Transforming syenite through alkaline-hydrothermal processes: A sustainable strategy to overcome potassic fertilizer shortages in tropical regions
- 1Geology & Sustainable Mining Institute (GSMI), Mohammed VI Polytechnic University, Lot 660, Hay Moulay Rachid, Benguerir 43150, Morocco; Institut de recherche en mines et en environnement, Université du Québec en Abitibi-Témiscamingue, 445 boulevard de l'Université, Rouyn-Noranda, Québec J9X 5E4, Canada.
- 2Geology & Sustainable Mining Institute (GSMI), Mohammed VI Polytechnic University, Lot 660, Hay Moulay Rachid, Benguerir 43150, Morocco.
- 3Geology & Sustainable Mining Institute (GSMI), Mohammed VI Polytechnic University, Lot 660, Hay Moulay Rachid, Benguerir 43150, Morocco; Géosciences Montpellier, Université de Montpellier & CNRS, 60 Place Eugène Bataillon, 30095 Montpellier Cedex 05, France.
- 0Geology & Sustainable Mining Institute (GSMI), Mohammed VI Polytechnic University, Lot 660, Hay Moulay Rachid, Benguerir 43150, Morocco; Institut de recherche en mines et en environnement, Université du Québec en Abitibi-Témiscamingue, 445 boulevard de l'Université, Rouyn-Noranda, Québec J9X 5E4, Canada.
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View abstract on PubMed
Summary
This summary is machine-generated.Alkaline hydrothermal treatment significantly enhances nutrient release from silicate rocks like syenite. This process improves potassium and multi-nutrient availability for soil health and crop productivity.
Area Of Science
- Geochemistry and Soil Science
- Materials Science
- Mineralogy
Background
- Silicate rocks are crucial for soil health and crop productivity, but their slow nutrient release limits agricultural potential.
- Understanding nutrient release mechanisms from silicate minerals is key to developing sustainable soil amendments.
- Alkaline hydrothermal treatment offers a potential method to accelerate nutrient availability from geological materials.
Purpose Of The Study
- To evaluate the effect of alkaline hydrothermal treatment on potassium (K) and multi-nutrient (P, Ca, Mg, S, Si) availability from syenite rock.
- To characterize the mineralogical, chemical, and structural changes induced by the treatment.
- To investigate the nutrient release kinetics and identify factors influencing weathering.
Main Methods
- Syenite rock was treated hydrothermally with CaO and KOH using a Design of Experiments (DOE) approach.
- Characterization involved petrography, X-ray fluorescence (XRF), X-ray diffraction (XRD), QEMSCAN, EPMA, and FTIR.
- Sequential leaching tests in deionized water followed by ICP-AES analysis quantified nutrient release.
Main Results
- Hydrothermal treatment induced significant mineralogical, chemical, and structural alterations in syenite.
- KOH-treated materials showed substantial potassium release (up to 1631 mg/L).
- Treated samples released 3 to 69 times more nutrients than raw material, with slow but sustained dissolution rates.
Conclusions
- Powdered syenite, after alkaline hydrothermal treatment, can serve as a valuable nutrient reservoir and soil buffer.
- The treatment effectively enhances the availability of essential nutrients for agricultural applications.
- Understanding rock weathering mechanisms through this treatment provides insights for soil amendment development.
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