70 research outputs found
ΠΡΠ½ΠΎΠ²Π½ΡΠ΅ ΡΠ»Π΅ΠΌΠ΅Π½ΡΡ ΠΌΠΎΠ΄Π΅Π»ΠΈ ΡΡΠ»ΠΎΠ²ΠΈΠΉ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΊΡΡΠΏΠ½ΡΡ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ Π°ΡΠ°Π½ΠΈΡΠΎΠ²ΡΡ ΡΠΎΡΡΠΎΡΠΈΡΠΎΠ² ΠΠΊΠΈΠ½ΠΎ-Π₯ΡΠ±ΡΡΠ³ΡΠ»ΡΡΠΊΠΎΠ³ΠΎ Π±Π°ΡΡΠ΅ΠΉΠ½Π° ΠΈ ΠΏΠ΅ΡΡΠΏΠ΅ΠΊΡΠΈΠ²Π½ΡΠ΅ ΠΌΠ΅ΡΠΎΠ΄Ρ ΠΈΡ ΠΎΠ±ΠΎΠ³Π°ΡΠ΅Π½ΠΈΡ
In order to find out a prospecting technique of Khubsugul basin, general conditions of phosphate formation are marked and described. They exhibit a complex of sedimentary environments, making some kind of major deposits' formation model. Factors affecting a phosphate concentrating are examined. A new high - efficiency and ecologically harmless microbiological beneficiating method is proposed for consideration.ΠΠ»Ρ ΡΠ°Π·ΡΠ°Π±ΠΎΡΠΊΠΈ ΠΌΠ΅ΡΠΎΠ΄ΠΈΠΊΠΈ ΠΏΠΎΠΈΡΠΊΠΎΠ² ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ ΠΠΊΠΈΠ½ΠΎ-Π₯ΡΠ±ΡΡΠ³ΡΠ»ΡΡΠΊΠΎΠ³ΠΎ Π±Π°ΡΡΠ΅ΠΉΠ½Π° Π²ΡΠ΄Π΅Π»Π΅Π½Ρ ΠΈ ΠΎΡ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΠ·ΠΎΠ²Π°Π½Ρ ΠΎΡΠ½ΠΎΠ²Π½ΡΠ΅ ΡΡΠ»ΠΎΠ²ΠΈΡ ΡΠΎΡΡΠΎΡΠΈΡΠΎΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΡ, ΠΎΡΡΠ°ΠΆΠ°ΡΡΠΈΠ΅ ΠΊΠΎΠΌΠΏΠ»Π΅ΠΊΡ ΠΎΠ±ΡΡΠ°Π½ΠΎΠ²ΠΎΠΊ, ΠΈΠ· ΠΊΠΎΡΠΎΡΡΡ
ΡΠΊΠ»Π°Π΄ΡΠ²Π°Π΅ΡΡΡ ΡΠ²ΠΎΠ΅ΠΎΠ±ΡΠ°Π·Π½Π°Ρ ΠΌΠΎΠ΄Π΅Π»Ρ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΊΡΡΠΏΠ½ΡΡ
ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ. Π Π°ΡΡΠΌΠΎΡΡΠ΅Π½Ρ ΡΠ°ΠΊΡΠΎΡΡ, Π²Π»ΠΈΡΡΡΠΈΠ΅ Π½Π° ΠΎΠ±ΠΎΠ³Π°ΡΠΈΠΌΠΎΡΡΡ ΡΠΎΡΡΠΎΡΠΈΡΠΎΠ², ΠΈ ΠΏΡΠ΅Π΄Π»ΠΎΠΆΠ΅Π½ Π½ΠΎΠ²ΡΠΉ Π²ΡΡΠΎΠΊΠΎΡΡΡΠ΅ΠΊΡΠΈΠ²Π½ΡΠΉ, ΡΠΊΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈ ΡΠΈΡΡΡΠΉ ΠΌΠΈΠΊΡΠΎΠ±ΠΈΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠΉ ΠΌΠ΅ΡΠΎΠ΄ ΠΈΡ
ΠΎΠ±ΠΎΠ³Π°ΡΠ΅Π½ΠΈΡ
ΠΠ΅ΠΎΡ ΠΈΠΌΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΎΡΠ΅ΠΎΠ»Ρ ΠΌΠ΅Π΄Π½ΠΎΡΡΠ΄Π½ΡΡ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ Π§ΡΠΊΠΎΡΠΊΠΈ
In article discussed about two porphyry-copper deposits in the Verkhoyan-Chukotka Folded area. The results of geological analysis about spatial location of the primary geochemical diffuse halo are presented.Π ΡΡΠ°ΡΡΠ΅ ΡΠ°ΡΡΠΌΠΎΡΡΠ΅Π½Ρ Π΄Π²Π° ΠΌΠ΅Π΄Π½ΠΎ-ΠΏΠΎΡΡΠΈΡΠΎΠ²ΡΡ
ΠΎΠ±ΡΠ΅ΠΊΡΠ°, ΡΠ°ΡΠΏΠΎΠ»ΠΎΠΆΠ΅Π½Π½ΡΡ
Π² ΠΏΡΠ΅Π΄Π΅Π»Π°Ρ
ΠΠ΅ΡΡ
ΠΎΡΠ½ΠΎ-Π§ΡΠΊΠΎΡΡΠΊΠΎΠΉ ΡΠΊΠ»Π°Π΄ΡΠ°ΡΠΎΠΉ ΠΎΠ±Π»Π°ΡΡΠΈ. ΠΠ·Π»Π°Π³Π°ΡΡΡΡ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΡ Π°Π½Π°Π»ΠΈΠ·Π° ΠΏΡΠΎΡΡΡΠ°Π½ΡΡΠ²Π΅Π½Π½ΠΎΠ³ΠΎ ΡΠ°Π·ΠΌΠ΅ΡΠ΅Π½ΠΈΡ ΠΏΠ΅ΡΠ²ΠΈΡΠ½ΡΡ
Π³Π΅ΠΎΡ
ΠΈΠΌΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΎΡΠ΅ΠΎΠ»ΠΎΠ²
ΠΠ΅ΠΊΠΎΡΠΎΡΡΠ΅ Π°ΡΠΏΠ΅ΠΊΡΡ Π³Π΅Π½Π΅Π·ΠΈΡΠ° ΡΠ½ΡΠ°ΡΡ ΠΏΡΠΈΠΌΠΎΡΡΠΊΠΎΠ³ΠΎ ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΡ
The new data ascertaining amberisation process and the amber s transfer mechanism into the sedimentation basin are considered.Π Π°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°Π΅ΡΡΡ Π½ΠΎΠ²ΡΠΉ ΡΠ°ΠΊΡΠΈΡΠ΅ΡΠΊΠΈΠΉ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π», ΡΡΠΎΡΠ½ΡΡΡΠΈΠΉ ΠΏΡΠΎΡΠ΅ΡΡΡ ΡΠΎΡΠΌΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΠ½ΡΠ°ΡΡ ΠΈ ΠΌΠ΅Ρ
Π°Π½ΠΈΠ·ΠΌ Π΅Π³ΠΎ ΡΡΠ°Π½ΡΠΏΠΎΡΡΠΈΡΠΎΠ²ΠΊΠΈ Π² Π±Π°ΡΡΠ΅ΠΉΠ½ ΠΎΡΠ°Π΄ΠΊΠΎΠ½Π°ΠΊΠΎΠΏΠ»Π΅Π½ΠΈΡ
ΠΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΡ Π»Π°ΡΠ΅ΡΠΈΡΠ½ΡΡ Π±ΠΎΠΊΡΠΈΡΠΎΠ² Π‘ΡΠ΅Π΄Π½Π΅Π³ΠΎ Π’ΠΈΠΌΠ°Π½Π°
A brief description of Middle Timan's bauxite region is done. An exploitation of those deposits became a momentous event in a development of the country economic potential at the beginning of the century.ΠΡΠΈΠ²ΠΎΠ΄ΠΈΡΡΡ ΠΊΡΠ°ΡΠΊΠ°Ρ Ρ
Π°ΡΠ°ΠΊΡΠ΅ΡΠΈΡΡΠΈΠΊΠ° ΠΌΠ΅ΡΡΠΎΡΠΎΠΆΠ΄Π΅Π½ΠΈΠΉ Π‘ΡΠ΅Π΄Π½Π΅ΡΠΈΠΌΠ°Π½ΡΠΊΠΎΠ³ΠΎ Π±ΠΎΠΊΡΠΈΡΠΎΠ½ΠΎΡΠ½ΠΎΠ³ΠΎ Π±Π°ΡΡΠ΅ΠΉΠ½Π°, Π½Π°ΡΠ°Π»ΠΎ ΠΎΡΠ²ΠΎΠ΅Π½ΠΈΡ ΠΊΠΎΡΠΎΡΠΎΠ³ΠΎ ΡΡΠ°Π»ΠΎ Π·Π½Π°ΠΊΠΎΠ²ΡΠΌ ΡΠΎΠ±ΡΡΠΈΠ΅ΠΌ Π² ΡΠ°Π·Π²ΠΈΡΠΈΠΈ ΡΠΊΠΎΠ½ΠΎΠΌΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»Π° ΡΡΡΠ°Π½Ρ Π² Π½Π°ΡΡΡΠΏΠΈΠ²ΡΠ΅ΠΌ Π²Π΅ΠΊΠ΅
ΠΠΎΡΡΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΈ ΠΏΠ΅ΡΡΠΎΠ³ΡΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ ΠΆΠΈΠ»ΡΠ½ΡΡ ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΠΉ Π₯Π°ΡΠ±Π΅ΠΉΡΠΊΠΎΠΉ ΠΏΠ»ΠΎΡΠ°Π΄ΠΈ ΠΠΎΠ»ΡΡΠ½ΠΎΠ³ΠΎ Π£ΡΠ°Π»Π°
The properties of mineral veiny formations which can be auriferous from one of the prospectives regions of Polar Urals are discussed.Π Π°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°ΡΡΡΡ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»ΡΠ½ΠΎ Π·ΠΎΠ»ΠΎΡΠΎΠ½ΠΎΡΠ½ΡΡ
ΠΌΠΈΠ½Π΅ΡΠ°Π»ΡΠ½ΡΡ
ΠΆΠΈΠ»ΡΠ½ΡΡ
ΠΎΠ±ΡΠ°Π·ΠΎΠ²Π°Π½ΠΈΠΉ ΠΎΠ΄Π½ΠΎΠ³ΠΎ ΠΈΠ· ΠΏΠ΅ΡΡΠΏΠ΅ΠΊΡΠΈΠ²Π½ΡΡ
ΡΠ΅Π³ΠΈΠΎΠ½ΠΎΠ² ΠΠΎΠ»ΡΡΠ½ΠΎΠ³ΠΎ Π£ΡΠ°Π»Π°
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Modeling of Parameters of Solar Microgeneration Systems
Π ΡΠ°Π±ΠΎΡΠ΅ ΠΏΡΠ΅Π΄ΡΡΠ°Π²Π»Π΅Π½ Π°Π½Π°Π»ΠΈΠ· ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠΎΠ² ΠΌΠΎΠ΄Π΅Π»ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΏΠ°ΡΠ°ΠΌΠ΅ΡΡΠΎΠ² ΡΠΎΠ»Π½Π΅ΡΠ½ΡΡ
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ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠΎΠ² ΡΠ½Π΅ΡΠ³ΠΈΠΈ Β«ΠΠΠ£ ΠΠΠΒ» Π.Π. Π€ΠΎΠΌΠ΅Π½ΠΊΠΎ.The study carried out with the support of the director of the Institute of Hydropower and Renewable Energy Sources βMPEIβ T.A. Shestopalova, as well as a student of the Institute of Hydropower and Renewable Energy Sources Β«MPEIΒ» D.V. Fomenko
The Arctic freshwater system : changes and impacts
Author Posting. Β© American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 112 (2007): G04S54, doi:10.1029/2006JG000353.Dramatic changes have been observed in the Arctic over the last century. Many of these involve the storage and cycling of fresh water. On land, precipitation and river discharge, lake abundance and size, glacier area and volume, soil moisture, and a variety of permafrost characteristics have changed. In the ocean, sea ice thickness and areal coverage have decreased and water mass circulation patterns have shifted, changing freshwater pathways and sea ice cover dynamics. Precipitation onto the ocean surface has also changed. Such changes are expected to continue, and perhaps accelerate, in the coming century, enhanced by complex feedbacks between the oceanic, atmospheric, and terrestrial freshwater systems. Change to the arctic freshwater system heralds changes for our global physical and ecological environment as well as human activities in the Arctic. In this paper we review observed changes in the arctic freshwater system over the last century in terrestrial, atmospheric, and oceanic systems.The authors gratefully acknowledge the
National Science Foundation (NSF) for funding this synthesis work. This
paper is principally the work of authors funded under the NSF-funded
Freshwater Integration (FWI) study
Water resources of the Russian rivers and their changes
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Hydrological Institute (SHI). The long-term water resources fluctuations and
their changes during the last decades including the significant changes in
seasonal runoff are presented. The preliminary estimates of the possible
future changes are also given
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