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Zawartość części lotnych w węglach kamiennych : parametr nie tylko chemiczno-technologiczny

Sivek M., Jirásek J., Hýlová L., Mirkowski Z.

Przegląd Geologiczny

2018

Vol. 66, nr 8

477--480

The volatile matter content is one of the most common chemical-technological parameters that have been determined for the vast majority of samples taken from the bituminous coal seams for more than 100 years. Its meaning is essentially triple. The oldest and also most well-known is its use for the determination of the degree of coalification (rank) of coal, but also of certain chemical-technological properties of coal (especially cokeability). With the development of coal geology and sedimentology, as well as the increasing importance of energy raw materials in the nation's economy, new ways ofusing the values of the volatile matter content have emerged. One of them was the study of the history of geological development of sedimentary, especially coal basins, the management of the mining industry economy, as well as the assessment andformulation of raw materials policy of the state. From a test originally designed to assess the suitability ofcoalfor coking, it has become a parameter used in the field of geology, economy and raw materials policy of the state.

Coal-bearing capacity of the Petřkovice Member (Ostrava Formation, Serpukhovian, Mississippian) of the Upper Silesian Basin (Czech Republic and Poland)

Hýlová L., Jirásek J., Sivek M., Jureczka J.

Geological Quarterly

2016

Vol. 60, No. 3

637--649

The Petřkovice Member is the basal unit of the paralic succession of the Ostrava Formation of the Upper Silesian Basin. This member is a valuable source of information about the transition from a marine basin filled with siliciclastic sediments into a paralic basin with the beginning of coal-bearing sedimentation. Models of: (1) the number of coal seams, (2) their total thickness, and (3) the coal content with respect to the total thickness of the succession were created to describe and assess the coal-bearing capacity of the Petřkovice Member. The authors present models for coal seam thicknesses exceeding either 10 or 40 cm. The coal-bearing capacity of the Petřkovice Member is very low. The average share of coal seams thicker than 0.1 m is 3%. The share of coal seams with a thickness that exceeds 0.4 m is only 1.66%. Moreover, in large areas of the basin, in the N and NE parts, the coal-bearing capacity is close to zero, because coal seams of greater thickness were detected only locally there. Based on these models and on other geological data, it is obvious that the onset of coal sedimentation was gradual and limited to particular sites showing the greatest subsidence of the basin floor. In places where minor subsidence took place, there were likely unfavorable conditions for accumulation of organic matter.