|
|
||||||||
a Centre de recherche en horticulture, Envirotron, Université Laval, QC, Canada G1K 7P4
b Département de biomédecine vétérinaire, École de médecine vétérinaire, Université de Montréal, QC, Canada G2S 7C6
* Corresponding author (suzanne.allaire{at}sga.ulaval.ca)
Received for publication September 15, 2005.
| ABSTRACT |
|---|
|
|
|---|
Abbreviations: CTC, chlortetracycline HPLC, high performance liquid chromatography Kd, linear sorption coefficient TYL, tylosin
| INTRODUCTION |
|---|
|
|
|---|
Up to 80% of antibiotics used as feed additives or for disease treatment are excreted through urine and feces (Levy, 1992). These urine and feces are then spread on agricultural field thus transferring the antibiotics to the environment. Antibiotics have been detected worldwide in soils, surface water, and ground water (Christian et al., 2003; Hamscher et al., 2002; Kolpin et al., 2002). As an example, 7 mo after liquid manure application, different antibiotics could be found in the soil (15 µg kg1 of sulfadimidine) and related waters (Christian et al., 2003).
It is believed that antibiotics in soils may favor the development of antibiotic-resistant microorganisms causing different health problems in animals and humans (Halling-Sørensen et al., 1998). Sengeløv et al. (2003) showed that resistance, measured by the presence of resistance genes by polymerase chain reaction (PCR), to tetracycline and streptomycin developed in less than a year in soils treated with pig manure slurry. It is therefore important to understand the behavior of antibiotics in soils.
Good reviews have been published regarding veterinary medications and antibiotics (Boxall et al., 2004). Boxall et al. (2003) listed chlortetracycline (CTC) and tylosin (TYL), among others, as having a high potential of entering the environment. These molecules have already been detected in soils, surface waters, and ground waters (Boxall et al., 2004; Christian et al., 2003) but little is known about their behavior in soils.
These two antibiotics are heavily used in pig production in Québec. Chlortetracycline is used for the treatment or prevention of contagious respiratory infections as well as a growth factor. Chlortetracycline inhibits protein synthesis in prokaryotes and eukaryotes. It also inhibits the binding of aminoacyl-tRNA to ribosomes. Tylosin is used against enteric digestive infections causing diarrhea as well as a growth promoter. Up to 5 and 9 mg L1 of CTC and TYL, respectively, can be found in liquid manure (Kumar et al., 2004) which is then applied on farm lands.
In spite of their widespread application on farm lands, CTC and TYL behavior in Québec soils has received little attention. Key chemical properties such as water solubility, soil pH, volatility, and sorption influence solute transport in soils. Sorption coefficients (Kd, Koc, Kow) have been used to predict antibiotic behavior in soils. Sorption coefficients reported in literature are usually obtained from experiments conducted over a 24-h period assuming equilibrium and no degradation. In addition, experiments on antibiotics may be conducted with sterilized or unsterilized soils, but the need for sterilization in short-term experiments is not clear. In addition to degradation, kinetics of chemical sorption onto soil particles is very important for solute transport studies and for modeling purposes because antibiotic movement depends on the time lapse between the chemical application (availability of compound in the soil water which depends, in part, on the sorption kinetics) and the first precipitation event. As an initial step for further experimentations and simulations, it is important to better understand sorption kinetics and the importance of sterilization.
The goals of this study were to measure sorption kinetics of CTC and TYL before equilibrium is reached, and the microbial and non-microbial degradation of these compounds during short-term experiments (<48 h).
| MATERIALS AND METHODS |
|---|
|
|
|---|
A sandy loam soil and a clay soil were chosen for their similar pH and low organic carbon content, and because they represent extremes in particle size distribution. Therefore, the difference between the behavior of both chemicals would be mostly related to particle size distribution (Table 1). Difference in organic matter contents should be minimal compared to the difference in clay contents. The aggregates between 0.2 and 0.6 mm were destroyed with a rammer before sieving with a 2-mm sieve. The soil was then oven-dried at 105°C for 24 h before the experiments.
|
A stock solution was prepared for each treatment, each replicate, and each antibiotic separately. The mixtures were made of 140 g of 200 mg L1 solution of CTC and 3000 mg L1 of TYL into 0.025-L polypropylene bottles with (i) soil blanks (no soil but with antibiotics), or with 70 g of (ii) sterilized sandy loam, (iii) non-sterilized sandy loam, (iv) sterilized clay, and (v) non-sterilized clay. Antibiotic blanks (no antibiotics but with soil) were also prepared. Sterilization was performed at 121°C for 20 min using an autoclave and by spreading the soil in fine layer on wide, shallow containers. The sterilized soil was then dried at 105°C for 24 h. The soil was allowed to cool down in a closed container before use.
Optimal soil homogeneity was achieved by destroying the aggregates first, then by sieving the soil, mixing up the soil from bottom to top many times (up to six times), using soil containers smaller than 0.5 L, with at least 15 g of soil and by composite sampling from at least five areas in the containers. A 2:1 solution to soil ratio gave good accuracy (<6% variability) and concentration above detection limits for TYL on both soils but too low solution concentration of CTC sorbing on the clay soil. A 4:1 ratio for CTC sorption on clay was used. In the case of CTC and clay mixtures, 35 g of soil instead of 70 g was used for proper solution to soil ratio. The polypropylene bottles were covered with aluminium tape to prevent light degradation. The mixtures were continuously shaken up to 1 h (depending on the sampling time) and put in darkness. The optimal stroke length and frequency were 0.1 m and 100 stokes per minute below which the solution and soil mixtures did not sufficiently move or above which the bottles' movement would cause friction. The friction results in 2°C temperature increase although the temperature of the environment was controlled. Even with long strokes, soil stratification in the bottles occurred unless they were rotated every 0.25 h. One hour of shaking was sufficient to obtain homogeneous mixtures. The samples were shaken by hand for 1 min right before sampling. A 400-µL of solution were sampled at 0.00, 0.017, 0.08, 0.25, 0.75, 3, 7, 24, and 48 h and put into small vials (Model 410870-840; Alltech, Deerfield, IL). The samples were immediately frozen at 80°C.
The samples were defrosted 1 min before analysis with high performance liquid chromatography (HPLC). The solution was passed through a 0.2-µm filter (nylon filter syringes; Chromatographic Specialties, Brockville, ON, Canada) to remove soil particles. Tests were performed to assure no additional sorption during freezing, storage, and defrosting. Samples were compared with analysis on filtered samples immediate after sampling. Freezing and defrosting both occurred in less than 2 min. The process of freezing, storing, and defrosting may have lead to 3- to 5-min overestimation of sorption kinetics. This is not significant considering that the point of interest of this study was to know if equilibrium was reached within 24 h. Two injections were done for each sample in the HPLC. There were no significant differences between the injections. The error was less than 0.1% except close to the detection limit. Thereafter, the following text refers to the average values of these two injections per sample.
Concentration analysis were performed on HPLC following the method of Loke et al. (2000) and Díaz-Cruz et al. (2003) using a BDS Hypersil C8 100 x 2.1 column (Thermo, Waltham, MA). The HPLC was an autosampler (Model 717; Waters, Milford, MA) with a detector (Model Tm 996; Waters). The flux was 0.25 mL min1. Two solvents were used, acid formic 0.5% and acetonitrile 100%. Tylosin is reported as the summation of both TYL A and B. Limit of detection was 0.05 mg L1. Three replications were completed. Statistical analyses were performed using SAS Stat software Version 8.0 (SAS Institute, 1999).
| RESULTS AND DISCUSSION |
|---|
|
|
|---|
The concentration of soil-blank solutions of both antibiotics did not significantly change over time. There was no significant degradation over a 48-h period at room temperature during storage over many days at 80°C (up to 60 d). Thus, the aluminium foil was sufficient to protect CTC against light degradation, sterilization of solution was not necessary, and the samples were properly stored and handled.
Sorption of TYL and CTC was highly different between soils but not significantly different between replicates neither between sterilized and non-sterilized soils. A period of 48 h was insufficient to measure the impact of microbial degradation for both chemicals in presence of either soil (Fig. 1). Therefore, soil sterilization is not required for short-term experiments (<48 h), which simplifies further experiments.
|
Tylosin sorbed on both soils almost one order of magnitude more than CTC, indicating lower risk of TYL transport in the soil profile. Although detection limits for both chemicals were similar, the variability in TYL sorption was much higher than that of CTC (Fig. 1). Variability of TYL was by far the highest on sandy loam. The difference in variability was not due to handling precision since both experiments were conducted simultaneously by the same people for both antibiotics and the variability of CTC concentration was low (<6%). Besides variability in stock solutions themselves, variability may have been due to small differences in the clay content of the sandy loam. This is because TYL is more sensitive to clay content, it is difficult to obtain perfectly mixed sandy loam soil, and for other unclear reasons. Note that in Fig. 1, each point is an average of two injections on HPLC and three replicates.
Sorption of the two chemicals on both soils occurred very fast (Fig. 1). Chlortetracycline sorption occurred within 10 min on both soils. Tylosin sorption occurred within 5 min on sandy loam and within 3 h on clay. A 24-h equilibrium time is more than enough for studying the sorption of CTC and TYL on both soils. In fact, a 1-h equilibrium time would probably be sufficient in most cases and 4 h for all cases.
The high sorption of the two antibiotics on soils having extreme particle size distribution combined with the very fast sorption kinetics indicates a small probability of leaching through the soil profile toward ground water. These antibiotics may however reach the ground water through preferential flow processes by which soil particles may be carried down in the profile (Kay et al., 2004). The results tend to indicate high probability of reaching surface water through erosion (i.e., attached to the eroded soil particles if erosion would take place). More study is needed on the movement of these chemicals in soil under cold climate.
| CONCLUSIONS |
|---|
|
|
|---|
| ACKNOWLEDGMENTS |
|---|
| REFERENCES |
|---|
|
|
|---|
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Journal of Natural Resources and Life Sciences Education |
Vadose Zone Journal | ||||
| Soil Science Society of America Journal | Journal of Plant Registrations | The Plant Genome | |||