Relationship between age of waste and natural electric potential generation in Sanitary Landfill
César Augusto Moreira
, Antonio Celso de Oliveira Braga
Autor para correspondencia
Departamento de Geologia Aplicada (DGA), Instituto de Geociências e Ciências Exatas (IGCE), Universidade Estadual Paulista (UNESP), Rio Claro, São Paulo State, Brazil, Av. 24-A, 1515, Bela Vista, CEP 13506-900, Rio Claro, São Paulo, State, Brazil
Letícia Hirata Godoy
Instituto de Geociências e Ciências Exatas (IGCE), Universidade Estadual Paulista (UNESP), Av. 24-A, 1515, Bela Vista. CEP 13506-900, Rio Claro, São Paulo State, Brazil
Diego de Sousa Sardinha
Instituto de Ciência e Tecnologia (ICT) Universidade Federal de Alfenas (UNIFAL) Poços de Caldas, Minas Gerais State, Brazil Rodovia BR 267, Km533 - CEP 37701-970 Poços de Caldas, Minas Gerais State, Brazil
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The epicentral distance is 90.10°. (a) The radial and transverse velocity components are shown. (b) The radial and transverse components are shown after correcting for splitting using the values that were measured.</p>" ] ] ] "autores" => array:3 [ 0 => array:2 [ "autoresLista" => "Steven A.C. van Benthem" "autores" => array:1 [ 0 => array:2 [ "nombre" => "Steven A.C." "apellidos" => "van Benthem" ] ] ] 1 => array:2 [ "autoresLista" => "Raúl W. Valenzuela" "autores" => array:1 [ 0 => array:2 [ "nombre" => "Raúl W." "apellidos" => "Valenzuela" ] ] ] 2 => array:2 [ "autoresLista" => "Gustavo J. Ponce" "autores" => array:1 [ 0 => array:2 [ "nombre" => "Gustavo J." 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CEP 13506-900, Rio Claro, São Paulo State, Brazil" "identificador" => "aff0010" ] ] ] 2 => array:3 [ "autoresLista" => "Diego de Sousa Sardinha" "autores" => array:1 [ 0 => array:2 [ "nombre" => "Diego" "apellidos" => "de Sousa Sardinha" ] ] "afiliaciones" => array:1 [ 0 => array:2 [ "entidad" => "Instituto de Ciência e Tecnologia (ICT) Universidade Federal de Alfenas (UNIFAL) Poços de Caldas, Minas Gerais State, Brazil Rodovia BR 267, Km<span class="elsevierStyleHsp" style=""></span>533 - CEP 37701-970 Poços de Caldas, Minas Gerais State, Brazil" "identificador" => "aff0015" ] ] ] ] "resumenGrafico" => array:2 [ "original" => 0 "multimedia" => array:7 [ "identificador" => "f0010" "etiqueta" => "Figure 2" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr2.jpeg" "Alto" => 1235 "Ancho" => 1362 "Tamanyo" => 191316 ] ] "descripcion" => array:1 [ "es" => "<p id="sp0010" class="elsevierStyleSimplePara elsevierViewall">Self-potential map with closure ages of the ditches.</p>" ] ] ] "textoCompleto" => "<span class="elsevierStyleSections"><span id="sec0005" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0025">Introduction</span><p id="par0020" class="elsevierStylePara elsevierViewall"><a name="p376"></a>There is a growing need to adapt the application of direct and indirect investigative techniques for use in environmental studies, due to the large amount of synthetic compounds or petroleum products for final use or as raw materials for other industries, spillage or leakage risk during transport and manipulation of these compounds, in addition to undue leaks or discharges of effluents and solid or liquid waste generated during industrial processes, domestic and urban activities.</p><p id="par0025" class="elsevierStylePara elsevierViewall">Detection of changes in physical properties caused by the percolation and residence of contaminants in soils and rocks is the object of study of geophysics applied to environmental studies. The contrast between assessed areas and surrounding areas with natural characteristics to the physical parameter measured, allows 2D and 3D delimitation of potentially contaminated areas.</p><p id="par0030" class="elsevierStylePara elsevierViewall">Studies aimed at analyzing and understanding the behavior of these compounds in the geological environment are necessary and essential, from the perspective of physical and chemical changes due to the presence and interaction with the environment, climatic seasonality, oxygen availability, physical-chemical conditions and others. These changes result in the reduction of compounds toxicity in many cases.</p><p id="par0035" class="elsevierStylePara elsevierViewall">However, in some cases, the release of metals possibly contained in mineral constituents or compounds may occur, as well as a possible increase of toxicity by compounds generated from the degradation of initial contaminants.</p><p id="par0040" class="elsevierStylePara elsevierViewall">Understanding the modifications of physical properties as for the presence of contaminants in geological environment is essential to geophysics application and interpretation in environmental studies.</p><p id="par0045" class="elsevierStylePara elsevierViewall">Measures of self-potential (SP) can promote means of detection and relative quantification of contaminants in groundwater. <a class="elsevierStyleCrossRef" href="#bib0010">Baker and Cull (2004)</a> applied the method in the valley of King river – Tasmania, to evaluate the presence of metals from tailings of the Mt. Lyell sulphide mine located nearby. The contours of electric potential were consistent with hydraulic potential estimated by piezometers, factor that assisted on the refinement of groundwater flow model and understanding the pressure gradients observed in drillings.</p><p id="par0050" class="elsevierStylePara elsevierViewall">In <a class="elsevierStyleCrossRef" href="#bib0070">Mota <span class="elsevierStyleItalic">et al</span>. (2004)</a> study, self-potential and electro resistivity methods were applied to evaluate the granitic massif structure underlying Póvoa de Lanhoso – Portugal landfill. The results allowed the definition of low resistivity zones correlated with negative values of self-potential, which indicates impacted areas by contaminants from the landfill.</p><p id="par0055" class="elsevierStylePara elsevierViewall">In this research line, <a class="elsevierStyleCrossRef" href="#bib0085">Nimmer and Osiensky (2002)</a> made self-potential and resistivity measurements in surface and in drilling holes to assess the flow of a salt plume in a partially fractured basalt in Idaho – United States. The results indicate that self-potential allows additional details about the plume dynamics in a complex environment, in relation to artificial electric field techniques, which in some surveys were insensitive to contaminants presence.</p><p id="par0060" class="elsevierStylePara elsevierViewall">These cases quoted above corroborate the hypothesis of self-potential generation by the flow of electrolyte solutions in porous and fractured aquifers, represented in these cases by contaminants from the landfill and saline solution.</p><p id="par0065" class="elsevierStylePara elsevierViewall">Measures of self potential and redox potential (Eh) were used in the works of <a class="elsevierStyleCrossRef" href="#bib0075">Naudet <span class="elsevierStyleItalic">et al</span>. (2003)</a> and <a class="elsevierStyleCrossRef" href="#bib0080">Naudet <span class="elsevierStyleItalic">et al</span>. (2004)</a> to study the evolution of a contaminant plume from a landfill. The results show that the electric potential progressively decreases in the aerobic zone, increases dramatically in the redox front and finally reaches the standard of the study area when achieve the oxidation zone. There is a high correlation between measurements of self-potential and redox potential in the profile.</p><p id="par0070" class="elsevierStylePara elsevierViewall">The previously mentioned works, in contrast, indicate the possible generation of natural electric potential by degradation processes of the organic compounds accumulated in solid waste landfills.</p><p id="par0075" class="elsevierStylePara elsevierViewall">This study evaluates the results of applying self-potential method at a domestic organic waste landfill, arranged in trenches with different closing dates. The relationship between time of closing trenches, decomposition of organic waste and variations of voltage measured by geophysical method, allow estimating the time necessary to geochemical stabilization of the area.</p></span><span id="sec0010" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0030">Methodology</span><p id="par0080" class="elsevierStylePara elsevierViewall">The self-potential method is characterized by natural electric field accuracy readings, without any electric current injection circuit or generation of electromagnetic field (<a class="elsevierStyleCrossRef" href="#bib0110">Orellana 1972</a>). The advantage lies in the simplicity of involved instrument and versatility of data acquisition into small areas, in addition to the variability of the physical parameter as measured in the geological environment. The main disadvantages associated with the method are the need of connecting cables between reading sensors and the equipment, use of non-polarizable electrodes, besides the high susceptibility to noises produced by electrical systems such as transformers, grounding and <a name="p377"></a>engines, elements that may hinder tests in large or urban areas.</p><p id="par0085" class="elsevierStylePara elsevierViewall">Contrasts of self-potential results in variations of temperature, pressure gradient, porosity, fluid migration, variation of resistivity and soil humidity (<a class="elsevierStyleCrossRef" href="#bib0030">Corwin 1990</a>). As for the generation process, self-potential can be classified as electrochemical potential, electrolytic and mineral. The mineral potential arises due to geochemical redox reactions in an ore body, corresponding to the galvanic cell defined by Electrochemistry.</p><p id="par0090" class="elsevierStylePara elsevierViewall">From the analysis of the main current theories, <a class="elsevierStyleCrossRef" href="#bib0105">Sato and Mooney (1960)</a> proposed a mechanism for the origin of self-potential, within the phenomenon of mineral potential. This mechanism involves a reaction between two electrochemical cells, present simultaneously in two different locations in an ore body. Normally, one cell is above and another below the phreatic level and are interconnected by ore body. These two cells are opposite in nature, an anode and a cathode, with reactions involving gain and loss of electrons. Above the phreatic level oxidation reactions occur, while below reduction takes place.</p><p id="par0095" class="elsevierStylePara elsevierViewall">The potential differences generate natural currents that arise due to redox potential differences of the surrounding solution through contact between the edges of the ore body. The dissolved substances around the upper body are in relative state of oxidation and reduction below the phreatic level, these relative differences in the degree of oxidation are revealed in different Eh values and result in electric current flow in the presence of an electronic conductor, in this case represented by the ore body.</p><p id="par0100" class="elsevierStylePara elsevierViewall">The reduced electrons from the lower portion are conducted to the oxidized upper portion through the ore body, in this way the lower portion is relatively oxidized opposite to the upper, relatively reduced. In this mechanism, the ore body does not participate directly in the electrochemical reactions, otherwise, would be consumed during the process. This acts only as a mean of transporting electrons chemically inert.</p><p id="par0105" class="elsevierStylePara elsevierViewall"><a class="elsevierStyleCrossRef" href="#bib0025">Corry (1985)</a> and <a class="elsevierStyleCrossRef" href="#bib0090">Nyquist and Corry (2002)</a> works analyzed <a class="elsevierStyleCrossRef" href="#bib0105">Sato and Mooney (1960)</a> proposal and raised some incongruent questions in the proposed model:</p><p id="par0110" class="elsevierStylePara elsevierViewall"><span class="elsevierStyleItalic">Width:</span> according to this model, values greater than 800mV are not possible based on the Eh potential of sulfides, whose maximum amplitude of the anomaly generated between the poles of geobattery in relation to the reference electrode is only 400mV. However, several studies of sulfide bodies have reported values of 1000mV or more (<a class="elsevierStyleCrossRef" href="#bib0045">Gay 1967</a>).</p><p id="par0115" class="elsevierStylePara elsevierViewall"><span class="elsevierStyleItalic">Loss of the positive pole:</span> This model requires positive and negative poles. Measures of self-potential in surface, subsurface and drill hole in ore bodies show negative anomalies relative to the reference electrode located near the body.</p><p id="par0120" class="elsevierStylePara elsevierViewall"><span class="elsevierStyleItalic">Groundwater level:</span> There are no references in this model regarding anomalies of self-potential in ore bodies completed dry or wet or over sulfides, characterized by central conductor not inert.</p><p id="par0125" class="elsevierStylePara elsevierViewall"><span class="elsevierStyleItalic">Stability:</span> direct measures of self-potential anomalies associated with sulfide bodies are stable for decades and, presumably, during geologic time. However, the model does not explain how the geobattery does not discharge or values do not fluctuate in the face of seasonal fluctuations of the phreatic level and the consequent seasonal variations in chemical composition of groundwater.</p><p id="par0130" class="elsevierStylePara elsevierViewall">Such authors suggest that the arrangement of pairs of electrodes only measure the difference of potential between the electrode on the anomaly and the reference electrode.</p><p id="par0135" class="elsevierStylePara elsevierViewall">In a galvanic cell electric current flow doesn’t occur unless the electrodes are set in environments with potential differences. This way self-potential would be generated between electrodes connected by a cable and not by an ore body, from the closed circuit between a relatively more oxidized zone and another more reduced.</p><p id="par0140" class="elsevierStylePara elsevierViewall">The electrochemical potential can be originated by biodegradation processes in soil or rock context with organic matter, present in landfill. These materials are frequently recovery by successive layers of soils after filling dispositions cells. Such context allows the predominance of physical and chemical reduction conditions in waste, responsible for stimulating a proliferation of anaerobic microorganism colonies.</p><p id="par0145" class="elsevierStylePara elsevierViewall">The action of microorganism in organic matter occurs by three successive stages (<a class="elsevierStyleCrossRef" href="#bib0120">Themelis & Ulloa, 2007</a>; <a class="elsevierStyleCrossRef" href="#bib0015">Barlaz <span class="elsevierStyleItalic">et al</span>., 2002</a>). In principle, fermentative bacteria hydrolyze the complex organic matter into soluble molecules, which in turn are converted by acid forming bacteria to simple organic acids, carbon dioxide and hydrogen; the principal acids produced are acetic acid, propionic acid, butyric acid and ethanol. In the third stage, methane is formed by methanogenic bacteria, either by breaking down the acids to methane and carbon dioxide, or by reducing carbon dioxide with hydrogen.</p><p id="par0150" class="elsevierStylePara elsevierViewall">The contrast between reduction in waste and oxidation in geologic substratum results in similar conditions to electrochemical cell, in intensity measurable by geophysical instruments.<a name="p378"></a></p></span><span id="sec0015" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0035">Study area</span><p id="par0155" class="elsevierStylePara elsevierViewall">The Cordeirópolis landfill is located at km<span class="elsevierStyleHsp" style=""></span>4.5 of Cássio Freitas Levy highway (CordeirópolisLimeira highway), Cordeirópolis city, São Paulo State, Brazil (<a class="elsevierStyleCrossRef" href="#f0005">Figure 1</a>). The city has about 17,000 inhabitants, with an economy based on the production of ceramic tiles and the cultivation of sugar cane. The daily production of domestic solid waste is approximately 6m<span class="elsevierStyleSup">3</span>.</p><elsevierMultimedia ident="f0005"></elsevierMultimedia><p id="par0160" class="elsevierStylePara elsevierViewall">The study area is a trench-type controlled landfill, for disposal of domestic solid waste only. The operating system consists in 5 m deep trenches, 4m wide and 80m long, for directly disposal of waste on the soil and subsequent coating with a soil layer of 1m.</p><p id="par0165" class="elsevierStylePara elsevierViewall">This area has 48.400<span class="elsevierStyleHsp" style=""></span>m<span class="elsevierStyleSup">2</span> available for waste disposal, starting with activities in 11/2001 and life expectancy to 20 years. The physical structure of the landfill is devoid of electric power distribution systems.</p><p id="par0170" class="elsevierStylePara elsevierViewall">The topography of the area is fairly flat, with average slope of 0.5 % in southeast direction and altitude between 660m and 659m. The landfill is surrounded by sugar cane cultivation.</p><p id="par0175" class="elsevierStylePara elsevierViewall">The substrate is constituted by clay soil with 10m thick, and above by a body of diabase with 15m thick. Below there are fine sandstones and siltstones belonging to Tatuí Formation. Groundwater level is located at an average depth of 50m, with flow direction to the southeast, both determined using vertical electrical sounding (<a class="elsevierStyleCrossRef" href="#bib0060">Moreira <span class="elsevierStyleItalic">et al</span>, 2009</a>). Field tests of saturated hydraulic conductivity revealed average values of 10<span class="elsevierStyleSup">-4</span>cm/s for the soil. There are no wells installed in the area or any other environmental monitoring systems.</p><p id="par0180" class="elsevierStylePara elsevierViewall">In this area 241 readings of self-potential were made through the fixed base arrangement, distributed in regular mesh of the acquisition, with start of recent ditch (extreme NW) from oldest ditch (extreme SE). The base electrode was fixed upstream of groundwater flow, precisely at the landfill access gate (<a class="elsevierStyleCrossRef" href="#f0005">Figure 1</a>).</p><p id="par0185" class="elsevierStylePara elsevierViewall">The acquisition was performed in two steps:</p><p id="par0190" class="elsevierStylePara elsevierViewall">- First step: voltage readings in square mesh of 20m x 20m, for a broad characterization of the area.</p><p id="par0195" class="elsevierStylePara elsevierViewall">- Second step: readings taken just about the ditches with closing date in December, between 2001 and 2007, with 5m spacing between readings. This step objective was to determine a possible relationship between the decomposition of buried waste and voltage variations over time.<a name="p379"></a></p><p id="par0200" class="elsevierStylePara elsevierViewall">This study used non-polarizable Pb-PbCl<span class="elsevierStyleInf">2</span> electrodes characterized by high stability over time (<a class="elsevierStyleCrossRef" href="#bib0115">Petiau 2000</a>). The data reduction involved the following proceedings: acquisition of absolute voltage, drift correction between initial and final lines and base tie-in correction, according <a class="elsevierStyleCrossRef" href="#bib0025">Corry (1985)</a> and <a class="elsevierStyleCrossRef" href="#bib0130">Telford <span class="elsevierStyleItalic">et al</span>. (1990)</a>.</p><p id="par0205" class="elsevierStylePara elsevierViewall">The obtained data after reduction are presented graphically. The measurements obtained in regular mesh were georeferenced and interpolated in the program Surfer 8.0, by the neighborhood method.</p><p id="par0210" class="elsevierStylePara elsevierViewall">In the neighborhood method, initial groups are established by the highest coefficients of mutual association, for the admission of new members is sufficient to determine which represent the highest association with the elements of a given group (<a class="elsevierStyleCrossRef" href="#bib0050">Landim 2004</a>). Hence, the choice of the interpolation method was based in fidelity to the interpolated values and limitations of the surface to the extreme input values.</p></span><span id="sec0020" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0040">Results</span><p id="par0215" class="elsevierStylePara elsevierViewall">The self-potential measurements in regular mesh are presented in map, below closure ages of waste ditches (<a class="elsevierStyleCrossRef" href="#f0010">Figure 2</a>).</p><elsevierMultimedia ident="f0010"></elsevierMultimedia><p id="par0220" class="elsevierStylePara elsevierViewall">The acquired data indicate more negative values in the ditches closed between 2007 and 2006 (0mV to 10mV), and widespread occurrence of values between 10mV and 30mV in ditches closed between 2005 and 2004. Measures between 30mV and 70mV occur in ditches closed between 2003 and 2001.</p><p id="par0225" class="elsevierStylePara elsevierViewall">The position of the groundwater level around 50m deep, waste ditches dug up to 5 m deep in clay soil, suggest that the values of self-potential are produced by geochemical activity. The relationship between voltages values increasing positively with increasing time of organic waste degradation contributes to this effect.</p><p id="par0230" class="elsevierStylePara elsevierViewall">Measures below 20mV are practically contained in the ditches limits closed between 2007 and 2006. The trend of increasing positive values in the oldest ditches may be associated with the decrease of available organic matter and consequent geochemical stability. The elevated measurements obtained in the ditches closed between 2003 and 2001 may indicate an advanced stage of degradation.</p><p id="par0235" class="elsevierStylePara elsevierViewall">The generation of leachate and its chemical, physical and microbiological characteristics are related to the decomposition of organic matter present in the solid waste stored in landfills.</p><p id="par0240" class="elsevierStylePara elsevierViewall">The fluids produced in landfills are often acidic, with variations associated with substrate type, climate, waste type, and seasonal variations, among others. From the production of leachate <a name="p380"></a>several changes occur that involve aerobic stages - acetogenic, and anaerobic - methanogenic (<a class="elsevierStyleCrossRef" href="#bib0005">Bagchi, 1987</a>; <a class="elsevierStyleCrossRef" href="#bib0035">Fang 1995</a>). The pH tends to increase with time since initial acid forms tend to neutralized states, with decrease of chemical oxygen demand (COD) and biological oxygen demand (BOD) (<a class="elsevierStyleCrossRef" href="#bib0040">Farquhar 1989</a>; <a class="elsevierStyleCrossRef" href="#bib0060">Moreira <span class="elsevierStyleItalic">et al</span>, 2009</a>). The total organic carbon content, total fatty acids or ketones and total dissolved solids are high during acetonagenesis and low for methanogenesis, ie decrease with residence time of organic matter (<a class="elsevierStyleCrossRef" href="#bib0020">Birks & Eyles, 1997</a>; <a class="elsevierStyleCrossRef" href="#bib0055">Meju, 2000</a>).</p><p id="par0245" class="elsevierStylePara elsevierViewall">The self-potential data acquired during the second stage surveys confirm the trend of increased self-potential for recent ditches to old ones (<a class="elsevierStyleCrossRef" href="#f0015">Figures 3</a> and <a class="elsevierStyleCrossRef" href="#f0020">4</a>). This increase is possibly associated with increased geochemical stability over the period of organic waste degradation.</p><elsevierMultimedia ident="f0015"></elsevierMultimedia><elsevierMultimedia ident="f0020"></elsevierMultimedia><p id="par0250" class="elsevierStylePara elsevierViewall">Large amounts of water can permeate the bit compressed waste in old landfills, when compared to landfills recently compressed, resulting in a relative low concentration of chemical constituents in leachate of old landfills, with high porosity and permeability (<a class="elsevierStyleCrossRef" href="#bib0100">Radnoff <span class="elsevierStyleItalic">et al</span>. 1992</a>).</p><p id="par0255" class="elsevierStylePara elsevierViewall">The study area is located in a context of clay soils and low hydraulic conductivity, also associated with the fact of the occurrence of a profound groundwater. In this case, it is likely that the oxygen supply in the ditches of waste occurs by percolation of rainwater in all the ditches, with an increase of atmospheric oxygen, especially in the oldest graves, where the compaction of waste results in the fracturing of the soil cover.</p><p id="par0260" class="elsevierStylePara elsevierViewall">Even further incursions of oxygen result in little geochemical activity due to drastic reduction in the supply of organic matter consumed over the years of the waste residence.</p><p id="par0265" class="elsevierStylePara elsevierViewall">The obtained values on the reference line are relatively less variable and higher than those acquired on the waste ditches. In contrast, the values obtained on the ditches have a tendency of increase or decrease towards the end of the line, respectively referring to the ditches in 2007 and 2003. Relatively higher values in the central portion of the lines are presented by the measurements obtained on the ditches in 2002 and 2001.</p><p id="par0270" class="elsevierStylePara elsevierViewall">The measurements on the 2007 ditch present relative lower values, with extreme measures between -1mV to 28mV. The ditches in 2006, 2005 and 2004 present higher values, with extremes measures between 20mV and 48mV.</p><p id="par0275" class="elsevierStylePara elsevierViewall">Statistical analysis of self-potential average values measured on the waste ditches indicates the period of 8 years to return to the natural values, from the first year of closure (<a class="elsevierStyleCrossRef" href="#f0025">Figure 5</a>).</p><elsevierMultimedia ident="f0025"></elsevierMultimedia><p id="par0280" class="elsevierStylePara elsevierViewall">Due to the low permeability of the landfill soil, it is likely that the electrical potential measured reflects almost exclusively the redox potential of the organic matter contained in the buried waste, as described in papers by <a class="elsevierStyleCrossRef" href="#bib0075">Naudet <span class="elsevierStyleItalic">et al</span>. (2003)</a>, <a class="elsevierStyleCrossRef" href="#bib0080">Naudet <span class="elsevierStyleItalic">et al</span>. (2004)</a> and <a class="elsevierStyleCrossRef" href="#bib0065">Moreira <span class="elsevierStyleItalic">et al</span>. (2011)</a>, to the detriment of electrical potential generated by the flow of inorganic solutions in porous and fractured aquifers, such as the work of <a class="elsevierStyleCrossRef" href="#bib0010">Baker and Cull (2004)</a>, <a class="elsevierStyleCrossRef" href="#bib0070">Mota <span class="elsevierStyleItalic">et al</span>. (2004)</a>, <a class="elsevierStyleCrossRef" href="#bib0085">Nimmer and Osiensky (2002)</a>.</p><p id="par0285" class="elsevierStylePara elsevierViewall">In this sense, the estimated period for return to the natural values of electric potential must indicate the time required for consumption of organic material from rapid decomposition. In a context of domestic solid waste, this organic material is represented mainly by food debris, oils and vegetal and animal residues, in addition to oil derived products and greases on a smaller scale.<a name="p381"></a></p></span><span id="sec0025" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0045">Conclusion</span><p id="par0290" class="elsevierStylePara elsevierViewall">The results show the possibility of applying the self-potential geophysical method in studies of domestic solid waste disposal areas, whether as preliminary studies in areas under the absence of environmental monitoring devices, or as a complementary technique of investigation.</p><p id="par0295" class="elsevierStylePara elsevierViewall">However, the applicability of the self-potential method and the results obtained in this work were made possible due to absence of electrical noise and the small area covered during the survey. The application of this method for studies in urban areas is severely impaired due to the frequent presence of electrical systems in this environment, which generate interference during measurements.</p><p id="par0300" class="elsevierStylePara elsevierViewall">The natural electrical potential measurements indicated a relationship with the decomposition period of the waste, ie gradual increase in the electrical potential concomitant with the increase in the residence period of the waste. The occurrence of values close to zero in the ditch in 2007 and positive values and rising towards the older ditches indicates that the decomposition of organic waste produces electric potential that can be measured by geophysicist instrumental.</p><p id="par0305" class="elsevierStylePara elsevierViewall">Decomposition processes of organic matter described in landfills involve the consumption of organic matter in aerobic and anaerobic stages, with oxygen consumption and generation of sub products such as CH<span class="elsevierStyleInf">4</span> and CO<span class="elsevierStyleInf">2</span>. The high oxygen consumption in latest ditches rich in organic matter results in a reducing environment, characterized by values that tend to negative. The decreasing availability of this material produces progressively less reducing conditions, reflected in increasingly positive electrical potential.<a name="p382"></a></p><p id="par0310" class="elsevierStylePara elsevierViewall">The progressive increase of the electric potential values enabled a statistical analysis that revealed the need for about 8 years so that the values measured on the waste ditches are similar to the electric potential of the uncontaminated adjacent area.</p><p id="par0315" class="elsevierStylePara elsevierViewall">This result is indicative of the average period for much of the organic matter consumption contained in domestic waste. However, the decomposition of waste such as paper, plastics and metals require tens to hundreds of years. The possibility of electric potential generation in this case is open to somewhat uncertain future studies.</p><p id="par0320" class="elsevierStylePara elsevierViewall">The predominance of organic matter in the buried waste, existence of a deep groundwater and lack of metallic conductor ore body are elements that do not favor the application of the geobattery model in an attempt to understand the factors that are responsible for the generation of electric potential contrast measured in the study area.</p><p id="par0325" class="elsevierStylePara elsevierViewall">Fixing the reference electrode in the external and topographically elevated area, different of the reading electrode moved to 241 measurement points and preferably fixed over waste ditches submitted to the action of organic matter decomposition processes, are elements that contribute to the understanding of the generation mechanism of natural electric potential in the study area, based on the proposed <a class="elsevierStyleCrossRef" href="#bib0090">Nyquist and Corry (2002)</a>. In this case, the contrast is generated by the potential difference between the reference electrode and the movable electrode.</p><p id="par0330" class="elsevierStylePara elsevierViewall">The likely predominance of the redox potential in the values generated by the decomposition of organic waste is indicative of the possibility of applying this geophysical method for monitoring areas contaminated by petroleum products.</p><p id="par0335" class="elsevierStylePara elsevierViewall">Even though involving relatively high complexity processes, the decomposition of oil in soils also requires the consumption of oxygen in several degrees, which depend on concentrations of contaminants within a plume of contamination, as suggested by the works of <a class="elsevierStyleCrossRef" href="#bib0095">Rabus and Heider (1998)</a> and <a class="elsevierStyleCrossRef" href="#bib0125">Thomas and Ward (1989)</a>. Therefore, similar results obtained in this work can also be achieved in areas contaminated by petroleum products.</p></span></span>" "textoCompletoSecciones" => array:1 [ "secciones" => array:11 [ 0 => array:3 [ "identificador" => "xres497949" "titulo" => "Resumen" "secciones" => array:1 [ 0 => array:1 [ "identificador" => "abst0005" ] ] ] 1 => array:2 [ "identificador" => "xpalclavsec519497" "titulo" => "Palabras clave" ] 2 => array:3 [ "identificador" => "xres497950" "titulo" => "Abstract" "secciones" => array:1 [ 0 => array:1 [ "identificador" => "abst0010" ] ] ] 3 => array:2 [ "identificador" => "xpalclavsec519496" "titulo" => "Key words" ] 4 => array:2 [ "identificador" => "sec0005" "titulo" => "Introduction" ] 5 => array:2 [ "identificador" => "sec0010" "titulo" => "Methodology" ] 6 => array:2 [ "identificador" => "sec0015" "titulo" => "Study area" ] 7 => array:2 [ "identificador" => "sec0020" "titulo" => "Results" ] 8 => array:2 [ "identificador" => "sec0025" "titulo" => "Conclusion" ] 9 => array:2 [ "identificador" => "xack160996" "titulo" => "Acknowledgements" ] 10 => array:1 [ "titulo" => "Bibliography" ] ] ] "pdfFichero" => "main.pdf" "tienePdf" => true "fechaRecibido" => "2012-10-24" "fechaAceptado" => "2013-01-30" "PalabrasClave" => array:2 [ "es" => array:1 [ 0 => array:4 [ "clase" => "keyword" "titulo" => "Palabras clave" "identificador" => "xpalclavsec519497" "palabras" => array:5 [ 0 => "zanja" 1 => "potencial espontáneo" 2 => "materia organic" 3 => "descomposición" 4 => "oxidación" ] ] ] "en" => array:1 [ 0 => array:4 [ "clase" => "keyword" "titulo" => "Key words" "identificador" => "xpalclavsec519496" "palabras" => array:5 [ 0 => "ditch" 1 => "self-potential" 2 => "organic matter" 3 => "decomposition" 4 => "oxidation" ] ] ] ] "tieneResumen" => true "resumen" => array:2 [ "es" => array:2 [ "titulo" => "Resumen" "resumen" => "<span id="abst0005" class="elsevierStyleSection elsevierViewall"><p id="spar0005" class="elsevierStyleSimplePara elsevierViewall">Los métodos geofísicos constituyen una herramienta efectiva para determinar alteraciones en las propiedades físicas de los ambientes geológicos, como son los suelos y aguas subterraneas influenciados por contaminantes. Este trabajo consistió en el análisis del potencial eléctrico natural obtenido en zanjas que contienedesechos sólidos con tiempo de confinamiento controlado. La interpretación de los resultados indica una correlación entre el tiempo de confinamiento de los residuos y el aumento de las variaciones de voltaje. Los datos sugieren que el potencial eléctrico resulta predominantemente de el fenómeno de potencial de oxidación/reducción, siendo el potencial del flujo insignificante. A través del análisis estadístico de los datos se estimó ocho años para volver a las características de una zona ausente de residuo, tiempo estimado para la descomposición de la mayor parte de la materia orgánica contenida en los residuos enterrados.</p></span>" ] "en" => array:2 [ "titulo" => "Abstract" "resumen" => "<span id="abst0010" class="elsevierStyleSection elsevierViewall"><p id="spar0010" class="elsevierStyleSimplePara elsevierViewall">The geophysical methods are effective tools for determining changes in physical parameters of the geological environment, as soil or groundwater in the presence of contamination. This work consisted on analyzing the natural electric potential obtained over domestic solid waste ditches with controlled closure dates. The interpretation data suggest the generation of electric potential predominantly through the redox phenomenon, as opposed to the flow potential phenomenon. The statistical data analysis indicates a correlation between residence time of the waste and growing variations of voltage. In addition highlights that eight years are required to achieve the reported values for the area with absence of waste, time estimated for decomposition of most organic matter contained in the buried waste.</p></span>" ] ] "multimedia" => array:5 [ 0 => array:7 [ "identificador" => "f0005" "etiqueta" => "Figure 1" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr1.jpeg" "Alto" => 1235 "Ancho" => 1363 "Tamanyo" => 287152 ] ] "descripcion" => array:1 [ "es" => "<p id="sp0005" class="elsevierStyleSimplePara elsevierViewall">Area of study.</p>" ] ] 1 => array:7 [ "identificador" => "f0010" "etiqueta" => "Figure 2" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr2.jpeg" "Alto" => 1235 "Ancho" => 1362 "Tamanyo" => 191316 ] ] "descripcion" => array:1 [ "es" => "<p id="sp0010" class="elsevierStyleSimplePara elsevierViewall">Self-potential map with closure ages of the ditches.</p>" ] ] 2 => array:7 [ "identificador" => "f0015" "etiqueta" => "Figure 3" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr3.jpeg" "Alto" => 764 "Ancho" => 1265 "Tamanyo" => 116998 ] ] "descripcion" => array:1 [ "es" => "<p id="sp0015" class="elsevierStyleSimplePara elsevierViewall">SP measures obtained over the ditches.</p>" ] ] 3 => array:7 [ "identificador" => "f0020" "etiqueta" => "Figure 4" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr4.jpeg" "Alto" => 821 "Ancho" => 1227 "Tamanyo" => 52984 ] ] "descripcion" => array:1 [ "es" => "<p id="sp0020" class="elsevierStyleSimplePara elsevierViewall">Mean and extreme values of SP for the second stage surveys.</p>" ] ] 4 => array:7 [ "identificador" => "f0025" "etiqueta" => "Figure 5" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr5.jpeg" "Alto" => 798 "Ancho" => 1255 "Tamanyo" => 80524 ] ] "descripcion" => array:1 [ "es" => "<p id="sp0025" class="elsevierStyleSimplePara elsevierViewall">Statistical analysis of the second stage data.</p>" ] ] ] "bibliografia" => array:2 [ "titulo" => "Bibliography" "seccion" => array:1 [ 0 => array:2 [ "identificador" => "bibs0005" "bibliografiaReferencia" => array:26 [ 0 => array:3 [ "identificador" => "bib0005" "etiqueta" => "Bagchi, 1987" "referencia" => array:1 [ 0 => array:2 [ "contribucion" => array:1 [ 0 => array:2 [ "titulo" => "Natural attenuation mechanisms of landfill leachate and effects of various factors on the mechanism" "autores" => array:1 [ 0 => array:2 [ "etal" => false "autores" => array:1 [ 0 => "A. 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The authors thank technician Francisco Manoel Garcia Barrera (DGA/UNESP) and geologist Gustavo Teixeira for their assistance in data acquisition.</p>" "vista" => "all" ] ] ] "idiomaDefecto" => "es" "url" => "/00167169/0000005200000004/v2_201505081341/S0016716913714843/v2_201505081341/es/main.assets" "Apartado" => array:4 [ "identificador" => "36047" "tipo" => "SECCION" "es" => array:2 [ "titulo" => "Original paper" "idiomaDefecto" => true ] "idiomaDefecto" => "es" ] "PDF" => "https://static.elsevier.es/multimedia/00167169/0000005200000004/v2_201505081341/S0016716913714843/v2_201505081341/es/main.pdf?idApp=UINPBA00004N&text.app=https://www.elsevier.es/" "EPUB" => "https://multimedia.elsevier.es/PublicationsMultimediaV1/item/epub/S0016716913714843?idApp=UINPBA00004N" ]
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