Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch

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Veröffentlicht in:Геофизический журнал
Datum:2010
Hauptverfasser: Maksymchuk, V., Orliuk, M., Tregubenko, V., Horodysky, Y., Nakalov, Y., Myasoyedov, V.
Format: Artikel
Sprache:Englisch
Veröffentlicht: Інститут геофізики ім. С.I. Субботіна НАН України 2010
Online Zugang:https://nasplib.isofts.kiev.ua/handle/123456789/101861
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Zitieren:Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch / V. Maksymchuk, M. Orliuk, V. Tregubenko, Y. Horodysky, Y. Nakalov, V. Myasoyedov // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 94-96. — Бібліогр.: 2 назв. — англ.

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Digital Library of Periodicals of National Academy of Sciences of Ukraine
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author Maksymchuk, V.
Orliuk, M.
Tregubenko, V.
Horodysky, Y.
Nakalov, Y.
Myasoyedov, V.
author_facet Maksymchuk, V.
Orliuk, M.
Tregubenko, V.
Horodysky, Y.
Nakalov, Y.
Myasoyedov, V.
citation_txt Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch / V. Maksymchuk, M. Orliuk, V. Tregubenko, Y. Horodysky, Y. Nakalov, V. Myasoyedov // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 94-96. — Бібліогр.: 2 назв. — англ.
collection DSpace DC
container_title Геофизический журнал
first_indexed 2025-12-07T16:39:32Z
format Article
fulltext ������� ���� ���� ���� 3" ������������������� �!�"#�$%�&'#�'()( Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch V. Maksymchuk1 ��M. Orliuk2 � V. Tregubenko3, Y. Horodysky1 � �Y. Nakalov1, V. Myasoyedov2, 2010 1Carpathian Branch of Institute of Geophysics, National Academy of Sciences of Ukraine, Lvov, Ukraine vmaksymchuk@cb-igph.lviv.ua Institute of Geophysics, National Academy of Sciences of Ukraine, Kiev, Ukraine orlyuk@igph.kiev.ua 3Ukrainian State Geological Prospecting Institute, Kiev, Ukraine vitr@ukrdgri.gov.ua During�����&���)�years�there�was�renewed�and enlarged�the�Ukrainian�geomagnetic�repeat�stations (RS)� network� by� the� co+workers� of� Carpathian Branch�of�Subbotin�Institute�of�Geophysics,�Sub- botin�Institute�of�Geophysics�and�Ukrainian State Geological Prospecting Institute.�At�present�time�RS network�contains�-'�points��The�distances�between RS�are�about�'�� km,�i� e��the�density�of�RS�is�about '�point�for�'� ����km�. Similar networks are created in most European countries. The works of this sci- entific branch are coordinated by MagNetE (Mag- netic Network in Europe) organization, which was founded in Potsdam in 2003. For accurate reduc- tion of geomagnetic field components it is neces- sary to refer the RS measurements data to the con- tinuous magnetic variation observations that are carried out on close by magnetic observatories (MO) or set of MO. There are 3 MO in Ukraine “Kyiv”, “Lviv” and “Odesa”, besides for the reduction accu- racy increasing we can use the data of neighbou- ring countries MO such as “Belsk”, “Tihany” etc. as well as the data of permanent magnetic variation on geophysical stations such as “Nyzhnje Selysche” etc. The main task of magnetic RS measurement consists in creating the maps of normal geomag- netic field components and theirs secular variation (SV) rates. Alongside of geomagnetic fundamental problems decision the results of RS measurement allows to perform reduction of different time mag- netic data to common epoch and unified normal field level. This is very important for creation of aggrega- ted anomalous field maps of large areas. The results of RS magnetic measurements may be very useful in navigation and topographic mapping where magnetic declination D and its yearly changes are given. Actuality of RS network magnetic measurements and creating the newest maps of normal magnetic field as well as its SV rate on the territory of Ukraine is emphasized also because of appearing of SV rate focus at the end of XX century in the Eastern Eu- rope. The appearing of this focus makes it more difficult to use the worked out local anomalous mag- netic field models and investigate this field tempo- ral changes for tectonic magnetic investigations as well as for geophycical exploration. Comparison of SV rates calculated due to model IGRF-2005 with rates obtained on MO of Europe reveal as notice- able distinctions of theirs special structures and morphology of time series between them as well [Maksymchuk et al., 2010]. We did follow the international recommendations [Newitt et al., 1996] when selecting the place of RS founding and performing measurements of magne- tic field components. The scalar of geomagnetic field ������������������� �!�"#�$%�&'#�'()( 34 +,� ��-.�,/�0 ��.������1 �, ��0.�0��0���,������ ����� �� Isogons�distribution on the territory of Ukraine reduced to epoch 2005.5. RS — Asterisks. MO — Black squares. vectors were measured by proton magnetometers with sensitivity 0.1 nT. Magnetic declination and in- clination (I) were determined with ferrosonde mag- netometer mounted on demagnetized theodolite of 1 arcsec scale accuracy. The reductions of mag- netic field X-, Y-, Z-components were done to mid- dle of observation years epochs and to common epoch 2005.5 as well. These reductions were per- formed referencing the data of permanent observa- tion of MO “Belsk”, “Kyiv”, “Lviv”. Standard devia- tions of obtained results are in the range from 2 nT to 3.5 nT for X-, Y-, Z-components and lesser then 30 for I and 50 for D. These results were summa- rized in catalogue of Ukrainian RS for the 2005.5 epoch. We also created a set of maps for geomag- netic field components. Comparison of components values that were obtained on Ukrainian RS network with the same components calculated due to IGRF-2005 model shows, that differences for linear (X, Y, Z) compo- nents lie in the range from several to several hun- dreds of nT. Apparently these differences are caused mainly by effect of magnetic anomalies localized in the Earth’s crust. The map of magnetic declination D (isogons) has a particular applied interest. Such map due to 1st cycle of Ukrainian RS network mea- surements is shown on Figure. The values of D, reduced to epoch 2005.5 on the territory of Ukraine lie in the range from 4 in the western region to 8 in the eastern region. The isogons shown on Figure noticeably differ from the same calculated by mod- el IGRF-2005. Unlikely to model isogons the ob- served ones are of very complicated configuration. One can easily distinguish several anomalies of re- gional scale on the background of global trend. The general features of isogons distribution configura- tion are in concordance with tectonic structure and anomalous magnetic field of regional scale. Conclusion. The RS network creation on the ter- ritory of Ukraine allows make use of the obtained data in process of new generation IGRF model con- struction. Even results of 1st cycle measurements may be useful as for IGRF model more precise de- finition and for tectonomagnetic investigations as well. Undoubtedly it is necessary to fulfill the next cycle of measurements on the created RS network and if it would be possible to enlarge the number of RS. ������� ���� ���� ���� 3� ������������������� �!�"#�$%�&'#�'()( References Newitt L. R., Barton C. E., Bitterly J. U. Guide for mag- netic repeat station surveys. — Boulder: IAGA, 1996. — 112 p. Maksymchuk V.��Orlyuk M.� Tregubenko V., Horody- sky Yu.��Nakalov Ye., Myasoyedov V. Land abso- lute magnetic survey on the basic network of re- peat stations in Ukraine for the epoch 2005.5 // Geophys. J. — 2010. — 32, � 5. — P. 82—85 (in Ukrainian).
id nasplib_isofts_kiev_ua-123456789-101861
institution Digital Library of Periodicals of National Academy of Sciences of Ukraine
issn 0203-3100
language English
last_indexed 2025-12-07T16:39:32Z
publishDate 2010
publisher Інститут геофізики ім. С.I. Субботіна НАН України
record_format dspace
spelling Maksymchuk, V.
Orliuk, M.
Tregubenko, V.
Horodysky, Y.
Nakalov, Y.
Myasoyedov, V.
2016-06-08T15:21:24Z
2016-06-08T15:21:24Z
2010
Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch / V. Maksymchuk, M. Orliuk, V. Tregubenko, Y. Horodysky, Y. Nakalov, V. Myasoyedov // Геофизический журнал. — 2010. — Т. 32, № 4. — С. 94-96. — Бібліогр.: 2 назв. — англ.
0203-3100
https://nasplib.isofts.kiev.ua/handle/123456789/101861
en
Інститут геофізики ім. С.I. Субботіна НАН України
Геофизический журнал
Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch
Article
published earlier
spellingShingle Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch
Maksymchuk, V.
Orliuk, M.
Tregubenko, V.
Horodysky, Y.
Nakalov, Y.
Myasoyedov, V.
title Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch
title_full Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch
title_fullStr Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch
title_full_unstemmed Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch
title_short Results of the geomagnetic survey on the Ukrainian repeat stations network for the 2005 year epoch
title_sort results of the geomagnetic survey on the ukrainian repeat stations network for the 2005 year epoch
url https://nasplib.isofts.kiev.ua/handle/123456789/101861
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AT tregubenkov resultsofthegeomagneticsurveyontheukrainianrepeatstationsnetworkforthe2005yearepoch
AT horodyskyy resultsofthegeomagneticsurveyontheukrainianrepeatstationsnetworkforthe2005yearepoch
AT nakalovy resultsofthegeomagneticsurveyontheukrainianrepeatstationsnetworkforthe2005yearepoch
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