Related Experiment Video
Updated: Jun 25, 2026

Temperature Response of Soil Organic Matter Decomposition Rates: Construction and Applications of a Temperature Gradient Block
Published on: January 30, 2026
Analysis of the dissipation kinetics of ivermectin at different temperatures and in four different soils
Kristine A Krogh1, Gitte G Jensen, Manuel K Schneider
1Copenhagen University, Faculty of Pharmaceutical Science, Department of Pharmaceutics and Analytical Chemistry, Section of Toxicology and Environmental Chemistry, Universitetsparken 2, DK-2100 Copenhagen, Denmark. kak@farma.ku.dk
Abstract:
The study target was to assess the usefulness of the OECD test guideline 307 for the veterinary pharmaceutical ivermectin. Laboratory microcosm studies were conducted to investigate the aerobic and anaerobic transformation of ivermectin in soils from three locations in Europe (York, Madrid and Tåstrup) and an artificial soil. The reason to include an artificial soil in the study was to understand the exposure potential of ivermectin in a parallel eco-toxicological study with non-target organisms in this soil for a longer duration. Three kinetic models (first-order (SFO), availability-adjusted first-order (AAFO) and bi-exponential first-order (BFO)) were applied to fit the observed transformation dynamics and to derive dissipation times. Dissipation rates were highly dependent on the tested soils. Under aerobic conditions, dissipation was remarkably faster in the three natural soils tested (DT(50)=16.1-36.1d) than in the artificial soil (DT(50)>500d). Furthermore, a clear increase in DT(50) values was seen when the temperature was lowered from 20 to 6 degrees C. The results indicated that dissipation in soils with comparably strong sorption and low degrees of desorption (i.e. the York soil and to some extent the Tåstrup soil) were best described by the AAFO model. While dissipation in the Madrid soil which had a lower sorption coefficient and a higher degree of reversibility of sorption could be satisfactorily described with the SFO model. Our data further showed that no significant dissipation occurred under anaerobic conditions.
Related Concept Videos
Physical Methods for Controlling Microbial Growth: Temperature
Theories of Dissolution: Diffusion Layer Model
This process starts with a thin layer, saturated with the drug, forming at the interface between the solid and liquid. The solute then diffuses from this layer into the main solution. The Noyes-Whitney equation suggests that the rate of dissolution relies on the diffusion...
In Vitro Drug Dissolution: Alternative Methods
Effect of Temperature Change on Reaction Rate
In Vitro Drug Dissolution: Compendial Testing Models II
Antimicrobial Effectiveness

