UDC: 
DOI: 
10.22389/0016-7126-2018-931-1-2-7
1 Jushkin V.D.
2 Zotov L.V.
3 Khrapenko O.A.
Year: 
№: 
931
Pages: 
2-7

Sternberg Astronomical Institute, Moscow State University

1, 
2, 

NIIMorgeofizika-Service, Ltd

3, 
Abstract:
The results of repeated measurements of the acceleration of gravity by the Russian absolute ballistic field gravimeter GABL-M on points of oil and gas deposits in the permafrost over a five year period are presented. The changes of gravity acceleration by the absolute gravimeter and GRACE satellite were compared. The results of comparisons of differences gravity acceleration by ballistic gravimeter GABL-M and relative Canadian gravimeters CG5 were [i]shown. The errors in determination of parameters of the gravitational field ballistic gravimeter GABL-M and CG5 gravimeters group were presented. The method of measurement with the gravimeter GABL-M and the method of determining the vertical gradients relative CG5 gravity meters was described. The necessity of introducing corrections of hydrogeology is caused by influence of hydro geological factors on the gravitational field in the permafrost. They are comparable with the values of the field change in the result of gas pumping.
References: 
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3.   Spiridonov Е. A., Vinogradova О. Yu. Rezultaty kompleksnogo modelirovania okeanicheskogo gravimetricheskogo effekta. Sejsmicheskie pribory, 2017, Vol. 53, no. 1, pp. 66–80.
4.   Jushkin V.D. (2012) Assessment of environment’s impact on gravity acceleration based on vertical gradients data. Geodezia i Kartografia, 860(3), pp. 3–7.
5.   Paulson A., Zhong S., Wahr J. (2007) Inference of mantle viscosity from GRACE and relative sea level data. Geophys. J. Int, no. 171, pp. 497–508. DOI: 10.1111/j.1365-246x.2007.03556.x.
Citation:
Jushkin V.D., 
Zotov L.V., 
Khrapenko O.A., 
(2018) Hydrogeology correction in the gravitational field from satellite data. Geodesy and cartography = Geodezia i Kartografia, 931(1), pp. 2-7 . (In Russian). DOI: 10.22389/0016-7126-2018-931-1-2-7
Publication History
Received: 05.07.2017
Accepted: 30.11.2017
Published: 20.02.2018

Content

2018 January DOI:
10.22389/0016-7126-2018-931-1

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