# Comparative Use of Soil Organic and Inorganic Amendments in Heavy Metals Stabilization

Authors: Agustina Branzini; Marta Susana Zubillaga
Journal: Applied and Environmental Soil Science
 (2012)

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## Abstract

Remediation strategies are capable to mitigate negative effects of heavy metals (HMs) on soils. The distribution of cooper (Cu), zinc (Zn), and chromium (Cr) was evaluated in a contaminated soil after adding biosolid compost (BC) and phosphate fertilizer (PF). A greenhouse assay and sequential extraction procedure were performed to determine the fractionation of HM in contaminated and remediated soil. In BC treatment, among 4 to 6% of Cu was associated with soil humic substances. Without amendments and with fertilizer application, Zn solubility increased by 15.4 and 8.4%, respectively, with experiment time. Although Cr was significantly adsorbed to the inorganic fraction, with compost application there was a transfer to organic fraction. A single amendment application is not suitable for immobilizing all metals of concern, because there are diverse union’s behaviors between HM and soil matrix. As the organic matter and phosphate fertilizer were effective in reducing mobility of Cu, the organic matter was more effective in the immobilization of Cr, and inorganic amendment induced the Zn precipitation, results from this pilot study suggest a combined use of these two amendments for soil remediation strategies. However, liming may be further needed to prevent soil acidification on longer time scales. Also, we propose the use of chemical and biological remediation strategies for potential improvement of effectiveness.


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## Body

## 1. Introduction

Point source and diffuse contamination of soils by heavy metals (HMs) is an environmental problem worldwide. An important input pathway is anthropogenic activities, such as disposal of industrial and hazardous residues, mining activities, incidental accumulations, industries atmospheric deposition, energy generation, and agricultural chemicals [2, 3]. High proportion of the contamination is retained by soil particles, so that is why this system is considered a vulnerable environment to being contaminated [4]. In addition, there is an increasing interest in HM contamination as a result of a continuous accumulation on top soil, with elevated availability to organisms [5]. Therefore, high concentrations of HM and their potential toxicity may affect soil ecology, agricultural production, and water quality, implicating risks for environment and human health [6].In Argentine, soil contamination has been mostly recorded in urban and periurban areas. Reference [7] indicated that concentrations of Cd, Cu, Pb, and Zn in urban soils exceeded the international standards referred to the human health, and according to [8], elevated levels of Cu, Pb, Cd, and Zn were found in horticultural soils of Buenos Aires. Contamination with Cu, Cr, Zn, As, Cd, Hg, and Pb occurred near the Ecological Reserve area of Buenos Aires, close to an automobile cemetery. Moreover, industrialized areas are affected by high Cu, Zn, and Cr concentrations in industrial effluents [9].Heavy metals partition in contaminated soils is influenced by several chemical and biological reactions [10, 11]. Soils retain HM by sorption, precipitation, and complexation; such reactions reduce the metal mobility and bioavailability [2, 12, 13]. However, this natural attenuation process can be complemented by in situ application of chemical technologies, as organic and inorganic amendments [14]. In situ chemical immobilization is a cost-effective remediation approach that stabilizes HM in contaminated soil [15, 16]. Generally, these technologies reduce HM availability, improve soil fertility, and increase plant growth [17, 18]. On one hand, organic amendments (compost) contain a high proportion of humified organic matter and could decrease HM bioavailability in soil, even though temporally and thus permitting the reestablishment of vegetation [19]. On the other hand, within the inorganic amendments, phosphate fertilizers are also effective in HM immobilization through formation of stable mineral HM phosphate [20]. The formation of these insoluble metal compounds, reduce their mobility through the soil profile and the pool available for biota [21]. In addition, the application of amendments simultaneously, could promote plant growth and biological activity of degraded soil [22].The objective of this study has been to assess the distribution of three heavy metals (Cu, Zn, and Cr) as a mixture in contaminated soil, after applying biosolid compost (BC) and phosphate fertilizer (PF), both independently and in combination.


## 2. Materials and Methods

### 2.1. Soil Sampling

Typic Hapludoll soil representative from sandy Pampas (35°37′S, 61°22′O) (Tables1 and 3) was chosen for the experiment. Five composite topsoil samples (0–20 cm depth) were randomly collected (10 individual samples). The sampled soil was air-dried and passed through a 2 mm sieve to obtain homogeneous particle size. Soil samples were enriched by adding metal solutions (CuCl22H2O, ZnSO47H2O, and H2CrO4), achieving final concentrations of 350 μg g−1 copper (Cu), 700 μg g−1 zinc (Zn), and 750 μg g−1 chromium (Cr). This enrichment overcame the maximum levels of total HM established in agricultural soils by Argentinean legislation (Table 3). Wetting cycles (at field capacity) and air-drying every five days were performed, during a period of three months.Table 1
Physicochemical characteristics of the Typic Hapludoll soil. All data are expressed as dry basis (DM).
ClaySiltSandTextureCECpHECOMtotalCsolubleNtotal%cmol·kg−11 : 2.5; H2OdS m−1%g kg Soil−119.223.257.6Sandy loam22.15.190.571.921.452.2OMtotal: total organic matter; Csoluble: soluble carbon; Ntotal: total nitrogen.


### 2.2. Greenhouse Experiment

The experiment consisted in 1 kg pots containing HM-enriched soil and two different amendments: Biosolid Compost (BC) (Tables2 and 3) as organic amendment and superphosphate triples (PF) as inorganic amendment (100 Mg ha−1 and 100 kg ha−1 rate, resp.). The compost was enriched with sawdust as bulking agents and biosolids from sewage sludge treatment plant located in the north of Buenos Aires City (1 : 1, biosolid: sawdust ratio by volume). Samples of enriched soil were thoroughly mixed with the amendments resulting in four treatments: (i) Contaminated Soil (CSC) as control, (ii) Contaminated Soil + Phosphate Fertilizer (CSC + PF), (iii) Contaminated Soil + Biosolid Compost (CSC + BC), and (iv) Contaminated Soil + Phosphate Fertilizer + Biosolid Compost (CSC + PF + BC). The experiment was carried out in a completely randomized design with three replications per treatment. Destructive samplings were performed at two time points of the experiment: beginning (0 days) and end (190 days).Table 2
Physical and chemical properties of the Biosolid Compost used as organic amendment. (DM: dry mater).
CECpHECOMtotalCsolubleNtotalC/N(cmol·kg−1)(1 : 2.5; H2O)dS m−1(%)(g kg Soil−1)14.37.51.294.250.0310.3213.2OMtotal: total organic matter; Csoluble: soluble carbon; Ntotal: total nitrogen; C/N: carbon-nitrogen coeficient.Table 3
Heavy metals content (in ppm) of soil samples and composted biosolids, and the maximum levels of total heavy metals established by Argentinean law (Hazardous wastes regime: soil quality guide).
Heavy metals (mg kg DM−1)Typical HapludollBiosolid CompostLaw 24051aAvailableTotalAvailableTotalTotalCu0.05117.01.52726.7150–500Zn0.04038.20.651183.3600–1500Cr<0.00114.913.2230.0750aLevels for soils with agricultural and industrial uses.


### 2.3. Soil Chemical Analysis

Sequential extraction procedure was performed on all samples from each pot (3 g in 50 cm3 polypropylene centrifuge tubes) to measure Cu, Zn, and Cr in different fractions after the application of BC and PF, separately and simultaneously, according to [23] methodology. This type of procedure has been successfully used for sludge-treated soils [24–26]. The procedure separates metals into four operationally defined fractions: soluble and exchangeable (EX), organic matter bound (OC), carbonate bound (CB), and residual (RES) (Table 4). After each extraction, the solution was separated from the solid by centrifugation at 3000 rpm for 45 min. The supernatant was decanted and filtered through Whatman N. 42 filter paper, and the wet residue in the tube was recorded. The pseudototal HM concentrations were determined by acid digestion with mixture of HCl, H2SO4, and HNO3 [1]. Heavy metals contents of each supernatant were measured at two time points by flame atomic absorption spectrophotometer (AAS). Soil pH and electricity conductivity (EC) was measured using a mixture of soil and deionized water (1 : 2.5 m/v) with a glass electrode [27] in each time point.Table 4
Sequential extraction procedure of heavy metals from soil samples and operationally defined fractions.
Phase/associationAbbr.StepOperational procedureSoluble—exchangeableEX130 mL 0.1 M CaCl2, shaken 16 h at room temperatureOrganic matter—boundOB230 mL 0.5 M NaOH, shaken 16 h at room temperatureCarbonates—boundCB330 mL 0.5 M Na2EDTA, shaken 1hResidualRES4Estimated by summation of three fractions and the total content (acid digestion with hydrochloric, sulfuric, and nitric acids) [1]


### 2.4. Statistical Analysis

Treatments effects were determined by factorial arrangement of 4 × 2 (amendment levels and time points), according to the general linear model procedure of Statistics, version 8.0. Differences between means were separated using least significant differences (LSDs). Variances were stabilized when necessary by a logarithmic transformation of some data set. In addition, a simple linear correlation between these variables was performed.


## 2.1. Soil Sampling

Typic Hapludoll soil representative from sandy Pampas (35°37′S, 61°22′O) (Tables1 and 3) was chosen for the experiment. Five composite topsoil samples (0–20 cm depth) were randomly collected (10 individual samples). The sampled soil was air-dried and passed through a 2 mm sieve to obtain homogeneous particle size. Soil samples were enriched by adding metal solutions (CuCl22H2O, ZnSO47H2O, and H2CrO4), achieving final concentrations of 350 μg g−1 copper (Cu), 700 μg g−1 zinc (Zn), and 750 μg g−1 chromium (Cr). This enrichment overcame the maximum levels of total HM established in agricultural soils by Argentinean legislation (Table 3). Wetting cycles (at field capacity) and air-drying every five days were performed, during a period of three months.Table 1
Physicochemical characteristics of the Typic Hapludoll soil. All data are expressed as dry basis (DM).
ClaySiltSandTextureCECpHECOMtotalCsolubleNtotal%cmol·kg−11 : 2.5; H2OdS m−1%g kg Soil−119.223.257.6Sandy loam22.15.190.571.921.452.2OMtotal: total organic matter; Csoluble: soluble carbon; Ntotal: total nitrogen.


## 2.2. Greenhouse Experiment

The experiment consisted in 1 kg pots containing HM-enriched soil and two different amendments: Biosolid Compost (BC) (Tables2 and 3) as organic amendment and superphosphate triples (PF) as inorganic amendment (100 Mg ha−1 and 100 kg ha−1 rate, resp.). The compost was enriched with sawdust as bulking agents and biosolids from sewage sludge treatment plant located in the north of Buenos Aires City (1 : 1, biosolid: sawdust ratio by volume). Samples of enriched soil were thoroughly mixed with the amendments resulting in four treatments: (i) Contaminated Soil (CSC) as control, (ii) Contaminated Soil + Phosphate Fertilizer (CSC + PF), (iii) Contaminated Soil + Biosolid Compost (CSC + BC), and (iv) Contaminated Soil + Phosphate Fertilizer + Biosolid Compost (CSC + PF + BC). The experiment was carried out in a completely randomized design with three replications per treatment. Destructive samplings were performed at two time points of the experiment: beginning (0 days) and end (190 days).Table 2
Physical and chemical properties of the Biosolid Compost used as organic amendment. (DM: dry mater).
CECpHECOMtotalCsolubleNtotalC/N(cmol·kg−1)(1 : 2.5; H2O)dS m−1(%)(g kg Soil−1)14.37.51.294.250.0310.3213.2OMtotal: total organic matter; Csoluble: soluble carbon; Ntotal: total nitrogen; C/N: carbon-nitrogen coeficient.Table 3
Heavy metals content (in ppm) of soil samples and composted biosolids, and the maximum levels of total heavy metals established by Argentinean law (Hazardous wastes regime: soil quality guide).
Heavy metals (mg kg DM−1)Typical HapludollBiosolid CompostLaw 24051aAvailableTotalAvailableTotalTotalCu0.05117.01.52726.7150–500Zn0.04038.20.651183.3600–1500Cr<0.00114.913.2230.0750aLevels for soils with agricultural and industrial uses.


## 2.3. Soil Chemical Analysis

Sequential extraction procedure was performed on all samples from each pot (3 g in 50 cm3 polypropylene centrifuge tubes) to measure Cu, Zn, and Cr in different fractions after the application of BC and PF, separately and simultaneously, according to [23] methodology. This type of procedure has been successfully used for sludge-treated soils [24–26]. The procedure separates metals into four operationally defined fractions: soluble and exchangeable (EX), organic matter bound (OC), carbonate bound (CB), and residual (RES) (Table 4). After each extraction, the solution was separated from the solid by centrifugation at 3000 rpm for 45 min. The supernatant was decanted and filtered through Whatman N. 42 filter paper, and the wet residue in the tube was recorded. The pseudototal HM concentrations were determined by acid digestion with mixture of HCl, H2SO4, and HNO3 [1]. Heavy metals contents of each supernatant were measured at two time points by flame atomic absorption spectrophotometer (AAS). Soil pH and electricity conductivity (EC) was measured using a mixture of soil and deionized water (1 : 2.5 m/v) with a glass electrode [27] in each time point.Table 4
Sequential extraction procedure of heavy metals from soil samples and operationally defined fractions.
Phase/associationAbbr.StepOperational procedureSoluble—exchangeableEX130 mL 0.1 M CaCl2, shaken 16 h at room temperatureOrganic matter—boundOB230 mL 0.5 M NaOH, shaken 16 h at room temperatureCarbonates—boundCB330 mL 0.5 M Na2EDTA, shaken 1hResidualRES4Estimated by summation of three fractions and the total content (acid digestion with hydrochloric, sulfuric, and nitric acids) [1]


## 2.4. Statistical Analysis

Treatments effects were determined by factorial arrangement of 4 × 2 (amendment levels and time points), according to the general linear model procedure of Statistics, version 8.0. Differences between means were separated using least significant differences (LSDs). Variances were stabilized when necessary by a logarithmic transformation of some data set. In addition, a simple linear correlation between these variables was performed.


## 3. Results and Discussion

### 3.1. Distribution of HM in Soil Fractions

The distribution of Cu, Zn, and Cr in contaminated and remediated soils for both sampling dates is reported in Table5. Heavy metals in contaminated and amended soils showed similar pattern of distribution between fractions. Furthermore, each metal was associated in a different way with soil components, as was expected. These differential trends are in agreement with other studies, which demonstrate that the adsorption process is metal specific [28, 29].Table 5
Distribution of copper (a), zinc (b), and chromium (c) in soil chemical fractions at two time points of the experiment: beginning (A) and end (B). Treatments: CSC: Contaminated Soil, CSC + PF: Contaminated Soil + Phosphate Fertilizer, CSC + BC: Contaminated Soil + Biosolid Compost, and CSC + PF + BC: Contaminated Soil + Phosphate Fertilizer + Biosolid Compost (Mean ± S.D.,n=3).
(a)Soluble and exchangeableHeavy metals concentration (mg kg−1)CuZnCrCSC (A)2.56 ± 0.8553.00 ± 2.60.27 ± 0.0CSC (B)4.25 ± 0.5457.00 ± 47.60.54 ± 0.1CSC + PF (A)4.70 ± 2.4569.33 ± 77.50.53 ± 0.0CSC + PF (B)5.14 ± 2.7438.17 ± 77.90.64 ± 0.2CSC + BC (A)3.72 ± 0.3547.67 ± 67.20.43 ± 0.0CSC + BC (B)3.75 ± 1.0426.17 ± 68.00.50 ± 0.5CSC + PF + BC (A)4.76 ± 0.7557.33 ± 19.00.62 ± 0.1CSC + PF + BC (B)4.95 ± 0.4422.67 ± 23.10.79 ± 0.2ANOVAAmendmentsMoment*Amendments × momentnsnsns(b)Organic matter boundHeavy metals concentration (mg kg−1)CuZnCrCSC (A)183.27 ± 16.3195.17 ± 6.732.63 ± 6.6CSC (B)200.73 ± 7.2115.73 ± 0.657.48 ± 2.9CSC + PF (A)186.20 ± 12.6141.33 ± 25.032.20 ± 2.7CSC + PF (B)199.93 ± 18.7110.80 ± 26.052.15 ± 10.6CSC + BC (A)196.93 ± 13.4193.33 ± 63.134.20 ± 7.4CSC + BC (B)206.30 ± 16.3140.20 ± 31.545.57 ± 6.9CSC + PF + BC (A)202.00 ± 10.1172.50 ± 13.528.87 ± 2.8CSC + PF + BC (B)189.80 ± 3.7126.20 ± 20.939.70 ± 0.8ANOVAAmendments*Moment**Amendments × momentnsnsns(c)Carbonate boundHeavy metals concentration (mg kg−1)CuZnCrCSC (A)189.20 ± 12.6330.33 ± 29.5139.47 ± 5.1CSC (B)183.97 ± 17.1199.83 ± 19.3152.13 ± 2.8CSC + PF (A)183.90 ± 2.5340.67 ± 111.6138.20 ± 9.0CSC + PF (B)166.73 ± 10.8197.17 ± 29.5143.83 ± 14.3CSC + BC (A)190.53 ± 11.3334.00 ± 84.3123.73 ± 14.6CSC + BC (B)150.85 ± 11.6234.67 ± 26.3145.95 ± 0.9CSC + PF + BC (A)187.20 ± 9.8317.67 ± 9.7115.93 ± 11.6CSC + PF + BC (B)162.30 ± 8.9242.33 ± 44.7143.47 ± 4.3ANOVAAmendments*Moment***Amendments × momentnsnsns(d)ResidualHeavy metals concentration (mg kg−1)CuZnCrCSC (A)29.25 ± 2.539.6 ± 12.2446.8 ± 1.0CSC (B)20.76 ± 3.230.2 ± 5.8466.28 ± 2.6CSC + PF (A)20.1 ± 8.3123.4 ± 39.6469.5 ± 6.0CSC + PF (B)39.52 ± 17.128.52 ± 5.6616.02 ± 14.4CSC + BC (A)32.8 ± 14.4113.2 ± 38.6476.3 ± 12.4CSC + BC (B)50.18 ± 0.863.21 ± 2.6496.43 ± 4.1CSC + PF + BC (A)31.2 ± 5.555.0 ± 4.4431.5 ± 6.0CSC + PF + BC (B)45.67 ± 4.339.99 ± 28.5543.13 ± 2.4ANOVAAmendments**Moment**Amendments × momentnsns*Significance levels:P<0.05; ns: not significant.In particular, copper was mainly associated with soil organic matter (Table5(b)) (P<0.001), forming that make metals less available for plants [30]. Copper-organic matter association was slightly higher at the end of the experiment, especially with biosolid compost application (among 4 to 6%) in comparison with the other treatments. In agreement with [31], extraction procedure showed that in contaminated soils Cu was mostly present in the acid-soluble and reducible fractions, and in soil amendment with organic matter the soluble and exchangeable Cu fraction was reduced. A possible explanation for this result is the precipitation and complexation by the presence of stabilized organic matter in the compost, such as humic substances (Table 2) [16, 32]. These results corroborate other investigator findings which indicated that organic matter plays a fundamental role in controlling soil HM adsorption, being Cu the preferentially associated with the organic fraction [33]. On the other hand, [34] reported that extractable amounts of Cu were always very small, indicating a low contribute from soluble organic Cu complexes. However, in this pilot study the amount of Cu-EX was lower than 1% of total heavy metal content, and at the end of the experiment, compost and BC + PF treatments had more Cu in residual fraction, indicating greater Cu immobilization.In all treatments, Zn was remained mostly in soluble and exchangeable fraction of soil as mobile Zn (P<0.001). In contaminated soil without amendments (CSC) and with fertilizer application, Zn solubility increased by 15.4 and 8.4%, respectively, with experiment time. These results differ with [35], who demonstrated that leached Zn concentration decreased 5.92 ± 2.74 mg kg−1 with phosphate amendment, as a result of immobilization by metal-phosphate precipitates. However, our results are in agreement with those of other studies, which confirm that this increase was possible associated with soil acidification [16, 36, 37]. It cannot be excluded that the simultaneous adding of metal cations could affect Zn adsorption, in agreement with [38], due to ionic competition between Zn, Cu, and Cr [8]. Metals with high water solubility pose higher risk of leaching into groundwater. In fact, [39] established that, according to maximum leached concentrations (as a fraction of the total concentration in soil), Zn was the most mobile element in a sequence composite by Zn, Cu, As, and Cr. As a consequence, Zn may offer major environmental risk compared to other metals, since mobile Zn is immediately available for absorption by plants and soil biota in accordance [40, 41].Chromium was initially adsorbed by soil carbonates as compared with soil organic matter (P<0.001) [42, 43]. In contrast, at the end of the experiment, a Cr redistribution among fractions was observed and the Cr fraction organic associated to the soil organic matter increased by 10% in the BC treatment, as compared to the beginning of the experiment. This suggests that the addition of organic amendments could enhance the reduction rate of Cr (VI) to Cr (III) increasing it temporal immobilization in soil [44]. According to [34] Cr amounts associated with organic matter increase with the increasing extent of soil contamination, thereby suggesting high constants values of organic-Cr complexes. Moreover, these authors demonstrated that Cr undergoes a progressive insolubilization (organically bound Cr into insoluble Cr) in about 20 years. In this pilot experiment we cannot corroborate this ageing process due to the soil metal spiking approach and the relatively short incubation time.According to [45] and assuming that mobility and availability of Cu, Zn, and Cr are associated with their solubility and geochemical forms and that these HMs reduce in the order of extraction sequence, the apparent mobility and potential availability in the soil were Zn > Cu > Cr. In addition, [46] reported that in carbonate soils Cr, Cu, and Pb had higher affinity for the reactive solid phases than Ni, Zn and Cd. The active role of amorphous Al silicates and interaction between clays and organic matter from compost, with formation of organoclays, would have improved the soil adsorbing capacity and enhanced this HM competition [34].


### 3.2. Effect of Amendments Application on Soil Chemical Characteristics

Application of amendments improved the soil chemical characteristics (Figure1). Initially, soil pH increased with the addition of both amendments, compared to untreated soil. Since these results were in agreement with those found in a previous study [47], this soil pH modification was slight (2.87%=BC and 2.87%=PF), and there was no correlation with HM bioavailability [48]. Soil acidification observed upon increasing of the experiment time for all treatments was possibly due to soil organic matter mineralization [49] and/or to H+ formation by the fertilizer solubilization [50]. Therefore, liming may be necessary to compensate potential soil acidification when using PF and BC application to reduce HM-contaminated soil [51]. Contrary to [52], we found that soil EC decreased significantly when organic amendment was added (P=0.044), at the end of the experiment, and no correlation was found between the EC and heavy metals availability.Figure 1
Changes in chemical characteristics of contaminated and organic and inorganic remediated soil, respect to assay time. Treatments: CSC = Contaminated Soil, CSC + PF = Contaminated Soil + Phosphate Fertilizer, CSC + BC = Contaminated Soil + Biosolid Compost, and CSC + PF + BC = Contaminated Soil + Phosphate Fertilizer + Biosolid Compost. The bars indicate Standard Error of the data.


## 3.1. Distribution of HM in Soil Fractions

The distribution of Cu, Zn, and Cr in contaminated and remediated soils for both sampling dates is reported in Table5. Heavy metals in contaminated and amended soils showed similar pattern of distribution between fractions. Furthermore, each metal was associated in a different way with soil components, as was expected. These differential trends are in agreement with other studies, which demonstrate that the adsorption process is metal specific [28, 29].Table 5
Distribution of copper (a), zinc (b), and chromium (c) in soil chemical fractions at two time points of the experiment: beginning (A) and end (B). Treatments: CSC: Contaminated Soil, CSC + PF: Contaminated Soil + Phosphate Fertilizer, CSC + BC: Contaminated Soil + Biosolid Compost, and CSC + PF + BC: Contaminated Soil + Phosphate Fertilizer + Biosolid Compost (Mean ± S.D.,n=3).
(a)Soluble and exchangeableHeavy metals concentration (mg kg−1)CuZnCrCSC (A)2.56 ± 0.8553.00 ± 2.60.27 ± 0.0CSC (B)4.25 ± 0.5457.00 ± 47.60.54 ± 0.1CSC + PF (A)4.70 ± 2.4569.33 ± 77.50.53 ± 0.0CSC + PF (B)5.14 ± 2.7438.17 ± 77.90.64 ± 0.2CSC + BC (A)3.72 ± 0.3547.67 ± 67.20.43 ± 0.0CSC + BC (B)3.75 ± 1.0426.17 ± 68.00.50 ± 0.5CSC + PF + BC (A)4.76 ± 0.7557.33 ± 19.00.62 ± 0.1CSC + PF + BC (B)4.95 ± 0.4422.67 ± 23.10.79 ± 0.2ANOVAAmendmentsMoment*Amendments × momentnsnsns(b)Organic matter boundHeavy metals concentration (mg kg−1)CuZnCrCSC (A)183.27 ± 16.3195.17 ± 6.732.63 ± 6.6CSC (B)200.73 ± 7.2115.73 ± 0.657.48 ± 2.9CSC + PF (A)186.20 ± 12.6141.33 ± 25.032.20 ± 2.7CSC + PF (B)199.93 ± 18.7110.80 ± 26.052.15 ± 10.6CSC + BC (A)196.93 ± 13.4193.33 ± 63.134.20 ± 7.4CSC + BC (B)206.30 ± 16.3140.20 ± 31.545.57 ± 6.9CSC + PF + BC (A)202.00 ± 10.1172.50 ± 13.528.87 ± 2.8CSC + PF + BC (B)189.80 ± 3.7126.20 ± 20.939.70 ± 0.8ANOVAAmendments*Moment**Amendments × momentnsnsns(c)Carbonate boundHeavy metals concentration (mg kg−1)CuZnCrCSC (A)189.20 ± 12.6330.33 ± 29.5139.47 ± 5.1CSC (B)183.97 ± 17.1199.83 ± 19.3152.13 ± 2.8CSC + PF (A)183.90 ± 2.5340.67 ± 111.6138.20 ± 9.0CSC + PF (B)166.73 ± 10.8197.17 ± 29.5143.83 ± 14.3CSC + BC (A)190.53 ± 11.3334.00 ± 84.3123.73 ± 14.6CSC + BC (B)150.85 ± 11.6234.67 ± 26.3145.95 ± 0.9CSC + PF + BC (A)187.20 ± 9.8317.67 ± 9.7115.93 ± 11.6CSC + PF + BC (B)162.30 ± 8.9242.33 ± 44.7143.47 ± 4.3ANOVAAmendments*Moment***Amendments × momentnsnsns(d)ResidualHeavy metals concentration (mg kg−1)CuZnCrCSC (A)29.25 ± 2.539.6 ± 12.2446.8 ± 1.0CSC (B)20.76 ± 3.230.2 ± 5.8466.28 ± 2.6CSC + PF (A)20.1 ± 8.3123.4 ± 39.6469.5 ± 6.0CSC + PF (B)39.52 ± 17.128.52 ± 5.6616.02 ± 14.4CSC + BC (A)32.8 ± 14.4113.2 ± 38.6476.3 ± 12.4CSC + BC (B)50.18 ± 0.863.21 ± 2.6496.43 ± 4.1CSC + PF + BC (A)31.2 ± 5.555.0 ± 4.4431.5 ± 6.0CSC + PF + BC (B)45.67 ± 4.339.99 ± 28.5543.13 ± 2.4ANOVAAmendments**Moment**Amendments × momentnsns*Significance levels:P<0.05; ns: not significant.In particular, copper was mainly associated with soil organic matter (Table5(b)) (P<0.001), forming that make metals less available for plants [30]. Copper-organic matter association was slightly higher at the end of the experiment, especially with biosolid compost application (among 4 to 6%) in comparison with the other treatments. In agreement with [31], extraction procedure showed that in contaminated soils Cu was mostly present in the acid-soluble and reducible fractions, and in soil amendment with organic matter the soluble and exchangeable Cu fraction was reduced. A possible explanation for this result is the precipitation and complexation by the presence of stabilized organic matter in the compost, such as humic substances (Table 2) [16, 32]. These results corroborate other investigator findings which indicated that organic matter plays a fundamental role in controlling soil HM adsorption, being Cu the preferentially associated with the organic fraction [33]. On the other hand, [34] reported that extractable amounts of Cu were always very small, indicating a low contribute from soluble organic Cu complexes. However, in this pilot study the amount of Cu-EX was lower than 1% of total heavy metal content, and at the end of the experiment, compost and BC + PF treatments had more Cu in residual fraction, indicating greater Cu immobilization.In all treatments, Zn was remained mostly in soluble and exchangeable fraction of soil as mobile Zn (P<0.001). In contaminated soil without amendments (CSC) and with fertilizer application, Zn solubility increased by 15.4 and 8.4%, respectively, with experiment time. These results differ with [35], who demonstrated that leached Zn concentration decreased 5.92 ± 2.74 mg kg−1 with phosphate amendment, as a result of immobilization by metal-phosphate precipitates. However, our results are in agreement with those of other studies, which confirm that this increase was possible associated with soil acidification [16, 36, 37]. It cannot be excluded that the simultaneous adding of metal cations could affect Zn adsorption, in agreement with [38], due to ionic competition between Zn, Cu, and Cr [8]. Metals with high water solubility pose higher risk of leaching into groundwater. In fact, [39] established that, according to maximum leached concentrations (as a fraction of the total concentration in soil), Zn was the most mobile element in a sequence composite by Zn, Cu, As, and Cr. As a consequence, Zn may offer major environmental risk compared to other metals, since mobile Zn is immediately available for absorption by plants and soil biota in accordance [40, 41].Chromium was initially adsorbed by soil carbonates as compared with soil organic matter (P<0.001) [42, 43]. In contrast, at the end of the experiment, a Cr redistribution among fractions was observed and the Cr fraction organic associated to the soil organic matter increased by 10% in the BC treatment, as compared to the beginning of the experiment. This suggests that the addition of organic amendments could enhance the reduction rate of Cr (VI) to Cr (III) increasing it temporal immobilization in soil [44]. According to [34] Cr amounts associated with organic matter increase with the increasing extent of soil contamination, thereby suggesting high constants values of organic-Cr complexes. Moreover, these authors demonstrated that Cr undergoes a progressive insolubilization (organically bound Cr into insoluble Cr) in about 20 years. In this pilot experiment we cannot corroborate this ageing process due to the soil metal spiking approach and the relatively short incubation time.According to [45] and assuming that mobility and availability of Cu, Zn, and Cr are associated with their solubility and geochemical forms and that these HMs reduce in the order of extraction sequence, the apparent mobility and potential availability in the soil were Zn > Cu > Cr. In addition, [46] reported that in carbonate soils Cr, Cu, and Pb had higher affinity for the reactive solid phases than Ni, Zn and Cd. The active role of amorphous Al silicates and interaction between clays and organic matter from compost, with formation of organoclays, would have improved the soil adsorbing capacity and enhanced this HM competition [34].


## 3.2. Effect of Amendments Application on Soil Chemical Characteristics

Application of amendments improved the soil chemical characteristics (Figure1). Initially, soil pH increased with the addition of both amendments, compared to untreated soil. Since these results were in agreement with those found in a previous study [47], this soil pH modification was slight (2.87%=BC and 2.87%=PF), and there was no correlation with HM bioavailability [48]. Soil acidification observed upon increasing of the experiment time for all treatments was possibly due to soil organic matter mineralization [49] and/or to H+ formation by the fertilizer solubilization [50]. Therefore, liming may be necessary to compensate potential soil acidification when using PF and BC application to reduce HM-contaminated soil [51]. Contrary to [52], we found that soil EC decreased significantly when organic amendment was added (P=0.044), at the end of the experiment, and no correlation was found between the EC and heavy metals availability.Figure 1
Changes in chemical characteristics of contaminated and organic and inorganic remediated soil, respect to assay time. Treatments: CSC = Contaminated Soil, CSC + PF = Contaminated Soil + Phosphate Fertilizer, CSC + BC = Contaminated Soil + Biosolid Compost, and CSC + PF + BC = Contaminated Soil + Phosphate Fertilizer + Biosolid Compost. The bars indicate Standard Error of the data.


## 4. Conclusions

Results from this pilot experiment, showed that application of BC and PF in combination affected the partition of Cr, Cu, and Zn added to soil. In particular, BC and PF in combination reduced the solubility and mobility of Cu and Cr whereas Zn stabilization was increased through compost with or without PF application. The use of PF alone increased the available Zn. These results show that combination of organic and inorganic amendments are needed for immobilizing different metals of concern and could provide a basis for future research about the existence of interactions between metals added simultaneously into the soil. However, the use of liming agents may be needed to buffer soil acidification on prolonged time scales.



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*Source: 721032-2012-04-05.xml*