Sorption of Phenanthrene on Agricultural Soils

• Published in: Water, air, and soil pollution air, and soil pollution, 2013-04, Vol.224 (4), p.1-11, Article 1519
• Main Authors: Soares, António Alves, Moldrup, Per, Minh, Luong Nhat, Vendelboe, Anders Lindblad, Schjonning, Per, de Jonge, Lis W.
• Format: Article
• Language: English
• Subjects: Adsorption; Agricultural ecosystems; Agricultural land; Applied sciences; Aquifers; Atmospheric Protection/Air Quality Control/Air Pollution; Carbon; Chemical contaminants; Climate Change/Climate Change Impacts; Cultivation; Culture media; Earth and Environmental Science; Environment; Environmental monitoring; Exact sciences and technology; Groundwater; Hazardous materials; Hazardous wastes; Hydrocarbons; Hydrogeology; Mobility; Organic carbon; Organic matter; Organic soils; Phenanthrene; Pollution; Polycyclic aromatic hydrocarbons; Porous media; Sediments; Soil contamination; Soil depth; Soil Science & Conservation; Soils; Sorption; Statistical analysis; Studies; Subsoils; Topsoil; Water Quality/Water Pollution; Water, Underground
• ISSN: 0049-6979; 1573-2932
• DOI: 10.1007/s11270-013-1519-z

Polyaromatic hydrocarbon (PAH) sorption to soil is a key process deciding the transport and fate of PAH, and potential toxic impacts in the soil and groundwater ecosystems, for example in connection with atmospheric PAH deposition on soils. There are numerous studies on PAH sorption in relatively low organic porous media such as urban soils and groundwater sediments, but less attention has been given to cultivated soils. In this study, the phenanthrene partition coefficient, K D (liter per kilogram), was measured on 143 cultivated Danish soils (115 topsoils, 0–0.25-m soil depth and 28 subsoils, 0.25–1-m depth) by the single-point adsorption method. The organic carbon partition coefficient, K OC (liter per kilogram) for topsoils was found generally to fall between the K OC values estimated by the two most frequently used models for PAH partitioning, the Abdul et al. ( Hazardous Waste & Hazardous Materials 4(3):211–222, 1987 ) model and Karickhoff et al. ( Water Research 13:241–248, 1979 ) model. A less-recognized model by Karickhoff ( Chemosphere 10:833–846, 1981 ), yielding a K OC of 14,918 L kg −1 , closely corresponded to the average measured K OC value for the topsoils, and this model is therefore recommended for prediction of phenanthrene mobility in cultivated topsoils. For lower subsoils (0.25–1-m depth), the K OC values were closer to and mostly below the estimate by the Abdul et al. ( Hazardous Waste & Hazardous Materials 4(3):211–222, 1987 ) model. This implies a different organic matter composition and higher PAH sorption strength in cultivated topsoils, likely due to management effects including more rapid carbon turnover. Finally, we applied the recent Dexter et al. ( Geoderma 144:620–627, 2008 ) theorem, and calculated the complexed organic carbon and non-complexed organic carbon fractions (COC and NCOC, grams per gram). Multiple regression analyses showed that the NCOC-based phenanthrene partition coefficient ( K NCOC ) could be markedly higher than the COC-based partition coefficient ( K COC ) for soils with a clay/OC ratio