Two new ring-shaped structures with Mt equal to 5.0 and 5.2, which began to form here since 1973, are distinguished. There are grounds to suppose that large earthquakes can be expected in the regions of these structures. We estimate the magnitudes of possible large earthquakes: Mw = 7.8 and 7.9 on the basis of the correlation dependences of the seismicity ring sizes and Mt values on the magnitudes of major events obtained earlier for the East Pacific. These data allowed us to conclude that processes of preparation for a great earthquake with Mw ~ 9.0, similar to the 1700 event, did not begin in the subduction zone. At the same time, a large earthquake (Mw = 7.9 ± 0.1) is possible in a few years in the region of Vancouver Island. We suppose that the formation of shallow rings and deep strips of seismicity is related to deep fluid migration, as occurs in other regions.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):745-752
pages 745-752 views

Macroseismic Manifestations of the Disastrous 2008 Wenchuan Earthquake (MS = 8.0) According to the Study of Surface Seismodislocations

Jiao Liu ., Rogozhin E.

Аннотация

On May 12, 2008, a catastrophic earthquake with magnitude MS = 8.0 occurred in Wenchuan County, Sichuan, China. Its epicenter was located in the Longmen Shan mobile tectonic belt and its hypocentral depth was 14 km. The mainshock produced the system of primary seismodislocations (ruptures) on the surface: Beichuan–Yingxiu Fault of more than 240 km long, Guanxian–Anxian Fault of about 70 km long, and Xiaoyudong Fault of 7 km long. The maximum measured vertical and dextral displacements along the faults were up to 10 m and 4.8 m, respectively. The rupturing and manifold landslides, rockfalls, and rock avalanches that followed caused significant destructions in a number of localities, damaged roads, and led to massive human deaths. Data collected on the distribution of primary and secondary effects of earthquakes has helped outline zones with shaking intensities of IX, X, and XI. Notably, the seismic intensity of surface shaking was anomalously low even close to the fault system. We have conducted a comprehensive seismotectonic study of the epicentral zone of the Wenchuan earthquake. When assessing the shaking intensities, we apply the Earthquake Environmental Effects (EEE) scale developed in the framework of INQUA project (2004–2016). A comparison shows that the isoseismals identified from macroseismic data on damages in buildings and structures coincide with the locations of zones with various seismic effects on the EEE scale.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):753-767
pages 753-767 views

Geodynamic Aspects of the Evolution of the Northwestern Indian Ocean

Illarionov V., Boyko A.

Аннотация

This work is devoted to studying the structure of the northwestern part of the Indian Ocean. Primary materials of the area geological and geophysical survey performed in the southern part of the midoceanic Carlsberg Ridge (research vessel Issledovatel’, PGO Yuzhmorgeologiya, 1987) and results of unique studies of the Equator Ridge (the Somali Basin) from a manned underwater vehicle are used. The Rodrigues block is isolated at the southern extremity of the Carlsberg Ridge, which is anomalous in its morphological characteristics. The conclusion is made that this block is a connecting link of the existed continental bridge between the Seychelles Islands and the Maldive Ridge. It is conjectured that the Carlsberg Ridge was formed on a transitional crust. A complex analysis of all data on the structure of the northwestern Indian Ocean convincingly demonstrates that differentiated tectonic movements were the leading geodynamic factor in its evolution.

Izvestiya, Atmospheric and Oceanic Physics. 2018;54(7):768-776
pages 768-776 views

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