Chemical risk assessment requires reliable models to describe the environmental fate of chemicals. Special attention should be given to those chemicals known to be bioactive and also have high production volumes. Benzalkonium compounds are one such gr...
Chemical risk assessment requires reliable models to describe the environmental fate of chemicals. Special attention should be given to those chemicals known to be bioactive and also have high production volumes. Benzalkonium compounds are one such group of chemicals, designed to be biocidal and also produced in large volumes due to their widespread use in industrial, domestic and agricultural applications. Although benzalkonium compounds present a risk to terrestrial and aquatic ecosystems, there are no suitable models to describe their environmental fate. One of the reasons for the absence of reliable models is the unavailability of suitable analytical techniques to measure free concentrations of benzalkonium compounds at environmentally relevant levels. Since benzalkonium compounds are solids at environmental temperatures, their distribution will be confined to water and soils. Novel approaches are therefore, required to determine benzalkonium ion distribution coefficients between water and soil components.
This study reports on a bioassay-based method for the determination of benzalkonium ion distribution coefficients between water and soil components. A standardized algal growth inhibition test using Pseudokirchneriella subcapitata was modified by including sorbents in the culture medium. The nominal median inhibitory concentrations obtained in sorbent free medium were subtracted from those obtained from media with sorbents in order to estimate the sorbed concentrations. A toxicokinetic model was then used to compute free concentrations after accounting for the chemical sorbed to algal cells. Sorption to soil components accounted for over 80% of the initial spiked amount. The algal growth inhibition assay was sufficiently sensitive to allow distribution coefficients to be determined at free concentrations below 1 µmol L-1 and sorbed concentrations that were below 10% of the sorbent cationic exchange capacity. These values are within the range of reported environmental concentrations.
The developed method was used to determine distribution coefficients for peat, kaolinite and montmorillonite. When distribution coefficients were corrected for each sorbent’s cation exchange capacity, the computed distribution coefficients for each compound were all within one order of magnitude. It was also noted that at low sorbate loadings, van der Waals interactions between the neutral organic surfaces on peat and the alkyl chains of benzalkonium ions did not make a significant contribution to sorption. Therefore, at environmentally relevant concentrations sorption to the tested soil components was attributed to charge-charge interactions between the cationic sorbate and negatively charged sorbent surfaces. However, there was a strong positive correlation between the computed distribution coefficients and the length of the alkyl chain of the benzalkonium ion. This correlation was attributed to the increase in hydration energy with molecular weight of the ion. Higher hydration energies favor the partitioning of cations away from the aqueous phase. This was further explained by computing sorption energies of each ion and comparing them with hydration energies of a homologous series of alkanes.
This study also developed a method to calculate the distribution coefficients for soils of a known composition. Since the magnitude of the distribution coefficient was determined by both length of the alkyl chain and the sorbent cation exchange capacity, the model considers the two parameters in predicting sorption coefficients. Although the developed model is not suitable for the 16 and 18 carbon alkyl chain homologues, it does cater for the most popular homologues (C12 and C14) in most commercial formulations and the environment.