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苯和萘在(半)干旱沿海土壤中随盐度和温度的变化的吸附作用。

Sorption of benzene and naphthalene on (semi)-arid coastal soil as a function of salinity and temperature.

机构信息

Ecohydrology Research Group and Water Institute, Department of Earth and Environmental Sciences, University of Waterloo, 200 University Avenue West, Waterloo, Ontario N2L 3G1, Canada; Department of Civil and Architectural Engineering, College of Engineering, Qatar University, P. O. Box 2713, Doha, Qatar.

Ecohydrology Research Group and Water Institute, Department of Earth and Environmental Sciences, University of Waterloo, 200 University Avenue West, Waterloo, Ontario N2L 3G1, Canada.

出版信息

J Contam Hydrol. 2018 Dec;219:61-71. doi: 10.1016/j.jconhyd.2018.11.001. Epub 2018 Nov 3.

Abstract

Considerable activities from the oil and natural gas sector have risen some concerns about the pollution of soil and groundwater by petroleum hydrocarbons (PHCs) in (semi)-arid coastal regions. The understanding of the fate and transport of PHCs in these regions is therefore necessary to develop strategies for remediation. To quantify the sorption rates of PHCs in (semi)-arid coastal soil environments, we conducted a series of controlled-laboratory batch experiments under variable temperature and salinity conditions. The soil samples were collected from the eastern coast of Qatar which is near the two largest off-shore oil and natural gas fields of the country (North Gas and Al-Shaheen Oil Fields), and the volatile benzene and naphthalene were used as PHCs. The characterization of soil samples showed sand classification with the texture class of sabkha and saline beach sandy soils with calcite as potential dominant mineral. The concentrations of dissolved chloride and sodium were found to be high (> 400 mg L) with a chloride-to‑sodium ratio of about 1.7. The results of sorption experiments showed that the rates of naphthalene sorption were more than for benzene, where the initial aqueous concentrations of benzene and naphthalene were reduced at equilibrium due to sorption by about 14-25% and 65-79%, respectively. This difference was attributed mainly to the organic carbon-water partitioning coefficient which is higher for naphthalene. The sorption rate experiments showed that sorption was stronger for benzene under higher salinity and lower temperature conditions. The sorption of naphthalene was not affected by the change in salinity but increased by 18% when the temperature decreased from 35 to 5 °C. A sorption kinetic model was also applied to define the sorption behavior of benzene and naphthalene for the coastal soil collected in Qatar and the best fits were achieved with the Langmuir sorption isotherm.

摘要

在(半)干旱沿海地区,石油和天然气部门的大量活动引起了人们对石油碳氢化合物(PHC)污染土壤和地下水的一些关注。因此,为了制定修复策略,有必要了解这些地区 PHC 的归宿和迁移。为了量化(半)干旱沿海土壤环境中 PHC 的吸附速率,我们在不同温度和盐度条件下进行了一系列控制实验室批量实验。土壤样品取自卡塔尔东海岸,该地区靠近该国最大的两个海上石油和天然气田(北气田和沙欣油田),挥发性苯和萘被用作 PHC。土壤样品的特征表明,其沙分类为盐沼和盐滩沙质土,方解石为潜在主要矿物。发现溶解的氯化物和钠的浓度很高(>400mg/L),氯化物与钠的比例约为 1.7。吸附实验的结果表明,萘的吸附速率大于苯,由于吸附作用,苯和萘的初始水相浓度在平衡时分别降低了约 14-25%和 65-79%。这种差异主要归因于萘的有机碳-水分配系数较高。吸附速率实验表明,在较高盐度和较低温度条件下,苯的吸附更强。萘的吸附不受盐度变化的影响,但当温度从 35°C 降至 5°C 时,吸附增加了 18%。还应用了吸附动力学模型来定义在卡塔尔采集的沿海土壤中苯和萘的吸附行为,Langmuir 吸附等温线得到了最佳拟合。

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