Fate of glyphosate and its degradation products AMPA, glycine and sarcosine in an agricultural soil: Implications for environmental risk assessment
Graphical Abstract
Introduction
Glyphosate is one of the most widely used herbicide worldwide due to its great efficacy against a wide variety of weeds [5]. Glyphosate and its transformation product aminomethylphosphonic acid (AMPA) were most frequently found pesticides in agricultural European Union soils [34]. Such a widespread occurrence of both glyphosate and AMPA in soils triggers public concern about the safety of glyphosate use for the environment and humans [35]. Glyphosate can be biodegraded via two well-documented pathways: the AMPA and the sarcosine pathway [10], [35], [40]. The two pathways of glyphosate biodegradation result in formation of different intermediate products that have different environmental fate and implications for environmental risk assessment [24], [40]. For instance, the AMPA pathway produces persistent AMPA and glyoxylate which may further form amino acid glycine [40]; see Fig. 1). In contrast, the sarcosine pathway yields sarcosine which is readily oxidized to glycine [31], [37]. However, Li et al. [22] suggested that the C-N bond of glyphosate also can be cleaved directly to glycine bypassing sarcosine formation.
Isotope mass balance of the glyphosate fate comprising mineralization, extractable parent compound & its degradation products and non-extractable residues (NERs) was well documented in various soils [28] and in planted filters [19]. In contrast, the isotope mass balance studies of the fate of AMPA, glycine or sarcosine in soils are still lacking. Previous studies reported only half-life dissipation (DT50) of AMPA (151–173 days; [4], [15] in soils, as well as of glycine (0.89 day; [36] and sarcosine (0.99 day; [36] in the soil-water system.
The NERs that can be only determined using isotope tracers are often a ‘black box’ in the mass balance study of the chemical fate in soils due to their unknown identity [33]. The NERs are remaining residues of an isotope labeled parent chemical or its degradation product(s) in soils that cannot be extracted using aquatic or organic solvents [23]. The parent chemical or its degradation product(s) can be strongly sorbed to soils as hazardous xenobiotic NERs (NERsxenobiotic) with a remobilization potential and delaying the environmental risk [23], [33]. However, a chemical also can undergo microbial degradation accompanied with the formation of CO2 and microbial biomass [33], [21]. After the death of microorganisms, biomass compounds and in particular proteins are stabilized in soil matrix as harmless biogenic NERs (NERsbiogenic) [29], [33]. The NERsbiogenic can be a result of assimilation of inorganic C and N (CO2 or NH4+) or monomeric molecules (e.g. amino acids) from a biodegraded compound into microbial biomass [39]. When the NERsbiogenic constitute a major portion of the NERs, the environmental risks associated with the NERsxenobiotic formation will be overestimated [29]. The lack of information about the NER speciation is thus a ‘bottleneck’ in fate studies of chemicals since it impedes an assessment of environmental risks related to the NERsxenobiotic [33], [21].
The intermediates of glyphosate, AMPA, glycine or sarcosine may determine the NER speciation resulting from the glyphosate degradation (Fig. 1). We hypothesize that an enhanced transformation of glyphosate to AMPA in the AMPA pathway will result in an increased formation of hazardous NERsxenobiotic. The AMPA (DT50: 151–173 days) is more resistant to biodegradation than glyphosate (DT50: 7–60 days) [4], [15], [37]; and it is thus expected to be mainly sorbed to soils as NERsxenobiotic with release potential to waters [39], [4], [6]. In contrast, enhanced degradation of glyphosate via the sarcosine/glycine pathway accompanied with the glycine formation may yield NERsbiogenic. Both glycine and sarcosine are biomolecules, which are readily transformed to CO2 and microbial biomass [12], [22]. The glycine may be either assimilated as a monomeric ‘building block’ into microbial biomass and then into the NERsbiogenic or mineralized to CO2 or NH4+ which are then integrated into the biomass (see Fig. 1 and S1).
Formation of three degradation products of glyphosate and their proportions: AMPA, glycine and sarcosine can therefore determine environmental risks associated with the NERsxenobiotic formation during the glyphosate degradation in soil. To date, mass balance of the fate of the three glyphosate degradation products and in particular the formation of NERsbiogenic has not been reported. This information may help to predict more accurately the NER speciation (hazardous NERsxenobiotic versus harmless NERsbiogenic) of glyphosate in soil and which may stem from glyphosate intermediates. Therefore, the objectives of this study were (i) to elucidate the fate of glyphosate & its three degradation products: AMPA, glycine and sarcosine in soil microcosm experiments, and (ii) to determine the NERsbiogenic formation from these compounds using stable isotope double-labeling approach (13C + 15N). The 13C- and 15N-mass balance of the fate of 2-13C,15N-glyphosate, 13C,15N-AMPA, 13C2,15N-glycine and 13C3,15N-sarcosine was determined and comprised of mineralization (CO2), extractable residues (ERs) of parent compound & its degradation products and NERs. The NERsbiogenic were based on the quantification of 13C- or 15N-amino acids (13C- or 15N-AAs) hydrolyzed from soil proteins.
Section snippets
Reference soil
The soil used in this study was a haplic Chernozem collected from the topsoil of the Static Fertilization Experiment in Bad Lauchstädt (51° 22′ 0″ N, 11° 50′ 0″ E) located in Saxony-Anhalt, Germany. We used a Haplic Chernozem as a reference soil for this study, since this soil is commonly used for agriculture in Europe. The plot in Bad Lauchstädt received organic fertilizers (30 t ha−1 farmyard manure) every second year and had previous history of glyphosate (as Roundup) application. The soil
Mineralization
We observed distinct patterns of compound mineralization in our experiment (Fig. 2). Mineralization of 2-13C-glyphosate occurred without a lag phase, and it increased by day 46. Soil used in this experiment was sampled from a field which had previous history of glyphosate application as Roundup; therefore, glyphosate degrading microorganisms were most likely already present in the haplic Chernozem soil [27], [39]. At the end (75 days) of incubation, about 39 ± 0.3% of initially added 13C was
CRediT authorship contribution statement
Conceptualization: Aslam, Jing, Nowak, Data curation: Aslam, Jing, Formal analysis: Nowak Funding acquisition: Aslam, Nowak, Investigation: Aslam, Methodology: Aslam, Jing, Project administration: Nowak, Resources: Aslam, Nowak, Software: Aslam, Supervision: Nowak, Validation: Aslam, Jing, Visualisation: Aslam, Writing – original draft: Aslam, Nowak, Writing – review & editing: Nowak.
Declaration of Competing Interest
The authors declare the following financial interests/personal relationships which may be considered as potential competing interests: Karolina Nowak reports financial support was provided by Helmholtz Centre for Environmental Research - UFZ. Karolina Nowak reports financial support was provided by German Research Foundation. Sohaib Aslam reports was provided by Alexander von Humboldt Foundation.
Acknowledgements
This study was financially supported by the Alexander von Humboldt Foundation, German Research Council (DFG, No 980/3–1) and Helmholtz Centre for Environmental Research-UFZ. The authors thank S. Kümmel (UFZ, Dept. of Isotope Biogeochemistry) and A. Miltner for assistance in the measurement of compound-specific isotope analysis.
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