Soil minerals refer to the inorganic components present in soils that are derived from weathering of rocks and minerals. These minerals play a crucial role in the physical, chemical, and biological properties of soils. Some common soil minerals include quartz, feldspar, mica, and clay minerals. Soil minerals influence soil fertility, nutrient availability, soil structure, and water retention capacity. Research in this area focuses on understanding the types, distribution, and properties of soil minerals and their interactions with other components of soil. This research is important for sustainable agriculture, land use planning, and environmental management.