Nanjing University, Jiangsu, China.
J Environ Qual. 2012 Jul-Aug;41(4):1284-9. doi: 10.2134/jeq2012.0016.
Batch sorption isotherms of 1,3,5-trichlorobenzene, 1,3,5-trinitrobenzene, and tetracycline to organic-free montmorillonites and soils receiving heat treatment (375°C for 24 h) were compared with those to unheated sorbents. Sorption of the nonpolar 1,3,5-trichlorobenzene to soil was lowered after the removal of humus by heating, consistent with the mechanism of hydrophobic partition into organic matter. For 1,3,5-trinitrobenzene, the enhanced sorption to heated soils was attributed to specific interactions with exchangeable cations facilitated by heating-induced irreversible partial dehydration of the clay interlayer. For tetracycline, an additional mechanism for sorption enhancement could be due to increased exposure of strong complexation sites on clay minerals after removal of the humic coating. These hypotheses were supported by the sorption data to heated and unheated Na-, K-, and Cs-saturated montmorillonites. The combustion method is commonly adopted to measure the content of black carbon in soils and sediments. However, findings from the present study indicate that combustion may greatly modify the structural properties of clay minerals, leading to misinterpreted sorption contributions of different soil components to sorption of polar or ionic compounds.
批量吸附等温线的 1,3,5-三氯苯、1,3,5-三硝基苯和四环素有机免费蒙脱石和土壤接受热处理 (375°C 24 小时)与未加热的吸附剂进行了比较。非极性 1,3,5-三氯苯的土壤吸附在加热去除腐殖质后降低,与疏水分配进入有机质的机制一致。对于 1,3,5-三硝基苯,加热土壤的吸附增强归因于加热诱导的粘土层间不可逆部分脱水促进的与可交换阳离子的特殊相互作用。对于四环素,吸附增强的另一个机制可能是由于去除腐殖质涂层后,粘土矿物上的强络合位点暴露增加。这些假设得到了加热和未加热的 Na-、K-和 Cs-饱和蒙脱石吸附数据的支持。燃烧法通常用于测量土壤和沉积物中黑碳的含量。然而,本研究的结果表明,燃烧可能会极大地改变粘土矿物的结构性质,导致对不同土壤成分对极性或离子化合物吸附的吸附贡献产生误解。