Release kinetics of multi-nutrients from volcanic rock mining by-products: Evidences for their use as a soil remineralizer
Great quantities of stone by-products are stored alongside different exploiting mines in south Brazil, which are becoming an unsustainable environmental issue. Powder materials of andesite and dacite rocks were obtained from two mining companies of Southern Brazil. The particle size classification o...
- Autores:
-
Gómez Plata, leandro
Gindri Ramos, Claudete
Silva Oliveira, Marcos Leandro
Silva O., Luis F.
- Tipo de recurso:
- http://purl.org/coar/resource_type/c_816b
- Fecha de publicación:
- 2020
- Institución:
- Corporación Universidad de la Costa
- Repositorio:
- REDICUC - Repositorio CUC
- Idioma:
- eng
- OAI Identifier:
- oai:repositorio.cuc.edu.co:11323/7294
- Acceso en línea:
- https://hdl.handle.net/11323/7294
https://repositorio.cuc.edu.co/
- Palabra clave:
- Multi-nutrients source
New procedure
Rock by-products
Sustainable agriculture
- Rights
- closedAccess
- License
- Attribution-NonCommercial-NoDerivatives 4.0 International
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| dc.title.spa.fl_str_mv |
Release kinetics of multi-nutrients from volcanic rock mining by-products: Evidences for their use as a soil remineralizer |
| title |
Release kinetics of multi-nutrients from volcanic rock mining by-products: Evidences for their use as a soil remineralizer |
| spellingShingle |
Release kinetics of multi-nutrients from volcanic rock mining by-products: Evidences for their use as a soil remineralizer Multi-nutrients source New procedure Rock by-products Sustainable agriculture |
| title_short |
Release kinetics of multi-nutrients from volcanic rock mining by-products: Evidences for their use as a soil remineralizer |
| title_full |
Release kinetics of multi-nutrients from volcanic rock mining by-products: Evidences for their use as a soil remineralizer |
| title_fullStr |
Release kinetics of multi-nutrients from volcanic rock mining by-products: Evidences for their use as a soil remineralizer |
| title_full_unstemmed |
Release kinetics of multi-nutrients from volcanic rock mining by-products: Evidences for their use as a soil remineralizer |
| title_sort |
Release kinetics of multi-nutrients from volcanic rock mining by-products: Evidences for their use as a soil remineralizer |
| dc.creator.fl_str_mv |
Gómez Plata, leandro Gindri Ramos, Claudete Silva Oliveira, Marcos Leandro Silva O., Luis F. |
| dc.contributor.author.spa.fl_str_mv |
Gómez Plata, leandro Gindri Ramos, Claudete Silva Oliveira, Marcos Leandro Silva O., Luis F. |
| dc.subject.spa.fl_str_mv |
Multi-nutrients source New procedure Rock by-products Sustainable agriculture |
| topic |
Multi-nutrients source New procedure Rock by-products Sustainable agriculture |
| description |
Great quantities of stone by-products are stored alongside different exploiting mines in south Brazil, which are becoming an unsustainable environmental issue. Powder materials of andesite and dacite rocks were obtained from two mining companies of Southern Brazil. The particle size classification of the materials was determined by sieving. The X-ray diffraction (XRD) technique was used to identify the mineral phases of the by-products and X-ray fluorescence (XRF) was applied to determine their chemical compositions. The concentrations of calcium (Ca), potassium (K), magnesium (Mg), phosphorus (P) and silicon (Si) released by the by-products were determined by inductively coupled plasma atomic emission spectrometry (ICP-AES). Dissolution rates of andesite and dacite rocks were measured in Milli-Q water, and in solutions of 0.1 mol L−1 citric acid, and Milli-Q water acidified with 0.5 mol L−1 acetic acid, as a function of reaction times at 24–96 h (short-term), and at 96–5760 h (long-term). The solutions were agitated continuously on a mechanical rotatory shaker at room temperature. The parabolic diffusion, simplified Elovich, and power function models were applied at both time slots of solid-solution reaction. The results indicated that the relationships of quantity of released multi-nutrients were well described by power equation: ln qt = ln a + b ln t. Dissolution rates were obtained based on the release of Ca, K, Mg, P and Si at a steady state under far from equilibrium conditions. Dissolution rates of both by-products were not affected, within the experimental uncertainty, by Milli-Q water. Although the by-products dissolution rates were unaffected by Milli-Q water, its rates are increased along the time. The dissolution of the by-products minerals was significantly affected by the pH of the solutions. The multi-elements release by both by-products in 0.1 mol L−1 citric acid solution was significantly larger than another solutions, indicating that exchangeable cations were readily available in citric acid solution. The results obtained from power function model in two reaction time intervals can contribute to estimate the multi-nutrients-supplying power of by-products to soil. The present study provides both to solving an environmental issue associated with Brazilian rock exploitation and to create an alternative for soil fertilization and a more sustainable agriculture. |
| publishDate |
2020 |
| dc.date.accessioned.none.fl_str_mv |
2020-11-12T21:15:16Z |
| dc.date.available.none.fl_str_mv |
2020-11-12T21:15:16Z |
| dc.date.issued.none.fl_str_mv |
2021 |
| dc.date.embargoEnd.none.fl_str_mv |
2023-01-10 |
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Pre-Publicación |
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http://purl.org/coar/resource_type/c_816b |
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Text |
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info:eu-repo/semantics/preprint |
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http://purl.org/redcol/resource_type/ARTOTR |
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info:eu-repo/semantics/acceptedVersion |
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http://purl.org/coar/resource_type/c_816b |
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acceptedVersion |
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09596526 |
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https://hdl.handle.net/11323/7294 |
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Corporación Universidad de la Costa |
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REDICUC - Repositorio CUC |
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https://repositorio.cuc.edu.co/ |
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09596526 Corporación Universidad de la Costa REDICUC - Repositorio CUC |
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| dc.language.iso.none.fl_str_mv |
eng |
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eng |
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Bortoluzzi Variability of amethyst mining waste: a mineralogical and geochemical approach to evaluate the potential use in agriculture J. Clean. Prod., 210 (2019), pp. 749-758, 10.1016/j.jclepro.2018.11.039 Leonardos and Theodoro, 1999 O.H. Leonardos, S.C.H. Theodoro Fertilizer tropical soils for sustainable development Proceedings. International workshop on Science for Sustainable development in Latin America and Caribe. Rio de Janeiro. Acad. Bras. Cienc., 1 (1999), pp. 143-153 Lu et al., 2007 X.N. Lu, J.M. Xu, W.Z. Ma, Y.F. Lu Comparison of seven kinetic equations for K release and application of kinetic parameters Pedosphere, 17 (2007), pp. 124-129, 10.1016/S1002-0160(07)60017-4 Lybrand and Rasmussen, 2014 R.A. Lybrand, C. Rasmussen Linking soil element-mass-transfer to microscale mineral weathering across a semiarid environmental gradient Chem. Geol., 381 (2014), pp. 26-39, 10.1016/j.chemgeo.2014.04.022 Manning, 2018 D.A. Manning Innovation in resourcing geological materials as crop nutrients Nat. Resour. Res., 27 (2018), pp. 217-227, 10.1007/s11053-017-9347-2 Mastinu et al., 2019 A. Mastinu, A. Kumar, G. Maccarinelli, S.A. Bonini, M. Premoli, F. Aria, A. Gianoncelli, M. Memo Zeolite clinoptilolite: therapeutic virtues of an ancient mineral Molecules, 24 (2019), p. 1517, 10.3390/molecules24081517 Meira et al., 2014 L.D.A.S. Meira, A.O.D.V. Machado, J.Y.P. Leite Potassium Release Kinetics in Vermiculite Tailings (2014) https://www.researchgate.net/publication/325722019_Potassium_release_kinetics_in_vermiculite_tailings/ accessed 24 April 2019 Nishanth and Biswas, 2008 D. Nishanth, D.R. Biswas Kinetics of phosphorus and potassium release from rock phosphate and waste mica enriched compost and their effect on yield and nutrient uptake by wheat (Triticum aestivum) Bioresour. Technol., 99 (2008), pp. 3342-3353, 10.1016/j.biortech.2007.08.025 Nunes et al., 2014 J.M.G. Nunes, R.M. Kautzmann, C. 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Kautzmann Evaluation of the potential of volcanic rock waste from southern Brazil as a natural soil fertilizer J. Clean. Prod., 142 (2017), pp. 2700-2706, 10.1016/j.jclepro.2016.11.006 Ramos et al., 2019 C.G. Ramos, D.S. de Medeiros, L. Gomez, L.F.S. Oliveira, I.A.H. Schneider, R.M. Kautzmann Evaluation of soil Re-mineralizer from by-product of volcanic rock mining: experimental proof using black oats and maize crops Nat. Resour. Res., 28 (2019), pp. 1-18, 10.1007/s11053-019-09529-x Raven and Hossner, 1994 K.P. Raven, L.R. Hossner Soil phosphorus desorption kinetics and its relationship with plant growth Soil Sci. Soc. Am. J., 58 (1994), pp. 416-423 https://doi:10.2136/sssaj1994.03615995005800020026x Rawat et al., 2016 J. Rawat, P. Sanwal, J. Saxena Potassium and its role in sustainable agriculture Potassium Solubilizing Microorganisms for Sustainable Agriculture, Springer, New Delhi (2016), 10.1007/978-81-322-2776-2_17 Silva et al., 2013 A.D.A. Silva, J.A. Sampaio, A.B.D. Luz, S.C. 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Garrido, M.E. Medeiros, J.A. Sampaio Effect of thermal treatments on the potassium and sodium availability in phonolite rock powder Int. J. Miner. Process., 145 (2015), pp. 57-65, 10.1016/j.minpro.2015.07.002 Tiwari et al., 2015 M.K. Tiwari, S. Bajpai, U.K. Dewangan, R.K. Tamrakar Suitability of leaching test methods for fly ash and slag: a review J. Radiat. Res. Appl. Sci., 8 (2015), pp. 523-537, 10.1016/j.jrras.2015.06.003 Turner et al., 1994 S. Turner, M. Regelous, S. Kelley, C.J. Hawkesworth, M.S.M. Mantovani Magmatism and continental break-up in the South Atlantic: high precision 40Ar-39Ar geochronology Earth Planet Sci. Lett., 121 (1994), pp. 333-348, 10.1016/0012-821X(94)90076-0 ance et al., 2003 C.P. Vance, C. Uhde-Stone, D.L. Allan Phosphorus acquisition and use: critical adaptations by plants for securing a non-renewable resource New Phytol., 157 (2003), pp. 423-447, 10.1046/j.1469-8137.2003.00695.x White and Brantley, 2003 A.F. White, S.L. Brantley The effect of time on the weathering of silicate minerals: why do weathering rates differ in the laboratory and field? Chem. Geol., 202 (2003), pp. 479-506, 10.1016/j.chemgeo.2003.03.001 Xiaofu et al., 2008 W. Xiaofu, Z. Fang, C. Mingli, Z. Yangli, Z. Chong, Z. Hailan Factors affecting the adsorption of Zn2+ and Cd2+ ions from aqueous solution onto vermiculite Adsorpt. Sci. Technol., 26 (2008), pp. 145-155, 10.1260/026361708786036115 Zhu, 2017 C. Zhu Book review: geochemical rate models: an introduction to geochemical kinetics Am. Mineral., 102 (4) (2017), pp. 921-922, 10.2138/am-2017-670 |
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Gómez Plata, leandro9eb2be3c0e7b0419783f6742178232c1Gindri Ramos, Claudete5e561ef3b253a1b05b1d347c40a04029Silva Oliveira, Marcos Leandro8593f6412a0dba9dc599d10d381fe9b2Silva O., Luis F.f7614986860cc1b557bba649d78ecbb42020-11-12T21:15:16Z2020-11-12T21:15:16Z20212023-01-1009596526https://hdl.handle.net/11323/7294Corporación Universidad de la CostaREDICUC - Repositorio CUChttps://repositorio.cuc.edu.co/Great quantities of stone by-products are stored alongside different exploiting mines in south Brazil, which are becoming an unsustainable environmental issue. Powder materials of andesite and dacite rocks were obtained from two mining companies of Southern Brazil. The particle size classification of the materials was determined by sieving. The X-ray diffraction (XRD) technique was used to identify the mineral phases of the by-products and X-ray fluorescence (XRF) was applied to determine their chemical compositions. The concentrations of calcium (Ca), potassium (K), magnesium (Mg), phosphorus (P) and silicon (Si) released by the by-products were determined by inductively coupled plasma atomic emission spectrometry (ICP-AES). Dissolution rates of andesite and dacite rocks were measured in Milli-Q water, and in solutions of 0.1 mol L−1 citric acid, and Milli-Q water acidified with 0.5 mol L−1 acetic acid, as a function of reaction times at 24–96 h (short-term), and at 96–5760 h (long-term). The solutions were agitated continuously on a mechanical rotatory shaker at room temperature. The parabolic diffusion, simplified Elovich, and power function models were applied at both time slots of solid-solution reaction. The results indicated that the relationships of quantity of released multi-nutrients were well described by power equation: ln qt = ln a + b ln t. Dissolution rates were obtained based on the release of Ca, K, Mg, P and Si at a steady state under far from equilibrium conditions. Dissolution rates of both by-products were not affected, within the experimental uncertainty, by Milli-Q water. Although the by-products dissolution rates were unaffected by Milli-Q water, its rates are increased along the time. The dissolution of the by-products minerals was significantly affected by the pH of the solutions. The multi-elements release by both by-products in 0.1 mol L−1 citric acid solution was significantly larger than another solutions, indicating that exchangeable cations were readily available in citric acid solution. The results obtained from power function model in two reaction time intervals can contribute to estimate the multi-nutrients-supplying power of by-products to soil. 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