Characteristics of Hydrosphere of the Oil and Gas Bearing Buzuluk Depression of Orenburzhye

A. Y. Gayev

Abstract


The main resources of fresh groundwater in the region are concentrated in the watershed areas, where the aquifers are presented by alluvium and fractured bedrock. Often this zone of fractured rock is not limited by the river bed area but extends to the depth and the aquifers of high permeability and discharge were encountered in the deep water wells. Instead of fresh water, the salt waters and brine may be used for technical purposes at the oil and gas fields.


Keywords


hydrosphere; neotectonics; updated fracturing; fresh water; water exchange

References


Atlas Orenburgskoy oblasti [Atlas of the Orenburg region]. Federalnaya sluzhba geodezii i kartografii Rossii, Moskva, 1992.

Budanov N.D. 1964. Gidrogeologiya Urala [Hydrogeology of the Urals]. Nauka, Moskva, p. 304. (in Russian)

Gaev A.Ya. 1989. Gidrogeokhimiya Urala i voprosy okhrany podzemnykh vod [Hydrogeochemistry of Urals and the protection of groundwater]. Izd-vo Ural. Univ., Sverdlovsk, p. 368. (in Russian)

Garrels R.M., Christ C.L. 1965. Solutions, minerals, and equilibria. Harper and Row, New York, p. 450.

Gidrogeologiya SSSR [Hydrogeology of the USSR ]. Tom XLIII. Orenburgskaya oblast'. Nedra, Moskva, 1972, p. 162. (in Russian)

Donetskova, A.A., Kleymenova I.E., Belikova N.G. 2007. Otsenka ekologicheskogo sostoyaniya okruzhayushchey prirodnoy sredy pered nachalom namechaemoy deyatelnosti [The ecological rating of the natural environment before the proposed development]. Proc. VII Vseros. nauchn.-tekhn. konf. Aktualnye problemy sostoyaniya i razvitiya nefte-gazovogo kompleksa Rossii. RGU nefti i gaza im. I. M. Gubkina, Moskva, pp. 460-461. (in Russian)

Metodicheskie rekomendatsii po sostavleniyu kart otsenki i prognoza ekologicheskogo sostoyaniya geologicheskoy sredy masshtabov 1:100000 - 1:200000, 1:500000 - 1:1000000 [Guidelines on methodology of mapping for assessment and forecasting the ecological state of geological environment of scale 1:100000 - 1:200000, 1:500000 - 1:1000000]. VSEGINGEO, Moskva, 2002, p. 67. (in Russian)

Sistemy monitoringa okruzhayushchey sredy i nedr neftegazonosnykh territoriy [Systems of monitoring of environment and subsurface of oil and gas areas]. Orenburgskoe kn. izd., Orenburg, 2011, p. 144. (in Russian)

Trebovaniya k geologo-ekologicheskim issledovaniyam i kartografirovaniyu massht-aba 1:1000000, 1:500000, 1:200000, 1:100000, 1:50000, 1:25000 [Requirements for geological and environmental studies and mapping in scale 1: 1,000,000 and 1: 500,000, 1: 200,000, 1: 100,000, 1: 50,000, 1: 25,000]. V. 3, VSEGINGEO. Moskva, 1990, p. 236. (in Russian)

Anderson G.M. 1996. Thermodynamics of natural systems. John Wiley and Jons, New York.

Jacobsen J.S. Carnahan C.L. 1990. Coupled Transport Processes in Semi permeable Media. Analytical Solutions of the Linearized Governing Equations. Report of Lawrence Berkeley Laboratory, LBL 24725, UC 403, 1990. p. 22.




DOI: http://dx.doi.org/10.17072/psu.geol.33.18

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