DEGRADATION KINETICS OF PTAQUILOSIDE IN SOIL AND SOIL SOLUTION

• Published in: Environmental toxicology and chemistry 2008-02, Vol.27 (2), p.252-259
• Main Authors: Ovesen, R.G, Rasmussen, L.H, Hansen, H.C.B
• Format: Article
• Language: English
• Subjects: Biodegradation; Biodegradation, Environmental; Bracken; Chemical compounds; chemical constituents of plants; Clay; clay soils; Degradation; Drinking water; environmental fate; Hydrolysis; Indans - chemistry; Indans - metabolism; Kinetics; Leaching; Life sciences; Microbial activity; Moisture content; Molecular Structure; Organic matter; phytotoxins; Pore water; provenance; ptaquiloside; Pteridium - chemistry; Pteridium aquilinum; Sandy soils; Sesquiterpenes - chemistry; Sesquiterpenes - metabolism; Silicates; Soil - analysis; soil horizons; Soil Microbiology; Soil Pollutants - chemistry; Soil Pollutants - metabolism; soil pollution; Soil solution; Soil water; Soils; Sorption; Studies; Subsoils; Surface water; Surface-groundwater relations; Topsoil; Toxin; Water - chemistry; weeds
• ISSN: 0730-7268; 1552-8618
• DOI: 10.1897/07-324R.1

Ptaquiloside (PTA) is a carcinogenic norsesquiterpene glycoside produced in bracken (Pteridium aquilinum (L.) Kuhn), a widespread, aggressive weed. Transfer of PTA to soil and soil solution eventually may contaminate groundwater and surface water. Degradation rates of PTA were quantified in soil and soil solutions in sandy and clayey soils subjected to high natural PTA loads from bracken stands. Degradation kinetics in moist soil could be fitted with the sum of a fast and a slow first-order reaction; the fast reaction contributed 20 to 50% of the total degradation of PTA. The fast reaction was similar in all horizons, with the rate constant k1F ranging between 0.23 and 1.5/h. The slow degradation, with the rate constant k1S ranging between 0.00067 and 0.029/ h, was more than twice as fast in topsoils compared to subsoils, which is attributable to higher microbial activity in topsoils. Experiments with sterile controls confirmed that nonmicrobial degradation processes constituted more than 90% of the fast degradation and 50% of the slow degradation. The lower nonmicrobial degradation rate observed in the clayey compared with the sandy soil is attributed to a stabilizing effect of PTA by clay silicates. Ptaquiloside appeared to be stable in all soil solutions, in which no degradation was observed within a period of 28 d, in strong contrast to previous studies of hydrolysis rates in artificial aqueous electrolytes. The present study predicts that the risk of PTA leaching is controlled mainly by the residence time of pore water in soil, soil microbial activity, and content of organic matter and clay silicates.