CV Lattes
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Universidade de São Paulo (USP). Escola Superior de Agricultura Luiz de Queiroz (ESALQ) (Institutional affiliation from the last research proposal) Birthplace: Brazil
Assistant Professor of Applied Soil Chemistry, Washington State University (WSU), Pullman, WA, USA. Previously Assistant Professor of Soil Science at Austin Peay State University (APSU), Clarksville TN, USA. Taught undergraduate courses in Soils, Soil Conservation, Fertility and Fertilizers, Fertilizers, Soil Taxonomy, and related fields. Doctor of Philosophy (Soil Science) at Oklahoma State University (Department of Plant and Soil Sciences). Masters of Science (Soils and Plant Nutrition) at University of Sao Paulo Paulo - ESALQ (2015) and Bachelor's in Agricultural Engineering at UNESP - Faculdade de Ciências Agronômicas (2012). Dr. Antonangelo was a Postdoctoral Research Associate at Oklahoma State University (OSU), Plant and Soil Sciences Department (PaSS). Has experience in Agronomy, focusing on Soil Fertilization, acting on the following subjects: soil speciation, phosphorus, no-till, soybean, heavy-metals, and biochar. (Source: Lattes Curriculum)
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Silicon (Si) is an element beneficial to plant development by providing increased capacity to defend against the attack of pests and diseases, and to ensure an more erect plant, which increases their photosynthetic capacity. Silicon sources such as silicates of calcium and magnesium, providing Si to the soil and can act as acidity correctors. No-till system - NT in conjunction with the ap…
The rational use of industrial and urban wastes in agriculture under no till system promotes many benefits on physical, chemical and biological soil properties, thus reducing the use of synthetic fertilizers, providing beneficial effects to soil and ecosystem. And act as attenuators of soil acidity, these residues are excellent sources of nutrients such as phosphorus. The characterization…
Aluminum is the most abundant metal in the soil. In addition to being a toxic element to plants, Al3+ may also serve as an indicator of silicon content in the soil. In soils found in a humid tropical climate, the clay minerals, specifically aluminum oxides, tend to adsorb silicic acid (H4SiO4) strongly. At low pH values, a great amount of Al3+ is released by the oxides during the weatheri…
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