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Soil formation
| Term | Definition |
|---|---|
| Soil | A loose mixture of weathered rock fragments, organic material, water, and air that can support the row the of vegetation. |
| Soil Composition | What it is made of. A mixture of rock particles, minerals, decayed organic material, water, and air. |
| Humus | A dark-colored substance that forms as a plant and animal remains decay. Makes the soil dark. Lighter soil has less. |
| Fertile Soil | Rich in the nutrients that plants need to grow. |
| Soil Texture | The soil quality that is based on the proportions of the soil particles. Depends on the size of the soil particles. |
| Soil Horizons | Layers of soil. |
| Horizon A | Topsoil with humus. Crumbly, dark brown soil that is a mixture of humus, clay, and other minerals. |
| Horizon B | Subsoil. Consists of clay and other particles washed down from Horizon A, but less humus. |
| Horizon C | Rock fragment (weathered rock) forms as bedrock weathers and rock breaks up into soil. |
| Horizon R | Bedrock- solid rock at the bottom |
| Loam | Soil that is up of about equal parts of clay, sand, and silt. Best for growing most types of trees. |
| Decomposition | How humus is formed. Rotting, decaying. |
| Leaching | The removal of substances that can be dissolved from rocks or layers of soil due to the passing of water. |
| Parent rock | The source of the weathered fragments (mineral fragments or sediments) |
| Bedrock | The layer of rock beneath the soil. |
| Transported Soil | Soil that is blown, washed away, or moved by glaciers. |
| Residual Soil | The soil that remains above its parent rock. |
| Litter | Loose layer of leaves on the ground from plants. |