Abstract
Clay compounds have been used by human societies since time immemorial, because they are abundant in nature, smaller than 4 microns, adherent, plastic, malleable, have ion exchange capacity and affinity with water. Due to their physical and chemical properties, they are used in agriculture, livestock, industry, commerce, tourism and the environment for the development of services and products such as bricks, crockery, paints, pharmaceuticals, agricultural inputs and natural filters. The clay composition of an environment depends on the rock that gave rise to it, weathering and pedogenesis, with the following groups standing out: kaolinite-serpentine, talc-pyrophyllite, mica, vermiculite, smectite, chlorite and sepiolite-palygorskite. Each of these groups has specific physicochemical properties, which will direct them to certain uses. Proper use requires prior characterization, so in this chapter we will discuss the main types of clay compounds, their structure, formation, occurrence, mineralogical and physicochemical characteristics and their environmental importance.
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Acknowledgements
In Memoriam, to professors Ilson Guimarães Carvalho, Lucedino Paixão Ribeiro and Tersandro Paz do Rego Monteiro, Brazilian geoscientists who taught so much about clay minerals and their environmental importance. The authors thank Leandro Fonseca Carvalho and biologist Mr. Jackson M. Ministro for his help with figures. The authors also thank Prof. MSc. Gileno Santos Moreira for kindly providing photomicrographs of the biotite.
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Nunes, F.C., de Carvalho, C.C.N., de Jesus Alves, L., Prasad, M.N.V. (2023). Clay Composites: Physicochemical Characterization. In: Vithanage, M., Lazzara, G., Rajapaksha, A.U. (eds) Clay Composites. Advances in Material Research and Technology. Springer, Singapore. https://doi.org/10.1007/978-981-99-2544-5_2
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