Sun Hou-Yun, Wei Xiao-Feng, Sun Xiao-Ming, Jia Feng-Chao, Li Duo-Jie, Li Jian
School of Water Resources and Environment, China University of Geosciences(Beijing), Beijing 100083, China.
Beijing Institute of Geology for Mineral Resources, Beijing 100012, China.
Huan Jing Ke Xue. 2021 Mar 8;42(3):1166-1176. doi: 10.13227/j.hjkx.202007200.
A total of 86 soil samples, 86 corn kernel samples, 50 tailings samples, and 33 ore rock samples were collected in reclaimed land and surrounding areas of typical vanadium-titanium magnetite tailings located in the Chengde Central Region and analyzed for 14 elements (P, Fe, Cu, Ni, Cd, Cr, Pb, Zn, Hg, Ti, Mn, and Mo) and speciation of heavy metals. This study investigated the bioaccumulation and translocation characteristics of heavy metals in a soil-maize system based on a descriptive statistical analysis, a geological accumulative index, bioconcentration factors, and a redundancy analysis. The results showed that the average accumulation index of surface soil followed an order of P > Cu > FeO > Cr > Ti > V > Ni > Mn > Cd > Zn > Mo > As > Pb > Hg, while the accumulation level of heavy metals was generally categorized as either no accumulation or moderate accumulation. Compared to China's soil environmental quality standard risk screening values (GB15618-2018), the over-standard rates of Cr and Cu were 2.32% and 1.16%, respectively. The content of Fe, Ti, As, Pb, and Mn in the corn kernels of the tailings and surrounding areas was relatively high, and the content of Mo, Ni, Cu, Zn, Cd, and Cr in the control area was relatively high. The over-standard rates of Ni, Zn, and Cu in the corn kernels were 13.61%, 13.23%, and 5.17% respectively, according to China's national food safety standard limits for contaminants in food (GB 2762-2017). The bioconcentration factors of Fe, Ti, As, Pb, and Mn in the corn kernels of the tailings and the surrounding areas were relatively higher, while the bioconcentration factors of Mo, Ni, Cu, Zn, Cd, and Cr were lower than in control area. The bioactive components of Cd accounted for 50.17%, which was the highest, followed by Ni, Zn, and Cu with average ratios of 13.61%, 13.23%, and 5.17%, respectively. Compared to the control area, the Pb, As and Hg elements in the soil samples of the reclaimed land showed a lower total amount but a higher bioavailability content and soil pH value, while the Cu and Hg elements showed a higher total amount but lower bioavailability content and soil pH value. These differences in total heavy metal concentrations, bioavailability amounts, and soil pH values made the bioconcentration intensity of As and Pb in the tailings reservoir and surrounding area relatively higher. When studying the ecological risk of heavy metal pollution or determining the remediation target value of reclaimed land in a mine tailings reservoir and the soil around the mine area, the bioavailable state limit of heavy metals should be should be taken into account as the evaluation standard.
在承德中部地区典型钒钛磁铁矿尾矿复垦地及其周边区域,共采集了86份土壤样品、86份玉米籽粒样品、50份尾矿样品和33份矿石样品,对其中14种元素(磷、铁、铜、镍、镉、铬、铅、锌、汞、钛、锰、钼)及重金属形态进行了分析。本研究基于描述性统计分析、地质累积指数、生物富集系数和冗余分析,对土壤-玉米系统中重金属的生物累积和迁移特征进行了研究。结果表明,表层土壤中重金属平均累积指数顺序为:磷>铜>氧化亚铁>铬>钛>钒>镍>锰>镉>锌>钼>砷>铅>汞,重金属累积水平总体为无累积或中度累积。与中国土壤环境质量标准风险筛选值(GB15618-2018)相比,铬和铜的超标率分别为2.32%和1.16%。尾矿及周边区域玉米籽粒中铁、钛、砷、铅和锰含量相对较高,对照区钼、镍、铜、锌、镉和铬含量相对较高。依据中国食品安全国家标准食品中污染物限量(GB 2762-2017),玉米籽粒中镍、锌和铜的超标率分别为13.61%、13.23%和5.17%。尾矿及周边区域玉米籽粒中铁、钛、砷、铅和锰的生物富集系数相对较高,钼、镍、铜、锌、镉和铬的生物富集系数低于对照区。镉的生物活性组分占比为50.17%,最高,其次是镍、锌和铜,平均占比分别为13.61%、13.23%和5.17%。与对照区相比,复垦地土壤样品中铅、砷和汞元素总量较低,但生物有效性含量和土壤pH值较高,而铜和汞元素总量较高,但生物有效性含量和土壤pH值较低。这些重金属总浓度、生物有效性含量和土壤pH值的差异,使得尾矿库及周边区域砷和铅的生物富集强度相对较高。在研究重金属污染生态风险或确定矿山尾矿库复垦地及矿区周边土壤修复目标值时,应将重金属生物有效态限值作为评价标准。