LE2 Flashcards
One of the most variable characteristic of soil
Water content
The soil acts as a ___________________, making it available for plants as it is needed
reservoir for water
Soil water is part of what cycle?
Global hydrological cycle
What factors of soil does water affect?
- Soil formation
- Structure
- Stability and Erosion
Water causes soil particles to :
- Swell and shrink
- Adhere to each other
- Form structural aggregate
Water alters the soil profile by?
Dissolving and translocating minerals
What causes the decrease in soil fertility under extreme rainfall events?
Leaching
Four reasons why water is essential to plants
- It constitutes 85-95% of the plant’s protoplasm
- Essential for photosynthesis
- Solvent in which nutrients are carried to, into and throughout the plant
- Provides turgidity
Classifications of Soil Water
Five categories of water surrounding a clay or soil particle :
- Adsorbed water (hygroscopic water)
- Water at permanent wilting point
- Capillary water (water at field capacity)
- Gravitational water
- Chemically-combined water
It is held in the surface of the particle by powerful forces of electrical attraction and virtually in a solid state of very small thickness
Adsorbed water (hygroscopic water)
Thickness of adsorbed water
0.005um
It cannot be removed by oven drying at 110 degrees celsius
Adsorbed water
Water that can be removed by oven drying but not by air drying
Water at permanent wilting point
Water that is not so tightly held
Water at permanent wilting point
Water that is held by surface tension, generally removable by air drying
Capillary water
Water that is removable by drainage, can move in the voids between soil grains
Gravitational water
Water that is not of much use to the plants
Gravitational water
Water that is in the form of water of hydration within the crystal structure
Chemically-combined water
Water that is not generally removable by oven drying
Chemically-combined water
What are the qualitative descriptions of soil wetness?
- Maximum retentive capacity
- Field capacity
- Permanent Wilting Point
- Available water storage capacity
It is a qualitative description of soil wetness when all soil pores are filled with water and becomes saturated
Maximum retentive capacity
A qualitative description of soil wetness where its matric potential is close to zero and the volumetric water content is essentially the same as total porosity
Maximum retentive capacity
TRUE OR FALSE
In maximum retentive capacity, the soil will remain at maximum retentive capacity as long as water continues to infiltrate, because water held in the largest pores will percolate downward under the influence of gravitational forces
TRUE
A qualitative description of soil wetness wherein moisture content of the soil after gravity has removed all the water it can. Usually occurs 1-3 days after rain
Field capacity