<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>0120-9965</journal-id>
<journal-title><![CDATA[Agronomía Colombiana]]></journal-title>
<abbrev-journal-title><![CDATA[Agron. colomb.]]></abbrev-journal-title>
<issn>0120-9965</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional de Colombia, Facultad de Agronomía]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0120-99652016000100011</article-id>
<article-id pub-id-type="doi">10.15446/agron.colomb.v34n1.53325</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Degradation and thermodynamic adsorption process of carbofuran and oxadicyl in a Colombian agricultural soil profile]]></article-title>
<article-title xml:lang="es"><![CDATA[Degradación y termodinámica del proceso de adsorción del carbofurano y oxadicil en un perfil de suelo agrícola de Colombia]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mosquera-Vivas]]></surname>
<given-names><![CDATA[Carmen S.]]></given-names>
</name>
<xref ref-type="aff" rid="A01"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Obregon-Neira]]></surname>
<given-names><![CDATA[Nelson]]></given-names>
</name>
<xref ref-type="aff" rid="A02"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Celis-Ossa]]></surname>
<given-names><![CDATA[Raúl E.]]></given-names>
</name>
<xref ref-type="aff" rid="A02"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Guerrero-Dallos]]></surname>
<given-names><![CDATA[Jairo A.]]></given-names>
</name>
<xref ref-type="aff" rid="A01"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González-Murillo]]></surname>
<given-names><![CDATA[Carlos A.]]></given-names>
</name>
<xref ref-type="aff" rid="A02"/>
</contrib>
</contrib-group>
<aff id="A01">
<institution><![CDATA[,Universidad Nacional de Colombia Faculty of Science Department of Chemistry]]></institution>
<addr-line><![CDATA[Bogota ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="A02">
<institution><![CDATA[,Universidad Nacional de Colombia Faculty of Engineering Department of Civil and Agricultural Engineering]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
</aff>
<pub-date pub-type="pub">
<day>01</day>
<month>04</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="epub">
<day>01</day>
<month>04</month>
<year>2016</year>
</pub-date>
<volume>34</volume>
<numero>1</numero>
<fpage>92</fpage>
<lpage>100</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0120-99652016000100011&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0120-99652016000100011&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0120-99652016000100011&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Carbofuran and oxadixyl pesticides are used in Colombia to control pests and fungi, but their mobility through the soil profile is poorly understood. This study showed degradation and adsorption processes of these compounds in a Melanudands soil (0-100 cm) from Colombia using laboratory incubation and the batch equilibrium methods. First-order kinetic models indicated that the degradation rates of carbofuran (0.013-0.006 day-1) and oxadixyl (0.013-0.008 day-1) decreased at deeper soil layers, suggesting that the pesticides were more persistent in the sub-surface (60-100 cm) than in the surface layers (0-40 cm). The thermodynamic approach showed that the adsorption of both pesticides was similar, an exothermic and spontaneous process. The carbofuran and oxadixyl coefficient of distribution (5.8-0.3 L kg-1) and the percentage of adsorption (71.2-11.3%) were very similar in the surface layers (0-40 cm) and decreased with the soil depth. The organic carbon (OC) and clay content showed a positive correlation with the pesticide adsorption throughout the soil profile; therefore, mathematical equations were developed from multiple linear regression models for these soil properties and initial concentration. The equations were important to the estimation of the mobility of the compounds using leaching models under laboratory and field conditions.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[El carbofurano y oxadicil se aplican en diferentes cultivos en Colombia, pero su transporte a través del perfil del suelo se ha estudiado muy poco. Se evaluó la degradación y la adsorción de ambos plaguicidas en un suelo Melanudands (0-100 cm) mediante el método indirecto e incubaciones bajo condiciones de laboratorio. Las tasas de degradación del carbofurano (0,013- 0,006 día-1) y oxadicil (0,013-0,008 día-1) disminuyeron en las capas más profundas del perfil; lo cual indica que los plaguicidas fueron más persistentes en las capas sub-superficiales (60- 100 cm) que en las capas superficiales (0-40 cm). La adsorción fue un proceso exotérmico y espontáneo. Los coeficientes de distribución (5,8-0,3 L kg-1) y los porcentajes de adsorción (71,2-11,3%) de ambos plaguicidas fueron muy similares en los primeros 40 cm y disminuyeron con la profundidad. Con modelos de regresión lineal múltiple entre la adsorción de los plaguicidas y el contenido de carbón orgánico (CO), las arcillas y la concentración inicial, se obtuvieron ecuaciones matemáticas, las cuales muestran como el CO y las arcillas controlan el transporte de ambos pesticidas a través del perfil. Estas ecuaciones son útiles para estimar el transporte del carbofurano y oxadicil en el suelo.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[pesticide persistence]]></kwd>
<kwd lng="en"><![CDATA[soil pollution]]></kwd>
<kwd lng="en"><![CDATA[sorption]]></kwd>
<kwd lng="en"><![CDATA[chemical degradation]]></kwd>
<kwd lng="en"><![CDATA[forecasting]]></kwd>
<kwd lng="es"><![CDATA[persistencia de los plaguicidas]]></kwd>
<kwd lng="es"><![CDATA[contaminación del suelo]]></kwd>
<kwd lng="es"><![CDATA[sorción]]></kwd>
<kwd lng="es"><![CDATA[degradación química]]></kwd>
<kwd lng="es"><![CDATA[técnicas de predicción]]></kwd>
</kwd-group>
</article-meta>
</front><body><![CDATA[  <font face="verdana" size="2">     <p>Doi:<a href="http://dx.doi.org/10.15446/agron.colomb.v34n1.53325" target="_blank"> 10.15446/agron.colomb.v34n1.53325</a></p> &nbsp;    <p align=center><font size="4"><b>Degradation and thermodynamic adsorption process of   carbofuran and oxadicyl in a Colombian agricultural soil profile</b></font></p> &nbsp;    <p align=center><font size="3"><b>Degradaci&oacute;n   y termodin&aacute;mica del proceso de adsorci&oacute;n del carbofurano y oxadicil en un   perfil de suelo agr&iacute;cola de Colombia</b></font></p> &nbsp;    <p align=center><b>Carmen   S. Mosquera-Vivas</b><b><sup>1</sup></b><b>, Nelson Obregon-Neira</b><b><sup>2</sup></b><b>,     Ra&uacute;l E. Celis-Ossa</b><b><sup>2</sup></b><b>, Jairo A. Guerrero-Dallos</b><b><sup>1</sup></b><b>,       and Carlos A. Gonz&aacute;lez-Murillo</b><b><sup>2</sup></b></p>     <p><sup>1 </sup>Department of Chemistry, Faculty of Science, Universidad Nacional de Colombia.   Bogota (Colombia). <a href="mailto:csmosquerav@unal.edu.co">csmosquerav@unal.edu.co</a>    <br><sup>2 </sup>Department of Civil and Agricultural Engineering, Faculty of Engineering,   Universidad Nacional de Colombia. Bogota (Colombia)</p>     <p>Received for publication: 1   October, 2015. Accepted for publication: 28 March, 2016</p>   <hr size="1">     <p><b>ABSTRACT</b></p>     <p>Carbofuran and oxadixyl pesticides are used in Colombia   to control pests and fungi, but their mobility through the soil profile is poorly   understood. This study showed degradation and adsorption processes of these compounds   in a Melanudands soil (0-100 cm) from Colombia using laboratory incubation and the   batch equilibrium methods. First-order kinetic models indicated that the degradation   rates of carbofuran (0.013-0.006 day<sup>-1</sup>) and oxadixyl (0.013-0.008 day<sup>-1</sup>) decreased at deeper   soil layers, suggesting that the pesticides were more persistent in the sub-surface   (60-100 cm) than in the surface layers (0-40 cm). The thermodynamic approach showed   that the adsorption of both pesticides was similar, an exothermic and spontaneous   process. The carbofuran and oxadixyl coefficient of distribution (5.8-0.3 L kg<sup>-1</sup>) and the percentage of   adsorption (71.2-11.3%) were very similar in the surface layers (0-40 cm) and decreased   with the soil depth. The organic carbon (OC) and clay content showed a positive   correlation with the pesticide adsorption throughout the soil profile; therefore,   mathematical equations were developed from multiple linear regression models for   these soil properties and initial concentration. The equations were important to   the estimation of the mobility of the compounds using leaching models under laboratory   and field conditions.</p>     ]]></body>
<body><![CDATA[<p><b>Key words: </b>pesticide persistence,   soil pollution, sorption, chemical degradation, forecasting.</p>   <hr size="1">     <p><b>RESUMEN</b></p>     <p>El carbofurano   y oxadicil se aplican en diferentes cultivos en Colombia, pero su transporte a trav&eacute;s   del perfil del suelo se ha estudiado muy poco. Se evalu&oacute; la degradaci&oacute;n y la adsorci&oacute;n   de ambos plaguicidas en un suelo Melanudands (0-100 cm) mediante el m&eacute;todo indirecto   e incubaciones bajo condiciones de laboratorio. Las tasas de degradaci&oacute;n del carbofurano   (0,013- 0,006 d&iacute;a<sup>-1</sup>) y oxadicil (0,013-0,008 d&iacute;a<sup>-1</sup>) disminuyeron   en las capas m&aacute;s profundas del perfil; lo cual indica que los plaguicidas fueron   m&aacute;s persistentes en las capas sub-superficiales (60- 100 cm) que en las capas superficiales   (0-40 cm). La adsorci&oacute;n fue un proceso exot&eacute;rmico y espont&aacute;neo. Los coeficientes   de distribuci&oacute;n (5,8-0,3 L kg<sup>-1</sup>) y los porcentajes de adsorci&oacute;n (71,2-11,3%) de ambos plaguicidas   fueron muy similares en los primeros 40 cm y disminuyeron con la profundidad. Con   modelos de regresi&oacute;n lineal m&uacute;ltiple entre la adsorci&oacute;n de los plaguicidas y el   contenido de carb&oacute;n org&aacute;nico (CO), las arcillas y la concentraci&oacute;n inicial, se obtuvieron   ecuaciones matem&aacute;ticas, las cuales muestran como el CO y las arcillas controlan   el transporte de ambos pesticidas a trav&eacute;s del perfil. Estas ecuaciones son &uacute;tiles   para estimar el transporte del carbofurano y oxadicil en el suelo.</p>     <p><b>Palabras clave: </b>persistencia de los plaguicidas, contaminaci&oacute;n del suelo,   sorci&oacute;n, degradaci&oacute;n qu&iacute;mica, t&eacute;cnicas de predicci&oacute;n.</p>   <hr size="1"> &nbsp;    <p><font size="3"><b>Introduction</b></font></p>     <p>Pesticides are chemicals used to control insects,   weeds and/or endemic diseases in order to enhance food production and to protect   forests, plantations and fibers (Ecobichon, 2001; Mamy and Barriuso, 2007; Sattler <i>et al., </i>2007). Car- bofuran is an insecticide banned in Europe and the USA   (PAN, 2015; EPA, 2015); in spite of this fact, Latin American and Asian farmers   have been using it regularly to control pests in vegetable and fruit crops (Farahani <i>et al., </i>2007; Valencia <i>et al., </i>2008; Pimmata <i>et al., </i>2013). On the other hand, oxadixyl is a fungicide applied to potato,   tomato, onion, cut roses and fruit crops (ICA, 2016). The fate of pesticides in   the atmosphere-plant-soil system depends on their behavior in the soil. Once the   foliar application was carried out, the pesticides moved to the air by volatilization,   to the surface water by runoff, to the groundwater by leaching or remained in the   soil (adsorption) and were perhaps degraded (Tiryaki and Temur, 2010). The degradation   and adsorption processes are critically important to understanding the off-site   impact of pesticides applied to field crops in order to protect the environment   (Gebre- mariam <i>et al., </i>2012).</p>     <p>Pesticide degradation rates in soils were dependent   upon: the soil type, microorganisms, pesticide type, soil temperature, soil water   content, and light irradiation (Shelton and Parkin, 1991; Tariq <i>et al., </i>2006;   Berm&uacute;dez-Couso <i>et al., </i>2013; Pimmata <i>et al., </i>2013; Dhanasekara <i>et     al., </i>2015). For instance, the natural pyrite degraded nearly 40% of the carbofuran   within 100 h (Dhanasekara <i>et al., </i>2015) and the degradation of the insecticide   in the soils with indigenous microorganisms was more rapid that in the sterile soils   (Pimmata <i>et al., </i>2013); although, Tariq <i>et al. </i>(2006) found similar   behaviors for sterile and non-sterile soils.</p>     <p>Soil adsorption was the main factor that was responsible   for the carbofuran dissipation under darkness (Berm&uacute;dez- Couso <i>et al., </i>2013).   Adsorption is the net accumulation of a substance at the interface between a solid   phase and an aqueous solution phase (Sposito, 1989; Delle, 2001). The physical and   chemical soil properties affect the amount of the chemical adsorbed on the soil   solid surface. The OC content, the clay content, the cation exchange capacity (CEC)   and the pH seemed to control the adsorption of carbofuran in both the tropical and   temperate soils (Delle, 2001; Gupta <i>et al., </i>2006; Krishna and Philip, 2008;   Valencia <i>et al., </i>2008; Singh and Srivastava, 2009; Berm&uacute;dez-Couso <i>et al., </i>2012). In regards to oxadixyl degradation and ad- sorption, the only available   data are those provided by the &quot;pesticide properties database&quot; (PPDB, 2015) for   temper- ate soils. Aldana <i>et al. </i>(2011) showed that oxadixyl was a mobile   fungicide in soil columns at a 0-30 cm depth and it might be leached through the   soil profile. In the under- standing of the adsorption equilibrium between the solid   (adsorbent) and liquid phases of soils, thermodynamics play a fundamental role.   To have significant adsorption of a chemical in soils, the free energy of adsorption   (&#916;G<sub>ads</sub>) must be negative and since (&#916;Gads) = (&#916;Hads)-T(&#916;Sads), this requires an enthalpy of adsorption (&#916;Hads) negative that adsorption entropy (&#916;Sads). The entropy of adsorption (&#916;S<sub>ads</sub>) must be negative due   a rotational freedom of the adsorbed substance that is less than the liquid phase   substance (Ruthven, 1984).</p>     <p>Most degradation and adsorption studies of carbofuran   and oxadixyl have focused on the topsoil layer (Shelton and Parkin, 1991; Tariq <i>et al., </i>2006; Farahani <i>et al., </i>2007; Valencia <i>et al., </i>2008;   Aldana <i>et al., </i>2011; Berm&uacute;dez-Couso <i>et al., </i>2012; Pimmata <i>et al., </i>2013; Mart&iacute;nez-Cord&oacute;n <i>et al., </i>2015). How these pesticides behave throughout   the soil profile is poorly understood. Therefore, the aim of this study was to assess   the degradation and adsorption of the pesticides carbofuran and oxadixyl (commonly   used in Colombia) in one Melanudand soil as a function of soil depth (0-100 cm).</p> &nbsp;    <p><font size="3"><b>Materials and methods</b></font></p>     ]]></body>
<body><![CDATA[<p><b>Soils</b></p>     <p>Five soil layers (Melanudands), S1 to S5, acquired   at different vertical depths in the soil profile (S1: 0-20 cm, S2: 20-40cm, S3:   40-60 cm, S4: 60-80 cm and S5: 80-100 cm), were used in this study. The soil layers   were taken in an agricultural landscape in the region of Tenjo-Cundinamarca (Colombia),   located at 2,595 m a.s.l. These layers were air- dried and sieved through a US standard   sieve with 2.38 mm mesh openings (number 8) for adsorption experiments; whereas,   the soil layers for degradation study were kept at field water content. The physical   and chemical properties of the soil are summarized in <a href="#t1">Tab. 1</a>.</p>     <p>    <center><a name="t1"><a href="img/revistas/agc/v34n1/v34n1a11t1.gif" target="_blank">Table 1</a></a></center></p>     <p><b>Pesticides</b></p>     <p>Carbofuran [(2,2-dimethyl-3H-1-benzofuran-7-yl)   N- methylcarbamate] and oxadixyl [N-(2,6-dimethylphenyl)- 2-methoxy-N-(2-oxo-1,3-oxazolidin-3-yl)   acetamide] pesticides (&#8805; 98% purity) were provided by Dr. Ehrenstorfer GmbH   (Augsburg, Germany).</p>     <p><b>Degradation process</b></p>     <p>The pesticide degradation was studied with laboratory   incubation experiments (Mamy and Barriuso, 2007; Mosquera-Vivas <i>et al., </i>2010).   Ten g (10.00) of dry soil (S1- S5) were placed in a 50 mL centrifuge tube and spiked   with 0.250 mL of the pesticide mixture. Carbofuran and oxadixyl were added at reported   field doses of a.i. 0.31 and 1.0 kg ha-1, respectively. These   samples were then inserted in 500 mL jars containing 20 mL of 2 M NaOH (on top)   and a sealed vial with 10 mL of distillated water. The samples were incubated under   unsaturated field moisture conditions (<a href="#t1">Tab. 1</a>) at 18ºC in the dark for 102 d. After   incubation times of 0, 1, 3, 7, 14, 31, 45, 60, 76 and 102 d, two soil samples from   each depth were dried on foil containers at room temperature (18&deg;C) for   3 d. The samples were then placed in centrifuge tubes, spiked with PCB 103 (surrogate   compound) and extracted with 20 mL of ethyl acetate and shaken for 15 min. Na<sub>2</sub>SO<sub>4</sub> (5.0 g) and NaHCO<sub>3</sub> (1.7 g) were then added and the samples were shaken   for 15 min again. The samples were centrifuged at 7,500 rpm for 15 min and the organic   supernatants (10 mL) concentrated to 2 mL. An aliquot of PCB 52 (internal standard)   was then added before injecting the samples into a CG-MS system. The limit of detection   (LOD) was 0.008 &#956;g g<sup>-1</sup> for carbofuran and 0.028 &#956;g g<sup>-1</sup> for oxadixyl. The limits of quantification (LOQ)   were 0.020 &#956;g g<sup>-1</sup> and 0.118 &#956;g g<sup>-1</sup> for carbofuran and oxadixyl,   respectively. The recovery of the pesticides was 103.3±7.8% for carbofuran and 79.1±5.9%   for oxadixyl. For instance, the recovery of PCB 103 was 91.9% with a RSD of 1.4%.</p>     <p>The first-order kinetic model was fitted to obtain   the degradation rate (k) and the half-life (t<sub>1/2</sub>) of the two pesticides (Eq. 1 and 2):</p>     <p>    ]]></body>
<body><![CDATA[<center><img src="img/revistas/agc/v34n1/v34n1a11e1.gif"></center></p>     <p>where C<sub>t</sub> is the pesticide concentration   at time t and C<sub>0</sub> is the initial concentration   of the pesticide.</p>     <p><b>Adsorption process</b></p>     <p>The adsorption process was obtained by using the   batch equilibrium method (Mamy and Barriuso, 2007; Langeron <i>et al., </i>2014).   All of the pesticides were studied together in a mixture solution according to the   field data. Five test substances were prepared in 0.01 M CaCl<sub>2</sub>. The concentration ranges were 0.13 - 0.40 mg L-1 for carbofuran and 0.49 - 2.16 mg L<sup>-1</sup> for oxadixyl. All of the experiments were executed   with samples of pesticides in 0.01 M CaCl<sub>2</sub> and blanks with soil in   0.01 M CaCl<sub>2</sub>.</p>     <p>Ten g (10.00) of dry soil (S1-S5) were placed in   50-mL centrifuge tubes and a 20.0 mL aliquot of the mixture was added to each tube.   The soil-water slurry was shaken for 24 h at 20&deg;C and centrifuged at   7,000 rpm for 30 min. The supernatant was removed, weighed and extracted by liquid-liquid   extraction. The supernatant was spiked with PCB 103 and the extraction was carried   out with 20.0 mL of ethyl acetate and shaken for 15 min. NaCl was added and the   sample was shaken again for an additional 15 min before sonication for 15 min. The   organic phase was concentrated to 1 mL. An aliquot of PCB 52 was added to the samples   before injection into a CG-MS system. The pesticide and PCB 103 recoveries by liquid-liquid   extraction were 89.5±8.5% for carbofuran, 81.9±5.8% for oxadixyl and 84.9±7.1% for   PCB 103.</p>     <p>The coefficient of distribution (k<sub>d</sub>) was calculated as the average of the subsamples   for each layer (Eq. 3):</p>     <p>    <center><img src="img/revistas/agc/v34n1/v34n1a11e2.gif"></center></p>     <p>Ceq is the equilibrium concentration of the pesticide   (mg L<sup>-1</sup>) in the soil solution and n is the number of the   data.</p>     <p>Finally, the soil organic carbon-water partitioning   coeffi- cient, k<sub>OC</sub>, was obtained by normalizing   the k<sub>d</sub> coefficients to the OC content (Eq. 4):</p>     ]]></body>
<body><![CDATA[<p>    <center><img src="img/revistas/agc/v34n1/v34n1a11e3.gif"></center></p>     <p>Pedotransfer functions (PTF) were used to estimate   the k<sub>d</sub> values of the pesticides from the OC content, clay   content and pH (Weber <i>et al</i>., 2004; Singh <i>et al</i>., 2014). Weber <i>et al</i>. (2004) used 13 data points to get a linear model   between linear model between the kd of carbofuran as the carbofuran   as a dependent variable, and the OC and the clay content as independent variables.   In order to obtain multiple linear regression models for both pesticides, we performed   a multicollinearity test using Pearson correlation coefficients and the variance   inflation factor (VIF) with all of the data (<i>n </i>= 22) throughout the soil   profile. Linear parameters were obtained for the combination of the OC content,   the clay content and the initial concentration of the substances, where VIF was   used to select the best linear equations.</p>     <p><b>Pesticide quantification</b></p>     <p>The quantification of the pesticides in the soil   and aqueous phases was performed using an Agilent (Santa Clara, CA) model 7890A   gas chromatography coupled to a 5975C mass spectrometer detector. The chromatography   system was equipped with a multimode inlet, autosampler and HP5- MS (30 m x 250 &#956;m x 0.25 &#956;m) column. The carrier gas used was helium and the   injection volume was 4 &#956;L with the solvent vent mode. The MS transfer line was kept at 280ºC and   the quantification was performed using selected ion monitoring (SIM).</p>     <p><b>Thermodynamic approach</b></p>     <p>Adsorption enthalpy (&#916;Hads) is given by (Goss and   Schwarzenbach, 1999):</p>     <p>    <center><img src="img/revistas/agc/v34n1/v34n1a11e4.gif"></center></p>      <p>where, <img src="img/revistas/agc/v34n1/v34n1a11e12.gif"> is the coefficient of distribution at T<sub>r</sub> (reference temperature = 293 K) and <img src="img/revistas/agc/v34n1/v34n1a11e13.gif"> is the average specific   surface of the soil, which can be estimated as (Vighi and Di Guardo, 1995)</p>     ]]></body>
<body><![CDATA[<p>    <center><img src="img/revistas/agc/v34n1/v34n1a11e5.gif"></center></p>     <p>where f<sub>oc</sub> is the soil   carbon fraction, f<sub>cl</sub> is the soil clay fraction,   f<sub>st</sub> is the soil silt fraction and f<sub>sd</sub> is the soil sand fraction.</p>     <p>Adsorption free energy at T<sub>r</sub> is calculated as:</p>     <p>    <center><img src="img/revistas/agc/v34n1/v34n1a11e6.gif"></center></p>     <p>where R is the gas   constant and k<sub>d</sub> is:</p>     <p>    <center><img src="img/revistas/agc/v34n1/v34n1a11e7.gif"></center></p>     <p>where [P<sub>ads</sub>] is the equilibrium concentration of the pesticide in the soil solid (mole   L<sup>-1</sup>), [P<sub>sln</sub>] is the equilibrium concentration of the pesticide in the soil solution   (mole L<sup>-1</sup>) and &#961;<sub>p</sub> is the density of the   particles (kg L<sup>-1</sup>).</p>     ]]></body>
<body><![CDATA[<p>Adsorption entropy   can be calculated according to (Ruthven, 1984)</p>     <p>    <center><img src="img/revistas/agc/v34n1/v34n1a11e8.gif"></center></p>     <p>&#916;S<sub>ads</sub> can be used to understand   the adsorption process described in the reaction below:</p>     <p>    <center><img src="img/revistas/agc/v34n1/v34n1a11e9.gif"></center></p>     <p>where S<sub>(s)</sub> is the soil   solid, P<sub>(sln)</sub> is the pesticide in the   soil solution and S – P<sub>(ads)</sub> is the pesticide adsorbed   in the soil solids.</p> &nbsp;    <p><font size="3"><b>Results and discussion</b></font></p>     <p><b>Degradation process</b></p>     <p>The first-order kinetic models for carbofuran and   oxadixyl in the soil profile are shown in <a href="#f1">Fig. 1</a>. The degradation rate (k) and the   half-life time (t<sub>1/2</sub>) calculated from this   model are given in <a href="#t2">Tab. 2</a>. Carbofuran was completely degraded in S1 after 7 d of   incubation. In S2-S4, the model fitted accurately to data with coefficients of determination   (<i>R</i><sup>2</sup>)&gt;0.75 and the null   hypothesis (H<sub>0</sub>: k = 0 and C<sub>0</sub> = 0) were rejected at a 95% confidence level. The   k values of the insecticide (0.006-0.013 d<sup>-1</sup>) decreased from S2 to S3 and remained constant in S4, which may be explained   by the change of microbial activity throughout the soil profile. Soil microorganisms   play an important role in the pesticide degradation process (Mosquera-Vivas <i>et     al., </i>2010; Pimmata <i>et al., </i>2013) and, in our soil, the amount of CO<sub>2</sub> evolved during the microbial respiration was found   to decrease in S1-S3, after which it was constant (<a href="#f2">Fig. 2</a>); accordingly, the decreasing   of microbial activity allowed the k values to decrease. It is seemed with k value   of carbofuran in S5 where the concentration remained unchanged; hence, the first-order   kinetic showed a poor fit, as was expected. The degradation rates of 2,4-D and atrazine   decreased with the increasing soil depth, which was due to the microbiota decrease   through the soil profile (Kruger <i>et al</i>., 1993; Veeh <i>et al., </i>1996).   Microbial degradation is an important degradation pathway of carbofuran in neutral   and acid soils (Evert, 1991; Pimmata <i>et al., </i>2013). t<sub>1/2</sub> values of the insecticide increased at deeper soil   depths. t<sub>1/2</sub> for soil layers S1 and   S2 (10.5-53.3 d<sup>-1</sup>) is within the range   reported by Pimmata <i>et al. </i>(2013) and Tariq <i>et al. </i>(2006) for Pakistan   and Thailand soils (1.6-69.3 d-1); although, t<sub>1/2</sub> in soil layers at a depth of 40-100 cm is higher   than the former ones, suggesting the insecticide was more persistent at the deeper   layers in the studied soil profile.</p>     ]]></body>
<body><![CDATA[<p>    <center><a name="f1"><a href="img/revistas/agc/v34n1/v34n1a11f1.gif" target="_blank">Figure 1</a></a></center></p>     <p>    <center><a name="f2"><img src="img/revistas/agc/v34n1/v34n1a11f2.gif"></a></center></p>     <p>The first-order kinetic fit well to oxadixyl degradation   data with <i>R</i>2 values between 0.83 and   0.95, and the null hypothesis (H0: k = 0 and C0 = 0) was rejected at a 95% confidence level, except   in S5 (Fig. 1 and Tab. 2). k values of the oxadixyl were similar in S1-S3 (0.012-0.013   d-1) and slightly decreased to 0.008 d-1 in S4. This behavior might be explained by the fact   that the biotic process occurs mainly in S1 and S2, where the amount of CO2 evolved during the microbial respiration was higher   than in S3 and S4 (<a href="#f2">Fig. 2</a>). In layers S3 and S4, the abiotic process probably degraded   the fungicide. It seems that hydrolysis controled the degradation process in layers   at a depth of 40-80 cm because the oxadixyl showed a heterocyclic ring system, which   is liable to hydrolysis (Roberts and Hutson, 1998). In contrast to the carbofuran,   the oxadixyl was degraded to nearly 10.0% of its maximum concentration during 102   d of incubation in S5, confirming the hydrolysis reaction as well. The t1/2 of the oxadixyl also increased at the deeper soil   layers (<a href="#t2">Tab. 2</a>). The t<sub>1/2</sub> of the fungicide in S1-S3   was smaller than the values published in the pesticide properties database in topsoils   from temperate regions (PAN, 2015; PPDB, 2015), showing that the oxadixyl degraded   faster under tropical conditions and it was more persistent at deeper soils layers,   i.e. in S4 and S5.</p>     <p>    <center><a name="t2"><a href="img/revistas/agc/v34n1/v34n1a11t2.gif" target="_blank">Table 2</a></a></center></p>     <p><b>Adsorption process</b></p>     <p>The k<sub>d</sub> and k<sub>oc</sub> values and the adsorption percentage for the carbofuran   and oxadixyl in soil layers S1-S5 are shown in <a href="#f3">Fig.3</a>. k<sub>d</sub> values and the adsorption percentage for both pesticides   were higher in S1-S2 than in S3-S5. Although the carbofuran and oxadixyl showed   an aromatic ring, a heterocyclic ring and oxygen atoms, which are liable to adsorb   the pesticides in our soil with the same physical interactions. The adsorption behavior   for the carbofuran and oxadixyl through the soil profile can be explained by the   decrease in the OC content, clay content, CEC and ECEC. The k<sub>d</sub> values revealed a positive correlation with the   OC content (<i>r </i>= 0,97 and 0.92), clay (<i>r </i>= 0.97 an d 0.93), CEC (<i>r </i>= 0.99 and 0.99) and ECEC (<i>r </i>= 0.88 and 0.95). Similar trends have been   published by Delle (2001), Valencia <i>et al. </i>(2008), Singh and Srivastava (2009),   Berm&uacute;dez-Couso <i>et al. </i>(2012), and Pimmata <i>et al. </i>(2013). Positive   correlation between k<sub>d</sub><sub>,</sub> ECEC and OC showed the role of the oxygen atoms   in the retention capacity of both pesticides in the soils. The oxygen atoms attracted   electron density (electronegativity) and the negative net of the soil repelled the   pesticides; as a consequence, the k<sub>d</sub> values were very small   (0.3-5.8 L kg<sup>-1</sup>). The decreasing values   of carbofuran and oxadixyl adsorption with soil depth might be explained by the   decreased concentration of the divalent cations, Ca<sup>2+</sup> and Mg<sup>2+</sup> (Tab. 1). These   cations form soil-divalent cation- pesticides linkages.</p>     <p>    ]]></body>
<body><![CDATA[<center><a name="f3"><img src="img/revistas/agc/v34n1/v34n1a11f3.gif"></a></center></p>     <p>The k<sub>oc</sub> values of the   insecticide and the fungicide in S1-S5 varied from 40.3 to 13.7 L kg<sup>-1</sup> and from 55.6 to 11.1 L kg<sup>-1</sup>, respectively. The carbofuran range of the k<sub>oc</sub> at a depth of 0-60 cm (<a href="#f3">Fig. 3</a>) was within the one   reported for Colombian soils (Valencia <i>et al.</i>, 2008); however, all of the   k<sub>oc</sub> values were lower than that found for tropical soils   from India and Malaysia. (Farahani <i>et al., </i>2007; Krishna and Philip, 2008;   Singh and Srivastava, 2009), it might suggest the adsorption of the insecticide   was affected by the soil genesis. In contrast, the oxadixyl range of the k<sub>oc</sub> at a depth of 0-40 cm soils; although, the range   of the Koc at a depth of 40-100 cm was within the range published in the literature   (PAN, 2015; EPA, 2015; Mart&iacute;nez-Cord&oacute;n <i>et al., </i>2015), indicating that the   adsorption of the fungicide in our topsoil (0-40 cm) was higher than those found   in other topsoils. This behavior could result from the composition of the soil organic   matter throughout the profile.</p>     <p>The multiple linear regression models for the carbofuran   and oxadixyl throughout the soil profile are summarized in Eqs 13-18:</p>     <p>Carbofuran:</p>     <p>    <center><img src="img/revistas/agc/v34n1/v34n1a11e10.gif"></center></p>     <p>Oxadixyl:</p>     <p>    <center><img src="img/revistas/agc/v34n1/v34n1a11e11.gif"></center></p>     <p>These models can be used to calculate the coefficient   of distribution and/or the adsorption percentage using the OC and clay content.   To calculate kd and the percentage of   adsorption from PTF may reduce the cost and time in chemical analysis to predict   the mobility of carbofuran and oxadixyl in Colombia soils. Furthermore, the models   confirmed the relationship between the adsorption of pesticides and the OC and clay   content.</p>     ]]></body>
<body><![CDATA[<p>The enthalpy, entropy and free energy values of the   adsorption of the pesticides in layers S1-S5 are summarized in <a href="#t3">Tab. 3</a>. The <a href="#f4">Fig.   4</a> shows the adsorption free energy of the carbofuran and oxadixyl throughout the   soil profile. All of the thermodynamic approaches were negative, except the free   energy for both pesticide in soil layer S5, suggesting that the adsorption of the   pesticides in our soils was exothermic and spontaneous and the rotational freedom   of the adsorbed chemicals was less than the liquid phase chemicals (Ruthven, 1984).   Furthermore, &#8710;G<sub>ads</sub> was similar for the carbofuran   and oxadixyl throughout the soil profile (<a href="#t3">Tab. 3</a> and <a href="#f4">Fig. 4</a>). Negative free energy   (&#8710;G<sub>ads</sub>) has also been published   for the adsorption of carbofuran in India soils at a depth of 0-30 cm (Singh and   Srivastava, 2009). Low values of free energy indicate that the adsorption of the   pesticides in soil solids is often promoted by weak physical forces (Weber, 1993;   Singh and Srivastava, 2009).</p>     <p>    <center><a name="f4"><img src="img/revistas/agc/v34n1/v34n1a11f4.gif"></a></center></p>     <p>    <center><a name="t3"><a href="img/revistas/agc/v34n1/v34n1a11t3.gif" target="_blank">Table 3</a></a></center></p>     <p>For instance, the carbofuran and oxadixyl were adsorbed   less than the dimethomorph (data not shown) and this is in accord with their chemical   structure. Dimethomorph shows two aromatic ring system and chlorine atom, while   carbofuran and oxadixyl exhibit one aromatic ring system without a chlorine atom.   The aromatic rings increase &#960;-&#960; stacking   interactions and the chlorine atom promotes hydrophobic interactions between pesticide   and aromatic components of soil organic matter.</p>     <p>Positive free energy for the insecticide and fungicide   in S5 showed that the adsorption of both pesticides was not a spontaneous process,   i.e. carbofuran and oxadixyl prefer the soil aqueous solution.</p> &nbsp;    <p><font size="3"><b>Conclusion</b></font></p>     <p>The high microbial activity played a key role reducing   the transport of both pesticides at a depth of 0-40 cm. If carbofuran and oxadixyl   reach deeper soil layers (60-100 cm), they might constitute a risk for groundwater   pollution due to their persistence and mobility, as shown above.</p>     <p><b>Acknowledgements</b></p>     ]]></body>
<body><![CDATA[<p>This study was funded by the Swiss National Science   Foundation (SNSF) and the Swiss Agency for Development and Cooperation (SDC) [Project   number: IZ70Z0_124080]. Furthermore, the authors would like to thank Colciencias   (Project number: 528) for economical support and Asocolflores (Direction of Environmental   Issues) for technical support.</p> &nbsp;    <p><font size="3"><b>Literature cited</b></font></p>     <!-- ref --><p>Aldana, M., R. de Prado, and M.J.  Mart&iacute;nez. 2011. Leaching  of oxadyxil and tebuconazole in Colombian soil. Commun. Agric. Appl. Biol. Sci.  76, 909-914.    &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;[&#160;<a href="javascript:void(0);" onclick="javascript: window.open('/scielo.php?script=sci_nlinks&ref=193937&pid=S0120-9965201600010001100001&lng=','','width=640,height=500,resizable=yes,scrollbars=1,menubar=yes,');">Links</a>&#160;]<!-- end-ref --></p>     <!-- ref --><p>Berm&uacute;dez-Couso,  A., D. 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