Published December 2021 | Version v1
Journal article

A survey of greenhouse gases production in central European lignites

  • 1. Institute of Agrophysics, Polish Academy of Sciences, ul. Doświadczalna 4, 20-290 Lublin (Poland)
  • 2. Institute of Biological Sciences, The John Paul II Catholic University of Lublin, Konstantynów 1 I, 20-708 Lublin (Poland)
  • 3. Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warszawa (Poland)
  • 4. Faculty of Mining and Geology, University of Belgrade, Djusina 7, 11000 Belgrade (Serbia)
  • 5. Kazan Federal University, Kremlovskaya 18, 420008 Kazan (Russian Federation)
  • 6. Department of Biochemistry and Environmental Chemistry, The John Paul II Catholic, University of Lublin, Konstantynów 1 I, 20-708 Lublin (Poland)

Description

Highlights: • The GWP of the gases released by xylitic lignite was the lowest among the samples. • Extraction of the detritic lignite may reduce GHG emissions from the abandoned mines. • Detritic lignites show the potential to serve as a source of coalbed methane. Due to changes in the energy market, it is projected that lignite excavation will be reduced in the near future. Cessation of exploitation is associated with restitution of natural water conditions and flooding of the resources left in the mines. Flooded lignite mines are a potential source of greenhouse gases (GHG) (CH4, CO2 and N2O), which should be monitored due to growing environmental concerns. Here, we aim to recognize GHG release from the lignites collected from the main deposits of Poland, Slovenia and Serbia. GHG production was studied along with a range of physical and chemical parameters that are crucial for microbial growth and activity. The microcosm experiments showed that the main gas emitted from the lignites was carbon dioxide. Daily CO2 production was highly variable. The highest values were recorded for detroxylitic lignite collected from the Konin deposit (402.05 nmol CO2 g-1 day-1) while the lowest were for the Kolubara xylitic lignite (19.64 nmol CO2 g-1 day-1). Methane production was much lower and ranged from nearly zero to 66.75 nmol g dry mass-1 d-1. Nitrous oxide production was not detected. It was found that CO2 production, being a general measure of microbial activity, was positively affected by NO3- concentration and redox potential. With respect to methane formation, the lower atmospheric oxygen exposure of the sample from the Velenje underground mine compared to the samples from the opencast mines has been identified as a possible cause of the high methane production. The overall global warming potential (GWP) of the gases released by xylitic lignite was lowest among the samples. Preferential extraction of the detritic lignites is suggested as a means to reduce GHG emissions from the abandoned lignite mines.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.scitotenv.2021.149551

Additional details

Identifiers

DOI
10.1016/j.scitotenv.2021.149551;
PII
S0048969721046258;

Publishing Information

Journal Title
Science of the Total Environment
Journal Volume
800
Journal Page Range
vp.
ISSN
0048-9697
CODEN
STENDL

Optional Information

Copyright
Copyright (c) 2021 The Author(s). Published by Elsevier B.V.