首页> 美国卫生研究院文献>International Journal of Environmental Research and Public Health >The Potential Environmental Impact of PAHs on Soil and Water Resources in Air Deposited Coal Refuse Sites in Niangziguan Karst Catchment Northern China
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The Potential Environmental Impact of PAHs on Soil and Water Resources in Air Deposited Coal Refuse Sites in Niangziguan Karst Catchment Northern China

机译:中国北方娘子关喀斯特流域空气沉积煤垃圾场中多环芳烃对土壤和水资源的潜在环境影响

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摘要

Long-term deposition of coal spoil piles may lead to serious pollution of soil and water resources in the dumping sites and surrounding areas. Karst aquifers are highly sensitive to environmental pollution. In this study, the occurrence and release/mobilization of polycyclic aromatic hydrocarbons (PAHs) in coal waste and coal spoils fire gas mineral (CSFGM) were evaluated by field and indoor investigations at Yangquan city, one of the major coal mining districts in the karst areas of northern China. Field investigations showed that dumping of coal waste over decades has resulted in soil and water pollution via spontaneous combustion and leaching of coal spoil piles. Indoor analysis revealed that the 2-ring and 3-ring PAHs contribute to 65–80% of the total PAHs in coal spoils, with naphthalene (Nap), Chrysene (Chr), and Phenanthrene (Phe) as the dominant compounds. Based on a heating/burning simulation experiment, the production of PAHs is temperature-dependent and mainly consists of low-ring PAHs: 2-ring, 3-ring, and part of the 4-ring PAHs. The PAHs in the leachate are light-PAHs (Nap, 20.06 ng/L; Phe, 4.76 ng/L) with few heavy-PAHs. The distribution modes of PAHs in two soil profiles suggest that the precipitation caused downward movement of PAHs and higher mobility of light-PAHs.
机译:煤渣堆的长期沉积可能导致倾倒场和周围地区的土壤和水资源受到严重污染。岩溶含水层对环境污染高度敏感。在这项研究中,通过对喀斯特主要煤矿区之一的阳泉市的野外和室内调查,对煤coal石和煤coal火矿物(CSFGM)中多环芳烃(PAHs)的发生和释放/迁移进行了评估。中国北方地区。现场调查表明,几十年来倾倒的煤waste石通过自燃和煤渣堆的浸出导致土壤和水污染。室内分析表明,二环和三环多环芳烃占煤泥中多环芳烃总量的65-80%,其中萘(Nap),ry(Chr)和菲(Phe)为主要化合物。根据加热/燃烧模拟实验,PAH的生产与温度有关,并且主要由低环PAH组成:2环,3环和部分4环PAH。渗滤液中的PAH是轻型PAH(Nap,20.06 ng / L; Phe,4.76 ng / L),重PAH很少。多环芳烃在两种土壤剖面中的分布模式表明,降水引起多环芳烃的向下运动和轻质多环芳烃的较高迁移率。

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