Intro to Geotechnical Science
Sedimentation is the process by which particles settle and accumulate in a fluid, forming layers over time. This process is essential in shaping soil composition and structure, as it affects how different materials are deposited, compacted, and transformed within the environment. The characteristics of sediment, such as grain size and mineral content, influence soil properties, including drainage, fertility, and stability.
congrats on reading the definition of Sedimentation. now let's actually learn it.