Since 2020, aggregated from related topics
Silicate mineral weathering is the process by which silicate minerals, such as feldspar and olivine, break down and release elements like silicon, calcium, magnesium, and potassium into the surrounding environment. This weathering process is important for the overall cycling of elements in the Earth's crust and has implications for soil formation, nutrient availability, and climate regulation. Silicate mineral weathering also plays a role in the carbon cycle, as it can impact the uptake and release of carbon dioxide from the atmosphere through interactions with rocks and soils. Researchers study silicate mineral weathering to better understand the Earth's geochemical processes and how they influence the environment on a global scale.