Institute of Organic Contaminant Control and Soil Remediation, College of Resource and Environmental Sciences, Nanjing Agricultural University , Nanjing 210095, China.
Department of Plant, Soil and Microbial Sciences, Michigan State University , East Lansing, Michigan 48824, United States.
Environ Sci Technol. 2017 Jun 6;51(11):6165-6173. doi: 10.1021/acs.est.7b00590. Epub 2017 May 19.
Increasing concentrations of anthropogenic antibiotics in soils are partly responsible for the proliferation of bacterial antibiotic resistance. However, little is known about how soil-sorbed antibiotics exert selective pressure on bacteria in unsaturated soils. This study investigated the bioavailability of tetracycline sorbed on three soils (Webster clay loam, Capac sandy clay loam, and Oshtemo loamy sand) to a fluorescent Escherichia coli bioreporter under unsaturated conditions using agar diffusion assay, microscopic visualization, and model simulation. Tetracycline sorbed on the soils could be desorbed and become bioavailable to the E. coli cells at matric water potentials of -2.95 to -13.75 kPa. Bright fluorescent rings were formed around the tetracycline-loaded soils on the unsaturated agar surfaces, likely due to radial diffusion of tetracycline desorbed from the soils, tetracycline uptake by the E. coli cells, and its inhibition on E. coli growth, which was supported by the model simulation. The bioavailability of soil-sorbed tetracycline was much higher for the Oshtemo soil, probably due to faster diffusion of tetracycline in coarse-textured soils. Decreased bioavailability of soil-sorbed tetracycline at lower soil water potential likely resulted from reduced tetracycline diffusion in soil pore water at smaller matric potential and/or suppressed tetracycline uptake by E. coli at lower osmotic potential. Therefore, soil-sorbed tetracycline could still exert selective pressure on the exposed bacteria, which was influenced by soil physical processes controlled by soil texture and soil water potential.
土壤中人为抗生素浓度的增加部分导致了细菌抗生素耐药性的扩散。然而,人们对于在非饱和土壤中,被土壤吸附的抗生素如何对细菌施加选择压力知之甚少。本研究采用琼脂扩散法、微观可视化和模型模拟,研究了三种土壤(Webster 粉质黏土、Capac 砂壤土和 Oshtemo 粉质砂壤土)上吸附的四环素在非饱和条件下对荧光大肠杆菌生物报告菌的生物可利用性。在基质水势为-2.95 至-13.75 kPa 时,被土壤吸附的四环素可以解吸并对大肠杆菌细胞具有生物可利用性。在非饱和琼脂表面上,载有四环素的土壤周围形成了明亮的荧光环,这可能是由于四环素从土壤中解吸、四环素被大肠杆菌细胞吸收以及其对大肠杆菌生长的抑制作用所致,这一结果得到了模型模拟的支持。Oshtemo 土壤中吸附态四环素的生物可利用性更高,可能是由于粗质地土壤中四环素的扩散速度更快所致。在较低的土壤水势下,土壤吸附态四环素的生物可利用性降低,可能是由于在较小的基质势下,土壤孔隙水中的四环素扩散减少,或者是由于较低的渗透压导致大肠杆菌对四环素的摄取减少。因此,被土壤吸附的四环素仍能对暴露的细菌施加选择压力,这受到土壤质地和土壤水势控制的土壤物理过程的影响。