Soil Composition and Texture
Soil composition and texture (i.e., particle-size distribution) vary, giving rise to different soil names. In this survey course, the names are not so import...
Soil composition and texture (i.e., particle-size distribution) vary, giving rise to different soil names. In this survey course, the names are not so import...
Soils form in layers, called “horizons”.
Soils are critical to civilization.
Soils form in response to five key factors: Climate, Organisms, Relief, Parent Material, and Time.
Soils form via four major processes: addition, loss, transformation, and leaching.
Mathematical relationships for weathering of parent material (mostly bedrock) into soil.
Integrating the soil-production function to see how thickness evolves over time.
Physical, chemical, and biological weathering processes break down material on Earth’s surface, forming regolith and soils.
Soils are the critical outer carapice of Earth’s surface, where water, life, rock, and energy meet and form the basis for the world that we know.