Introduction

In practice, pesticides are usually applied simultaneously or one after another for crop protection, and this type of pesticide application often leads to a combined contamination of pesticide residues in the soil environment. Many interactions are possible, including those related to changes in the size or species composition of the soil microbial population, effects upon specific enzymatic reactions, or those related to physiochemical effects such as competition for adsorption sites (Singh et al. 2002a). As of now, numerous publications exist pertaining to the interactions between pesticides and soil microorganisms as is the case with the in pesticide combinations. On the other hand, the role of pesticide mixtures or pesticide degradation products in exerting influence on the persistence of parent compounds can be significant. For example, studies with a mixture of isoproturon and chlorothanoil showed that interactions between pesticides are possible in soil (Fogg et al. 2003).

Pendimethalin [N-(1-ethylpropyl)-2,6-dinitro-3,4-xylidine] is a preemergence dinitroaniline herbicide, which is commonly used for selective weed control in cotton, soybeans, maize, wheat, rice, peas, and vegetable crops. Persistence of pendimethalin (PDM) is influenced by cultivation practices, soil temperature, and moisture conditions, as well as soil type (Smith et al. 1997; Lee et al. 2000; Stranberg and Scott-Fordsmand 2004). PDM is characterized by low water solubility, moderate to high vapor pressure, strong adsorption to soil, and high octanol–water partition coefficients. The movement of this herbicide in surface runoff and leaching is expected to be low except where soil erosion results in sediment transport of the adsorbed herbicide (Stranberg and Scott-Fordsmand 2004; Chopra et al. 2010). The US Environmental Protection Agency has classified this herbicide as persistent-bioaccumulative toxics (Roca et al. 2009). The dinitroaniline herbicides are subject to a variety of biotic and abiotic transformation processes (Jaźwa et al. 2009; Stranberg and Scott-Fordsmand 2004; Singh et al. 2002b).

The insecticide thiamethoxam (3-(2-chloro-thiazol-5-yl methyl)-5-methyl-[1,3,5] oxadiazinan-4-ylidene-N-nitroamine) is a nitromethylene-derived neonicotinoid with contact, stomach, and systemic activity. Gupta et al. (2008) have conducted a laboratory study on the persistence of thiamethoxam a 90-day period. They have reported the half-life of 91–94 days under normal field capacity moisture regime. However, Karmakar et al. (2006) have reported half-life of 16.9 days. Though much work has been carried out on its bioefficacy as seed treatment or foliar spray, not much published information is available on its persistence and leaching behavior (Gupta et al. 2008).

Mancozeb [manganese ethylenebis(dithiocarbamate)(polymeric)complex with zinc salt] is an ethylene bisdithiocarbamate. In soil, mancozeb is metabolized to ethylene thiourea, ethylene urea, and ethylene bisisothiocyanate sulfide. The data concerning persistence of these substances in soil are not consistent and the reported values vary from 1 to 165 days (Rhodes 1977; Wauchope et al. 1992; Hanumantharaju and Awasthi 2004).

Metribuzin [4-amino-6-t-butyl-3-(methylthio)-1,2,4-triazin-5 (4H)-one] is a selective systemic herbicide used for pre- and post-emergence control of many grasses and broad-leaved weeds in soya beans, potatoes, tomatoes, sugar cane, alfalfa, asparagus, maize, and cereals. Metribuzin belongs to the group of triazinone herbicides and moderates persistence in soils, the half-lives measurements have been specified between 5 and 50 days. The decomposition of metribuzin in the environment is due to microbiological and chemical processes (Locke and Harper 1991).

Quantification of the fate of pesticides in the environment is therefore essential, but apparently very difficult. The decline of residues is estimated by simple first-order kinetics but this model is not adequate to describe the degradation of PDM, therefore empirical non-linear equations or mechanistic models have been used to describe existing bi-phasic degradation patterns (Zimdahl and Gwynn 1977; Walker and Bond 1977; Zimdahl et al. 1984, 1994; Leake et al. 1995; Tsiropoulos and Miliadis 1998; Lee et al. 2000). Additionally, there have been attempts to describe the non-linear decline of herbicide residues in soil, including bi-exponential kinetics model and the hockey-stick model (FOCUS 2006). This study was designed to reevaluate previous work on pendimethalin assuming that other empirical equations might compensate for the observed deficiencies in the first-order model. Our proposition was to use the non-linear empirical model assuming that the degradation rate of a herbicide in soil is proportional to the difference between the observed concentration of herbicide in soil at time (C) and concentration of herbicide in the last day of measurement (C L). It is described by differential equation:

$$ {\text{d}}C/{\text{d}}t = - k\left( {C-{C_L}} \right) $$
(1.1)

where t is the time (days), k is degradation rate constant (per day).

Integration of this differential rate equation yields:

$$ C\left( {\text{t}} \right) = \left( {{C_0}-{C_L}} \right)\cdot {e^{{ - kt}}} + {C_{\text{L}}} $$
(1.2)

where C(0) = C 0 is the initial concentration, C L is the residue of herbicide in soil in the last day of measurement.

This function has a horizontal asymptote:

$$ \begin{array}{*{20}{c}} {\lim C\left( {\text{t}} \right) = {C_{\text{L}}}} \\ {{\text{t}} \to \infty } \\ \end{array} $$
(1.3)

For half-life (DT50) for a herbicide, we have:

$$ {\text{D}}{{\text{T}}_{{50}}} = \frac{1}{k}\ln \frac{{2 \cdot \left( {{C_0} - {C_L}} \right)}}{{{C_0} - 2 \cdot {C_L}}}\quad {C_{\text{L}}} < 0.5{C_0} $$
(1.4)

where C 0 is the initial concentration (milligrams per kilogram of soil), C L is the residue of herbicide in soil in the last day of measurement (milligrams per kilogram of soil), k is the degradation rate constant (per day).

The main objective of this study was to provide a better understanding of the interaction mechanisms involved in degradation of PDM in soil considering various mixtures of pesticide in controlled conditions. This study compares residual concentration after application of pendimethalin (herbicide), mancozeb (fungicide), thiamethoxam (insecticide), and metribuzin (herbicide). This research also examines the role which a mixture of chemicals plays in pendimethalin degradation. The two incremental objectives for this study are: (1) to determine the rates of PDM in the various mixtures, type of soils, and soil moistures, (2) to compare two models: the first-order kinetic model and a new non-linear differential model (Eq. 1.1).

The choice of pendimethalin as a model herbicide was somewhat arbitrary, except that it has been widely used in Poland for many years. This herbicide is one of several preemergence herbicides available for controlling weeds that invade potato crops.

Materials and methods

Commercial formulations of pendimethalin (Stomp 330 EC, 330 g a.i. l−1, BASF), mancozeb (Dithane NeoTec 75 WG, 75 g a.i. kg−1, Dow AgroSciences), thiamethoxam (Actara 25 WG including 25 g a.i. kg−1, Syngenta Crop Protection), metribuzin (Sencor 70WG, 70 g a.i. kg−1, BayerCropScience AG), and analytical grade of PDM were used throughout these studies.

Two soils were used for all studies. The first was a sandy loam from Lipnik with textural composition of 72% sand, 16% silt, and 12% clay. This soil had a pH of 6.4, organic matter 1.7%, and cation exchange capacity of 2.20 cmol kg−1. The second Ostoja soil was a clay loam with 40% sand, 34% silt, 26% clay, 1.5% organic matter, and a pH of 6.3. Both soils are commonly used in agricultural production, and all soil characteristics presented describe the 0- to 10-cm soil zone. The sandy loam and the clay loam were collected from upper layer of soil (0–10 cm), air-dried and finally screened through a 3-mm sieve.

Portions of soil (450 g) were treated with aqueous solution of PDM alone, and four mixtures: (1) pendimethalin and mancozeb; (2) pendimethalin and thiamethoxam; (3) pendimethalin and metribuzin; (4) pendimethalin, mancozeb, and thiamethoxam. Persistence of PDM in soil under laboratory condition was studied using PDM concentration of 2 mg kg−1 air-dried soil, mancozeb at 2.1 mg kg−1, metribuzin at 2.0 mg kg−1, thiamethoxam at 10 mg kg−1. The pesticide solutions were used to adjust the water content of the soil to 60% of field capacity.

In the second part of the study, soils were treated with aqueous solution of PDM alone, and three mixtures: (1) pendimethalin and mancozeb; (2) pendimethalin and thiamethoxam; (3) pendimethalin, mancozeb, and thiamethoxam under 30% and 90% of field capacity. We used the same concentrations of pesticides, as above. After mixing the soil, samples were transferred to jars and incubated at 22°C ± 2°C. All treatments were replicated three times. The jars were opened once a week, for the sake of aeration and the water content was adjusted by weighing. Three 50-g samples of each soil were taken for herbicide residue analysis 1 h after the initial mixing, and 2, 10, 15, 30, 45, 60, 90 days after treatment. All treatments were replicated three times. A 50-g portion of each sample was taken for moisture measurement and 50-g soil samples were shaken for 1 h on a wrist-action shaker with 100 mL of acetone. After shaking, the soil was allowed to remain in contact with the extracting solvent for further 20 h before being shaken for another 1-h period. The extract was filtered through a Whatman no.2 filter paper in a Buchner funnel. After the final extraction, the soil was rinsed with several portions of acetone. To the acetone extract 25 mL distilled water and 75 mL n-hexane were added in a separatory funnel and that was shaken to transfer the PDM into the hexane phase. The hexane layer was collected, and stored over anhydrous Na2SO4. The extract was evaporated to obtain 2 mL and cleaned on a Florisil column, gas chromatography on Carlo Erba-Vega 6180 as capillary. Recoveries for soil fortified at the 2 mg kg−1 level were 98% ± 4% for PDM (Swarcewicz 2002).

Data on soil degradation of PDM were subjected to one-way analysis of variance. Homogeneous groups were formed on the base of multiple range Tukey's test. All statistical hypotheses were verified at the significant level 0.05. Plots of models predicting curves were obtained with the non-linear regression procedures, available with Statistica package. Values of the estimated parameters in Eq. 1.1 and the first-order reaction were found using the Lavenberg–Marquardt method. As a measure of approximation for accuracy of theoretical curves in relation to experimental data we accepted the determination coefficient (R 2), which can be calculated as a square of the correlation coefficient between the observed and estimated values.

Results and discussion

Effect of pesticide mixtures

In the present study, measurements of the residual pendimethalin (PDM) concentration in four pesticide mixtures were compared with disappearance of this herbicide alone in the two soils under various soil moisture. The values of DT50 increased from 26.9 to 62.2 days in sandy loam (Table 1) and from 44.4 to 63.3 days, when PDM was alone and in mixture with mancozeb and thiamethoxam in clay loam at 60% of field capacity, using Eq. 1.4. The dissipation curves for PDM had the initial rapid rate of loss and were slower after 30 days (Fig. 1). Presence of mancozeb in both soils can also significantly influence the rate of disappearance of PDM (DT50 46.1 and 63.9 days, respectively). No significant effect was noticed when the substance in soils was thiametoxam (Table 1). Presence of metribuzin in soil did not affect the behavior of PDM in soil. In most agronomic situations, any single herbicide treatment is frequently a small part of the overall crop protection program. This often involves a sequence of herbicide, fungicide, and insecticide applications. There is not much information available about the behavior of multiple applications of either individual or combinations of pesticides. Many interactions are possible, including those related to changes in the size or species composition of the soil microbial population (Hurle and Walker 1980) to effects on specific enzymatic reactions (Kaufman and Edwards 1982), or to physicochemical effects such as competition for adsorption sites. PDM is known to be strongly adsorbed by soil and organic matter, possibly due to its high potential for hydrogen bonding (Weber 1990), resulting in a decrease of mobility and bioavailability of this compound. The clay content of soil may be also important in determining a herbicide persistence. Analysis of PDM variance residues in soil in controlled conditions showed a significant difference between soil types. The degradation rates of PDM in soil in presence of other pesticides also decreased as clay content increased, presumably because of increased adsorption, hence a decreased availability for degradation in heavier soil. A mixture of PDM, thiamethoxam, and mancozeb significantly inhibited the rate of degradation of PDM (Table 1). Similar observations have been reported for PDM and mancozeb in pot and field experiments in our early study (Swarcewicz 2002). Study of Wybieralski et al. (2000) and Swarcewicz et al. (2003) showed that mancozeb and its mixture with the insecticides bromfenvinphos, diazinon, and metribuzin affected the respiration and nitrification processes in a loamy sand. This suggested that mancozeb could influence the biodegradation of PDM in soil, too. The effect of different herbicides, fungicides, and insecticides on the degradation of PDM in the soil was investigated by Plieth and Börner (1985). The results showed that in presence of mecoprop salt, triadimefon, thiophanate methyl, bromophos, and oxydementon methyl did not influence the decomposition of PDM in field conditions. The loss of both triallate and trifluralin from the plots treated with the mixture was the same as from plots treated with the individual compounds (Smith 1979). This result is in contrast with a study regarding the other pesticides. Kaufman (1966) showed that dalapon is more persistent in soil when applied in combinations with amitrole. This increased persistence was probably affected through the inhibition of dalapon-decomposing microorganism by amitrole. The same effect showed Fogg et al. (2003) for isoproturon DT50 values increased from 18.5 to 71.5 days in the presence of chlorothalonil in topsoil. The preplant fumigant Vorlex can induce destruction of soil fungi resulting in an increasing persistence of linuron (Smith 1982). From the few studies reported, it may be concluded that the breakdown of major herbicides is not being significantly affected by application in combination with other herbicides. It was confirmed in this study. This may not be true when herbicides are applied to soils receiving treatments of fungicides and insecticides which tend to appear more toxic to soil microorganisms than herbicides, and clearly more research in this area would be desirable. In this study, mancozeb as a fungicide has more significantly affected the persistence of PDM than insecticide thiamethoxam.

Table 1 Influence of the presence of other pesticides on dissipation of pendimethalin in soil at 60% of field capacity and incubated at 22°C ± 2°C
Fig. 1
figure 1

Dissipation of pendimethalin alone and in mixture with mancozeb and thiametoxam in soils under 60% of field capacity, using the differential model. Symbols are average of three replications, and bars represent 95% confidence intervals. Black square pendimethalin alone; white square pendimethalin plus mancozeb plus thiamethoxam

Effect of soil moisture

Dissipation of PDM proceeds more rapidly under flooded, anerobic conditions than cold or dry conditions (Stranberg and Scott-Fordsmand 2004; Kulshrestha and Singh 1992). Zimdahl et al. (1984; 1994) suggested that soil type may have less influence than temperature and soil moisture. It was the reason why in the second part of study, PDM dissipation in two soils under three moisture levels and three mixtures of pesticides was performed. Results showed that increasing the moisture level in soil from 30% to 90% of field capacity could result in an almost fourfold increase of degradation rate of PDM alone in sandy loam and clay loam (Table 2). It confirmed early studies of Walker and Bond (1977), Kulshrestha and Singh (1992), Savage (1978) that persistence of several dinitroaniline herbicides was affected by soil moisture. Combinations with thiametoxam and mancozeb showed the same correlation only in sandy loam soil. Persistence of PDM was almost doubled under 60% of field capacity in sandy loam soil. Combination with mancozeb and thiametoxam influenced on the PDM more prominently under 90% than at 60% of field capacity in clay loam soil. Figure 2 showed comparison of dissipation of PDM alone and in the presence of mancozeb in two soils under two extreme moisture levels (30% and 90% f.c.). In this case, the PDM was more persistenct in clay loam than sandy loam soil and the presence of mancozeb influenced on herbicide, too. This study indicated that effect of soil moisture on dissipation and adsorption of xenobiotics mixture can be different depending on the kind of soil.

Table 2 Influence of the presence of other pesticides on dissipation of pendimethalin in three soil moisture contents in the laboratory and incubated at 22°C ± 2°C
Fig. 2
figure 2

Comparison of pendimethalin dissipation alone and in the presence of mancozeb in soils under two moisture levels (30% and 90% fc), using the differential model. Symbols are average of three replications, and bars represent 95% confidence intervals. black square pendimethalin alone at 30% fc; black triangle pendimethalin alone at 90% fc; white square pendimethalin plus mancozeb at 30% fc; white triangle pendimethalin plus mancozeb at 90% fc

Comparison of models

Several mathematical equations have been used to describe pendimethalin (PDM) degradation in soil (Lee et al. 2000). In this study, using bi-phasic degradation was not adequate. A bi-exponential equation was superior for describing PDM dissipation in the field studied by Zimdahl et al. (1994). To illustrate different ways of quantifying PDM degradation rates in soil, Eq. 1.2 was used and a comparison to simple first-order model was applied. The simple first-order model was empirically fitting to data and R 2 from 0.938 to 0.979 was obtained. The linear regression analysis of concentration of PDM against time of incubation was statistically significant (P < 0.05) for each treatment, and the calculated half-lives are shown in Table 3. The half-life values of PDM alone were ranged from 42 to 62 days depending on the type of soil. The first-order model however, commonly underestimates the initial rate and over-estimates the final rate. It was the reason for using modification of the first-order reaction as a new differential model (Eq. 1.1). The constant rates of PDM in soil from 32 · 10−3 to 49 · 10−3 day−1 and R 2 from 0.994 to 0.998 were obtained (Table 3). Prediction of pesticide concentration in soil is a significant part of the data package submitted for pesticide registration (Beulke and Brown 2001). The equation chosen to describe dissipation determines whether or not the presence of xenobiotic residues in soil may influence the value of PDM residues as compared in this study. The results of these experiments also indicate that soil properties and climatic factors are much more important than the presence of xenobiotic residues in soil. The differential model may be useful for simple and fast adjusting of data to a mathematical equation.

Table 3 A comparison of pendimethalin constant rates, half-life, correlation coefficients in the presence of other pesticides in two soils under 60% of field capacity derived from the first-order kinetic and differential model

Crop protection products are commonly applied as formulations where the active ingredient can be present at higher concentration. Inert ingredients can be solvents, carriers, surfactants, synergists, polymers, UV absorbers, dyes, and others, which are added in various amounts. Further studies of the persistence of crop protection agent combinations in soil may provide insight into the mechanism of degradation of other herbicides and may suggest other ways in which formulations may be modified to control rates of loss.