Han Lanfang, Gao Bo, Zhou Yang, Xu Dongyu, Gao Li, Yu Hui, Wang Shiyan
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing, 100038, China.
State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing, 100875, China.
Environ Sci Pollut Res Int. 2016 Oct;23(20):20772-20782. doi: 10.1007/s11356-016-7306-9. Epub 2016 Jul 30.
The South-to-North Water Diversion Project has aroused widespread concerns about the potential ecological risks posed by the project, especially for the Miyun Reservoir (MYR). The potential release risk of metals from the flooded riparian soils into MYR after water impoundment is one of key scientific problems. In this study, riparian soil samples were collected considering three vertical heights (130, 140, and 145 m) and four types of land uses in the MYR areas, namely, forestland, grassland, wasteland, and recreational land. We analyzed soils texture, the content and chemical fractionations of seldom monitored trace elements (SMTEs): Li, Be, B, V, Co, Ni, Ga, Sn, Sb, Tl, and Bi). Results showed that the four types of soils in MYR had the similar textures, while recreational land showed significantly higher contents of Ni and V. Additionally, there were no significant differences found for most SMTEs (except for V) at different vertical heights in each soil type, while the concentrations of V at 140 and 145 m in forestland and recreational land were significantly higher than those at 130 m. However, a comprehensive evaluation of potential ecological risk (contamination factor (CF), modified degree of contamination (mCd), and geoaccumulation factor (I )) consistently indicated the insignificant contaminations of all SMTEs in MYR soils before water impoundment. The Community Bureau of Reference (BCR) sequential extraction results showed that the chemical fractionations of SMTEs were independent of land use patterns and vertical heights. Co in reducible fractions and Ni were identified as the candidates which had potential to release into MYR when the lands were submerged. Principal component analysis (PCA) and cluster analysis (CA) results suggested that a portion of V, Co, and Ni may originate from anthropogenic activities, and the coal combustion was possibly the main anthropogenic source. The findings of this work would provide valuable information on the environment management of MYR and offer a reference for the investigation on the effect of water impoundment on potential release risk of SMTEs in MYR.
南水北调工程引发了人们对该工程潜在生态风险的广泛关注,尤其是对密云水库(MYR)的影响。蓄水后淹没的河岸土壤中金属向密云水库的潜在释放风险是关键科学问题之一。在本研究中,考虑了密云水库地区的三个垂直高度(130、140和145米)以及四种土地利用类型,即林地、草地、荒地和休闲用地,采集了河岸土壤样本。我们分析了土壤质地、很少监测的微量元素(SMTEs):锂、铍、硼、钒、钴、镍、镓、锡、锑、铊和铋的含量及化学形态。结果表明,密云水库的四种土壤质地相似,而休闲用地的镍和钒含量显著更高。此外,每种土壤类型在不同垂直高度下,大多数SMTEs(除钒外)没有显著差异,而林地和休闲用地中140米和145米处的钒浓度显著高于130米处。然而,对潜在生态风险的综合评估(污染因子(CF)、修正污染程度(mCd)和地累积指数(I))一致表明,蓄水前密云水库土壤中所有SMTEs的污染程度均不显著。欧盟委员会参考物质局(BCR)连续提取结果表明,SMTEs的化学形态与土地利用模式和垂直高度无关。可还原态的钴和镍被确定为土地被淹没时可能释放到密云水库中的候选元素。主成分分析(PCA)和聚类分析(CA)结果表明,部分钒、钴和镍可能源自人为活动,煤炭燃烧可能是主要人为来源。本研究结果将为密云水库的环境管理提供有价值的信息,并为研究蓄水对密云水库中SMTEs潜在释放风险的影响提供参考。