Wang Jianxu, Feng Xinbin, Anderson Christopher W N, Qiu Guangle, Bao Zhengduo, Shang Lihai
State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, China; Graduate University of Chinese Academy of Sciences, Beijing, China.
Environ Toxicol Chem. 2014 Sep;33(9):2147-55. doi: 10.1002/etc.2664. Epub 2014 Aug 1.
The authors studied the concentration of heavy metals and mercury fractionation in contaminated soil in 2 agricultural land use systems (paddy rice and dry land) at the Wanshan mercury mine in China. The average concentrations of chromium, lead, copper, nickel, and zinc were generally lower in paddy rice soil relative to corn field soil. Soil under corn field production was slightly contaminated with lead (22-100 mg/kg), copper (31-64 mg/kg), and nickel (22-76 mg/kg) and moderately contaminated with zinc (112-635 mg/kg). In both soils, correlation of these metals with the titanium concentration in the soil indicates a geogenic origin for each metal (lead, r = 0.48; copper, r = 0.63; nickel, r = 0.47; zinc, r = 0.48). The mercury and antimony concentration in soil was high under both cropping systems, and future remediation efforts should consider the potential environmental risk presented by these metals. The concentration of bioavailable mercury in soil ranged from 0.3 ng/g to 11 ng/g across the 2 cropping systems. The majority of mercury (>80%) was associated with organic matter and the residual fraction. However, soil under paddy rice production exhibited a significantly lower concentration of Fe/Mn oxide-bound mercury than that under corn field production. This may be a function of the reduction of Fe/Mn oxides in the paddy rice soil, with the subsequent release of adsorbed metals to the soil solution. Sequential change from corn field to paddy rice production, as practiced in Wanshan, should therefore be avoided. Mercury adsorbed to Fe/Mn oxides in corn field soil potentially could be released into the soil solution and be made available for biomethylation under the flooded water management conditions of a rice paddy.
作者研究了中国万山汞矿2种农业土地利用系统(稻田和旱地)中受污染土壤的重金属浓度和汞的形态分布。相对于玉米地土壤,稻田土壤中铬、铅、铜、镍和锌的平均浓度总体较低。玉米地生产下的土壤受到轻度铅污染(22 - 100毫克/千克)、铜污染(31 - 64毫克/千克)和镍污染(22 - 76毫克/千克),并受到中度锌污染(112 - 635毫克/千克)。在这两种土壤中,这些金属与土壤中钛浓度的相关性表明每种金属的地质成因(铅,r = 0.48;铜,r = 0.63;镍,r = 0.47;锌,r = 0.48)。两种种植系统下土壤中的汞和锑浓度都很高,未来的修复工作应考虑这些金属带来的潜在环境风险。两种种植系统下土壤中生物可利用汞的浓度范围为0.3纳克/克至11纳克/克。大部分汞(>80%)与有机质和残渣态相关。然而,稻田生产下的土壤中与铁/锰氧化物结合的汞浓度明显低于玉米地生产下的土壤。这可能是由于稻田土壤中铁/锰氧化物的还原作用,随后吸附的金属释放到土壤溶液中。因此,应避免像万山那样从玉米地生产依次转变为稻田生产。玉米地土壤中吸附在铁/锰氧化物上的汞在稻田淹水管理条件下可能会释放到土壤溶液中并可用于生物甲基化。