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Sustainability via soil remineralization: blend of diabase, shale, and dolostone in Ferralsol and nutrient dynamics
Luís Felipe Bruno Locatelli1, Vania Silvia Rosolen2, José Carlos Gasparro3
1Center of Applied Natural Sciences (UNESPetro), São Paulo State University (UNESP), Avenida 24-A, 1515, Rio Claro, SP, 13506-900, Brazil. luis.locatelli@unesp.br.
Abstract:
Rock powders are increasingly considered a sustainable alternative to soluble fertilizers, particularly in highly weathered tropical soils. In this context, this study aimed to evaluate the short-term chemical and mineralogical changes induced by a diabase-shale-dolostone blend applied as a soil remineralizer to a Ferralsol under controlled laboratory conditions. Specifically, the experiment assessed nutrient release, changes in soil chemical attributes, and dissolution-precipitation features on mineral surfaces. A 1-year pot experiment was conducted in Rio Claro (SP, Brazil), using four remineralizer treatments and a control, each with three replicates. The treatments combined two application rates (15 and 20 t ha-1) with two particle-size fractions: filler (< 0.3 mm) and powder (0.3-2.0 mm). Additionally, individual fragments of diabase and dolostone (2-5 mm) were enclosed in mesh bags to monitor surface weathering. Soil and fragments were sampled twice a year, while leached water was collected monthly. The remineralizer's application positively affected the soil, raising pH, base saturation, and the available levels of SO42-, Ca2+, and Mg2+, as well as reducing Al3+ and Al saturation. New phases of clay minerals such as chlorite, vermiculite, and hydroxy-interlayered minerals (HIMs) were observed. The leachate evaluations showed the availability of K+, Ca2+, Mg2+, and Na+, along with the soil's permanence of Al3+, Si, and P. In fragments, the rapid precipitation of poor crystalline material-kaolinite-like phase (KLP)-demonstrates that rock powder reduced exchangeable acidity. The rock powder blend holds potential as a nutrient source for soil, especially secondary macronutrients, warranting future agronomic testing.
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