Field Study on Correlation between CO(2) Concentration and Surface Soil CO(2) Flux in Closed Coal Mine Goaf

[Image: see text] Self-heating of coal mine goaf or shallow coal seams can release an outbreak of unimaginable pollution disaster under suitable circumstances. As an indicator gas, CO(2) is always used to determine the coal spontaneous combustion state during the self-heating process. Based on this, the paper investigated the influence of abandoned coal mine goaf CO(2) on the surface environment by measuring the CO(2) concentration in the borehole connected to the goaf and CO(2) flux on the soil surface. Furthermore, rainfall and atmospheric temperature effects are discussed to illustrate the correlation between the CO(2) concentration and surface soil CO(2) flux in the closed mine goaf. Subsequently, the tracer gas experimental method is employed to analyze the effect of air leakage from an open-pit slope on CO(2) flux. The experimental results demonstrated that the distribution of CO(2) concentration in the borehole confirms the continuous diffusion of goaf CO(2) onto the surface. The value of CO(2) flux in the goaf is significantly higher than that of a normal area. Temperature is one of the primary factors that affect the CO(2) flux on the field. Air leakage from the slope promotes the surface soil-overlying goaf CO(2) diffusion. The study provides important reference data for the assessment of the mining area field environment and the determination of the spontaneous combustion risk of the residual coal in the goaf.