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Chemical composition of various petrographic constituents of brown coal from the Balakhtinskoe deposit

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Abstract

The ozonolytic destruction of the organic matter of the semibright and dull lithotypes of brown coal from the Balakhtinskoe deposit and the component composition of the products were studied. It was established that the organic matter of fusinite brown coal is more reactive with respect to ozone. The products obtained from it were characterized by the presence of aliphatic acids with shortened carbon chains and an increased concentration of hydroxy acids.

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References

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Authors and Affiliations

  1. Institute of Coal, Siberian Branch, Russian Academy of Sciences, Kemerovo, 650610, Russia

    Yu. F. Patrakov

  2. Institute of Coal Chemistry and Chemical Materials Science, Siberian Branch, Russian Academy of Sciences, Kemerovo, Russia

    S. A. Semenova

Authors
  1. Yu. F. Patrakov
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  2. S. A. Semenova
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Corresponding author

Correspondence to Yu. F. Patrakov.

Additional information

Original Russian Text © Yu.F. Patrakov, S.A. Semenova, 2012, published in Khimiya Tverdogo Topliva, 2012, No. 1, pp. 3–8.

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Patrakov, Y.F., Semenova, S.A. Chemical composition of various petrographic constituents of brown coal from the Balakhtinskoe deposit. Solid Fuel Chem. 46, 1–6 (2012). https://doi.org/10.3103/S0361521912010119

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  • DOI: https://doi.org/10.3103/S0361521912010119

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