Organic Matter and Barium Absorption by Plant Species Grown in an Area Polluted with Scrap Metal Residue

Abreu, Cleide Aparecida; Cantoni, Mariana; Coscione, Aline Renée; Paz-Ferreiro, Jorge

doi:https://doi.org/10.1155/2012/476821

Applied and Environmental Soil Science

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Soil Management for Sustainable Agriculture

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Volume 2012 | Article ID 476821 | https://doi.org/10.1155/2012/476821

Organic Matter and Barium Absorption by Plant Species Grown in an Area Polluted with Scrap Metal Residue

Cleide Aparecida Abreu,¹Mariana Cantoni,²Aline Renée Coscione,¹and Jorge Paz-Ferreiro³

Academic Editor: Philip White

Received18 Oct 2011

Revised27 Dec 2011

Accepted08 Jan 2012

Published20 Mar 2012

Abstract

The effect of organic matter addition on Ba availability to Helianthus annuus L., Raphanus sativus L., and Ricinus communis L. grown on a Neossolo Litólico Chernossólico fragmentário (pH 7.5), contaminated with scrap residue was evaluated. Four rates (0, 20, 40, and 80 Mg ha⁻¹, organic carbon basis) of peat or sugar cane filter, with three replicates, were tested. Plant species were grown until the flowering stage. No effect of organic matter addition to soil on dry matter yield of oilseed radish shoots was observed, but there was an increase in sunflower and castor oil plant shoots when sugar cane filter cake was used. The average Ba transferred from roots to shoots was more than 89% for oilseed radish, 71% for castor oil plants, and 59% for sunflowers. Organic matter treatments were not efficient in reducing Ba availability due to soil liming.

1. Introduction

Accumulation of some chemical elements in the environment is of great concern because they can reach concentrations that may cause risks to human health and to the environment. Their concentration in soils depends on lithogenic and pedogenic processes, but also on anthropogenic activities. Soil pollution is a serious problem in many countries around the world. In São Paulo State, Brazil, since 2002, when the first survey was performed by the local environmental agency, more than 1600 contaminated areas have been identified [1].

The extensive industrial use of barium (Ba) adds up to the release of Ba in the environment and, as a result, Ba concentrations in air, water, and soil may be higher than naturally occurring concentrations on many locations [2–5]. Recently, it was observed that successive sewage sludge applications increased soil Ba concentration and accumulation in maize plants grown in the State of São Paulo [6]. Some research has shown probable Ba toxicity in plants, but such studies were short term and performed in nutrient solution [7, 8]. Ba is an alkaline earth element which occurs as a trace metal in igneous and sedimentary rocks. In nature it occurs mainly as low soluble minerals such as barite (BaSO₄) and witherite (BaCO₃). Ba solubilization and, consequently, the release of Ba²⁺ ions may occur under specific conditions. It has been shown to happen in acidic conditions [9], in the absence of oxygen, or even due to microbial action [10–13]. In contrast, Ba precipitates as a sulfate and/or carbonate salt in neutral or basic pH conditions. Therefore, the mobility of Ba is negligible in neutral or basic pH conditions, thus, reducing the risks of leaching and harmful health effects.

The application of lime and the addition of organic materials are considered the most efficient options to reduce heavy metal availability in soils [14–16]. The use of organic matter in chemically degraded areas can also be beneficial since plant development in such areas is frequently affected, exposing the soil to physical degradation.

Peat and humic materials concentrate reduced extractable Zn, Cu, Pb, and B in soil and mustard shoots [14] while liming reduced the available concentrations of Cd, Pb, Cu, and Zn in soils as well as its content in velvetbean shoots [16].The bioavailability of heavy metals to soybean and black-oat cultures was close to zero, when 8 Mg ha⁻¹ sewage sludge, flue dust, and aqueous lime was applied to soil surface in no-till system [15]. However, lime and organic matter addition to the Ba contaminated soil and its availability to soil and its plants absorption have not received a great deal of attention and few information on the topic has been reported. The organic matter complexation of Ba ions can lead to insoluble species, decreasing the availability of Ba and enabling the growth of vegetation in highly contaminated areas [3]. Consequently, Ba effects on plant grown in soils containing Ba still needs to be further investigated.

The aim of the present work was to evaluate the effect of application rates of peat and sugar cane filter cake on Ba concentration in soil and its potential availability to sunflowers (Helianthus annuus L.), oilseed radish (Raphanus sativus L.), and castor oil plants (Ricinus communis L.) grown in a soil (pH 7.5) contaminated with scrap metal residue.

2. Material and Methods

In 2005, automobile scrap “shredder residue” was applied to the soil of an agricultural area of approximately 3 ha located in Piracicaba (22°42'30” S, 47°38'01” W), São Paulo State, Brazil. The residue’s metal content, obtained by the SW-846 3051 method [18] was, in mg kg⁻¹: 170 of B, 7.4 of Cd, 2497 of Cu, 775 of Pb, 178 of Cr, 153 of Ni, 8157 of Zn, and 920 of Ba. Residue addition was performed based on the supposition that it may provide Zn and Cu to sugar cane crops, and the residue was incorporated into the soil at a depth of 30 cm. The local environmental agency (CETESB) later verified that the area was contaminated by heavy metals (copper and zinc) and boron. Lime (10 Mg ha⁻¹) was added to the soil in order to reduce heavy metals mobility and potential leaching. The soil in this area is classified as Lithic Udorthent [19].

Soil samples were taken from the 0–20 cm depth layer, dried at room temperature, and sieved to 2.0 mm. The soil fertility attributes were measured as follows: ; g dm⁻³; mg dm⁻³; mmol_c dm⁻³; mmol_c dm⁻³; mmol_c dm⁻³; mmol_c dm⁻³; mmol_c dm⁻³; according to [20]. For the determination P, K, Ca a mixed (cationic and anionic) ion exchange resin method (Amberlite IRA 120 and Amberlite IRA 400) was used to simulate elements soil availability. It employs a ratio of 2.5 of soil per 2.5 cm³ of resin, which is kept in contact for 16 hours. The elements adsorbed by resin are washed away with 50 mL of a 0.8 mol L⁻¹ NH₄Cl + 0.2 mol L⁻¹ HCl, producing an extract where the elements are determined. Some of total elements content in the soil were measured by SW-846 3051 method [20] as follows, in mg kg⁻¹: 241 of Ba, 62 of B, 4.3 of Cd, 335 of Cu, 332 of Pb, 88.2 of Cr, 53.6 of Ni, and 2998 of Zn. This procedure consists of adding 10 mL of HNO₃ to 500 mg soil in a teflon capped vessel in a laboratory microwave system (CEM, Mars 5 model, Xpress vessels). The extraction is performed by raising the temperature to 170°C for 5 min and keeping it at this temperature during 10 minutes.

The experiment was carried out in a greenhouse at Campinas (São Paulo State, Brazil) in plastic pots (5 dm⁻³). The following plant species: sunflowers (Helianthus annuus L.), oilseed radish (Raphanus sativus L.), and castor oil plants (Ricinus communis L.) were selected for the experiment due to previous works showing them to be tolerant to high concentration of heavy metals and boron in soil [21–24].

The experimental design was in randomized complete blocks with four rates (0, 20, 40, and 80 Mg ha⁻¹, organic carbon basis) of two organic matter sources (peat and sugar cane filter cake), with three replicates. The treatments were applied at (g pot⁻¹): 0.0, 37.9, 75.8, and 151.6 g of sugar cane filter cake per pot, respectively and 0.0, 61.3, 122.6, and 245.2 g of peat per pot. The chemical compositions of the peat and sugar cane filter cake (Table 1) were obtained by determination of elements in a 0.5 mg of sample extractred with nitric perchloric acids (3 : 1 ratio) [17].

The soil/organic materials were carefully homogenized and incubated at room temperature for 20 days with soil moisture maintained at 60% water holding capacity (WHC). The pots received 200 mg kg⁻¹ of P as triple superphosphate (41% P₂O₅) and the samples were homogenized and incubated for an additional 15 days after the sowing of seeds.

Three sunflowers and castor oil plants and ten oilseed radish were grown per pot. Deionized water was supplied by weighing the pots daily and adding the water needed to maintain 60% WHC. Nitrogen (30 mg N kg⁻¹ soil) was applied as ammonium nitrate (32% N) on emerging seedlings and again 15 days later.

Sunflower and oilseed radish were harvested 65 days after sowing, while castor oil plants were harvested 74 days after sieving. Shoots were separated from roots at harvest. The flowers were also separated when the oilseed radish and sunflowers were harvested. Roots were sieved, washed and soaked for 90 min in a solution of 0.02 mmol L⁻¹ EDTA (disodium salt). After soaking, the oilseed radish roots were washed again with distilled water. Plant samples were washed, dried, and weighed and then digested using HNO₃/H₂O₂ in a CEM Mars 5 microwave oven and analyzed for macro- and micronutrients, and barium, lead, cadmium, chromium, and nickel.

Soil samples collected after incubation were air-dried and sieved through a 2 mm mesh screen and then characterized for total and available metal contents. Available Ba content was analyzed using Mehlich-3 method (CH₃COOH 0.2 mol L⁻¹ + NH₄NO₃ 0.25 mol L⁻¹ + NH₄F 0.015 mol L⁻¹ + HNO₃ 0.015 mol L⁻¹ + EDTA 0.001 mol L⁻¹ at pH 2.5) by agitation of five cm³ of soil and 20 mL the Mehlich-3 solution for 5 min [25]. The availability of several nutrients (P, K, Ca, and Mg) was evaluated by the ion exchange method [20].

Ba transported from soil to shoots was evaluated using the transfer factor (TF) as follows: TF = PC (mg kg⁻¹)/SC (mg kg⁻¹), where CP is the Ba concentration in the whole plant (root and shoot), and CT is the concentration of Ba in the soil [26]. The ability of each species to translocate Ba from the roots to the shoots was calculated using the following translocation index (TI): TI (%) = QPA (mg pot⁻¹)/QAP (mg pot⁻¹) × 100, where QPA is the element accumulation in the shoots, and QAP is the element accumulation in the whole plant (shoots and roots) [26].

The plant efficiency for the removal of elements (removal factor, ) was calculated using the following equation: (%) = QPA (mg pot⁻¹)/QR (mg pot⁻¹) × 100, where QR is the amount of Ba to be removed from the soil (mg pot⁻¹) [27]. When considering a 75% reduction of Ba concentration in the soil as a target, the time (, in years) needed for Ba removal was calculated as follows: , where is the percentage of Ba reduction in the soil, is the removal factor, and NC is the number of crop cycles/year (considered as 1 cycle/year).

The data were submitted to analyses of variance (ANOVA), and the mean values were compared according to Tukey’s test (). When significant, the results obtained with the different concentrations of organic material were also examined using regression analysis (linear and quadratic models tested).

3. Results and Discussion

The concentration of Ba found during the soil characterization (241 mg kg⁻¹) was close to the intervention levels (300 mg kg⁻¹) established by the Environmental Agency of the State of São Paulo [28]. Although the concentration of zinc, copper, and boron in this area is also worrisome, the use of plants that could help to remediate the soil was studied on previous works and was not significant in the present work as also discussed below [24, 29].

Mehlich-3 available Ba increased in soils amended with 40 Mg ha⁻¹ of peat and 80 Mg ha⁻¹ of sugar cane filter cake, with an average of 32.9 mg dm⁻³ in the soils amended with sugar cane filter cake and 36.2 mg dm⁻³ in the soils amended with peat (Table 2), which corresponded to a 12.3% and 14.4% recovery, respectively. The recovery found in this study was lower than the one reported by others which was in a range from 50% to 78% [30]. The correlation between extractable Ba and soil organic carbon was 0.96 (sugar cane filter cake) and 0.95 (peat). However, no significant correlation was found between extractable Ba in the soil and the Ba accumulated in all of the plant tissues.

In most plants, the concentration of Ba ranges from 4 to 50 mg kg⁻¹ [31], and concentrations of 200 and 500 mg kg⁻¹ are considered to be slightly toxic or toxic, respectively [32]. The average Ba concentrations in the shoots after addition of sugar cane filter cake or peat were as follows: 44.47 or 50.97 mg kg⁻¹, respectively, in sunflowers; 29.68 or 30.03 mg kg⁻¹, respectively, in castor oil plants; and 77.23 or 74.46 mg kg⁻¹, respectively, in oilseed radish (Table 3). Similar results have been reported for the same plant species grown in Rhodic Hapludox using BaSO₄additions of 0, 150, and 300 mg kg⁻¹. The plant tissue Ba concentrations found in the present study were higher than previously reported (21.3 mg kg⁻¹ for sunflowers, 19.4 mg kg⁻¹ for mustard plants, and 10.6 mg kg⁻¹ for castor oil plants [30]).

However, Ba concentrations in this study were less than those reported by Suwa et al., 2008 [8] who observed that high Ba concentrations affected soybeans and resulted in reduced development, stomatal closing, and reduced photosynthetic activity. In contrast, Ba accumulation in maize plants grown in soil with much lower Ba concentrations (soil pH in the range of 5.1 to 5.7) has also been reported and no phytotoxic symptoms or nutritional imbalance correlations were observed [6].

In this study no effects or symptoms of phytotoxicity were found in the plants. Moreover, no nutritional imbalance was observed in the soil samples. In the presence of high Ca concentrations, such as those of the area studied, Ba can precipitate [9]. The absence of phytotoxic in this study might bel explained by the high levels of available Ca (294 dm⁻³).

Shoot dry matter yields varied depending on the treatment and plant species (Table 4). Among the species tested, oilseed radish was the least affected by the treatments, and the peat addition promoted a higher dry matter yield in the oilseed radish roots. Sunflowers and castor oil plants showed similar results regarding shoot and root dry matter production, which were both higher when the sugar cane filter cake was used. Sugar cane filter cake has a low C/N ratio (Table 1), which may explain the trend to be a more useful source of nutrients than peat, as sugar cane is more easily decomposed than peat. Figure 1 shows that the increased organic material positively affected the shoot dry matter yield in the castor oil plants. However, despite the statistical significance of the regression models, from the agronomic or ecological point of view no marked quantitative difference in dry matter production among treatments would be enough to recommend one amendment over the other since the increase in dry matter production was, overall, discrete.

The addition of organic material to the soil affected differently Ba concentration among the three plant species (Table 3). Oilseed radish did not show a significant effect, but an increase in Ba in the castor oil plant roots was observed after the addition of sugar cane filter cake, from 39.8 mg/kg (no addition) to 50.2 mg/kg (80 Mg ha⁻¹), which corresponded to an increase of 26%. In castor bean shoots, Ba increased from 533.7 mg/kg in the control to 618 mg/kg in soils amended with 80 Mg ha⁻¹ peat respectively, which represented an increase of 16%. In sunflowers, the Ba concentrated in the flowers and straw+flower tissues was higher when the sugar cane filter cake was used. Moreover, the increase in the organic material rate (sugar cane filter cake and peat) resulted in a linear decrease in the Ba concentration in the flowers of the sunflower plants (Figure 2), up to 15% with sugar cake filter cake and 16% with peat addition.

When peat was used a negative correlation was observed for Ba and P in the castor oil plants () and sunflower tissues () (Table 5).The same trend was observed for K in the oilseed radish () and Ca in the castor oil plants () and sunflowers () with the use of sugar cane filter cake (Table 5). A nutritional imbalance of Ca, K, and S in the presence of Ba has been reported by several authors. These reports suggest that the imbalance is related to the plant species [7, 8, 31].

The transfer index (calculated as the Ba shoot concentration divided by the total Ba in the soil) decreased as follows: oilseed radish (0.70) > sunflowers (0.47) > castor oil plants (0.29). The average Ba transfer from the roots to the shoots in the oilseed radish, castor oil plants, and sunflowers was found to be 89%, 71%, and 59%, respectively. These values indicated that the Ba was highly mobile in the xylem of the oilseed radish and castor oil plants. From the total Ba transfer values, at least 50% of the Ba shoot concentration was found in the flowers of the sunflowers, and 35% of the Ba shoot concentration was found in the pods of the oilseed radish (Table 3). Ba concentrations in flowers with the addition of sugar cane filter cake and peat were as follows: 20.2 and 16.0 mg kg⁻¹, respectively, for oilseed radish; 15.3 and 21.0 mg kg⁻¹, respectively, for sunflowers. A high Ba mobility has also been observed in cotton and white beets during development and flowering, whereas a large amount of Ba accumulation has been reported in the leaves of corn (105.7 mg kg⁻¹) when compared with the grains of corn (1.05 mg kg⁻¹) [6, 33].

The obtained transfer factors (lower than 1) suggested that the tested species were inadequate in accumulating or extracting Ba from soil (Table 6). Similarly, low transfer factors have also been reported for castor oil plants, sunflowers, and mustard plants [30]. Indeed, these authors [30] reported that none of the plants grown in soils containing Ba ranging from 132.3 to 1,130 mg kg⁻¹ were able to accumulate measurable concentrations of Ba, thus, highlighting the low transfer of this element from soil to plants [34].

A decreasing trend for Ba transfer to oilseed radish and sunflowers was found when the sugar cane filter cake concentration increased (Table 6). In addition to improving the physical and chemical conditions of the soil, organic ligands are promising in the mitigation of heavy metal contaminated soils. Peat and a concentrate containing humic substances from coal favor mustard development in a contaminated soil due to the mitigation of Zn, Cu, Mn, Pb, and B by the organic ligands [14].

4. Conclusions

Under the conditions studied the elevated soil pH reached due to liming overcame the organic matter addition effect and determined the barium availability and its absorption by the plant species grown in the area polluted with scrap metal residue. This is suggested by the absence of phytotoxic effects on plants, the moderate Ba accumulation in shoots compared to the usual content of Ba in plants, the small effect of organic matter treatments on plants dry matter yields, and finally the levels of Ba extracted by Mehlich-3.

Acknowledgment

The authors would like to thank Fundação de Apoio a Pesquisa do Estado de São Paulo (FAPESP) for the financial support with the 2006/60987-0 Research Grant.

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Copyright © 2012 Cleide Aparecida Abreu et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

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