Degradation of the potato glycoalkaloid α-solanine in three agricultural soils

The toxic glycoalkaloids produced by the potato plant (Solanum tuberosum L.) have previously been found in upper soil from a potato field during several months. Further insight into the fate of the glycoalkaloids is needed, as only little information about their degradation in soil is available. Degradation of the glycoalkaloid, α-solanine, has been followed for 42 d in three agricultural soils with common texture and carbon contents. A similar degradation pattern was found in all soils, and the kinetics was well described by a sum of two first-order equations. Overall, degradation rates for the initial first reaction were in the range 0.22–1.64 d−1. Estimated half-lives were in the range 1.8–4.1 d for the three top soils at 15 °C; the fastest degradation was observed in the sandy soil. The major proportion of α-solanine in the sandy soil was degraded by the fast process, while the proportion was lower for the two other soils. Fast degradation appeared to be related to the presence of low amount of sorbents. Additionally, degradation was followed at 5 °C in A- and C-horizon soil from the sandy location, and for both horizons the half-lives were of similar length (4.7–8.7 d). For the slow process, degradation rates were in the range 0.000–0.123 d−1, and residuals were still present in all soils and all temperatures at the end of the experiment (d 42). Overall, fast degradation was found in both top- and subsoil even at low temperatures, and the risk for α-solanine leaching to the groundwater appears to be low.