CHAPTER 4: Water balance of plants Flashcards
The water content and the rate of water movement in soils depend to a large extent on (2)
soil type and soil structure
Particle Diameter (µm)
-Coarse sand
-Fine sand
-Silt Clay
-Clay
-Coarse sand 2000-200
-Fine sand 200-20
-Silt Clay 20-2
-Clay <3
Difference of Sandy Soils to Clay Soils
-diameter
-surface area
-channels
Sandy soils
diameter- 1 mm or more
surface area- low surface area
channels- low surface area
Clay Soils
diameter- 2 µm
surface area-greater surface areas
channels- smaller channels
(decomposing organic matter)
humus
help improve soil aeration and infiltration
of water
crumbs
clay crumbs help improve (2)
-soil aeration
-infiltration of water
the spaces in between particles are large that water drains from them;
water remains only on the soil particle surfaces and at interstices between soil
particles
sandy soil
Sandy soils, the spaces in between particles are __ that water ___ from them;
water remains only on the ____ and at ____
large
drains
soil particle surfaces
interstices between soil particles
Characteristics of Sandy Soil and Clay Soil in terms of
-water in soil
- surface of the soil particles
Sandy Soil- the spaces in between particles are large that water drains from them;
water remains only on the soil particle surfaces and at interstices between soil
particles
Clay Soil- water does not freely drain from them and is held more tightly
water does not freely drain from them and is held more tightly
clay soils
Clay soil, water ____ from them and is held ___
does not freely drain more tightly
he moisture-holding capacity of soils.
field capacity
water content of a soil after it has been saturated with water and
excess water has been allowed to drain away.
field capacity
clay soils or soils with__ have a large field capacity
humus
clay soils might retain ___water by volume ____ after being saturated
sandy soils, which retain __ water by volume after saturation
40%
a few days
3%
Soil has water potentials and can be dissected into two components:
o Osmotic Potential
o Hydrostatic Pressure
A Negative Hydrostatic Pressure in Soil Water Lowers__
Soil Water Potential
Lowers Soil Water Potential
Negative Hydrostatic Pressure
the osmotic potential of soil water is generally negligible because
solute concentrations are low
for soils with __ concentrations of salts, Ψs is significant
substantial
osmotic pressure
-soil water
-soil
Osmotic Potential (Ψs)
▪ the osmotic potential of soil water is generally negligible because solute concentrations are low
▪ but for soils with substantial concentrations of salts, Ψs is significant
Hydrostatic Pressure (Ψp)
▪ for wet soils, Ψp is very __
▪ as a soil dries out, Ψp ___ and can become __
close to zero
decreases, quite negative
reason why Ψp decreases and can become quite negative
soil dries out
Hydrostatic Pressure (Ψp)
-difference in wet soil and dry soil
▪ for wet soils, Ψp is very close to zero
▪ as a soil dries out, Ψp decreases and can become quite negative