Large variation in glyphosate mineralization in 21 different agricultural soils explained by soil properties
Creators
- 1. Helmholtz Zentrum München, German Research Center for Environmental Health (GmbH), 85764 Neuherberg (Germany)
- 2. Cantho University, Department of Soil Science, Cantho City (Viet Nam)
- 3. Technische Universität München, Wissenschaftszentrum Weihenstephan für Ernährung, Landnutzung und Umwelt, 85354 Freising (Germany)
- 4. University of Ljubljana, Biotechnical Faculty, Jamnikarjeva 101, 1000 Ljubljana (Slovenia)
Description
Highlights: • Glyphosate mineralization ranged from 7 to 70% in 32 days, depending on soil composition. • Glyphosate degradation in soils is strongly and mainly influenced by exchangeable acidity. • A reliable parameter of soil potential to mineralize glyphosate is "NaOH-extractable residues". Glyphosate and its main metabolite aminomethylphosphonic acid (AMPA) have frequently been detected in surface water and groundwaters. Since adequate glyphosate mineralization in soil may reduce its losses to environment, improved understanding of site specific factors underlying pesticide mineralization in soils is needed. The aim of this study was to investigate the relationship between soil properties and glyphosate mineralization. To establish a sound basis for resilient correlations, the study was conducted with a large number of 21 agricultural soils, differing in a variety of soil parameters, such as soil texture, soil organic matter content, pH, exchangeable ions etc. The mineralization experiments were carried out with 14C labelled glyphosate at a soil water tension of −15 kPa and at a soil density of 1.3 g cm−3 at 20 ± 1 °C for an incubation period of 32 days. The results showed that the mineralization of glyphosate in different agricultural soils varied to a great extent, from 7 to 70% of the amount initially applied. Glyphosate mineralization started immediately after application, the highest mineralization rates were observed within the first 4 days in most of the 21 soils. Multiple regression analysis revealed exchangeable acidity (H+ and Al3+), exchangeable Ca2+ ions and ammonium lactate extractable K to be the key soil parameters governing glyphosate mineralization in the examined soils. A highly significant negative correlation between mineralized glyphosate and NaOH-extractable residues (NaOH-ER) in soils strongly suggests that NaOH-ER could be used as a simple and reliable parameter for evaluating the glyphosate mineralization capacity. The NaOH-ER were composed of glyphosate, unknown 14C-residues, and AMPA (12%–65%, 3%–34%, 0%–11% of applied 14C, respectively). Our results highlighted the influential role of soil exchangeable acidity, which should therefore be considered in pesticide risk assessments and management to limit efficiently the environmental transfers of glyphosate.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.scitotenv.2018.01.204Additional details
Identifiers
- DOI
- 10.1016/j.scitotenv.2018.01.204;
- PII
- S0048969718302456;
Publishing Information
- Journal Title
- Science of the Total Environment
- Journal Volume
- 627
- Journal Page Range
- p. 544-552
- ISSN
- 0048-9697
- CODEN
- STENDL
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 53034305
- Subject category
- S54: ENVIRONMENTAL SCIENCES;
- Descriptors DEI
- ALUMINIUM IONS; AMMONIUM COMPOUNDS; CALCIUM IONS; CARBON 14; GROUND WATER; HYDROGEN IONS 1 PLUS; INCUBATION; LACTATES; METABOLITES; MINERALIZATION; ORGANIC MATTER; PH VALUE; REGRESSION ANALYSIS; RISK ASSESSMENT; SODIUM HYDROXIDES; SOILS
- Descriptors DEC
- ALKALI METAL COMPOUNDS; BETA DECAY RADIOISOTOPES; BETA-MINUS DECAY RADIOISOTOPES; CARBON ISOTOPES; CARBOXYLIC ACID SALTS; CATIONS; CHARGED PARTICLES; EVEN-EVEN NUCLEI; HYDROGEN COMPOUNDS; HYDROGEN IONS; HYDROXIDES; IONS; ISOTOPES; LIGHT NUCLEI; MATHEMATICS; MATTER; NUCLEI; OXYGEN COMPOUNDS; RADIOISOTOPES; SODIUM COMPOUNDS; STATISTICS; WATER; YEARS LIVING RADIOISOTOPES
Optional Information
- Copyright
- Copyright (c) 2018 Elsevier B.V. All rights reserved.