Geomicrobiology
Clay minerals are a group of hydrous aluminum phyllosilicate minerals that are typically formed through the weathering of feldspar and other silicate minerals. These tiny particles play a crucial role in soil formation and nutrient cycling, significantly impacting microbial habitats and the chemical properties of soils. Their unique physical and chemical properties, such as high surface area and cation exchange capacity, make them vital for understanding the interactions between microorganisms and minerals in the environment.
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