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我国3种自然土壤中稀有金属的化学形态分布特征研究
引用本文:文方,姚娜,周友亚,谷庆宝,李发生,侯红.我国3种自然土壤中稀有金属的化学形态分布特征研究[J].环境科学,2011,32(5):1422-1429.
作者姓名:文方  姚娜  周友亚  谷庆宝  李发生  侯红
作者单位:中国环境科学研究院土壤污染与控制研究室,北京,100012
基金项目:中央级公益性科研院所基本科研业务专项(2007KYYW03);科技部科技基础性工作专项项目(2007FY240200);环保公益性行业科研专项(201009032-01);环保公益性行业科研专项经费项目(200809095)
摘    要:以我国3种典型土壤黑土、潮土和红壤为研究对象,在相对清洁未扰动自然土壤区域采集了土壤的剖面样品,分析了土壤中的稀有金属银(Ag)、铋(Bi)、铟(In)、锡(Sn)的含量水平,利用元素富集率(ER)的垂向分布探讨了外源污染对金属含量的影响,并采用连续逐级提取法研究了土壤中稀有金属的化学形态分布特征,用金属可交换态和碳酸...

关 键 词:自然土壤  稀有金属  化学形态  元素富集率  迁移性
收稿时间:2010/10/12 0:00:00
修稿时间:1/4/2011 12:00:00 AM

Chemical Speciation of Rare Metals in Three Natural Soils of China
WEN Fang,YAO N,ZHOU You-y,GU Qing-bao,LI Fa-sheng and HOU Hong.Chemical Speciation of Rare Metals in Three Natural Soils of China[J].Chinese Journal of Environmental Science,2011,32(5):1422-1429.
Authors:WEN Fang  YAO N  ZHOU You-y  GU Qing-bao  LI Fa-sheng and HOU Hong
Institution:Department of Soil Pollution Control, Chinese Research Academy of Environmental Science, Beijing 100012, China. wenfang0718@163.com
Abstract:Soil profile samples of isohumosol, primosol, and ferrosol were obtained in relatively clean areas of China. Concentrations and chemical speciation of rare metals e.g., Ag (Silver), Bi (Bismuth), In (Indium) and Sn (Tin)] were determined, in which sequential extraction was used to fraction metals. Vertical distributions of elemental enrichment ratios (ERs) were used to study the anthropogenic influence. The mobility of metals was characterized by the sum of exchangeable form and carbonate-bound form. Average concentrations of Ag, Bi, In and Sn in the A horizon were (0.14 +/- 0.01), (0.49 +/- 0.09), (0.050 +/- 0.01), and (2.8 +/- 0.9) mg x kg(-1), respectively. The ERs were close to 1. Average distributions of metal speciation were: Ag, residual (65.8%) > H202-extractable organically bound (H2O2-Org) (25.9%) > Amorphous metal oxide-bound (am-MeOx) (4.2%) > Metal-organic complex-bound (Me-Org) approximately Crystalline Fe oxide-bound (cr-FeOx) (2.0%); Bi, residual (29.2%) > H2O2-Org (27.1%) > cr-FeOx (22.7%) > am-MeOx (18.8%) > Me-Org (1.0%) > carbonate-bound (0.9%) > easily reducible metal oxide-bound (re-MeOx) (0.3%); In, residual (67.8%) > cr-FeOx (17.0%) > am-MeOx (6.8%) > H2O2-Org (6.0%) > carbonate-bound (1.4%) > Me-Org (1.0%); Sn, residual (58.1%) > am-MeOx (23.0%) > cr-FeOx (15.6%) > H2O2-Org (1.8%) > Me-Org (1.1%) > exchangeable approximately carbonate-bound (0.2%). the results indicated that the exogenous elements enrichment was deficiency to minimal, and the concentrations of the rare metals were close to background values of soil in studied areas. Rare metals were stable in soils. The mobility of metals was in the order In > Bi > Sn > Ag.
Keywords:natural soil  rare metals  chemical speciation  elemental enrichment ratio  mobility
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