Uptake of zwitterionic antibiotics by rice (Oryza sativa L.) in contaminated soil

被引:44
作者
Hawker, Darryl W. [1 ]
Cropp, Roger [1 ]
Boonsaner, Maliwan [2 ]
机构
[1] Griffith Univ, Sch Environm, Atmospher Environm Res Ctr, Nathan, Qld 4111, Australia
[2] Silpakorn Univ, Fac Sci, Dept Environm Sci, Nakhon Pathom 73000, Thailand
关键词
Antibiotics; Maximum plant concentration; Temporal behaviour; Root concentration factor; Chemical activity model; ORGANIC-CHEMICALS; PLANT UPTAKE; OXYTETRACYCLINE; TETRACYCLINES; TRANSLOCATION; ACCUMULATION; DEGRADATION; ENVIRONMENT; CHLORTETRACYCLINE; LIPOPHILICITY;
D O I
10.1016/j.jhazmat.2013.09.066
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Antibiotics, including members of the tetracycline and fluoroquinolone families, are emerging organic environmental contaminants. Uptake from soil by plants is a means for antibiotics to enter terrestrial food chains. Chemical exchange between plant and the soil/water matrix occurs simultaneously with degradation in the soil/water matrix. In this study, the comparative temporal behaviour of rice (Oryza sativa L) towards the zwitterionic antibiotics oxytetracycline, chlortetracycline and norfloxacin at initial soil/water concentrations of 10,20 and 30 mu g g(-1) (dry weight) is investigated. This is accomplished within the framework of an activity-based mass-conserving dynamic model. Plant antibiotic concentrations are observed to increase to a maximum then decline. Maximum concentrations in rice are compound-dependent linear functions of initial soil/water concentrations, but the relationships are not related to the compound octan-1-ol/water distribution ratio (D-ow). The times required to attain maximal concentrations are independent of initial soil/water levels for a given antibiotic, but again vary between antibiotics and are not related to D-ow values. Translocation from root to other tissues is not observed. The magnitudes of Root Concentration Factors (RCFs), the ratio of root and soil/water concentrations, are consistent with significant sorption to soil and consequent relatively low concentrations in interstitial water. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:458 / 466
页数:9
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