Production of Ultra Clean Coal

化学 硅酸铝 氢氟酸 灰化 黄铁矿 浸出(土壤学) 矿物 无机化学 水溶液 矿物学 有机化学 催化作用 土壤水分 地质学 物理 量子力学 土壤科学
作者
Karen M. Steel,John Besida,Thomas A. O’Donnell,David G. Wood
出处
期刊:Fuel Processing Technology [Elsevier BV]
卷期号:70 (3): 171-192 被引量:114
标识
DOI:10.1016/s0378-3820(01)00171-0
摘要

The mineral matter in an Australian black coal has been isolated using a low-temperature ashing (LTA) procedure. This LTA procedure is a modification of the Australian Standard for LTA at 370°C, and alleviates adverse effects to the minerals caused by the heat of combustion. The leaching behaviour of the mineral matter towards aqueous HCl and hydrofluoric acid (HF) is presented. HCl can dissolve simple compounds such as phosphates and carbonates, yet it cannot completely dissolve the clays. HF reacts with almost every mineral in the mineral matter, except pyrite, and most of the reaction products are water soluble. However, at HF concentrations greater than that required to dissolve the aluminosilicate compounds in the mineral matter, insoluble compounds form. These compounds include CaF2, MgF2 and a compound containing Na, which is believed to be NaAlF4. It is proposed that HF reacts preferentially with the aluminosilicates in the mineral matter to form largely AlF2+, AlF3 and SiF4, and that the concentrations of free fluoride (F−) and AlF4− are not high enough to complex cations such as Ca2+, Mg2+ and Na+. When the mineral matter is treated with HF concentrations greater than that required to dissolve all of the aluminosilicates, AlF3, AlF4− and SiF62− form, the concentration of F− is high enough to complex Ca2+ and Mg2+ and form insoluble CaF2 and MgF2, and the concentration of AlF4− is high enough to complex Na+ and form insoluble NaAlF4. This work has application toward the development of a process for producing Ultra Clean Coal with less than 0.1% by weight mineral matter.
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