Zhang Jin-qiang, Dong Yuan-hua
State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China.
Huan Jing Ke Xue. 2007 Oct;28(10):2383-8.
On the basis of OECD Guideline 106, batch sorption methods were employed to reveal the effect of Ca2+ ion strength and different cations (0.01 mol/L solution of NaCl, KCl, NH4LCl, MgCl2, CaCl2, ZnCl2 and AlCl3) on norfloxacin (NOR) sorption-desorption process in four tested soils (Ustic Cambosols, Udic Argosols, Gleyic-Stagnic Anthrosols and Ali-Perudic Ferrosols). Results indicate that sorption coefficient Kf values of NOR gradually decrease to a steady state with the increased concentration of calcium ion in solution. There exists a significantly negative correlation between Ca2+ ion strength and Kf value (p < or = 0.05). Compared with higher NOR concentrations, the effect of calcium ion concentration is negligible to the sorption at lower NOR concentrations. At the low pH, cationic form of NOR is predominant in equilibrium solutions, so cation sorption and hydrogen bonding could be the main sorption mechanism. Whilst at the zwitterionic form of NOR (pH 6.3-8.4), electrostatic adsorption or dipole moment may control the sorption process. This causes the different sorption behavior of NOR in the four soils. Thus, the calcium ion in solutions is competitively adsorbed to the active sorption sites so as to decrease the NOR sorption amount. Moreover, the different cations result in difference of NOR sorption. Cations of higher valencies are adsorbed more strongly to surface active sorption sites, with the following order: M+ (Na+, K+, NH4+) < M2+ (Ca2+, Mg2+, Zn2+) < M3+ (Al3+).
根据经合组织准则106,采用批量吸附法揭示了Ca2+离子强度和不同阳离子(0.01 mol/L的NaCl、KCl、NH4Cl、MgCl2、CaCl2、ZnCl2和AlCl3溶液)对四种受试土壤(干润始成土、潮湿富铁土、潜育-潴育人为土和铝质-弱发育铁铝土)中诺氟沙星(NOR)吸附-解吸过程的影响。结果表明,随着溶液中钙离子浓度的增加,NOR的吸附系数Kf值逐渐降低至稳态。Ca2+离子强度与Kf值之间存在显著负相关(p≤0.05)。与较高的NOR浓度相比,钙离子浓度对较低NOR浓度下的吸附影响可忽略不计。在低pH值时,NOR的阳离子形式在平衡溶液中占主导地位,因此阳离子吸附和氢键可能是主要的吸附机制。而在NOR的两性离子形式(pH 6.3 - 8.4)下,静电吸附或偶极矩可能控制吸附过程。这导致了NOR在四种土壤中的吸附行为不同。因此,溶液中的钙离子竞争性地吸附到活性吸附位点,从而降低了NOR的吸附量。此外,不同的阳离子导致了NOR吸附的差异。高价阳离子对表面活性吸附位点的吸附更强,顺序如下:M+(Na+、K+、NH4+)<M2+(Ca2+、Mg2+、Zn2+)<M3+(Al3+)。