4 Water Balance of Plants Flashcards
the atmosphere is the source of _ , which is needed for photosynthesis.
carbon dioxide
the atmosphere is
relatively _ and can _ the plant
dry
dehydrate
_ water loss from
the leaf is driven by a gradient in water vapor concentration.
Transpirational
Long-distance transport in the
xylem is driven by _ , as is water movement in the soil.
pressure gradients
The water content and the rate of water movement in soils depend to a large extent on
_
soil type and soil structure
have a relatively low surface particles may be 1 mm or more in diameter
Sandy Soils
have a relatively low surface area per gram of soil and have large spaces or channels between particles
Sandy Soils
have particles that are smaller than 2 µm in diameter
Clay Soils
have much greater surface areas and smaller channels between particles
Clay Soils
with the aid of organic substances such as _ (decomposing organic matter), clay particles may aggregate into “crumbs” that help improve soil aeration and infiltration
of water
humus
Water in the soil may exist as a _ adhering to the surface of the soil particles, or it may fill the entire channel between particles.
film
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 soils
water does not freely drain from them and is held more tightly
clay soils
the moisture-holding capacity of soils
Field capacity
the 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 humus have a _
large field capacity
clay soils might retain _ % water by volume a few days after being saturated unlike sandy soils, which retain _ % water by volume after saturation
40
3
A Negative Hydrostatic Pressure in Soil Water Lowers _
Soil Water Potential
2 components of soil water potential
- osmotic potential
- hydrostatic pressure
is generally negligible because solute
concentrations are low
the osmotic potential of soil water
but for soils with substantial concentrations of salts, _ is significant
osmotic potential Ψs
for wet soils, Ψp is very _
close to zero
as a soil _ , Ψp decreases and can become quite negative
dries out
As a soil dries out, water is first removed from the center of the largest spaces between particles. Because of _ , water tends to cling to the surfaces of soil particles, so a large surface area between soil water and soil air develops.
adhesive forces