James Gavin, Sabatini David A, Chiou Cary T, Rutherford David, Scott Andrew C, Karapanagioti Hrissi K
School of Civil Engineering and Environmental Science, University of Oklahoma, Norman, OK 73019, USA.
Water Res. 2005 Feb;39(4):549-58. doi: 10.1016/j.watres.2004.10.015. Epub 2004 Dec 23.
A certain amount of wood char or soot in a soil or sediment sample may cause the sorption of organic compounds to deviate significantly from the linear partitioning commonly observed with soil organic matter (SOM). Laboratory produced and field wood chars have been obtained and analyzed for their sorption isotherms of a model solute (phenanthrene) from water solution. The uptake capacities and nonlinear sorption effects with the laboratory wood chars are similar to those with the field wood chars. For phenanthrene aqueous concentrations of 1 microg l(-1), the organic carbon-normalized sorption coefficients (log K(oc)) ranging from 5.0 to 6.4 for field chars and 5.4-7.3 for laboratory wood chars, which is consistent with literature values (5.6-7.1). Data with artificial chars suggest that the variation in sorption potential can be attributed to heating temperature and starting material, and both the quantity and heterogeneity of surface-area impacts the sorption capacity. These results thus help to corroborate and explain the range of logK(oc) values reported in previous research for aquifer materials containing wood chars.
土壤或沉积物样品中一定量的木炭或煤烟可能会导致有机化合物的吸附与通常在土壤有机质(SOM)中观察到的线性分配有显著偏差。已获取实验室制备的和野外的木炭,并分析了它们对模型溶质(菲)从水溶液中的吸附等温线。实验室木炭和野外木炭对菲的吸附容量和非线性吸附效应相似。对于1微克/升的菲水溶液浓度,野外木炭的有机碳归一化吸附系数(log K(oc))范围为5.0至6.4,实验室木炭为5.4 - 7.3,这与文献值(5.6 - 7.1)一致。人工木炭的数据表明,吸附潜力的变化可归因于加热温度和起始材料,并且表面积的数量和非均质性都会影响吸附容量。因此,这些结果有助于证实和解释先前研究中报道的含木炭含水层材料的logK(oc)值范围。