Cuicui Qi

Assessment and distribution of antimony in soils around three coal mines, Anhui, China.

ABSTRACT Thirty-three soil samples were collected from the Luling, Liuer, and Zhangji coal mines in the Huaibei and Huainan areas of Anhui Province, China. The samples were analyzed for antimony (Sb) by inductively coupled plasma-optical emission spectrometry (ICP-OES) method. The average Sb content in the 33 samples was 4 mg kg−1, which is lower than in coals from this region (6.2 mg kg−1). More than 75% of the soils sampled showed a significant degree of Sb pollution (enrichment factors [EFs] 5–20). The soils collected near the gob pile and coal preparation plant were higher in Sb content than those collected from residential areas near the mines. The gob pile and tailings from the preparation plant were high in mineral matter content and high in Sb. They are the sources of Sb pollution in surface soils in the vicinity of coal mines. The spatial dispersion of Sb in surface soil in the mine region shows that Sb pollution could reach out as far as 350 m into the local environment conditions. Crops in rice paddies may adsorb some Sb and reduce the Sb content in soils from paddyfields. Vertical distribution of Sb in two soil profiles indicates that Sb is normally relatively immobile in soils. IMPLICATIONS This work was carried out to analyze the pollution situation and environmental distribution of Sb in three important mines in Anhui Province of China. A detailed concentration analysis of Sb was used to indicate the anthropogenic source of human operation such as coal mining and depositing, coal cleaning, and electricity generation by coal power plants in the mine region. The investigation provides special useful information on the environmental behavior characteristics of Sb for environmental scientists and policy-makers.

Sequential Solvent Extraction for Forms of Antimony in Five Selected Coals

Abundance of antimony in bulk samples has been determined in five selected coals, three coals from Huaibei Coalfield, Anhui, China, and two from the Illinois Basin in the United States. The Sb abundance in these samples is in the range of 0.11–0.43 μg/g. The forms of Sb in coals were studied by sequential solvent extraction. The six forms of Sb are water soluble, ion changeable, organic matter bound, carbonate bound, silicate bound, and sulfide bound. Results of sequential extraction show that silicate‐bound Sb is the most abundant form in these coals. Silicate‐ plus sulfide‐bound Sb accounts for more than half of the total Sb in all coals. Bituminous coals are higher in organic matter–bound Sb than anthracite and natural coke, indicating that the Sb in the organic matter may be incorporated into silicate and sulfide minerals during metamorphism.