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Pesquisa Agropecuária Brasileira

Print version ISSN 0100-204XOn-line version ISSN 1678-3921

Pesq. agropec. bras. vol.41 no.3 Brasília Mar. 2006 



Imazaquin sorption in surface and subsurface soil samples


Sorção do imazaquin em amostras de solos superficiais e subsuperficiais



Maurílio Fernandes de OliveiraI; Hélio Teixeira PratesI; Derli Prudente SantannaI; Rubem Silvério de Oliveira JúniorII

IEmbrapa Milho e Sorgo, Rod. MG 424, Km 65, Caixa Postal 151, CEP 35701-970 Sete Lagoas, MG, Brasil. E-mail: maurí,,
IIUniversidade Estadual de Maringá, Dep. de Agronomia, Av. Colombo, nº 5.790, CEP 87020-900 Maringá, PR, Brazil. E-mail:




The objective of this work was to study the sorption and desorption of imazaquin, in surface and subsurface soil samples from Brazil. Sorption and desorption steps were carried out using batch equilibration and high performance liquid chromatography analytical routines. The value of Kf,ads was positively correlated with clay content, and negatively correlated with pH of supernatant. Samples from Typic Haplustox, clayey soil profile having high clay content, provided higher Kf,ads values, and negative correlation with organic carbon, silt content, cation exchange capacity and pH.

Index terms: retention, desorption, oxisol, sustainability.


O objetivo deste trabalho foi estudar a sorção e dessorção do herbicida imazaquin em amostras de solos brasileiros, superficiais e subsuperficiais. Para os ensaios de sorção e dessorção, utilizou-se metodologia de equilíbrio de partição e quantificação por cromatografia líquida de alto desempenho. Os valores de Kf,ads foram positivamente correlacionados com os teores de argila, e negativamente correlacionados com o pH do sobrenadante. Para as amostras do Latossolo Vermelho férrico textura argilosa, maiores teores de argila acarretaram maiores valores de Kf,ads, e a correlação com carbono orgânico, silte, capacidade de troca catiônica e pH foi negativa.

Termos para indexação: retenção, dessorção, latossolos, sustentabilidade.




The sustainable use of a soil should be based on the knowledge of its mineralogical, morphological, physical, chemical and biological characteristics, and also on its interactions with chemicals. The fate of chemicals in tropical soils has only recently been the subject of systematic research (Racke et al., 1997), and only in a limited number of countries. In Brazil, herbicides are the most important class of pesticides, representing 55–60% of the total annual comsumption of agrochemicals (Inoue, 2002).

Imazaquin is an imidazolinone herbicide widely used as a selective soil-applied herbicide for broadleaf weed control in soybean in Brazil. In general, the behavior of imidazolinones in soil is strongly affected not only by pH (Oliveira Júnior et al., 2001; Regitano et al., 2001), but also by organic carbon (OC) content and soil texture (Regitano et al., 2001), mineralogy (Regitano et al., 1997; Rocha et al., 2003) and water retention (Regitano et al., 2002).

Imazaquin has a unique group of acid-base properties, due to the presence of carboxylic and quinoline groups in its structure, which are both ionizable. Several factors such as speciation, soil-solution and sorbent-surface pH, charge, ionic strength, and solution composition must be considered due to its amphoteric nature, in order to successfully predict sorption by soil (Regitano et al., 1997, 2001; Rocha et al., 2003).

Imazaquin speciation is the main factor influencing sorption by soil. Soil pH influences both sorption and herbicide activity, because it affects the ionic character of soil, of organic matter and clay. At the most common pH range for tropical soils (pH 5.0–6.5), imazaquin behaves predominantly as an organic anion in a 99% ionized form (Lee et al., 1990), causing low sorption by soil colloids, which are also negatively charged at this pH range. However, organic matter (pKa ~ 5.2) can react with polivalent cations, forming chelates or ionic bridges with acid herbicides decreasing pH effect (Renner et al., 1988). As the pH decreases, imazaquin achieves the neutral form, which increases its sorption to soil organic matter, through hydrophobic interactions. However, this fenomenon has been observed mainly in soils from temperate areas, where organic matter plays important rule on imazaquin sorption. At very low pH values (lower than the pKa value), protonation of quinoline group may occur, resulting in a molecule that is able to form cationic bonds with soil particles (Regitano et al., 2001; Rocha et al., 2002), especially with negatively charged minerals such as iron and aluminum oxides in oxisols.

Sorption of imazaquin increased with pH variation from 8 to 3, and soil sorption capacity of soil was not reached at pH 3 (Renner et al., 1988). The increase in imazaquin sorption under acidic conditions is attributed to positively charged molecule bonds with the soil, especially, pH dependent minerals, such as kaolinite and iron/aluminum oxides (Regitano et al., 1997). In Brazil, the acric soils group comprehend the end point of the weathering scale and can have a net positive charge in the B horizon (Alleoni & Camargo, 1995), due to low organic matter and to high Fe and Al oxides. In these soils, the values of point of zero salt effect (PZSE) – the pH value where the sum of the negative and positive charges on the soil surfaces is equal to zero – are higher than those of the temperate soils, and even higher in subsurface horizons. However, weakly sorbed molecules at neutral or alkaline pH may represent a potential leacher in soil. In this case, leaching may transfer the herbicides to deeper soil layers with different properties, as compared to surface layers. Variations in soil properties with depth can affect retention, movement, and degradation of herbicides (Felding, 1997; Jenks et al., 1998).

The objective of this study was to measure the sorption and desorption behaviour of imazaquin, by a range of surface and subsurface Brazilian soils.


Material and Methods

Soils in this study were collected from 0–15 cm depth, air dried, and passed through a 2 mm sieve. According to Sociedade Brasileira de Ciência do Solo, soils are classified as: Latossolo Vermelho distrófico textura média (quartzipsammentic Haplustox, DRm), Latossolo Vermelho distroférrico textura argilosa (Clayey Rhodic Haplustox, PL) and Gleissolo Háplico textura média (quartzipsammentic Aeric Fluvaquent, HG). These soils, considered as standards by Brazilian Environmental Agency (Ibama), were collected in the Universidade de São Paulo, campus "Luiz de Queiroz", in Piracicaba, SP. The fourth sampled soil was a Latossolo Vermelho férrico (Typic Haplustox, THx), collected from Embrapa National Maize and Sorghum Research Center (Embrapa Milho e Sorgo), located at Sete Lagoas, MG, Brazil. For this specific site, a soil profile was sampled every 15 cm, from top, down to 120 cm depth.

Selected chemical, physical and mineralogical attributes of soil samples are listed in Table 1: organic carbon (OC) content was determined by the Wakley-Black method (Nelson & Sommers, 1982); pH by a 1:2 soil:water ratio; soil texture was determined by the hydrometer method (Gee & Bauder, 1986); and soil moisture by gravimetric method. Clay mineralogy data was adapted from Sans (1986) for THx soil sample, and from Silva et al. (1996) for DRm and PL soils.

Technical grade imazaquin (99.6% w/w pure, supplied by Brazilian Cyanamid) was used without further purification. Fresh imazaquin stock solutions were prepared for each experiment, by dissolving herbicide overnight in 0.01 M CaCl2 solution. All the analytical procedure was accomplished at room temperature (27±1ºC).

To determine equilibration time, 10 mL of imazaquin 4 mg L-1 solution were added to 10 g of soil in 60 mL centrifuge tubes and shaken at room temperature. The supernatant was removed from each tube after 1, 5, 9, 24 and 48 hours of soil-solution contact. The supernatant was centrifuged for 10 minutes at 2,200 rpm (921.53 g), and stored in freezer (-15ºC) until analysis. All samples were run in duplicates. Equilibration time was stablished as the necessary time for the herbicide concentration remains constant for 34 hours (Ibama, 1996).

Herbicide concentration in solution was determined by HPLC. Solutions were analyzed directly by injecting 100 µL of imazaquin solution into a 15 cm by 4.6 mm ODS Adsorbosil C18 column. Isocratic elutions were performed at a 1 mL min-1 flow rate, with a mobile phase of 50% acetonitrile, in water at pH 3 (calibrated with 0.04% phosphoric acid), and detected at 240 nm wavelenght. Peak area was used for residue quantification. The amount of imazaquin sorbed to soil was calculated from the difference between the initial and remaining concentration in solution after equilibration.

Sorption coefficients were measured in seven imazaquin concentrations for each isotherm at a 1:1 soil:solution ratio for DRm, PL, THx and 1:8 soil: solution ratio for HG. Therefore, 10 g of the soils DRm, PL, THx and 1.25 g of the soil HG were placed in 60-mL centrifuge tubes. Ten millilitres of 0.01 M CaCl2 solution were added to the tubes containing imazaquin at concentrations of 0, 0.3, 0.6, 1, 1.3, 1.6 and 2 mg L-1 in DRm and PL soils, and 0, 0.5, 1, 1.5, 2, 3 and 4 mg L-1 for HG and THx soils. Higher concentrations were used in this study to facilitate imazaquin detection in desorption experiments. The soil:solution ratio was chosen from previous experiments, which stablished the ratios that would permit that not less than 20% or not more than 80% of the total herbicide applied would sorb to soil in a 24-hour period). Duplicate samples were run for each imazaquin concentration. Tubes were then placed on a shaker (200 rpm for 24 hours), at room temperature (26±1ºC).

After equilibration, tubes were centrifuged at 2,200 rpm (921.53 g) for 10 minutes. The supernatant was filtered through a 0.45 µm polyvinilidene difluoride (PVDF) membrane filter, to remove any particulate material. Preliminary experiments to test how much of the herbicide can be retained by the filters and glassware showed that sorption was <1%. The suspensions were analyzed as already described.

Desorption of imazaquin was determined in tubes after sorption analysis. A volume of 0.01 M CaCl2 herbicide-free solution was added to the soil pastes, that remained in tubes after sorption experiments, until complete 10 mL. The suspensions were shaken for 24 hours and centrifuged at 2,200 rpm for 10 minutes. Aliquots of the supernatant were filtered, stored and analyzed as described above. The amount sorbed in the desorption steps was calculated by subtracting the amount of imazaquin in the entrapped solution after sorption experiments, from the solution concentration measured in this step, desorption experiment.

For sorption and desorption procedures, the pH of the supernatant was measured before the injection of the samples in the HPLC. Sorption and desorption were described by the Freundlich equation (Green & Karickhoff, 1990) X = Kf C1/n, where X is the amount sorbed (mg kg-1), C is the equilibrium concentration (mg L-1), and Kf and n are constants. Nonlinear regression was used to fit Freundlich equation to the sorption isotherms with Kf,ads and nads (sorption), Kf,des and ndes (desorption) as fitting parameters.

The OC normalized sorption constant (Kfoc) was calculated by normalizing Kf,ads to the OC fraction of each soil sample: Kfoc = (Kf,ads/%OC) 100.


Results and Discussion

Preliminary studies demonstrated that equilibration time is to be completed within 24 hours, with no imazaquin degradation occurring over this period (Regitano et al., 1997, 2001). Freundlich parameters adjusted for sorption and desorption of imazaquin are in Table 2. Except for PL soil, all 1/n values for sorption were lower than unity, indicating a nonlinear relationship between imazaquin concentration and its retention in soil.

The values of Kf,ads for imazaquin ranged from 0.25 to 11. Regitano et al. (2001) studying the imazaquin sorption on oxisols, with similar physical chemistry properties, found different Kf,ads values ranging from low to moderate (Kf<3 for most oxisols), except to HG, in which Kf was 19.29. While these authors used 1:2.5 soil-solution ratio to measure the Kf, for all soils studied in this work a 1:1 soil-solution ratio was used, except for HG. For the HG soil sample, a 1:8 soil-solution ratio was used in this study explaining the lowest value obtained, compared with the Kf,ads value obtained by Regitano et al. (2001). Normally, large soil-solution ratio promotes lower herbicide retention compared with the straight ones. Another reason that can explain the highest Kf values, obtained in this study, can be attributed to the highest clay content in the soils, compared with the ones used by Regitano et al. (2001), especially, for the subsurface soil samples (i.e. THx samples). Except for the HG soil, all the other samples belong to the same soil class having a similar mineralogy and texture (Table 1). From this result, it can be observed that a good comparison between Kf,ads values might be done between soils of the same class or the ones having similar mineralogy.

The lowest imazaquin retention for the DRm soil, in both sorption and desorption studies, is due to an accumulative effect of low clay content and high pH. At pH 6.7, approximately 99.8% of imazaquin molecules are in anionic form (Lee et al., 1990) having repulsion from the soil particles also negatively charged. Rocha et al. (2002) also described very low imazaquin sorption on oxisols having high pH values, compared with the ones having low pH. In the present study, for the DRm soil sample, the supernatant carted more than 72.4% of the initial concentration, in all concentrations after the sorption step (Table 3). Data in Table 3 provide evidences that the largest concentration of imazaquin in solution were obtained with the surface soil samples (0–15 cm), i.e., those with highest pH values. Smaller amounts of imazaquin in solution were obtained with the subsurface soil samples – THx, where lower pH values were found.

For PL soil sample, Kf,ads value is almost six times higher than that obtained by Regitano et al. (2001), with the same soil. Again, the highest Kf,ads value obtained in this study is due to the 1:1 soil:solution ratio used. The amount of sorbed imazaquin, which remained in the supernatant after desorption experiment for PL and HG samples, decreased compared with the other soil samples (Table 3). The imazaquin Kf,des for PL increased almost 7 times while for HG it decreased almost 50% (Table 2). This result showed that imazaquin has stronger affinity for the PL sample compared with the HG sample, especially after desorption experiment. Since the HG sample had highest sorption (Kf,ads), its desorption seems to be more easily compared with the PL sample. In this situation, it can be expected more imazaquin leaching on the organic soil, compared with the PL soil sample. The strongest imazaquin affinity by the PL sample is due to its highest amount of Fe2O3 and gibbsite (27.8 and 22.0%), compared with other samples, which had almost half amount of these minerals (Oliveira, 1998).

The highest values of Kf,ads of imazaquin were obtained in soils with higher clay contents and low pH value (Table 4), as it was also observed by several authors (Regitano et al., 1997, 2001; Rocha et al., 2002). These two soil properties were related each other which is shown by the negative correlation between pH and clay content (Table 4). Generally, the pH value of the THx subsurface samples were low, compared with the other surface samples. At this pH value range (from 4.2 to 4.6), approximately, 71 to 86% of imazaquin molecules are in anionic form (Lee et al., 1990). At this pH range (Table 2) these soils samples, mainly constituted of iron and aluminum oxides, may have developped a net negative charge because their point of zero salt effects (PZSE) are around 3.1 (Hyun et al., 2003). Therefore, cationic connections can be expected between the anionic herbicide and the positive sites of the oxides, as described by Rocha et al. (2002). Such influence of iron and aluminum oxides has also been shown for other ionic compounds, such as 2,4,5-T and imazaquin (Regitano et al., 1997, 2001), pentachlorophenol (Hyun et al., 2003) and prosulfuron (Hyun & Lee, 2004). Besides, this high retention of imazaquin can also be explained by the narrow soil: solution relationship adopted in this study (Koskinen & Cheng, 1983). Moreover, as pH decreases, the amount of imazaquin neutral species increases, and consequently, sorption is also expected to increase, due to hydrophobic interactions with soil organic matter, as observed by Regitano et al. (1997, 2001), or interactions with siloxane surfaces on the clay minerals (Regitano et al., 2001; Johnston et al., 2001, 2002).



Oliveira Junior et al. (1999) studying imazethapyr sorption proposed that the higher sorption of this herbicide, in more acidic conditions, could be an effect of its water solubility reduction, once the herbicide partition in organic surfaces is usually inversely correlated to Kow coefficient. However, even the pH has indicated possibly interaction between imazaquin and organic carbon in a neutral condition, no significant correlation was found between these two parameters, neither for surface nor subsurface soils (Table 4).

The organic carbon content and the CEC of the THx samples increased the amount of imazaquin in solution on the sorption step (Table 4), indicating that around pH 4.3 (pH level of those samples), both the herbicide molecules and organic carbon were in anionic form. Although the pH of these samples had shown similar values, no significant correlation between imazaquin sorption and pH can be observed (Table 4). In this situation, the amount of imazaquin sorbed can be described as a reaction of organic carbon, with polivalent cations forming chelates or ionic bridges with acid herbicides, decreasing the pH effect (Renner et al., 1988). These results indicated that the nature of the organic carbon (i.e. degree of degradation, acidity) in the oxisol might play an important role on pesticides sorption.

As well as clay content, moisture content showed a positive and significant correlation with values of Kf,ads of imazaquin (Table 3). The increasing imazaquin retention with increases in moisture content can be attributed to the hydration of clay/iron oxides under low pH. In these conditions, kaolinite and oxides link to water molecules forming an eletropositive surface (for instance, iron oxides as FeOH2+) (Koskinen & Harper, 1990; Schwarzenabach et al., 1992), which leads to higher sorption of the herbicide (Regitano et al., 2001, 2002). Baughman & Shaw (1996) also verified high retention of imazaquin, under high soil moisture conditions, especially in the pH range from 3 to 8, and concluded that this could be an important factor controlling its sorption in soil.

The values of Kf,ads of imazaquin (Table 2), in general, increased with sampling depth, following a similar pattern as compared to clay content variation in THx soil profile (Table 1). The correlation analysis between Kf,ads and soil properties accomplished only with these samples was positive for clay content (r = 0.77), and negative for the silt content (r = -0.75), both at p<0.05 (Table 4). For this oxisols, silt particles are very stable microagregates between clay and sand fraction that are not totally destroyed during the fractionation process. Since these particles had no charge, it is expected that they had no effect on imazaquin sorption.

The increasing imazaquin affinity by the soils during desorption step (Kf,des) demonstrated that imazaquin had low desorption (Table 2). This can be better evidenced by the average percentage of imazaquin in solution after desorption (Table 3). Except for DRm, less than 11% of imazaquin sorbed concentration remained in solution, after desorption steps. Comparing the average of imazaquin concentration in solution, the amount of herbicide in solution was more intensively reduced after desorption step than after sorption with the time of agitation. This tendency was not observed for the subsurface samples. Presumably, the processes and forces of imazaquin sorption in soil tended to remain constant or to increase with time of shaking, except for DRm subsurface soil samples. For the THx subsurface samples, the similar amount of imazaquin in solution was found after sorption and desorption step (Table 3), characterized by the increasing of correlation value between OC and Kf,ads and OC and Kf,des (Table 4), consecutively, such amount can be explained by the increasing of the soluble OC content in solution, after desorption step. At the pH level of this sample, the OC might have a negative charge, as imazaquin as well. The increasing tendecy of pH with increasing of OC content, for the subsurface samples (Table 4), showed that OC is playing role as a buffer in the supernatant, capturing H+ and raising the pH, which shows the negative nature of the OC.

In PL soil, the concentration of imazaquin remained in solution, after sorption, was constant in all concentrations (Table 3), demonstrating that the sorbed concentration is directly proportional to the amount of the herbicide in solution (1/nads~1,0) (Table 2), and that the imazaquin capacity of retention by soil was not saturated. That fact can be further explained by Kf,des value, which was six times higher in relation to Kf,ads value (Table 2), showing high imazaquin interaction with this soil. Except for the PL soil, all of the 1/nads values were lower than unity, indicating a nonlinear relationship between concentration of imazaquin and its retention in soil.



1. The clay content and pH values are the main soil properties controlling the imazaquin sorption on these soils.

2. The clay content and pH values have a positive and negative correlation, respectively, with imazaquin Kf,ads, but the correlation analysis between Kf,ads and soil properties should only be accomplished for soils of the same class.

3. The clay content and pH values have bigger influence on imazaquin sorption than organic carbon content for these tropical soils.

4. For samples of the profile of THx, soil water content presents a positive correlation with imazaquin Kf,ads and the sorption increases with depth of sampling.



To Uenf, Embrapa Milho e Sorgo and Fapemig, for the financial support; to Brazilian Cyanamid for the technical imazaquin; to Mr. Nilson M. Lopes, Embrapa's technician, for HPLC help; to undergraduate students Tricia C. L. de Faria, Gibson A. S. Soares and Roqueline R. Silva, for their collaboration to this work.



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Received on February 4, 2004 and accepted on July 18, 2005

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