Soil Freeze

Soil freeze occurs when the temperature of the soil drops below the freezing point, causing moisture in the soil to freeze. This process can affect plant growth, as frozen soil restricts root expansion and water absorption. It also influences soil structure, potentially leading to cracking or shifting when it thaws. In colder climates, freeze-thaw cycles can create challenges for agriculture, infrastructure, and ecosystems. Understanding soil freeze is essential for managing agricultural practices and mitigating its impacts on the environment and built structures.