Sri Rama Steels & Coal

In Indonesian origin, we offer our clients a wide range of choice which makes it easier for them to select the appropriate Coal for their boiler. Generally, Indonesian origin Coal ranks from 5000 GCV to 7000 GCV differing in some or the other parameter (specification). Most of the Indonesian origin Coal has high percentage of Volatile Matter, but they benefit from low ash and low sulfur content. Indonesian origin Coal is the most widely used in all industries due to easy availability & lower in price, compared to Coal mined from other origin. Indonesian Coal is also used to blend along with Coal from other origin in order to lower production cost.

We offer high Fixed Carbon content south-African Coal. In general south-African Coal is termed high rank Coal by Coal traders & end-users globally. South-African Coal application is specialized & limited to modern Steel production units, blast furnaces, cement plant boilers & sponge Iron producing kilns.
Product specification:
Total Moisture (AR)-12-13%     
Inherent Moisture (ADB)-4%
Ash Content (ADB)-15%
Sulphur (ADB)-<1%   
Calorific value (ADB)-6500 Kcal/kg 
Volatile Matter (ADB)-28%
Fixed carbon (ADB)-55%                                                                                                                                                           

We supply Indian Coal which includes:
ROM Coal: Run of Mine Coal isl which comes from mines directly. ROM Coal comprises of size ranging from 0 MM-500 MM or bigger as it is not subject to screening or crushing
Size Coal: Steam Coal or size Coal is retained when ROM Coal is subject to crushing or screening. Steam Coal is also obtained handpicked or shovel picked from ROM Coal.
Slack Coal: Portion of Coal that remains after steam Coal is screened from ROM Coal is slack Coal.

We supply indigenous Coal from Maharashtra, and Andhra Pradesh.

: We are reckoned as one of the most astounding Coal suppliers in India. We supply diversified range of imported steam Coal. Coal is believed to be formed during the carboniferous era. In the earlier days of our earth, the plants that lived then eventually died and coalification began. The layers of the plant matter died and started accumulating at the bottom of the seabed. Conversion of these organic matters due to the action of pressure, temperature, and a hundreds of years went into the making of this wonderful energy fuels. They helped in trapping atmospheric carbon in the ground in huge peat bogs that eventually were covered and deeply buried by sediments as a result of which those plants remain transformed into fuel. With the passing time, the chemical and physical properties of the plant remains were changed by geological action to create a solid matter-Coal.