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在有氧含水层物质中,低浓度除草剂灭草灵和2,4-滴的生物降解动力学变化。

Shifts in biodegradation kinetics of the herbicides MCPP and 2,4-D at low concentrations in aerobic aquifer materials.

作者信息

Toräng Lars, Nyholm Niels, Albrechtsen Hans-Jørgen

机构信息

Environment & Resources DTU, Groundwater Research Centre, Technical University of Denmark, DK-2800 Lyngby, Denmark.

出版信息

Environ Sci Technol. 2003 Jul 15;37(14):3095-103. doi: 10.1021/es026307a.

DOI:10.1021/es026307a
PMID:12901656
Abstract

Biodegradation kinetics of two phenoxy acid herbicides, MCPP [(+/-)-2-(4-chloro-2-methylphenoxy)propanoic acid; mecoprop] and 2,4-D [2,4-dichlorophenoxyacetic acid] were studied in laboratory batch microcosms at low concentrations (0.025-100 microg/L) using 14C technique with sediments and groundwater from a shallow aerobic sandy aquifer. Below a certain threshold concentration of approximately 1 microg/L for 2,4-D and 10 microg/L for MCPP, the biodegradation followed first-order nongrowth kinetics, and no adaptation was observed within the experimental period of 341 d. Half-lifes for ultimate degradation were 500 d for 2,4-D and 1100 d for MCPP at 10 degrees C in unpolluted aquifer sediment in this environmentally relevant concentration regime. Above the threshold concentrations, the biodegradation rate accelerated gradually due to selective growth of specific biomass, which was ascertained from 14C most probable number enumerations of specific phenoxy acid degraders. Atthe highest concentration tested (100 microg/ L), specific degraders increased from 10(-1) to 10(5) cells/g during the experiment, and half-lifes after adaptation decreased to approximately 5 d. The enhanced rate of degradation by adapted systems was maintained during degradation of the last residuals measured to less than 0.1 microg/L. In situ long-term preexposure of the aquifer sediment also resulted in significant higher degradation rates of the phenoxy acids.

摘要

使用来自浅层好氧砂质含水层的沉积物和地下水,采用¹⁴C技术,在实验室批次微观系统中研究了两种苯氧基酸除草剂,即灭草丙酸[(±)-2-(4-氯-2-甲基苯氧基)丙酸;麦草畏]和2,4-滴[2,4-二氯苯氧基乙酸]在低浓度(0.025-100μg/L)下的生物降解动力学。对于2,4-滴,低于约1μg/L的特定阈值浓度,对于灭草丙酸低于10μg/L时,生物降解遵循一级非生长动力学,并且在341天的实验期内未观察到适应性变化。在该与环境相关的浓度范围内,在10℃的未受污染含水层沉积物中,2,4-滴最终降解的半衰期为500天,灭草丙酸为1100天。高于阈值浓度时,由于特定生物量的选择性生长,生物降解速率逐渐加快,这是通过对特定苯氧基酸降解菌的¹⁴C最可能数计数确定的。在测试的最高浓度(100μg/L)下,实验期间特定降解菌从10⁻¹增加到10⁵个细胞/克,适应后的半衰期降至约5天。在将最后残留量降解至低于0.1μg/L的过程中,适应系统提高的降解速率得以维持。含水层沉积物的原位长期预暴露也导致苯氧基酸的降解速率显著提高。

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