Sun Hong-Fei, Li Yong-Hu, Ji Yan-Fang, Yang Lin-Sheng, Wang Wu-Yi
Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.
Huan Jing Ke Xue. 2009 Apr 15;30(4):1159-65.
Ores, waste tailings and slag, together with three typical soil profiles (natural soil profiles far from mine entrance and near mine entrance, soil profile under slag) in Chatian mercury mining deposit (CMD), western Hunan province were sampled and their concentrations of mercury (Hg), arsenic (As), lead (Pb), cadmium (Cd), zinc (Zn) were determined by HG-ICP-AES and ICP-MS. Enrichment factor and correlation analysis were taken to investigate the origins, distribution and migration of Hg, as well as other heavy metals in the CMD. The results show that Hg is enriched in the bottom of the soil profile far from mine entrance but accumulated in the surface of soil profiles near mine entrance and under slag. The soil profiles near mine entrance and under slag are both contaminated by Hg, while the latter is contaminated more heavily. In the soil profile under slag, Hg concentration in the surface soil, Hg average concentration in the total profile, and the leaching depth of soil Hg are 640 microg x g(-1), (76.74 +/- 171.71) microg x g(-1), and more than 100 cm, respectively; while 6.5 microg x g(-1), (2.74 +/- 1.90) microg x g(-1), and 40 cm, respectively, are found in the soil profile near mine entrance. Soil in the mercury mine area is also polluted by Cd, As, Pb, Zn besides metallogenic element Hg, among which Cd pollution is relatively heavier than others. The mobility of the studied heavy metals in soil follows the order as Hg > Cd > As > Zn approximately equal to Pb. The leaching depth of the heavy metals is influenced by total concentration in the surface soil and soil physico-chemical parameters. The origins, distribution and migration of heavy metals in soil profile in the mining area are related to primary geological environment, and strongly influenced by human mining activities.
对湘西茶田汞矿(CMD)的矿石、尾矿和矿渣,以及三种典型土壤剖面(远离矿井口和靠近矿井口的天然土壤剖面、矿渣下的土壤剖面)进行了采样,并采用氢化物发生电感耦合等离子体发射光谱法(HG-ICP-AES)和电感耦合等离子体质谱法(ICP-MS)测定了其中汞(Hg)、砷(As)、铅(Pb)、镉(Cd)、锌(Zn)的含量。通过富集因子和相关性分析,研究了茶田汞矿中汞以及其他重金属的来源、分布和迁移情况。结果表明,汞在远离矿井口的土壤剖面底部富集,但在靠近矿井口和矿渣下的土壤剖面表层累积。靠近矿井口和矿渣下的土壤剖面均受到汞污染,而后者污染更严重。在矿渣下的土壤剖面中,表层土壤汞含量、全剖面汞平均含量以及土壤汞的淋溶深度分别为640μg·g⁻¹、(76.74±171.71)μg·g⁻¹和超过100cm;而在靠近矿井口的土壤剖面中,上述数值分别为6.5μg·g⁻¹、(2.74±1.90)μg·g⁻¹和40cm。汞矿区土壤除了成矿元素汞外,还受到镉、砷、铅、锌污染,其中镉污染相对较重。研究的重金属在土壤中的迁移性顺序为Hg>Cd>As>Zn≈Pb。重金属的淋溶深度受表层土壤总浓度和土壤理化参数影响。矿区土壤剖面中重金属的来源、分布和迁移与原生地质环境有关,并受人类采矿活动的强烈影响。