LECTURE 4D: SOIL WATER Flashcards
1 of most variable charac of soil
water content
reservoir for water (and nutrients); making it avail for plants when needed
soil
part of global hydrological cycle (continuous circulation of water in earth-atmosphere system)
soil water
how well soil stores water is of great importance to
crop production and vitality to land
water causes soil particles to: 3 bullets
- swell and shrink
- adhere to each other
- form structural aggregate
water is essential to plants for 4 reasons:
- constitutes 85% - 95% of plant’s protoplasm (physical basis of life)
- essential for photosynthesis
- solvent in which nutrients are carried into
- provides turgidity (keeps plants in proper position)
5 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
category of water surrounding clay/soil particle: held on surface of particle by powerful forces of attraction; solid state of very small thickness (0.005um); can’t be removed by oven drying at 110C; considered as part of solid soil grain
adsorbed water (hygroscopic water)
water that can be removed by oven drying but not air drying; not so tightly held
water at permanent wilting point
what state is soil in when mesopores (2-50 nm) are filled with water and macropores are drained of water
soil at field capacity
category of water surrounding clay/soil particle: held by surface tension, generally removed by air drying
capillary water (water at field capacity)
- category of water surrounding clay/soil particle: removable by drainage, can move in voids between soil grains.
- flooded field will drain gravi water under influence of gravity until water’s adhesive and cohesive forces resist further drainage and finally reaches FC
- not much use to plants
gravitational water
in form of water of hydration within chemical structure; not removable by oven drying
chemically-combined water
4 qualitative descriptions of soil wetness
- maximum retentive capacity
- field capacity
- permanent wilting point
- available water storage capacity (AWSC)
- all soil pores are filled with water and soil is saturated
- matric potential is close to zero and volumetric water content is same as total porosity
- soil will remain at ________ as long as water continues to ______________, bcs water held in largest pores perlocate downward under influence of gravi forces
it is at maximum retentive capacity; infiltrate