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Factors influencing adsorption and desorption of trimethoprim on marine sediments: mechanisms and kinetics

机译:影响林地沉积物吸附和解吸的因素:机制和动力学

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Adsorption-desorption behavior of ionic antibiotics in natural aquatic environment is complex, especially in coastal or estuary area where influencing factors such as pH and salinity usually varied in a wide range. In this study, batch-type and stirred flow chamber (SFC) experiments were carried out to simulate the sorption-desorption behavior of trimethoprim (TMP) in seawater-sediment system. Equilibrium and kinetic modeling were carried out to determine the rate and extent of TMP sorption on two marine sediments with different properties. Sediment BHB (K-d, 6.40 L kg(-1)) has a greater sorption capacity compared with sediment LZB (K-d, 3.40 L kg(-1)), which is related to the higher content of organic carbon and clay of sediment BHB. Adsorption of TMP varied in the pH range of 6.9 to 8.1 with maximum adsorption at pH 7.4. Increasing salinity and presence of phosphate and nitrate led to decreased TMP sorption. Attenuated total reflection Fourier transform infrared (ATR-FTIR) analysis demonstrated the formation of hydrogen bond between TMP and marine sediments. Adsorption of TMP on marine sediments was a non-equilibrium process that can be described with second-order kinetic model. Our analysis suggested that chemical non-equilibrium was the rate controlling process and intraparticle diffusion was also involved in TMP adsorption. A moderate desorption percentage (16.4-22.8% for LZB and 32.5-42.0% for BHB) was observed. Overall, the results showed that environmental factors and time-dependent processes need to be considered in modeling the fate and transport of TMP in coastal/estuarine waters.
机译:离子抗生素在天然水生环境中的吸附 - 解吸行为是复杂的,特别是在沿海或河口区域,影响因素,如pH和盐度通常在宽范围内变化。在该研究中,进行了批型和搅拌的流量室(SFC)实验,以模拟海水沉积物系统中Trimethokim(TMP)的吸附解吸行为。进行平衡和动力学建模,以确定两种海洋沉积物的TMP吸附速率和程度。沉积物BHB(K-D,6.40L kg(-1))与沉积物LZB(K-D,3.40L kg(-1))相比具有更高的吸附能力,其与沉积物BHB的有机碳和粘土的更高含量有关。 TMP的吸附在6.9至8.1的pH范围内变化,最大吸附在pH7.4时。增加盐度和磷酸盐的存在和硝酸盐导致的TMP吸附降低。减弱的全反射傅里叶变换红外(ATR-FTIR)分析证明了TMP和海洋沉积物之间的氢键形成。 TMP对海洋沉积物的吸附是一种非平衡过程,可以用二阶动力学模型描述。我们的分析表明,化学非平衡是速率控制过程,骨盆扩散也参与了TMP吸附。观察到中度解吸百分比(LZB的16.4-22.8%,BHB的32.5-42.0%)。总的来说,结果表明,需要考虑环境因素和时间依赖过程在沿海/河口水域中的TMP的建模和运输。

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