Efficiency of Seismic Prospecting in the Northern Regions of Western Siberia

Author(s):  
V.I. Kuznetsov ◽  
Y.A. Kuryanov ◽  
V.P. Torgashov
Author(s):  
S. V. Grigorieva ◽  
A. V. Olshansky

The article is devoted to the problems of maintenance of overhead power lines in the Far North of Western Siberia. For improvement of quality and reliability of power supply of consumers in the conditions of the Far North of Western Siberia, decrease in operational costs and volumes of the carried-out emergency works the hardware-software complex for expeditious inspection, assessment and forecasting of change of technical condition of constructive part of air lines (VL) of 35-220 kV is developed, the structure of the hardware-software complex of registration of the condition of constructive part of VL of 35-220 kV and structure of the hardware-software complex of storage., processing and analysis of the obtained data on the States of the constructive part of the VL 35-220 kV. 


Author(s):  
N. V. Pertsev ◽  
O. V. Ryabkova ◽  
A. N. Sabarov

The historical and geographical description of the most northern regions of Russia is still a poorly understood topic. The article analyzes historical material concerning the Tazovsky Peninsula (Western Siberia) presented in the cartographic source of the 17thcentury Chorographic drawing book of outstanding cartographer Semen Remezov. The authors reveal the peculiarities of the creation of the entire book as a whole and of the drawing itself, which had direct office sources. Identification of areas of historical events mentioned at the source, was carried out by means of comparing toponymic information in the source with modern data. As a result, it became possible not only to reconstruct the events outlined by the author of the drawing, but also to establish their spatial localization, which make possible detailed historical and archaeological research.


Author(s):  
E. A. Romanenko ◽  
D. V. Moskovchenko ◽  
A. A Kudryavtsev ◽  
G. N. Shigabaeva

The total concentrations of metals (Fe, Mn, Cu, Ni, Cr, Sr) and their mobile forms extracted by an ammonium acetate buffer (pH = 4,8) were studied in soils samples collected from Nadym-Pur interfluve (West Siberia), near the northern limit of the taiga zone. The heavy metal content was determined in 55 background soil samples and in 25 pyrogenic ones. Gross content was determined on a spectrometer "SPECTROSCAN MAX-GV" using X-ray fluorescence analysis. Mobile forms of metals were determined on a ContrAA 700 atomic absorption spectrometer by flame and electrothermal methods. The statistics are calculated using the Excel software package. The study confirmed the weak accumulation of metals in the soils of the northern regions of Western Siberia. The total content below the soil world average for Fe is 5 times, Mn – 3 times, Sr – 2 times, Cr – 1,4 times. The content of mobile forms varies widely depending on the amount of organic matter. The percentage of mobile forms of metals from the total content was: Cr – 0.84%, Fe – 1,2%, Sr – 3,8%, Mn – 8,7%, Ni – 15%. In the profile of podzols, the distribution of mobile forms of metals has an eluvial-illuvial character. Mn and Sr accumulate intensively in the surface organogenic horizons, and the Fe content increases in the BF horizon. Minimum values are marked in horizon E. In pyrogenic soils, there is an increase in the content of mobile forms of metals due to the intake of ash. Metal content usually not exceeded the maximal permissible concentrations for soils.


2012 ◽  
Vol 46 (4) ◽  
pp. 317-320 ◽  
Author(s):  
V. S. Grigor’ev ◽  
V. G. Ol’shanskii ◽  
A. D. Starostenkov ◽  
N. K. Khromyshev ◽  
K. P. Shevtsov

2012 ◽  
pp. 135-138
Author(s):  
B. M. Mirkin ◽  
L. G. Naumova ◽  
E. Z. Baisheva ◽  
V. B. Martynenko

Progress floristic classification of the vegetation of Russia is obvious (Mirkin, Ermakov, 2010; Mirkin, Naumova, 2011). However, in the vast territory of the country are still many «white spots», vegetation which syntaxonomically not been studied. One of these large «white spots» — the vegetation of the bogs. For years, the «monopolist» in ecologo-floristic classification of wetlands was V. A. Smagin (student major Soviet bolotoved M. S. Boch). He studied the vegetation of wetlands of the Northern regions of the European taiga and the basin of Myriagon Surgut Polesie (Smagin, 1998, 2000, 2003, etc.). Peer-reviewed monograph on the vegetation of mires in Western Siberia can be considered as a breakthrough in the syntaxonomy of this type of vegetation. Moreover, as a result of the work of E. D. Lapshina picture of syntaxonomy of bog vegetation has changed so much that one can speak about a kind of «syntaxa of the revolution».


2021 ◽  
Vol 2 (1) ◽  
pp. 291-300
Author(s):  
Mikhail A. Fomin ◽  
Rashid M. Saitov ◽  
Elena A. Kostyreva ◽  
Svetlana V. Rizhkova ◽  
Inga S. Sotnich ◽  
...  

The article presents a methodology developed by the authors for calculating the lithological composition of the Bazhenov Formation in Western Siberia. It is based on the identified relationships between the mineral-component composition and physical properties of rocks. The physical meaning of the identified connections has been substantiated. Satisfactory convergence of the calculated values and core data is shown. Possibilities of using the developed technique in wells not characterized by core material and limitations for its application are described.


Author(s):  
V. V. Zuev ◽  
E. M. Korotkova ◽  
A. V. Pavlinsky

The paper considers the results of the trend and correlation analysis of air temperature and vegetative index NDVI for the warm period for the territory of taiga and tundra of Western Siberia in 19822015. It was revealed that with significant ( = 0.05) positive air temperature trends in some months of the spring-summer period, both for the taiga zone and for the tundra zone, a significant increase in NDVI is observed. The trends of air temperature and NDVI for the taiga and tundra zones from April to October 19822015 have been calculated and the unevenness of their spatial distribution over the territory under consideration is shown. It is revealed that the development of vegetation in the warm period is largely determined by its development in the first month of the warm period May for taiga and June for tundra. It is shown that the NDVI value in May in the taiga zone is formed under the influence of April-May temperatures, and in June in the tundra zone under the influence of June temperatures; significant NDVI correlation coefficients with the average temperature of April-May and May-June are characteristic of practically the entire territory of the region, with the exception of the coastal northern regions in the first case and the south-western regions in the second.


2021 ◽  
Vol 3 (121) ◽  
pp. 92-104
Author(s):  
B Biyarov

The article reveals some aspects of the Russian colonization of the SiberianKhanate, which was formed in the second half of the 15th century in Western Siberia. Historicalplace names prove that before Yermak's detachment, the Russians did not cross the Ural Mountains,where Siberians and Turkic tribes lived for a long time. At the same time, the author considers thecampaign of Yermak's detachment to be aggression and considers its use unworthy of such a forceas Russia.The article notes that Kushim Khan, who fought for the independence of the Siberian Khanateuntil the end of his life, could not get a proper assessment of history. It was only natural that hisarmy, armed with bows, swords and spears, would not be able to withstand guns and rifles. At thesame time, Kushim Khan fought until the end of his life, and then his sons continued and stoppedthe process of colonization for decades.The article provides an etymological analysis of the macrotoponyms of the Siberian Khanate.The author also offers his own conclusions, referring to long-standing scientific opinions about themeaning of certain historical toponyms. Since the etymology of toponyms is revealed only in theUgric or Turkic languages, it is known that this region has long been inhabited by the Ostyaks,Voguls and Turkic peoples. Everyone knows that Western Siberia, Eastern Siberia and the Far Eastwere later colonized by Russia.This article can be considered a response to the inappropriate, unreasonably expressedopinions of some Russian politicians that “the northern regions of Kazakhstan (not to mentionWestern Siberia – the author) belonged to Russia, these lands were a “gift” to Kazakhstan”. Theoutstanding Russian scientist G. Potanin also, on the contrary, claims that “Siberia was a gift toRussia”.


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