Survey Of Energy Resources
COAL (INCLUDING LIGNITE)


RUSSIAN FEDERATION

Proved recoverable reserves (total coal, million tonnes) 157 010
Production (total coal, million tonnes, 1999) 249.4

The levels quoted for Russian coal resources and reserves are unchanged from those given in the 1998 Survey of Energy Resources, as the WEC Member Committee was unable to obtain any more recent coal data for the present Survey.

The proved amount of coal in place at end-1996 comprised 75.8 billion tonnes of bituminous coal, based on a maximum deposit depth of 1 200 metres and a minimum seam thickness of 0.6-0.7 metres; 113.3 billion tonnes of sub-bituminous grades (at depths of up to 600 metres and minimum thickness 1-2 metres); and 11.5 billion tonnes of lignite (at 300 metres and 1.5-2 metres, respectively).

Proved recoverable reserves were reported as just over 49 billion tonnes of bituminous coal, of which 23% was considered to be surface-mineable and 55% was suitable for coking. Of the 97.5 billion tonnes of proved recoverable reserves of sub-bituminous coal, 74% was suitable for surface mining, while all of the 10.5 billion tonnes of recoverable lignite reserves fell into this category. Overall, about 94 billion tonnes of Russia’s proved reserves were deemed to be recoverable by opencast or strip mining. Further enormous tonnages of coal, of the order of over 30 times the quoted proved reserves, were reported to be recoverable in the future.

Russian coal reserves are widely dispersed and occur in a number of major basins. These range from the Moscow basin in the far west to the eastern end of the Donetsk basin (most of which is within the Ukraine) in the south, the Pechora basin in the far northeast of European Russia, and the Irkutsk, Kuznetsk, Kansk-Achinsk, Lena, South Yakutia and Tunguska basins extending across Siberia to the Far East.

The principal economic hard coal deposits of Russia are found in the Pechora and Kuznetsk basins. The former, which covers an area of some 90 000 km2, has been extensively developed for underground operations, despite the severe climate and the fact that 85% of the basin is under permafrost. The deposits are in relatively close proximity to markets and much of the coal is of good rank, including coking grades. The Kuznetsk basin, an area of some 26 700 km2, lies to the east of the city of Novosibirsk and contains a wide range of coals; the ash content is variable and the sulphur is generally low. Coal is produced from both surface and underground mines.

Lying east of the Kuznetsk and astride the trans-Siberian railway, the Kansk-Achinsk basin contains huge deposits of brown (sub-bituminous) coal with medium (in some cases, low) ash content and generally low sulphur; large strip-mines are linked to dedicated power stations and carbo-chemical plants. The vast Siberian coal-bearing areas of the Lena and Tunguska basins constitute largely unexplored resources, the commercial exploitation of which would probably be difficult to establish.

The transportation of coal from mining to consuming areas is often problematical in a country of Russia’s proportions. As the reserves in the western areas have been increasingly depleted the focus of production has moved further east and the burden on the rail system has increased.

From a peak of around 425 million tonnes in 1988, Russia’s total coal production declined dramatically following the disintegration of the USSR, and now stands at about 250-260 million tonnes per annum. In 1998 about 70% of Russian consumption was accounted for by power stations and district heating plants. In recent years Russia has been a net exporter of coal, but on a declining scale

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