Soil Water Flashcards
Soil Water
Properties of water that give it the ability to influence soil processes.
Water Polarity
Charges are not evenly distributed
Hydrogen Bonding
Water is attracted to itself. Responsible for Cohesion and Adhesion.
Cohesion (Surface tension)
attraction of molecules to each other (water droplets)
Adhesion
attraction of water molecules to solid surface (water drops on a window)
How do trees take up water?
Adhesion and Cohesion
Capillary Force
Due to adhesion and surface tension (cohesion), water will move upwards against the force of gravity. (thanks to soil micropores)
Do smaller pores (Sand Macropores) have more or less capillary (suction) force?
Less
Do larger pores (Clay Micropores) have more or less capillary (suction) force?
More
Water is present in soil in what 3 states? (Sponge example)
- Saturated soil-gravitational water
* Sponge full of water - Field Capacity
* Sponge not dripping but still contains water - Permanent wilting point
* Sponge is completely dry
Saturation
All pores filled with water-max water retention of a soil
Water content is equal to TOTAL porosity
Immediately after a rain or irrigation event
Water drains easily from macropores under the influence of gravitational forces
Field Capacity
The amount of water a soil can hold against the pull of gravity
Occurs when all gravitational water has drained out, typically 1 to 3 days after saturation.
Macropores are empty. Micropore are still filled with water and this is plant available water.
Permanent Wilting Point
Occurs after plants have used all plant available water
Soils that are fine textures or high in organic matter retain the greatest amount of water
Macropores
Gravitational pull is stronger than suction force so water drains freely
Micropores
Suction forces are greater than gravity so water will be pulled into micropores