College of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing, 100083, China.
State Key Laboratory of Coal Resources and Safety Mining, China University of Mining and Technology, Beijing, 100083, China.
Environ Geochem Health. 2018 Jun;40(3):1093-1109. doi: 10.1007/s10653-017-9990-x. Epub 2017 Jun 9.
The junction area of Yunnan, Guizhou, and Sichuan provinces is the heaviest coal-burning endemic fluorosis zones in China. To better understand the pathogenicity of endemic fluorosis in this area, 87 coal samples from the late Permian outcrop or semi-outcrop coal seams were collected in eight counties of the junction area of Yunnan, Guizhou, and Sichuan provinces. The total fluorine and sulfate content, etc. in the coal was determined using combustion-hydrolysis/fluoride-ion-selective electrode method and ion chromatography, respectively. The results show that the total fluorine concentrations in the samples ranged from 44 to 382 µg g, with an average of 127 µg g. The average pH of the coals is 5.03 (1.86-8.62), and the sulfate content varied from 249 to 64,706 µg g (average 7127 µg g). In addition, the coals were medium- and high-sulfur coals, with sulfur mass fraction ranging from 0.08 to 13.41%. By heating the outcrop coals, HF release from the coal was verified quantitatively without exception, while simulated combustion directly confirmed the release of sulfuric acid (HSO). The acid in coal may be in the form of acidic sulfate ([Formula: see text]/HSO) because of a positive relationship between pH and [Formula: see text] in the acidic coal. The possible reaction mechanism would be that a chemical reaction between the acid (HSO or [Formula: see text]) and fluorine in the coal occurred, thereby producing hydrogen fluoride (HF), which would be the chemical form of fluorine released from coal under relatively mild conditions. The unique chemical and physical property of HF may bring new insight into the pathogenic mechanism of coal-burning endemic fluorosis. The phenomenon of coal-burning fluorosis is not limited to the study area, but is common in southwest China and elsewhere. Further investigation is needed to determine whether other endemic fluorosis areas are affected by this phenomenon.
滇、黔、川三省交界地区是中国燃煤型氟中毒最严重的地区。为了更好地了解该地区地方性氟中毒的发病机制,采集了滇、黔、川三省交界地区 8 个县晚二叠世出露或半出露煤层的 87 个煤样。采用燃烧水解/氟离子选择电极法和离子色谱法分别测定煤中总氟和硫酸盐等含量。结果表明,样品中总氟浓度为 44382μg/g,平均为 127μg/g。煤的平均 pH 值为 5.03(1.868.62),硫酸盐含量为 24964706μg/g(平均值为 7127μg/g)。此外,煤为中高硫煤,硫质量分数为 0.0813.41%。通过加热露头煤,定量验证了煤中 HF 的释放,而模拟燃烧直接证实了硫酸(HSO)的释放。煤中的酸可能以酸性硫酸盐([Formula: see text]/HSO)的形式存在,因为酸性煤中 pH 值与[Formula: see text]呈正相关。可能的反应机制是酸(HSO 或[Formula: see text])与煤中的氟发生化学反应,从而产生氢氟酸(HF),这将是煤在相对温和的条件下释放氟的化学形式。HF 的独特化学和物理性质可能为燃煤型地方性氟中毒的发病机制提供新的见解。燃煤型氟中毒现象不仅限于研究区,在中国西南地区和其他地区也很普遍。需要进一步调查以确定其他地方性氟中毒地区是否受到这种现象的影响。