ABSTRACT
The main residue of iron and nickel mining is slag, a solid residue of low solubility and rich in magnesium silicate. A residue with potential use as a soil conditioner, however, it is still necessary to investigate whether its use brings impacts to the environment. Microorganisms are extremely sensitive to environmental changes, changes that can be used as environmental quality indicators. Among the organisms that act as microbiological indicators of soil quality, the activity of arbuscular mycorrhizal fungi stands out. With this, this study aimed to verify the mycorrhizal activity as a quality indicator under application of nickel iron mining slag as soil conditioner. The experiment was carried out in the greenhouses of the agronomy course and in the laboratory of agricultural microbiology of the Evangelical College of Goianésia. Magnesium silicate was supplied by Anglo American Mining Company, located in Barro Alto, Goiás. Agronomic and microbiological analyses were performed at the Evangelical College of Goianésia, Goiás. The experimental design used was completely randomized, arranged with five treatments and with five replications, where the treatments were composed of four doses of magnesium silicate: 9, 12, 15, and 18 g dm-3 of soil in addition to the control without application. Ten golden saw rice seeds were planted in 10-L pots. Soil analysis used in the experiment was performed to determine soil nutritional parameters. The application of iron and nickel mining slag does not influence the development of rice in the first application. The application of 9 dm³g-1 of iron and nickel mining slag soil positively influences mycorrhizal activity on roots and soil.
Key words: Mycorrhiza, magnesium silicate, stress, cerrado.
The mining industry generates a gigantic amount of solid and liquid waste, which is accumulated and causes great socio-environmental impact. According to the Brazilian Mineral Yearbook (2019),iron and nickel are among the main ores extracted in Brazil and occupy the range of 71.1% and 2.5% of metals extracted in the country, respectively, reaching the financial movement of 88.5 billion reais in 2017.
The state of Goiás is the third with the highest production of ores in Brazil, surpassed only by Minas Gerais and Pará and is the main nickel producer in Brazil. Anglo American mining company, located in the municipality of Barro Alto, occupies the first place in the country in the production and commercialization of Nickel and the third in the production and commercialization of Iron (Brasil, 2020).
The main residue of iron and nickel mining is slag, a solid residue of low solubility and rich in magnesium silicate. The slag produced from iron and nickel mining at anglo american mining company's Barro Alto plant reaches 2.4 million tons per year. These residues are packed in the form of dried batteries and require a large physical space to be stored, which causes great socio-environmental impact (Corrêa et al., 2009).
In this respect, a good alternative to this problem would be the use of this waste, which would add economic value to the material and prevent it from being accumulated in large quantities, thus generating an environmental liability. Magnesium Silicate is one of the main components of iron and nickel mining slag, and this substance has potential for use as soil conditioners in agroecosystem (Fortes et al., 2008). For Prado et al., (2003b) slag can be an excellent source of Ca and Mg for plants, as well as an acidity corrective and soil conditioner in depth.
However, the chemical characteristics of each tailing vary from each extractor unit and more detailed analyses are fundamental. The use of these wastes as soil conditioners can prove to be an excellent ecological and economic alternative for the industries that produce them, adding value to a by-product with great potential for pollution and environmental impact (Prado et al., 2003a).
Mycorrhizal fungi are excellent indicators of environmental changes because they are sensitive to negative and positive variations in soils. By using mycorrhizal fungi as bioindicators of environmental quality, it is possible to evaluate the impacts that the use of mining slag cause on soil microbial activity, as well as to all edaphic biodiversity (Souza et al., 2016).
Magnesium is one of the most important elements in plant nutrition, acting in the structure of proteins and enzymatic components; it is also fundamental in the constitution of chlorophyll and photosynthesis (Faquin, 2005). Composing the group of secondary macronutrients, the main source of magnesium for agriculture is the application of limestone. The use of silicon in agriculture also brings benefits, especially in grasses. This element decreases the severity of the attack of diseases and pests, promotes increased productivity and increases resistance to water stress (Haridasan, 2000).
The use of magnesium silicate as a source of these elements can add value to a residue, which has caused an environmental impact in the place where it is stored. With this, this study aimed to verify mycorrhizal activity as a quality indicator under application of nickel iron mining slag as soil conditioner.
The experiment was carried out in the greenhouse of the agronomy course and in the laboratory of agricultural microbiology of the Evangelical College of Goianésia. Magnesium silicate was supplied by Anglo American Mining Company, located in Barro Alto, Goiás. Agronomic and microbiological analyses were performed at the Evangelical College of Goianésia, Goiás.
The experimental design used was completely randomized, arranged in five treatments and with 10 replications, where the treatments composed of four doses of magnesium silicate: 9, 12, 15, and 18 g dm-3 of soil and the control without application. Ten golden saw rice seeds were planted in 10-L pots. Soil analysis used in the experiment was performed to determine soil nutritional parameters (Table 1).
As response variable, vegetative characteristics of the plants (root length, root volume, root fresh mass, root dry mass, shoot length, aerial fresh mass and shoot dry mass) and mycorrhizal activity (mycorrhizal colonization rate, soil spore density and Identification of associated genera) were evaluated. The collection and analysis of the response variables were performed at the beginning of the flowering stage.
The analyses were carried out at the Laboratory of Agricultural Microbiology of the Evangelical College of Goianésia. The spores of arbuscular mycorrhizal fungi (AMF) were extracted from 500 cm3 of rhizospherical soil by the wet sieving technique, according to the methodology described by Gerdemann and Nicolson (1963) followed by centrifugation in water and sucrose solution 50%. The spores were separated according to their phenotypic characteristics such as color, size and shape, composing the different morphotypes, under stereoscopic binocular magnifying glass.
To determine the percentage of colonization, the roots were clarified and colored with 0.05% Trypan Blue in lactoglycerol (Phillips and Hayman, 1970) under stereoscopic microscope, following the technique of intersection of the quadrants (Giovannetti and Mosse, 1980).
To identify the genera of AMF from morphological characteristics, the spores were separated according to their morphotypes and mounted on blades with pure polyvinyl-lactoglycol (PVLG) and PVLG mixed with Melzer (1:1 v/v). To support the identification work, original articles of the description of the species provided on the website of the "International Culture Collection of Arbuscularand Vesicular-Arbuscular Mycorrhizal Fungi" (INVAM, 2018) were used.
The data were submitted to analysis of variance by the Assistat program (Silva, 2008) and the graphs constructed by prism software (Swift, 2020) and canonical correspondence statistics were performed by the Past software (Hammer, 2018).
The application of iron and nickel mining slag in order to use it as a soil conditioner did not present a significant minimum difference in the statistics in vegetative parameters such as length, volume, fresh mass and root dry mass (Figure 1) and in the parameters plant height, fresh mass and shoot dry mass (Figure 2).
When analyzing mycorrhizal activity in rice rhizosphere under application of iron and nickel slag, it was possible to observe statistical difference in mycorrhizal colonization rate and spore density in rhizospherical soil (Figure 3).
The dose of 9 g/dm³ showed the highest values of mycorrhizal colonization rate and spore density. The other dosages presented values identical to the treatment and control for the two parameters evaluated.
The genera Acaulospora, Scutellospora, Sclerocystis, Glomus and Gigasporas were identified associated with rice rhizosphere (Table 2). The genera Acaulospora and Scutellospora were found in the rhizosphere of all treatments, except for control. The genus Glomus was found in all treatments, except in the treatment with application of 18 g/dm³ of iron and nickel mining slag. The genus Gigaspora was found only in the treatment with application of 18 g/dm³, and the genus Sclerocystis was identified only in the control treatments and with application of 9 g/dm³.
The analysis of main components of the genera of identified mycorrhizal fungi and the dosages of nickel iron mining slag (Figure 4) showed an approximation of some genera in relation to the applied treatments.
The genera Acaulospora and Scutellospora showed greater proximity to treatments with doses of 12 and 15 g/dm³ of mining slag. The genus Glomus approached the dose of 9 g/dm³ of mining slag. The genera Slcerocystis and Gigaspora did not present proximity to any of the treatments evaluated, demonstrating that they may have occurred casually in the samples evaluated. The treatments and control of 18 g/dm³ of slag were also not close to any identified mycorrhizal fungus genus.
Root colonization rate and spore density in the soil can be used as a parameter when measuring the level of impact caused by the application of slag. Mycorrhizal fungi act in the plant, aiding the absorption of nutrients and water in the soil (Moura and Cabral, 2019; Silveira and Freitas, 2007), working with organisms that promote growth and plant health. They act mainly when the plant is in a situation of stress, where the main triggers for the beginning of this symbiotic association is the low availability of water and nutrients (Johnson and Pfleger, 1992). High values of colonization in the roots and spores in the soil indicate a higher activity of the fungus because of a possible stress situation of the plant.
When comparing the behavior of the treatments in the vegetative characteristics (Figures 1 and 2), no statistical difference was observed in any of the response variables, demonstrating that the treatments did not influence the development of the plant, neither positively nor negatively. This is due to the high insolubility of the compounds found in slag, such as magnesium and silicon, which, if available, could positively influence plant development (Fortes et al., 2008).
Based on this interpretation, the plant did not suffer stress caused by the presence of the tailings, which is not responsible for the statistical difference verified when analyzing the mycorrhizal colonization rate and density of spores in the soil (Figure 3). These same insoluble compounds found in slag can be solubilized by soil microorganisms, among which mycorrhizal fungi are part (Sylvester-Bradley et al., 1982). The treatment of 9 g/dm³ of slag presented better conditions for the development of mycorrhizal fungi in soil and plant, being statistically superior to other treatments and that of control treatment.
This behavior can be explained by the solubilization of compounds beneficial to the development of microorganisms (Lapeyrie et al., 1991; Prado et al., 2003; 2003b), which in this dosage, worked more efficiently, bringing better development to fungi and indirectly can bring benefits to associated plants. If the slag can be solubilized over time by the action of microorganisms, the application over time may present good results in the production and development of plants.
The application of iron and nickel mining slag does not influence the development of rice in the first application. However, the application of 9 g/dm³ of soil of iron and nickel mining slag positively influenced mycorrhizal activity in roots and soil.
The authors have not declared any conflict of interests.
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