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Research Article

Pore Morphology and Oxidation Behaviour of Deep-Loaded Granular Coal at High Initial Temperatures

, , , &
Received 01 Jun 2024, Accepted 29 Jul 2024, Published online: 05 Aug 2024
 

ABSTRACT

As coal mining proceeds deeper, fragmented coal is subjected to high geostress and elevated thermal environments, causing changes in its micro-physical properties and spontaneous combustion (SC) risks. Deep mining operations entail significant risks of coal fires. In order to investigate the effects of high stress and high thermal environments on the microstructural and physicochemical damage of fragmented coal, and to elucidate the mechanisms influencing oxidation behavior, we conducted experiments including low-temperature nitrogen adsorption, synchronous thermal analysis, and in-situ diffuse reflectance spectroscopy. These experiments aimed to explore the pore morphology and oxidation characteristics of high initial temperature unloading granular coal (HITU-GC) unloading conditions. The results indicate that with increasing initial temperature, characteristic point temperatures initially rise and then decrease, while both the mass loss and heat release during the low-temperature oxidation stage decrease. After pressure-unloading composite treatment, the oxidation process accelerates with more intense reactions, resulting in an overall increase in heat release. The pore shapes of HITU-GC show no significant difference compared to the original coal, mainly comprising non-rigid aggregates of micropores, platy or layered matrix particles, including numerous slit-shaped pores. The coal surface also exhibits ink bottle-shaped pores and cone-shaped pores. Higher pre-oxidation temperatures correlate with higher specific surface areas. Higher stress levels from pressurized unloading correlate with lower specific surface areas. The specific surface area of sample O60-P16 is reduced by 0.879 m2/g compared to sample O60-P0. Pressurized unloading treatment disrupts mesoporous pores. Following thermal environment and pressure-unloading, the coal’s aromatic hydrocarbon content decreases, while the contents of hydroxyl, aliphatic hydrocarbons, and oxygen-containing functional groups (FG) all increase. Sample O60-P4 shows the highest content of active FG. While thermal environments enhance coal oxidation activity, pressure-unloading treatment increases the extent of coal surface fragmentation. The synergistic effect of both significantly increases the SC risk of coal. This study provides a theoretical basis for controlling thermal hazards associated with high-initial-temperature unloading fragmented coal in deep goaf areas.

Nomenclature

HITU-GC=

High initial temperature unloading granular coal

SC=

Spontaneous combustion

FG=

Functional groups

RC=

Raw coal

O45-P0=

Initial temperature 45°C Pressure 0 MPa unloading coal sample

O45-P4=

Initial temperature 45°C Pressure 4 MPa unloading coal sample

O45-P16=

Initial temperature 45°C Pressure 16 MPa unloading coal sample

060-P0=

Initial temperature 60°C Pressure 0 MPa unloading coal sample

O60-P4=

Initial temperature 60°C Pressure 4 MPa unloading coal sample

O60–16=

Initial temperature 60°C Pressure 16 MPa unloading coal sample

-COOH-=

Carboxy

-C=O-=

Carbonyl group

-OH-=

Oxhydryl

-CH2-=

Methylene group

-CH3-=

Methyl group

CH4=

Methane

Ar-C-O=

Aromatic ether

TG=

Thermogravimetric

DSC=

Differential scanning calorimetric

BET=

Brunauer-Emmett-Teller surface area analysis method

HK=

Horvath-Kawazoe micropore distribution calculation method

BJH=

Barrett-Joyner-Halenda (BJH) pore size distribution calculation model

FTIR=

Fourier Transform Infrared Spectrometer

TD0=

Temperature at zero heat release rate

TDmax=

Maximum heat release rate temperature

IUPAC=

International Union of Pure and Applied Chemistry

Disclosure statement

No potential conflict of interest was reported by the author(s).

CRediT authorship contribution statement

Hui-Yong Niu: conceptualization, funding acquisition, writing – original draft, writing – review and editing. Xi Yang: conceptualization, Writing – original draft; Qing-qing Sun: writing – review and editing; Si-wei Sun: writing – review and editing, Visualization; Xiao-dong Yu: writing – original draft, Conceptualization.

Additional information

Funding

The authors wish to acknowledge gratefully the financial support of the research funding provided by the National Natural Science Foundation of China [Nos. 52174163 & 51874131&51474106].

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