Sorption and mineralisation of S-metolachlor in soils from fields cultivated with different conservation tillage systems

作者：Alletto Lionel^*; Benoit Pierre; Bolognesi Benoit; Couffignal Matthieu; Bergheaud Valerie; Dumeny Valerie; Longueval Christian; Barriuso Enrique

来源：Soil and Tillage Research, 2013, 128: 97-103.

DOI：10.1016/j.still.2012.11.005

• Herbicide
• No-tillage
• Cover crop
• Soil properties
• Cropping system

Conservation tillage is promoted to improve the sustainability of agricultural systems and reduce the environmental impact of agricultural activities. These techniques strongly influence soil properties that can modify the fate of pesticides. S-metolachlor (SMOC) is a selective chloroacetamide pre- and post-emergence herbicide used on a variety of crops including maize, soybean, sunflower and sorghum and frequently detected in natural waters. The purpose of this study was to evaluate the effects of conservation tillage management, crop rotation, fallow period management and soil type on sorption and mineralisation of SMOC. During spring 2010, soil samples were collected from 51 agricultural fields located in the central basin of the Midi-Pyrenees (south-west France) at two depths in the topsoil layers (0-5 cm and 5-10 cm). Soils were mainly Calcisols, Luvisols and Cambisols. The SMOC adsorption coefficient (K-d) was measured for each sample using a batch equilibration technique. Mineralisation was monitored during laboratory incubations made at field capacity and 25 degrees C for 113 days. K-d values ranged from 0.8 to 8.7 L kg(-1) with a mean of 3.0 L kg(-1) and a CV of 44%. Sorption was positively correlated with organic carbon (OC) content (rho = 0.74) and negatively with pH (rho = -0.42). The presence of cover crop during the fallow period was found to enhance SMOC sorption. The mineralisation of SMOC after 113 days was found to be highly variable between samples and ranged from 0.8% to 28.3% of applied C-14-SMOC with a higher mineralisation in the 5-10 cm-depth samples. It was positively correlated with soil pH (rho = 0.58) and with total microbial biomass (rho = 0.32). Mineralisation was also negatively correlated with OC content (rho = -0.34) and adsorption coefficient K-d (rho = -0.49). A better correlation (rho = 0.66) was obtained between mineralisation and the ratio 'total microbial biomass/adsorption coefficient (K-d)' of each sample. This correlation could be interpreted as an illustration of the competition between retention and degradation, directly depending on the modification of soil organic matter and microbial activity by the different conservation tillage systems.

• 出版日期2013-4