摘要
We studied the adsorption of glyphosate (GPS) onto soil mineral particles, using FT-IR and Mossbauer spectroscopy. From IR measurements for samples collected under native vegetation of a forest reserve, bands at 1632 and 1407 cm(-1) could be attributed to the interaction between the carboxylic group of GPS and structural Al(3+) and Fe(3+) on the surface of mineral particles; bands at 1075 and 1000 cm(-1) were observed only for cultivated soil. Mossbauer spectra for these soils were definitely fitted using a broad central doublet in addition to the magnetic component. This multiple quadrupolar component may be attributed to all non-magnetic Fe(3+) contributions, including that of the GPS/Fe(3+) complex.
- 出版日期2010