Distribution and enrichment characteristics of trace elements during underground coal gasification
LI Yulong, LIANG Dongyu, SHENG Xunchao, WANG Zhangqing, LIANG Jie
2018, 37(04):
1590-1598.
doi:10.16085/j.issn.1000-6613.2017-1450
Abstract
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Underground coal gasification technology is a situ mining technology,leaving the produced pollutants in the ground. The grid-based sampling of gasification zone under different process conditions was carried out by oxygen-water gasification model test. The residue of content of zinc,arsenic,lead,chromium,nickel and mercury was analyzed by inductively coupled plasma mass spectrometry(ICP-MS) and atomic fluorescence spectrometry. Finally,the migration and enrichment coefficients were used to evaluate the migration and enrichment characteristics of trace elements. Results showed that the total amount of trace element residues decreases with the increase of oxygen concentration of the process conditions. In the oxidation zone,the residual amount of chromium and nickel was very high. The residual amount of copper and lead in the three regions was very low. The residual amount of zinc in the three regions was the highest,and the residual amount decreases with the increase of oxygen concentration in the three regions,and is easy to remain in the reducing area. Arsenic is enriched in three regions,and its residuals increase with the incresase of oxygen concentration in three regions. Due to the higer temperature at the outlet,the residual amount of mercury in the three areas was the least,and there was no obvious regularity. The average content of trace elements Hg,As,Zn and Cr in the residue of gasification channel was much higher than that in raw coal,while that of nickel,copper and lead was less than that of raw coal. By the method of the relative enrichment factor and the average residual ratio analysis,it is carried out that the relative enrichment factors of Cr,Ni,Zn,As,Hg are all less than 1. The residual rates of Zn,As and Hg are more than 100%. Cr and Ni are from 50% to 100%. The relative enrichment factors of Cu and Pb in three regions are less than 1. The residual rates are less than 50%.