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
Where does the negative pressure in soil water came from?
-water is removed from the soil
As the water content of the soil decreases, the water recedes into the interstices
between soil particles, and the air–water surface develops
curved air–water interfaces
The value of Ψp in soil water can become ___ because the __ of curvature of air–water surfaces may become___ in drying soils.
quite negative
radius
very small
Water moves through soils predominantly by bulk flow driven by a
pressure gradient
Water Moves through the Soil by
Bulk Flow
As plants absorb water from the soil, they deplete the soil of water near the
surface of the roots.
b. The rate of water flow in soils depends on two factors:
▪ Size of the pressure gradient through the soil
▪ Soil hydraulic conductivity
it is a measure of ease with which water moves through the soil and it varies with the: 1) type of soil; and
2) water content
Soil hydraulic conductivity
Soil hydraulic conductivity it is a measure of ease with which water moves through the soil and it varies with the:
1) type of soil
2) water content
Soil hydraulic conductivity
o Sandy soil
o Clay soil
o Sandy soil- large hydraulic conductivity
o Clay soil- low hydraulic conductivity
hydraulic conductivity as water content decreases
decreases drastically
the decreases in hydraulic conductivity is due primarily to the
replacement of water in the soil spaces by air
when air moves into a soil channel previously filled with water, water
movement through that channel is ____ of the channel.
restricted to the periphery
as more of the soil spaces become filled with air, water can flow through fewer and narrower channels ___
hydraulic conductivity falls
microscopic extensions of root epidermal cells
root hais
Rot hair helps in increasing the
surface area of the root
Increase in the surface area of the root provide
greater capacity for absorption of ions and
water from the soil.
Water enters the root most readily in the
apical part
More mature regions of the root have an outer protective tissue called
exodermis or hypodermis
characteristic exodermis or hypodermis
impermeable to water
Water Moves in the Root via(3)
the Apoplast, Transmembrane, and Symplast Pathways
In the symplast pathway, water flows between cells through the ____without crossing the plasma membrane.
plasmodesmata
In the symplast pathway, water flows between cells through the plasmodesmata _____
without crossing the plasma membrane
water flows between cells through the plasmodesmata without crossing the plasma membrane
symplast pathway,
, water moves across the plasma membranes, with
a short visit to the cell wall space.
In the transmembrane pathway