Departament de Química Analítica, Carrer Martí i Franquès 1, 08028, Universitat de Barcelona, Barcelona, Spain.
Environ Sci Technol. 2013 Jun 18;47(12):6197-205. doi: 10.1021/es400911c. Epub 2013 May 28.
Commercial hardwood biochars ranging in N2 specific surface area of 0.1-427 m(2) · g(-1) were added to an agricultural soil at 0, 1, or 2% levels to determine whether they would predictably reduce the pore water concentration of sulfamethazine (SMT). The soil and biochar-soil mixtures were preweathered under mild (2 d, 20 °C) or more severe (28 d, 40 °C) conditions before spiking. The carbon-normalized biochar-water distribution coefficient (KBC) of the biochars varied by a factor of up to 10(4), depending on biochar properties and SMT concentration. Except for the fast-pyrolysis biochar, KBC greatly exceeded the soil organic carbon-water distribution coefficient KOC. Sorption in the mixtures increased as expected with biochar and dose. However, sorption was dramatically overpredicted (by up to 10(2.5)) by the sum of sorption to the individual components, indicating a strong weathering effect even under the mild conditions. The soil-subtracted weathered biochar-water isotherms were more linear, and the KBC values approached or lay within the range of KOC values reported for SMT in 19 soils. Biochars both in intimate contact with soil and placed in a membrane bag suspended in the solution showed reduced N2-B.E.T. surface area after weathering, implicating fouling of the biochar surface by humic substances transferred through water. The results indicate that only highly surfaceous, carbonaceous biochars would be useful for stabilizing soil contaminated with compounds such as SMT. They also suggest that weathering may attenuate the contribution of native (environmental) black carbon to sorption of such compounds in soils and sediments.
商业硬木生物炭的 N2 比表面积范围为 0.1-427 m(2)·g(-1),以 0、1 或 2%的水平添加到农业土壤中,以确定它们是否能可预测地降低磺胺甲恶唑(SMT)的孔隙水浓度。在添加之前,土壤和生物炭-土壤混合物在温和(2 d,20°C)或更剧烈(28 d,40°C)条件下进行预风化。生物炭的碳归一化生物炭-水分配系数(KBC)变化幅度高达 10(4),取决于生物炭特性和 SMT 浓度。除了快速热解生物炭外,KBC 大大超过了土壤有机碳-水分配系数 KOC。混合物中的吸附随着生物炭和剂量的增加而增加。然而,吸附被大大高估(高达 10(2.5)),这表明即使在温和条件下,风化作用也很强。减去土壤的风化生物炭-水等温线更线性,KBC 值接近或位于 19 种土壤中 SMT 的 KOC 值范围内。与土壤密切接触的生物炭和放置在悬挂在溶液中的膜袋中的生物炭在风化后表现出较低的 N2-B.E.T. 表面积,这表明腐殖质物质通过水转移到生物炭表面造成了污染。结果表明,只有高度多孔的碳质生物炭才有助于稳定受 SMT 等化合物污染的土壤。它们还表明,风化可能会减弱天然(环境)黑碳对土壤和沉积物中此类化合物吸附的贡献。