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低温及饱和流动条件下丙二醇降解的限制因素。

Constraints of propylene glycol degradation at low temperatures and saturated flow conditions.

作者信息

Lissner Heidi, Wehrer Markus, Reinicke Martin, Horváth Nikoletta, Totsche Kai Uwe

机构信息

Institut für Geowissenschaften, Friedrich-Schiller-Universität Jena, Burgweg 11, 07749, Jena, Germany,

出版信息

Environ Sci Pollut Res Int. 2015 Feb;22(4):3158-74. doi: 10.1007/s11356-014-3506-3. Epub 2014 Sep 21.

Abstract

During snowmelt, the infiltration of large amounts of propylene glycol (PG), the major compound of many aircraft deicing fluids, affects redox processes and poses a contamination risk for the groundwater. To gain a better understanding about the degradation of PG and the associated biogeochemical processes under these conditions, we conducted saturated soil column experiments at 4 °C. During two successive PG pulses, we monitored the effect of the runway deicer formate (FO) and changing redox conditions on PG degradation. Furthermore, we applied first-order and simplified Monod kinetics to describe PG and FO transport. The transport of 50 mg l(-1) PG showed three stages of microbial degradation, which were defined as lag phase, aerobic phase, and anaerobic phase. During the second pulse, lag effects diminished due to the already accomplished microbial adaption, and the initial degradation rate of PG increased. Degradation of PG was most efficient during aerobic conditions (aerobic phase), while the subsequent drop of the redox potential down to -300 mV decreased the degradation rate (anaerobic phase). Formate addition decreased the overall degradation of PG by 50 and 15 % during the first and second pulse, illustrating the inhibitory effect of FO on PG degradation. The concurrent increase of Fe(III), organic carbon, and the turbidity in the column effluent after PG and FO application suggest the combined export of Fe adsorbed to fragments of detached biofilm. Neither the first-order nor the simplified Monod model was able to reconstruct the dynamic breakthrough of 50 mg l(-1) PG. The breakthrough of 1,000 mg l(-1), however, was described reasonably well with first-order kinetics. At low temperature and high water saturation, the application of first-order degradation kinetics seems therefore appropriate to describe the transport of high concentrations of PG.

摘要

在融雪期间,大量丙二醇(PG)(许多飞机除冰液的主要成分)的渗入会影响氧化还原过程,并对地下水构成污染风险。为了更好地了解在这些条件下PG的降解及相关生物地球化学过程,我们在4℃下进行了饱和土壤柱实验。在连续两次PG脉冲期间,我们监测了跑道除冰剂甲酸盐(FO)的影响以及氧化还原条件变化对PG降解的影响。此外,我们应用一级动力学和简化的莫诺德动力学来描述PG和FO的迁移。50 mg l(-1) PG的迁移显示出微生物降解的三个阶段,分别定义为延迟期、好氧阶段和厌氧阶段。在第二次脉冲期间,由于微生物已经完成适应,延迟效应减弱,PG的初始降解速率增加。PG在好氧条件下(好氧阶段)降解效率最高,而随后氧化还原电位降至-300 mV会降低降解速率(厌氧阶段)。添加甲酸盐在第一次和第二次脉冲期间分别使PG的总体降解降低了50%和15%,说明了FO对PG降解的抑制作用。在施加PG和FO后,柱流出物中Fe(III)、有机碳和浊度同时增加,表明吸附在脱落生物膜碎片上的Fe被联合输出。一级动力学模型和简化的莫诺德模型都无法重建50 mg l(-1) PG的动态穿透曲线。然而,1000 mg l(-1)的穿透曲线用一级动力学能得到较好的描述。因此,在低温和高水饱和度条件下,应用一级降解动力学似乎适合描述高浓度PG的迁移。

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