Land Use: Different land uses have varying impacts on soil carbon levels. For example, forests typically store more carbon in their soils than agricultural or degraded lands.
Vegetation Type: The type of vegetation covering an area significantly affects soil carbon. Natural ecosystems, such as grasslands and forests, tend to accumulate more carbon compared to croplands.
Soil Type: Soil properties, including texture, depth, and mineral content, influence the potential for carbon sequestration. Loamy soils with good organic matter content generally sequester more carbon.
Management Practices: Farming and land management practices, such as no-till farming, cover cropping, and agroforestry, can enhance soil carbon sequestration.
Climate and Weather: Climate conditions, especially temperature and precipitation patterns, affect the rate of decomposition of organic matterand, therefore, the sequestration process.