Dissipation Of Metolachlor Research Articles

Degradation of Metolachlor in Tobacco Field Soil

The extensive use of metolachlor to control weeds in tobacco fields in China has aroused concern about its environmental fate. The aim of this study was to investigate the degradation and residue fate of metolachlor in tobacco field soil (silt loam) under laboratory and field conditions. In laboratory experiments, metolachlor in bulk soil exhibited fast degradation in a temperature range from 10 to 35°C and a soil moisture level of 20–80%, with half-lives (T1/2) from 66.7 to 28.8 days. The degradation rate of metolachlor decreased as the application dose increased. Owing to higher microbial populations and enzymatic activities, metolachlor rapidly dissipated in rhizosphere soil as compared to bulk soil. Field persistence of metolachlor was evaluated in the same soil during the tobacco (Nicotiana tabacum K326) growing season in 2012 and 2013. The dissipation of metolachlor followed the first-order kinetics and its T1/2 values were 11.7–13.5 days in soil and 9.0–9.6 days in green tobacco leaves, respectively. At harvest time, the residual levels of metolachlor in soil and green tobacco leaves were in the range of 0.626–1.623 and 0.083-0.481 mg kg−1, respectively. These findings might have practical implications for the fate of metolachlor residue in tobacco fields. Environmental factors, especially temperature and moisture, should be considered in combination with the appropriate application dose of metolachlor for achieving satisfactory weed-control efficacy, reducing runoff, and minimizing effects on environmental quality.

Impact of grass filter strips length on exported dissolved masses of metolachlor, atrazine and deethylatrazine: a four‐season study under natural rain conditions

AbstractHerbicides atrazine and metolachlor have been detected in water bodies across the world. The objective of this study was to assess the efficiency of 0‐m, 3‐m, 6‐m and 9‐m grass filter strips to reduce masses of dissolved metolachlor, atrazine and deethylatrazine (a degradation product of atrazine) exported in runoff. For that purpose, 16 uncultivated plots (3‐m wide × 65‐m long) with 0‐m‐, 3‐m‐, 6‐m‐ and 9‐m‐long grass filter strips were setup in a completely randomized block design. During four seasons, masses of dissolved atrazine, metolachlor and deethylatrazine were determined for the first four to five rain events, under natural rain conditions, after atrazine and metolachlor application. Generally, grass filter strips reduced exported herbicide masses by more than 90% and influenced atrazine and metolachlor dissipation kinetics in the field. The 3‐m grass filter strip (area ratio source/strip of 22:1) usually provided a reduction in exported herbicide masses similar to the 6‐ or 9‐m grass filter strips. Therefore, under the present experimental soil and climate conditions, a grass filter strip of 3 m would be a good compromise between environmental protection of surface waters against atrazine and metolachlor contamination and conservation of agricultural land use. Such an approach contributes to the acceptability by producers to implement optimized best management practices such as vegetated filter strips for the preservation of the quality of water resources.

Metolachlor and chlorothalonil dissipation in gypsum-amended soil

This work focused on the interactive effects of the fungicide chlorothalonil (2,3,4,6-tetrachloro-1,3-benzendicarbonitrile) and gypsum on the persistence of the soil-residual herbicide metolachlor (2-chloro-N-(6-ethyl-o-tolyl)-N-[(1RS)-2-methoxy-1-methylethyl]acetamide). Gypsum application was included due to its widespread use on peanut (Arachis hypogaea). Both agricultural grade gypsum and reagent CaSO4-2H2O were tested. A laboratory soil incubation was conducted to evaluate interactive effects. Results indicated 1.5X greater metolachlor half-life (DT50) in soil amended with chlorothalonil (37 d) as compared to control soil (25 d). The two gypsum sources alone increased metolachlor DT50 to about 32 d and with the combination of chlorothalonil and gypsum, DT50 was 50 d, 2-fold greater than the control. Chlorothalonil dissipation was rapid (DT50 < 4d). A possible explanation for metolachlor dissipation kinetics is a build-up of the chlorothalonil intermediate (4-hydroxychlorothalonil) which limited soil microbial activity and depleted glutathione S-transferase (GST) from chlorothalonil detoxification. Further information related to gypsum impacts is needed. Results confirm previous reports of chlorothalonil impeding metolachlor dissipation and showed the gypsum application extended persistence even longer. Farming practices, such as reducing metolachlor application rates, may need to be adjusted for peanut cropping systems where chlorothalonil and gypsum are used.

Reduction in Metolachlor and Degradate Concentrations in Shallow Groundwater through Cover Crop Use

Pesticide use during crop production has the potential to adversely impact groundwater quality. In southern Florida, climatic and hydrogeologic conditions and agronomic practices indicate that contamination risks are high. In the current study, dissipation of the widely used herbicide, metolachlor, and levels of the compound and selected degradates in shallow groundwater beneath six 0.15-ha plots in sweet corn (Zea mays) production were evaluated over a two-year period. During fallow periods (May to October), plots were either left bare or cover cropped with sunn hemp (Crotalaria juncea L.). Metolachlor was broadcast applied at label recommended rates prior to planting sweet corn each year. Groundwater monitoring wells hydraulically upgradient and downgradient, and within each plot were sampled biweekly. Results showed that metolachlor dissipation was rapid, as evidenced by the detection of relatively high levels of the metolachlor ethane sulfonic degradate (MESA) in groundwater beneath plots and a rapid metolachlor DT(50) (9-14 days) in a companion laboratory soil incubation. Other degradates detected included hydroxymetolachlor in soil and in groundwater metolachlor oxanilic acid (MOA) and a product tentatively identified as 2-chloro-N-(2-acetyl-6-methylphenyl-N-(2-methoxy-1-methylethyl) acetamide, a photo-oxidation product. Metolachlor and MESA levels, up to 16 and 2.4 times higher in groundwater beneath the noncover cropped plots when compared to those of the cover cropped plots, indicate that cover cropping results in more rapid dissipation and/or reduced leaching. The study demonstrated that integration of cover crops into agronomic systems in the region may yield water quality benefits by reducing herbicide inputs to groundwater.

Solute Transport in Eroded and Rehabilitated Prairie Landforms. 2. Reactive Solute

The impact of varying soil, landscape, and climate conditions on the off-site transport of pesticides must be determined to develop improved pesticide management practices. This study quantified the rate of S-metolachlor dissipation after fall and spring application in eroded and rehabilitated landforms in which topsoil was moved from the lower slope to the upper slope. Fall-applied metolachlor provided no control of annual grasses because approximately 80% was removed from the root zone during the winter and early spring, presumably by leaching and runoff. S-Metolachlor dissipated in the spring with a DT(50) of 24-29 days. These results suggest that fall-applied metolachlor may not provide economic weed control and presents an increased risk of water contamination. Although landscape position and bulk soil movement within the landform had a large impact on soil properties, no significant differences in metolachlor dissipation between different landscape positions and between eroded and rehabilitated landforms were observed.

Adsorption, desorption and dissipation of metolachlor in surface and subsurface soils

Variations in soil properties with depth influence retention and degradation of pesticides. Understanding how soil properties within a profile affect pesticide retention and degradation will result in more accurate prediction by simulation models of pesticide fate and potential groundwater contamination. Metolachlor is more persistent than other acetanilide herbicides in the soil environment and has the potential to leach into groundwater. Reasonably, information is needed about the dissipation and eventual fate of metolachlor in subsoils. The objectives were to evaluate the adsorption and desorption characteristics and to determine the dissipation rates of metolachlor in both surface and subsurface soil samples. Adsorption of metolachlor was greater in the high-organic-matter surface soil than in subsoils. Lower adsorption distribution coefficient (K(ads)) values with increasing depth indicated less adsorption at lower depths and greater leaching potential of metolachlor after passage through the surface horizon. Desorption of metolachlor showed hysteresis, indicated by the higher adsorption slope (1/n(ads)) compared with the desorption slope (1/n(des)). Soils that adsorbed more metolachlor also desorbed less metolachlor. Metolachlor dissipation rates generally decreased with increasing soil depth. The first-order dissipation rate was highest at the 0-50 cm depth (0.140 week(-1)) and lowest at the 350-425 cm depth (0.005 week(-1)). Degradation of the herbicide was significantly correlated with microbial activity in soils. Metolachlor that has escaped degradation or binding to organic matter at the soil surface might leach into the subsurface soil where it will dissipate slowly and be subject to transport to groundwater.

Spatial Variability of Atrazine and Metolachlor Dissipation on Dryland No‐tillage Crop Fields in Colorado

An area of interest in precision farming is variable-rate application of herbicides to optimize herbicide use efficiency and minimize negative off-site and non-target effects. Site-specific weed management based on field scale management zones derived from soil characteristics known to affect soil-applied herbicide efficacy could alleviate challenges posed by post-emergence precision weed management. Two commonly used soil-applied herbicides in dryland corn (Zea mays L.) production are atrazine and metolachlor. Accelerated dissipation of atrazine has been discovered recently in irrigated corn fields in eastern Colorado. The objectives of this study were (i) to compare the rates of dissipation of atrazine and metolachlor across different soil zones from three dryland no-tillage fields under laboratory incubation conditions and (ii) to determine if rapid dissipation of atrazine and/or metolachlor occurred in dryland soils. Herbicide dissipation was evaluated at time points between 0 and 35 d after soil treatment using a toluene extraction procedure with GC/MS analysis. Differential rates of atrazine and metolachlor dissipation occurred between two soil zones on two of three fields evaluated. Accelerated atrazine dissipation occurred in soil from all fields of this study, with half-lives ranging from 1.8 to 3.2 d in the laboratory. The rapid atrazine dissipation rates were likely attributed to the history of atrazine use on all fields investigated in this study. Metolachlor dissipation was not considered accelerated and exhibited half-lives ranging from 9.0 to 10.7 d in the laboratory.

Evaluation of microbial inoculation and vegetation to enhance the dissipation of atrazine and metolachlor in soil

Four greenhouse studies were conducted to evaluate the effects of native prairie grasses and two pesticide-degrading bacteria to remediate atrazine and metolachlor in soils from agricultural dealerships (Alpha site soil, northwest Iowa, USA; Bravo site soil, central Iowa, USA). The Alpha soil contained a low population of atrazine-degrading microorganisms relative to the Bravo soil. Each soil freshly treated with atrazine or metolachlor was aged for a short or long period of time, respectively. An atrazine-degrading bacterium, Agrobacterium radiobacter strain J14a; a metolachlor-degrading bacterium, Pseudomonas fluorescens strain UA5-40; and a mixture of three native prairie grasses-big bluestem (Andropogon gerardii Vitman), yellow Indian grass (Sorghastrum nutans [L.] Nash), and switchgrass (Panicum virgatum L.)-were added to the soils after the soils were aged for long periods of time. The soils aged for short periods of time were treated with J14a, the prairie grasses, or both after aging. The J14a and the grasses significantly reduced the concentration of atrazine in Alpha soil when the soil was aged for a short period of time. However, these treatments had no statistically significant effect when the soil was aged for a long period of time or on atrazine in Bravo soil. Inoculation with UA5-40 did not enhance metolachlor dissipation in either soil, but vegetation did increase metolachlor dissipation. Our results indicate that the dissipation of atrazine by J14a is affected by the presence of indigenous atrazine-mineralizing microorganisms and probably by the bioavailability of atrazine in the soil.

Degradation and persistence of metolachlor in soil: Effects of concentration, soil moisture, soil depth, and sterilization

The present study evaluated the influence of soil depth, soil moisture, and concentration on the persistence and degradation of metolachlor in soil. Greater percentages of metolachlor persisted in subsurface soils than in surface soil regardless of the soil moisture or initial herbicide concentration. Larger quantities of bound residues and extractable degradation products were found in the surface soils as a result of the increased soil sorption and biodegradation of metolachlor associated with the surface soil, which had more organic matter. Saturated soil favored the dissipation of metolachlor and the formation of soil-bound residues. Significantly greater quantities of a dechlorinated metabolite were measured in the saturated surface soil compared to the unsaturated soil. Mineralization of metolachlor to CO2 and volatilization of metolachlor or metolachlor degradates was minimal in surface and subsurface soils at both soil moistures and herbicide concentrations. Increased metolachlor concentrations did not inhibit microbial activity; however, the greater rate of application did result in the reduced percentage of applied [14C]metolachlor that was bound to surface or subsurface soil. A significant reduction in the quantity of extractable metolachlor degradates and unextractable soil-bound residues in sterile soil revealed the significance of biodegradation to the dissipation of metolachlor in soil.

Behaviour of metolachlor in tropical and mediterranean plain field conditions

The movement and dissipation of metolachlor [2-chloro-6′-ethyl- N-(2-methoxy-1-methylethyl) ace- o-toluidide] were evaluated in plain field wet tropical conditions in Martinique (French West Indies) and in a Mediterranean area (Languedoc, South of France). Adsorption parameters are discussed with the Freundlich equation, and desorption evaluated using a model with two compartments corresponding of two different energy levels. Higher clay content in tropical and ferrisol involved adsorption parameters ( K fa) higher than that found for the Mediterranean fluvisol, as also for K 1, K 2 and Q ads n desorption parameters. During our studies, rainfall was largerly more important in tropical conditions. As these two main factors (adsorption-desorption parameters and rainfall) partly conterbalanced each other, metolachlor aptitude to leaching appeared relatively moderate under the conditions chosen for this work. Half-life of the compound (in the 0- to 25-cm soil layer) varied from 21 to 31 days.

Atrazine and Metolachlor Dissipation in Soils Incubated in Undisturbed Cores, Repacked Cores, and Flasks

AbstractThis study compared three different laboratory methods for determining soil pesticide dissipation kinetics and pathways. The dissipation kinetics of the herbicides atrazine (2‐chloro‐4‐ethylamino‐6‐isopropylamino‐1,3,5‐triazine) and metolachlor (2‐chloro‐6′‐ethyl‐N‐(2‐methoxy‐1‐methylethyl)acet‐o‐toluidine) were examined in three soils (sandy loam, loam, clay loam) incubated for 63 d in flasks or intact cores (20 by 20 cm) under controlled moisture (field capacity) and temperature (25°C) conditions in the laboratory. The dissipation of metolachlor and atrazine were also examined in repacked cores of the loam soil adjusted to the field bulk density. The rates of atrazine or of metolachlor dissipation in soils incubated in flasks or in intact cores were indistinguishable (P&lt;0.05). The rate of net accumulation of extractable transformation products from radiolabeled atrazine and the rate of nonextractable residue formation in soils incubated in flasks and intact cores were likewise the same. However, the rate of dissipation of metolachlor, the rate of accumulation of atrazine transformation products, and the rate of formation of nonextractable atrazine residues were all significantly slower in repacked cores of the loam soil. These results indicate that, under controlled laboratory conditions, atrazine and metolachior dissipation occured at the same rate in undisturbed soil cores and in flask incubations with soil that had been disrupted by previous air‐drying and sieving. We conclude that, at least in some soils, structure need not necessarily be maintained in laboratory soil pesticide dissipation experiments.

Distribution and dissipation of metolachlor in soil columns

Abstract Distribution and dissipation of metolachlor [2‐chloro‐N‐(2‐ethyl‐6‐methylphenyl)‐N‐(2‐methoxy‐l‐methylethyl) acetamide] in a soil of Montpellier were evaluated in laboratory conditions for 8 weeks using 100 cm PVC pipes. The half‐lives of metolachlor varied from 31 to 54 days according to the application dose (1.2, 4.5 and 9 kg a.i./ha respectivelly). The rate of herbicide migration increased with stronger dose. Adsorption and desorption of metolachlor were studied in the same soil at three difierent depths. Soil Freundlich adsorption coefficients (Kfa ) were 1.0,0.7 and 0.6 for 0 to 10, 10 to 50 and 50 to 95 cm depths respectively. Desorption coefficients (K fd ) varied more slightly (3.6 ‐ 3.9). Ratio soil quantity/water volume may influence adsorption parameters.