Photodegradation of the synthetic fragrance OTNE and the bactericide triclosan adsorbed on dried loamy sand – Results from models and experiments
Graphical abstract
Photodegradation on dried loamy sand was measured for OTNE and triclosan, and the shading effect was proved to be important and related to soil properties.
Highlights
► Photodegradation of chemical compounds on dried loamy sand surfaces was measured. ► Photodegradation was not restricted by diffusion in soil but by the shading effect of light. ► The shading effect was quantified from the concentration decrease profile.
Introduction
OTNE ([1,2,3,4,5,6,7,8-octahydro-2,3,8,8-tetramethylnaphthalene-2yl]ethan-1-one) is the one of the major constituents of fragrance mixtures and is produced as a technical mixture (e.g., Iso-E-Super®) with 2500–3000 t annually (Gautschi et al., 2001). Triclosan is used as an antibacterial agent in toothpaste, mouthwash, functional clothing such as sport shoes and underwear as well as a stabilizing agent in detergents and cosmetics (Adolfsson-Erici et al., 2001). 1500 t of this bactericide are produced annually worldwide (Singer et al., 2002). Since the emissions and impacts to environment of such compounds are becoming an issue, several researchers have measured the concentrations and the fate of them in aquatic environments (Kolpin et al., 2002, Lindström et al., 2002, Simonich et al., 2002, Bester, 2005, Bester et al., 2008a, Bester et al., 2008b). Both compounds are used in consumer products for cleaning and personal care, thus a major fraction of the used amount is disposed of with waste water. Waste water treatment plants can perform a partial cleaning of the water (Lindström et al., 2002, Bester, 2005, Bester et al., 2008b). During this process a considerable fraction of the triclosan and OTNE is partitioning into the sludge during waste water treatment (Singer et al., 2002, Simonich et al., 2002, Bester, 2003, Bester et al., 2008b). In those countries that use sludge as fertilizer, such as Denmark, these xenobiotics are then easily transported to the soil this way. Another way to expose soil is using the treated water that still contains some of the pollutants for irrigation (Oppel et al., 2004). On the soil surfaces, OTNE and triclosan can possibly be either be persistent, be degraded microbially or decompose with solar irradiation (photo-oxidation). In this study we focus on the photo-oxidation. In aquatic environments, the photolytic decomposition of triclosan has been measured extensively (Kanetoshi et al., 1992, Tixier et al., 2002, Ferrer et al., 2004, Latch et al., 2005, Chen et al., 2008) whereas the photolytic decomposition on the soil surface has not been investigated well. Further, for OTNE, the information of photolytic behavior is very limited (Aschmann et al., 2001). Triclosan undergoes degradations and conversions when irradiated with UV- or sunlight (Tixier et al., 2002, Latch et al., 2005, Chen et al., 2008). The half-life varies with pH values, as chinoidic structures are formed, and the half-life in water is estimated to be in the order of minutes to hours in natural sunlight conditions, and the extent is strongly dependent on pH values. Photolysis of triclosan in water leads to hydrolysis, dechlorination, and catechol products (Kanetoshi et al., 1992), or 2,8-dichlorodibenzo-p-dioxin and 2,4-dichlorophenol by high energy UV light (Ferrer et al., 2004) or natural sunlight (Latch et al., 2005).
In this work OTNE and triclosan were used as markers as they are (a) present in sludge in relatively high concentrations, (b) allow some comparison, as triclosan is a phenolic structure with relatively well understood photodegradation pattern, while very little is known about the photodegradation of the aliphatic OTNE. It was studied whether OTNE and triclosan can be decomposed or converted at the soil surface layer (top few millimeters) under light irradiation in similar ways as in the water phase. In this study the photodegradation of OTNE and triclosan on dried loamy sand (as typical for Denmark) is measured by artificial sunlight in the laboratory. From the result, three different models describing the limitation of the reactions of the compounds on the solids were compared with the measured data. Factors affecting the extent of photodegradation on the soil were discussed.
Section snippets
Materials
OTNE (Iso-E-Super®) was used as provided from the market stock of IFF, Hilversum, Netherlands. Triclosan was purchased from Ehrenstorfer (Augsburg, Germany). Toluene and other solvents were purchased residue grade (z.R.) from Merck (Darmstadt, Germany).
The soil used was a loamy sand retrieved from the 6 to 8 m depth at a former manufactured gas plant site at Hjørring, Denmark. The soil samples were collected at a non-contaminated location. The soil was air-dried and sieved to <1 mm. The physical
Modeling of photodegradation process on soils
Several different mechanisms were presented based on the heterogeneity of soils, or diffusion of chemicals in soils (Gustafson and Holdern, 1990, Balmer et al., 2000, Katagi, 2004). A model based on a physicochemical assumption is desirable, and diffusion or light penetration-limited model (Balmer et al., 2000), were fitted on the experimental data.
In the photolytic degradation processes, the two processes, direct photolytic degradation and diffusion of the chemicals into the irradiation zone
Results and discussion
The concentration changes during the experiment are shown in Fig. 2 along with the results of model fitting (explained hereafter). The concentrations in the light decreased significantly while the concentration in the dark did not significantly change from the initial value throughout the experiment for both compounds. During the first 2 weeks of the experiments, the OTNE and triclosan concentrations decreased to 50%. The measured half-life (T1/2) was 7.1 and 16.7 d for OTNE and triclosan,
Conclusions
In this paper, photodegradation of OTNE and triclosan on a dried loamy sand was measured under artificial sunlight conditions and compared with three different degradation models. Their decrease did not simply follow first-order kinetics. The apparent decrease rate constant decreased in the latter stage of reaction, suggesting some portion of the chemical is more available for photodegradation than others. With comparing the obtained parameters with the physico-chemical parameters of soils and
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Present address: National Environmental Research Institute, Aarhus University, Frederiksborgsvej 399, 4000 Roskilde, Denmark.