Anhui Province Engineering Laboratory for Mine Ecological Remediation, School of Life Sciences, Anhui University, Hefei, 230601, China.
State Grid Anhui Electric Power Corporation Research Institute, Hefei, 230601, China.
Environ Geochem Health. 2023 May;45(5):2241-2262. doi: 10.1007/s10653-022-01337-2. Epub 2022 Aug 2.
Chromium (Cr), one of the prime hazardous trace elements in coals, may engender adverse effects on eco-environment and threaten human health during utilization of coal. Based on the samples obtained in our laboratory and published literature, the abundance and modes of occurrence of Cr in Chinese coals, and the environmental impacts associated with coal-fired power plants (CFPPs) were elucidated in this study. With a total of 1397 sets of data, the mean concentration of Cr in Chinese coals was calculated as 21.33 μg/g by the "reserve-concentration" weighted calculation method. Spatially, the average Cr contents increased gradually from North China to South China. Temporally, coals from T, E-N and P were relatively enriched in Cr compared to the other geological time. The Cr concentration in coal varied with different coal ranks. The geological factors accounted for Cr enrichment in coals could be divided into the primary, secondary and epigenetic processes. Higher percentages of organically Cr occurred in low-rank coals, while inorganically associated Cr was mainly found in clay minerals. After coal combustion, most of Cr was enriched in solid wastes (e.g., fly ash and bottom ash). The leaching of Cr from solid wastes in the rainy season (especially acid rain) needs to be a concern for CFPPs. It was estimated that the atmospheric emission of Cr from CFPPs increased annually from 2015 to 2019 and reached approximately 159 tons in 2019.
铬(Cr)是煤中主要的有害痕量元素之一,在煤的利用过程中可能会对生态环境产生不利影响,并威胁人类健康。本研究基于实验室采集的样品和已发表的文献,阐述了中国煤中 Cr 的丰度、赋存形态以及燃煤电厂(CFPPs)的环境影响。通过对 1397 组数据的分析,采用“储量-浓度”加权计算方法,计算得出中国煤中 Cr 的平均浓度为 21.33μg/g。从空间上看,Cr 的平均含量从华北到华南逐渐增加。从时间上看,与其他地质时期相比,T、E-N 和 P 时期的煤中 Cr 含量相对较高。煤中 Cr 的浓度随煤级的不同而变化。导致煤中 Cr 富集的地质因素可分为原生、次生和后生作用过程。低煤级煤中有机结合态 Cr 的比例较高,而无机结合态 Cr 主要存在于粘土矿物中。煤燃烧后,大部分 Cr 富集在固体废物(如飞灰和底灰)中。雨季(尤其是酸雨)中固体废物中 Cr 的浸出需要引起 CFPPs 的关注。据估计,2015 年至 2019 年,CFPPs 向大气排放的 Cr 量逐年增加,2019 年达到约 159 吨。