Category Ranking

98%

Total Visits

921

Avg Visit Duration

2 minutes

Citations

20

Article Abstract

To explore the differences in biological gas production in the waterlogged zone of a coal seam fire-affected area, in this study the gas production experiment was conducted with the mine water from aquitard layers in coal seam fire zones in Xinjiang. The results showed that the biogas production first increased and then decreased with the increase in distance, and the highest gas production reached 216.55 mL. The changes in key metabolic pathways during the anaerobic fermentation of coal were analyzed, which showed that as the distance from the aquitard layer in the coal seam fire zone increased, the methanogenesis pathways gradually shifted from acetic acid decarboxylation and carbon dioxide reduction to acetic acid decarboxylation and methylamine methanogenesis. The significant variability in the mine water reservoir conditions contributed to the differences. In addition, the reservoir pressure and temperature increased as the distance from the fire zone became longer, and the salinity of the farthest mine water in the reverse fault was the highest due to the lack of groundwater supply. Pearson correlation analysis revealed significant correlations of microbial communities with key functional genes and the types and concentrations of ions. The ions significantly influencing microbial enzymatic metabolic activities included Al, Fe, Co, Ni, Cu, Zn, Mg, PO, and Mo. The differences in metabolic pathways were attributed to the integrated effects of a co-occurring environment with multiple ions. The gas production simulation experiments and metagenomic analyses provide data support for the practical application of biogas experiments, laying a foundation for engineering applications.

Download full-text PDF

Source
http://dx.doi.org/10.13345/j.cjb.240657DOI Listing

Publication Analysis

Top Keywords

coal seam
16
gas production
16
seam fire
12
mine water
12
biogas production
8
aquitard layers
8
layers coal
8
metabolic pathways
8
fire zone
8
acetic acid
8

Similar Publications

How does large-scale underground mining affect the water cycle? - Comprehensive analysis based on isotopes, water levels and hydrogeological conditions.

J Environ Manage

September 2025

State Key Laboratory of Water Engineering Ecology and Environment in Arid Area, Inner Mongolia Agricultural University, Hohhot, 010018, China; Inner Mongolia Key Laboratory of Ecohydrology and High Efficient Utilization of Water Resources, Hohhot, 010018, China; Inner Mongolia Section of the Yellow

Large-scale underground coal mining alters regional water cycles, yet the mechanisms governing interactions among water bodies in deep mining areas are poorly understood. For this purpose, by integrating hydrogen and oxygen isotopes, water levels, hydrogeological conditions, and end-member mixing analysis (EMMA), this study systematically analyzed and quantified the circulation and transformation mechanisms among different water bodies influenced by coal mining. Key findings reveal: (1) Mining-induced fractures disrupt the aquitard above the coal seam, establishing a direct hydraulic link between Zhiluo Formation confined groundwater and mine water, with the former contributing 87.

View Article and Find Full Text PDF

Guizhou Province is an important late Permian coal-producing area in China, and the resource potential of critical metal elements in its coal urgently needs to be studied. This paper systematically analyzes the geochemical characteristics of REY (rare earth elements and Y) in the No. 12 coal seam of the Late Permian Tucheng Mine in Guizhou Province using technologies such as inductively coupled plasma mass spectrometry (ICP-MS), X-ray fluorescence spectroscopy (XRF), scanning electron microscopy with energy dispersive spectrometry (SEM-EDS), and correlation analysis and discusses the environmental indication significance of REY (rare earth elements and Y) in coal.

View Article and Find Full Text PDF

Taking a mine in Guizhou Province as the research background, a combination of similar simulation experiments and numerical simulation was used to analyse the spatial distribution of overburden collapse and the development of fissures during the mining process. The results indicate that: (1) During the mining of the upper coal seam, the overlying rock is not affected by faults, the 'three zones' are significantly developed, the collapse morphology exhibits a typical 'trapezoidal' structure, and the fractures undergo stages of formation, expansion, and closure; (2) The lower coal seam is affected by reverse faults, resulting in asymmetrical overburden collapse patterns and discontinuous fissure development. When mining across faults, periodic pressure is intense, and the stride length is significantly reduced, with severe rock fragmentation near the faults.

View Article and Find Full Text PDF

Physical simulation experiments of CO flow adsorption under various stratigraphies were conducted in the coal seam CO injection project for gas replacement, as CO is in the flow state and the mechanism of CO adsorption in the flow state in the coal seam is still unclear. In the process of CO flow adsorption, the results indicate that seepage in the horizontal stratigraphic direction is predominant, while diffusion in the vertical stratigraphic direction is predominant. The ratio of CO flow adsorption in the horizontal stratigraphic direction is primarily distributed below 50%, and seepage is the dominant process during the CO flow adsorption test.

View Article and Find Full Text PDF

With the gradual extension of global coal mining to the deep, the problem of surface subsidence caused by repeated mining of multiple coal seams has attracted much attention. In this paper, the methods of theoretical analysis, numerical simulation and field monitoring are used to study the settlement model and settlement law under the condition of repeated mining of multiple coal seams, and the engineering application is carried out. Through theoretical analysis, it is concluded that there is a linear relationship between the amount of broken expansion of overlying rock mass, the buried depth of coal seam, the thickness of coal seam and the maximum subsidence value of surface.

View Article and Find Full Text PDF