College of Geography and Environmental Science, National Demonstration Center for Experimental Environment and Planning Education, Henan University, Kaifeng 475004, Henan, China; State Key Laboratory of Cryosphere Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, China.
College of Geography and Environmental Science, National Demonstration Center for Experimental Environment and Planning Education, Henan University, Kaifeng 475004, Henan, China.
Environ Pollut. 2024 Apr 1;346:123498. doi: 10.1016/j.envpol.2024.123498. Epub 2024 Feb 9.
Heavy metals present a substantial threat to both the environment and human health. Considering the delicate ecological equilibrium of the Tibetan Plateau (TP) and its heightened susceptibility to anthropogenic impacts, scholarly attention has progressively turned toward the examination of heavy metal pollution within the plateau's environment. In this study, we conducted a comprehensive analysis of various heavy metals (As, Cr, Co, Ni, Cu, Mo, Cd, Pb, and Sb), utilizing topsoil samples collected from the TP during the period of 2018-2021. Additionally, snow and cryoconite samples obtained from TP glaciers during the same timeframe were also subjected to analysis. The results indicate elevated concentrations of total heavy metals in the eastern and western TP (328.7 μg/g), as opposed to the central and southern TP (145.7 μg/g). Most heavy metals exhibit a consistent spatial distribution pattern. High Enrichment Factors (EFs) and Geoaccumulation Index (I) values for As and Cd suggest their enrichment in TP topsoil. Receptor modeling identified three primary sources of heavy metals within the topsoil: industrial sources (42.3%), inherent natural sources within the surface soil (20.6%), and vehicular emissions (14.2%). Substantial differences in heavy metal concentrations and spatial distribution were observed between the topsoil and the glacial snow-cryoconite matrix. The prominent presence of Sb in the snow-cryoconite matrix, in contrast to its low abundance in the topsoil, indicates distinct source influences of long-range transported materials between the two environments. Our inference suggests that the influence of heavy metals from distant pollutants undergo mixing and dilution in the topsoil due to the presence of local indigenous heavy metals, although such influence is notably observed on the glacier surface of the TP. Consequently, this underscores the significant impact of long-range transported sources on heavy metals, surpassing the influence of local TP soils, to the alpine glaciers and even other atmospheric sediments in Tibetan Plateau.
重金属对环境和人类健康构成了重大威胁。考虑到青藏高原(TP)生态环境的脆弱性及其对人为影响的高度敏感性,学者们越来越关注高原环境中的重金属污染问题。在这项研究中,我们对 2018 年至 2021 年期间从青藏高原采集的表层土壤样本进行了各种重金属(As、Cr、Co、Ni、Cu、Mo、Cd、Pb 和 Sb)的综合分析。此外,还对同一时期从青藏高原冰川采集的雪和冰核样本进行了分析。结果表明,青藏高原东部和西部的总重金属浓度较高(328.7μg/g),而中部和南部的总重金属浓度较低(145.7μg/g)。大多数重金属表现出一致的空间分布模式。As 和 Cd 的高富集因子(EF)和地质累积指数(I)值表明它们在青藏高原表层土壤中富集。受体模型确定了表层土壤中重金属的三个主要来源:工业源(42.3%)、表层土壤固有天然源(20.6%)和车辆排放源(14.2%)。表层土壤和冰川雪冰核基质之间重金属浓度和空间分布存在显著差异。Sb 在雪冰核基质中的显著存在,而在表层土壤中含量较低,表明这两个环境之间存在长距离传输物质的不同源影响。我们的推断表明,由于当地土著重金属的存在,远距离污染物中的重金属在表层土壤中发生混合和稀释,尽管在青藏高原的冰川表面可以明显观察到这种影响。因此,这突显了长距离传输源对重金属的重大影响,超过了当地青藏高原土壤对高山冰川甚至其他大气沉积物的影响。