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Interactions of polycyclic aromatic hydrocarbons with mineral surfaces

机译:多环芳烃与矿物表面的相互作用

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摘要

The toxicity and ubiquitousness of PAHs within different terrestrial environments has been an increasing cause for concern amongst environmental scientists in the last decades, in particular regarding their transport within the soil. In an attempt to understand the role of pure inorganic phases in PAH-mobility; experiments exposing mineral soil components with low organic matter content to a PAH-representative were carried out. The systems consisted of four different mineral phases (quartz sand, hematite, iron coated quartz sand and montmorillonite) which were individually exposed to naphthalene in electrolyte solutions prepared at increasing ionic strengths (NaNO3: 0.001 M; 0.01 M; 0.1 M) and pH (4.0 and 5.5). All experiments were conducted over at 24 reaction intervals and at ambient temperature conditions.Mineral geosorbents are traditionally known to be poor PAH-scavengers; in particular when compared to organic, high surface area materials such as activated carbons. On this basis, a preliminary validation experiment (Proof of Concept Experiment) was conducted to test the sensitivity of the selected extraction method (SPME) under complete uptake (activated carbon) and very low uptake (quartz sand) conditions. By extracting and analysing the supernatant after 24 hr of exposure of both sorbents to naphthalene under identical conditions it was concluded that SPME was a feasible extraction technique, yielding good reproducibility (n=3, inter-day RSD%= 11.18% ) even at very low PAH concentrations (0.2 µg / L). The final concentration of naphthalene in the sample supernatant after 24 hours was determined by GC-FID. All samples were extracted using the Solid Phase Microextraction method developed during the Proof of Concept which allowed the rapid extraction of naphthalene in the headspace HS-SPME (extraction time = 3 minutes) using temperature control and ultrasonication as means of agitation. Each sample set included triplicates of blanks and samples as well as calibration standards (in duplicate where possible)Out of the four minerals, only quartz sand and hematite showed a slight tendency towards naphthalene removal from solution; a finding which correlated well with increasing ionic strength. The other two minerals did not show any such trend and the results were deemed inconclusive. In regards to the results for quartz and hematite; the detected uptake was found to be below the sensitivity of the current SPME extraction method according to the error analysis carried out by comparing the sample and blank means whilst accounting for error equal to 1σ. The overlapping of both means in the majority of the samples indicated that both averages were too close to be accurately resolved (due to very low naphthalene uptake). Modifications to the SPME method could improve the reproducibility and decrease the spread of the data; however, this measure would only guarantee higher statistical confidence (95 %) and not higher naphthalene uptake by these minerals. These observations lead to the conclusion that naphthalene was being salted out of solution rather than being removed by sorption; and under these experimental conditions it would not have been possible to detect any real PAH-mineral interaction. In view of this outcome, a different approach was attempted in order to detect surface reactions between the minerals and naphthalene. A series of preliminary (qualitative) surface analysis (AFM, XPS and ATR-FTIR) on pre-loaded mineral specimens were carried out in air at ambient temperature conditions. No naphthalene was positively identified on the surfaces of the studied sorbents. Factors such as molecular size, sorbents characteristics (i.e. roughness, surface charge) and loading conditions impeded the detection of the target molecules. Innovative sample preparation protocols as well as controlled analytical conditions would need to be implemented and evaluated before this kind of analytical tool can be used. The main outcome of this research work was the successful adaptation of SPME to the rapid extraction of naphthalene in electrolyte solutions at optimal and sub-optimal concentration levels; as the proof of concept preliminary experiment showed.
机译:在过去的几十年中,PAHs在不同陆地环境中的毒性和普遍存在已引起越来越多的环境科学家的关注,尤其是关于它们在土壤中的运输。试图了解纯无机相在PAH流动性中的作用;进行了将有机物含量低的矿物土壤成分暴露于PAH代表的实验。该系统由四种不同的矿物相(石英砂,赤铁矿,铁涂层的石英砂和蒙脱石)组成,分别在离子强度(NaNO3:0.001 M; 0.01 M; 0.1 M)和pH( 4.0和5.5)。所有实验都是在24个反应间隔和环境温度条件下进行的。传统上,矿物地质吸附剂是不良的PAH清除剂。特别是与有机高表面积材料(例如活性炭)相比时。在此基础上,进行了初步验证实验(概念验证实验),以测试所选提取方法(SPME)在完全吸收(活性炭)和极低吸收(石英砂)条件下的敏感性。通过在相同条件下将两种吸附剂暴露于萘24小时后,对上清液进行提取和分析,得出的结论是SPME是一种可行的提取技术,即使在非常高的温度下也具有良好的重现性(n = 3,日间RSD%= 11.18%)。低PAH浓度(0.2 µg / L)。 24小时后,样品上清液中萘的最终浓度通过GC-FID测定。所有样品均采用在概念验证期间开发的固相微萃取方法进行萃取,该方法可使用温度控制和超声作为搅拌手段在顶空HS-SPME中快速萃取萘(萃取时间= 3分钟)。每个样品组包括三份空白和样品,以及校准标准品(可能的话,一式两份)。在四种矿物中,只有石英砂和赤铁矿显示出从溶液中除去萘的轻微趋势。这一发现与增加的离子强度密切相关。其他两种矿物没有显示出任何这种趋势,因此结果没有定论。关于石英和赤铁矿的结果;根据对样品和空白均值的比较进行的误差分析,发现误差等于1σ,因此检测到的摄取量低于当前SPME提取方法的灵敏度。大多数样品中两种方法的重叠表明,这两个平均值太接近而无法准确解析(由于萘的吸收非常低)。对SPME方法的修改可以提高重现性并减少数据的传播。但是,该措施只能保证更高的统计置信度(95%),而不能保证这些矿物对萘的吸收更高。这些观察得出的结论是,萘是从溶液中盐析出来的,而不是通过吸附去除的。在这些实验条件下,不可能检测到任何真实的PAH-矿物相互作用。鉴于此结果,尝试了一种不同的方法以检测矿物与萘之间的表面反应。在环境温度下的空气中,对预加载的矿物样品进行了一系列初步(定性)表面分析(AFM,XPS和ATR-FTIR)。在所研究的吸附剂表面上未鉴定出萘。诸如分子大小,吸附剂特性(即粗糙度,表面电荷)和负载条件等因素阻碍了目标分子的检测。在使用这种分析工具之前,需要实施和评估创新的样品制备规程以及受控的分析条件。这项研究工作的主要成果是成功地使SPME适应了在最佳和次最佳浓度水平下电解质溶液中萘的快速萃取。正如概念验证初步实验所示。

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