Availability and biodegradation of metribuzin in alluvial soils as affected by temperature and soil properties

Herbicide degradation in soils is highly temperature-dependent. Laboratory incubations and field experiments are usually conducted with soils from the temperate climatic zone. Few data are available for cold conditions and the validation of approaches to correct the degradation rate at low temperatu...

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Bibliographic Details
Published in:Weed Research
Main Authors: Benoit, Pierre, Perceval, J., Stenrod, M., Moni, C, Eklo, O.M., Barriuso, Enrique, Sveistrup, T., Kvaerner, J.
Other Authors: Environnement et Grandes Cultures (EGC), Institut National de la Recherche Agronomique (INRA)-AgroParisTech, Plant Health and Plant Protection Divison, Plant Health and Plant Protection Division, Soil and Environment Division
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
METRIBUZIN
TEMPERATURE
MICROBIAL DEGRADATION
SOIL SOLUTION
[SDV.BV]Life Sciences [q-bio]/Vegetal Biology
Northern Norway
Online Access:https://hal.science/hal-01191977
https://doi.org/10.1111/j.1365-3180.2007.00589.x
Description
Summary:Herbicide degradation in soils is highly temperature-dependent. Laboratory incubations and field experiments are usually conducted with soils from the temperate climatic zone. Few data are available for cold conditions and the validation of approaches to correct the degradation rate at low temperatures representative of Nordic environments is scarce. Laboratory incubation studies were conducted at 5, 15 and 28°C to compare the influence of temperature on the dissipation of metribuzin in silt/sandy loam soils in southern and northern Norway and in a sandy loam soil under temperate climate in France. Using 14C-labelled metribuzin, sorption and biodegradation were studied over an incubation period of 49 days. Metribuzin mineralisation and total soil organic carbon mineralisation rates showed a positive temperature response in all soils. Metribuzin mineralisation was low, but metabolites were formed and their abundance depended on temperature conditions. The rate of dissipation of 14C-metribuzin from soil pore water was strongly dependent on temperature. In Nordic soils with low organic content, metribuzin sorption is rather weak and biodegradation is the most important process controlling its mobility and persistence.

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