Pakistan must turn to coal – both from its own large untapped reserves and from imports – to fuel power generation beyond the next decade if it is to ease the energy crisis which is capping economic growth, trade and industry.
The Thar coalfield is located in Thar Desert, Tharparkar District of Sindh province in Pakistan. The deposits - 6th largest coal reserves in the world, were discovered in 1991 by Geological Survey of Pakistan (GSP) and the United State Agency for International Development.
Pakistan has emerged as one of the leading countries - seventh in the list of top 20 countries of the world after the discovery of huge lignite coal resources in Sindh. The economic coal deposits of Pakistan are restricted to Paleocene and Eocene rock sequences. It is one of the world’s largest lignite deposits discovered by GSP in 90’s, spread over more than 9,000 km2. comprise around 175 billion tonnes sufficient to meet the country’s fuel requirements for centuries.
The Thar coalfield is located in Thar Desert, Tharparkar District of Sindh province in Pakistan. The deposits - 6th largest coal reserves in the world, were discovered in 1991 by Geological Survey of Pakistan (GSP) and the United State Agency for International Development.
Pakistan has emerged as one of the leading countries - seventh in the list of top 20 countries of the world after the discovery of huge lignite coal resources in Sindh. The economic coal deposits of Pakistan are restricted to Paleocene and Eocene rock sequences. It is one of the world’s largest lignite deposits discovered by GSP in 90’s, spread over more than 9,000 km2. comprise around 175 billion tonnes sufficient to meet the country’s fuel requirements for centuries.
Distance from Karachi : | 360 Km |
Total Area : | 9,100 sq. Km |
Coal Reserves: | 175 Billion Tons |
The Thar coalfield with a resource
potential of 175 billion tonnes of coal covers an area of over 9,000 sq
km in the Thar Desert in Thar Parkar district, in southeastern part of
Sindh. The investigated area is covered by stable sand dunes and there
are no rock exposures. To establish the coal resources in six selected
blocks a total of 237 holes were drilled. The coal resources of the area
within clastic sediments ofthe Bara Formation of Paleocene age. The
measured reserves are over 2,357 million tonnes, indicated millions
tonnes and inferred 1,362 million tonnes.
The number of coal seams varies from
hole to hole and a maximum of 20 seams have been logged in some of the
drill holes. The thickness of coal seams ranges between 0.21 to 22.81
meters. The cumulative coal thickness varies and attains a maximum of 36
meters in one of the drill holes. Clay stone and loose sand beds form
the roof as well as the floor-rock of coal seams. The overburden
consists of three kinds of material; dune sand, alluvium and sedimentary
rocks. The thickness of the overburden varies from 114 to over 203
meters. The sand dunes above the average ground level in the area will
also add another 30 meters of thickness to the overburden.
Chemical analyses of coal samples from
the drill holes show that the weighted average of as received values of
the Ash content ranges between 5.14 and 6.56 %, Volatile matter 26.50
and 33.04 %, Moisture 43.24 and 49.01 %, Sulphur 0.92 %, 1.34 % and 1.3%
and Heating Values range between As Received 5,780 and 6,398 Btu/lb,
Dry10,723 and 11,353 Btu/Lb MMM Free 6,101 and 6,841 Btu/lb, DAF 11605
and 12,613. The Volatile Matter Dry Ash Free (DAF) basis varies between
57.72 and 60 % the rank of coal is Lignite B to Lignite A.
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