Institute of Surface-Earth System Sciences, Tianjin University, Tianjin, 300072, China.
Liaoning Technical University, Fuxin, 123000, China; CCTEG Shenyang Research Institute, Fushun, 113122, China; China State Key Laboratory of Coal Mine Safety Technology, Fushun, 113122, China.
Ecotoxicol Environ Saf. 2019 Oct 30;182:109409. doi: 10.1016/j.ecoenv.2019.109409. Epub 2019 Jul 6.
The Wuda Coalfield, Inner Mongolia suffers from serious coal fires for more than half a century. Fire-extinguishing projects have been carried out to suppress the coal fires since the last decade, but sporadic surface fires still occur and underground fires are more prevailing. Here, we used a real-time RA-915M Mercury Analyzer with modified inlet to monitor gaseous Hg concentrations in fumes emitted from boreholes that were designed to detect and control the underground coal fires. Meanwhile, offline methods were used to collect the fumes and analyze the contents of the gases including CO, CO, CH, CH, CH and CH. The results showed that gaseous Hg concentrations in fumes from boreholes ranged from 6.42 ± 0.73 to 123.53 ± 34.66 ng m, with an average value of 49 ± 44 ng m. We suggest that the amounts of coal left for burning or smoldering mainly accounted for the large variation in fume Hg concentrations of underground coal fires. The gaseous Hg concentrations in near-surface air surrounding boreholes varied from 2.38 ± 0.28 to 13.10 ± 0.97 ng m, with a mean value of 6.68 ± 3.09 ng m. They were higher than the ambient air Hg concentrations measured at a background site near the Yellow River (<2 ng m), suggesting underground coal fires were one significant Hg pollution source. Importantly, we found that gaseous Hg concentrations in the boreholes had significantly positive correlations with temperatures and CO (a traditional coal-fire index gas) contents, implying that Hg has the potential to serve as an index gas to monitor the occurrences of underground coal fires in mining goafs.
内蒙古乌达煤田遭受了半个多世纪的严重煤炭火灾。自上个十年以来,已经开展了灭火项目来抑制煤火,但仍有零星的地表火发生,地下火更为普遍。在这里,我们使用带有改进入口的实时 RA-915M 汞分析仪来监测从设计用于探测和控制地下煤火的钻孔中排放的烟雾中的气态 Hg 浓度。同时,还使用离线方法收集烟雾并分析包括 CO、CO、CH、CH、CH 和 CH 在内的气体含量。结果表明,钻孔烟雾中的气态 Hg 浓度范围为 6.42±0.73 至 123.53±34.66ng/m,平均值为 49±44ng/m。我们认为,主要是燃烧或闷烧的煤量导致地下煤火烟雾 Hg 浓度的巨大变化。钻孔周围近地表空气中的气态 Hg 浓度范围为 2.38±0.28 至 13.10±0.97ng/m,平均值为 6.68±3.09ng/m。它们高于在黄河附近背景点测量的环境空气中的 Hg 浓度(<2ng/m),这表明地下煤火是一个重要的 Hg 污染源。重要的是,我们发现钻孔中的气态 Hg 浓度与温度和 CO(一种传统的煤火指标气体)含量呈显著正相关,这表明 Hg 有可能作为监测采空区地下煤火发生的指标气体。