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Water Balance of Plants

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Title: Water Balance of Plants


1
Water Balance of Plants
2
Water balance of plants
  • Earths atmosphere presents problems to plants
  • The atmosphere is a source of CO2
  • Required for photosynthesis
  • Atmosphere is relatively dry
  • Can dehydrate the plant
  • Plants have evolved ways to control water loss
    from leaves and to replace water loss to
    atmosphere
  • Involves
  • A gradient in water vapor concentration (leaves)
  • Pressure gradients in xylem and soil

3
Water in the Soil
  • Water content in soil and rate of water movement
    depends on the type and texture of soil
  • Soil Particle size surface area
  • (um) per gram (m2)
  • Course sand 2000 200 lt1-10
  • Fine sand 200 20 lt1-10
  • Silt 20 2 10-100
  • Clay lt2 100-1000
  • Sandy soil
  • Low surface area per gram and large spaces
    between particles
  • Clay
  • Large surface area per gram and small spaces
    between particles

4
Water and plant cells
  • 80-90 of a growing plant cell is water
  • This varies between types of plant cells
  • Carrot has 85-95 water
  • Wood has 35-75 water
  • Seeds have 5-15 water
  • Plant continuously absorb and lose water
  • Lost through the leaves
  • Called transpiration

5
Water
6
Water
  • (A) Hydrogen bonds between water molecules
    results in local aggregations of water molecules
  • (B) Theses are very short lived, break up rapidly
    to form more random configurations
  • Due to temperature variations in water

7
Cell water potential - yw
  • The equation yw ys yp yg
  • Affected by three factors
  • ys Solute potential or osmotic potential
  • The effect of dissolved solutes on water and the
    cell
  • yp Hydrostatic pressure of the solution. A ve
    pressure is known as Turgor pressure
  • Can be ve, as in the xylem and cell wall this
    is important in moving water long distances in
    plants
  • yg Gravity - causes water to move downwards
    unless opposed by an equal and opposite force

8
Water in the Soil
  • The main driving forces for water flow from the
    soil through the plant to the atmosphere include
  • Differences in
  • H2O vapor
  • Hydrostatic pressure
  • Water potential
  • All of these act to allow the movement of water
    into the plant.

9
Water absorption from soil
  • Water clings to the surface of soil particles.
  • As soil dries out, water moves first from the
    center of the largest spaces between particles.
  • Water then moves to smaller spaces between soil
    particles.
  • Root hairs make intimate contact with soil
    particles amplify the surface area for water
    absorption by the plant.

10
Water Moves through soil by bulk flow
  • Bulk flow
  • Concerted movement of groups of molecules en
    masse, most often in response to a pressure
    gradient.
  • Dependant on the radius of the tube that water is
    traveling in.
  • Double radius flow rate increases 16
    times!!!!!!!!!!
  • This is the main method for water movement in
    Xylem, Cell Walls and in the soil.
  • Independent of solute concentration gradients
    to a point
  • So different from diffusion

11
Water Moves through soil by bulk flow
  • In addition, diffusion of water vapor accounts
    for some water movement.
  • As water moves into root less in soil near the
    root
  • Results in a pressure gradient with respect to
    neighboring regions of soil.
  • So there is a reduction in yp near the root and a
    higher yp in the neighboring regions of soil.
  • Water filled pore spaces in soil are
    interconnected, water moves to root surface by
    bulk flow down the pressure gradient

12
Water Moves through soil by bulk flow
  • The rate of water flow depends on
  • Size of the pressure gradient
  • Soil hydraulic conductivity (SHC)
  • Measure of the ease in which water moves through
    soil
  • SHC varies with water content and type of soil
  • Sandy soil high SHC
  • Large spaces between particles
  • Clay soil low SHC
  • Very small spaces between particles

13
Water Moves through soil by bulk flow
  • As water moves from soil into root the spaces
    fill with air
  • This reduces the flow of water
  • Permanent wilting point
  • At this point the water potential (yw) in soil is
    so low that plants cannot regain turgor pressure
  • There is not enough of a pressure gradient for
    water to flow to the roots from the soil
  • This varies with plant species

14
Plant roots
  • Meristematic zone
  • Cells divide both in direction of root base to
    form cells that will become the functional root
    and in the direction of the root apex to form the
    root cap
  • Elongation zone
  • Cells elongate rapidly, undergo final round of
    divisions to form the endodermis. Some cells
    thicken to form casparian strip
  • Maturation zone
  • Fully formed root with xylem and phloem root
    hairs first appear here

15
Mycorrhizal associations
  • Not unusual
  • 83 of dicots, 79 of monocots and all
    gymnosperms
  • Ectotrophic Mycorrhizal fungi
  • Form a thick sheath around root. Some mycelium
    penetrates the cortex cells of the root
  • Root cortex cells are not penetrated, surrounded
    by a zone of hyphae called Hartig net
  • The capacity of the root system to absorb
    nutrients improved by this association the
    fungal hyphae are finer than root hairs and can
    reach beyond nutrient-depleted zones in the soil
    near the root

16
Mycorrhizal associations
  • Vesicular arbuscular mycorrhizal fungi
  • Hyphae grow in dense arrangement , both within
    the root itself and extending out from the root
    into the soil
  • After entering root, either by root hair or
    through epidermis hyphae move through regions
    between cells and penetrate individual cortex
    cells.
  • Within cells form oval structures vesicles
    and branched structures arbuscules (site of
    nutrient transfer)
  • P, Cu, Zn absorption improved by hyphae
    reaching beyond the nutrient-depleted zones in
    the soil near the root

17
Water transport processes
  • Moves from soil, through plant, and to atmosphere
    by a variety of mediums
  • Cell wall
  • Cytoplasm
  • Plasma membranes
  • Air spaces
  • How water moves depends on what it is passing
    through

18
Water across plant membranes
  • There is some diffusion of water directly across
    the bi-lipid membrane.
  • Auqaporins Integral membrane proteins that form
    water selective channels allows water to
    diffuse faster
  • Facilitates water movement in plants
  • Alters the rate of water flow across the plant
    cell membrane NOT direction

19
Water uptake in the roots
  • Root hairs increase surface area of root to
    maximize water absorption.
  • From the epidermis to the endodermis there are
    three pathways in which water can flow
  • 1 Apoplast pathway
  • Water moves exclusively through cell walls
    without crossing any membranes
  • The apoplast is a continuous system of cell walls
    and intercellular air spaces in plant tissue

20
Water uptake in the roots
  • 2 Transmembrane pathway
  • Water sequentially enters a cell on one side,
    exits the cell on the other side, enters the next
    cell, and so on.
  • 3 Symplast pathway
  • Water travels from one cell to the next via
    plasmodesmata.
  • The symplast consist of the entire network of
    cell cytoplasm interconnected by plasmodesmata

21
Water uptake in the roots
  • At the endodermis
  • Water movement through the apoplast pathway is
    stopped by the Casparian Strip
  • Band of radial cell walls containing suberin , a
    wax-like water-resistant material
  • The casparian strip breaks continuity of the
    apoplast and forces water and solutes to cross
    the endodermis through the plasma membrane
  • So all water movement across the endodermis
    occurs through the symplast

22
Water transport through xylem
  • Compared with water movement across root tissue
    the xylem is a simple pathway of low resistance
  • Consists of two types of tracheary elements.
  • Tracheids
  • Vessile elements only found in angiosperms, and
    some ferns
  • The maturation of both these elements involves
    the death of the cell. They have no organelles
    or membranes
  • Water can move with very little resistance

23
Water transport through xylem
  • Tracheids Elongated spindle-shaped cells
    arranged in overlapping vertical files.
  • Water flows between them via pits areas with no
    secondary walls and thin porous primary walls
  • Vessel elements Shorter wider. The open end
    walls provide an efficient low-resistance pathway
    for water movement.
  • Perforation plate forms at each end allow
    stacking end on to form a larger conduit called a
    vessel
  • At the end there are no plates- communicate with
    neighboring vessels via pits

24
Water transport through xylem
  • Water movement through xylem needs less pressure
    than movement through living cells.
  • However, how does this explain how water moves
    from the roots of a tree up to 100 meters above
    ground?
  • Cohesion-tension theory
  • Relies on the fact that water is a polar molecule
  • Water is constantly lost by transpiration in the
    leaf. When one water molecule is lost another is
    pulled along. Transpiration pull, utilizing
    capillary action and the inherent surface tension
    of water, is the primary mechanism of water
    movement in plants.

25
Water transport through xylem
  • Plants can get embolisms too!
  • Air bubbles can form in xylem
  • Air can be pulled through microscopic pores in
    the xylem cell wall
  • Cold weather allows air bubbles to form due to
    reduced solubility of gases in ice
  • Once a gas bubble has formed it will expand as
    gases can not resist tensile forces
  • Called Cavitation

26
Water transport through xylem
  • Such breaks in the water column are not unusual.
  • Impact minimized by several means
  • Gas bubbles can not easily pass through the small
    pores of the pit membranes.
  • Xylem are interconnected, so one gas bubble does
    not completely stop water flow
  • Water can detour blocked point by moving through
    neighboring, connected vessels.

27
Water transport through xylem
  • Gas bubbles can also be eliminated from the
    xylem.
  • At night, xylem water pressure increases and
    gases may simply dissolve back into the solution
    in the xylem.
  • Many plants have secondary growth in which new
    xylem forms each year. New xylem becomes
    functional before old xylem stops functioning
  • As a back up to finding a way around gas bubbles.

28
Water evaporation in the leaf affects the xylem
  • The tensions needed to pull water through the
    xylem are the result of evaporation of water from
    leaves.
  • Water is brought to leaves via xylem of the leaf
    vascular bundle, which branches into veins in
    the leaf.
  • From the xylem, water is drawn in to the cells of
    the leaf and along the cell wall.

29
Water evaporation in the leaf affects the xylem
  • Transpiration pull, which causes water to move up
    the xylem begins in the cell walls of leaf cells
  • The cell wall acts as a capillary wick soaked
    with water.
  • Water adheres to cellulose and other hydrophilic
    wall components.
  • Mesophyll cells within leaf are in direct contact
    with atmosphere via all the air spaces in the leaf

30
Water evaporation in the leaf affects the xylem
  • So, negative pressure exists in leaves- cause
    surface tension on the water
  • As more water is lost to the atmosphere the
    remaining water is drawn into the cell wall
  • As more water is removed from the wall
    the pressure of the water becomes
    more ve
  • This induces a motive force to pull water up the
    xylem

31
Water movement from leaf to atmosphere
  • After water has evaporated from the cell surface
    of the intercellular air space diffusion takes
    over.
  • So the path of water
  • Xylem
  • Cell wall of mesophyll cells
  • Evaporated into air spaces of leaf
  • Diffusion occurs water vapor then leaves via
    stomatal pore
  • Goes down a concentration gradient.

32
Water Vapor diffuses quickly in air
  • Diffusion of water out of the leaf is very fast
  • Diffusion is much more rapid in a gas than in a
    liquid
  • Transpiration from the leaf depends on two
    factors
  • ONE
  • Difference in water vapor concentration between
    leaf air spaces and the atmosphere
  • Due to high surface area to volume ratio
  • Allows for rapid vapor equilibrium inside the
    leaf
  • TWO
  • The diffusional resistance of the pathway from
    leaf to atmosphere

33
Water Vapor diffuses quickly in air
  • The diffusional resistance of the pathway from
    leaf to atmosphere
  • Two components
  • The resistance associated with diffusion through
    the stomatal pore.
  • Leaf stomatal resistance (rs)
  • Resistance due to a layer of unstirred air next
    to the leaf surface
  • Boundary layer resistance

34
Boundary layer resistance
  • Thickness of the layer is determined by wind
    speed.
  • Still air layer may be so thick that water is
    effectively stopped from leaving the leaf
  • Windy conditions moving air reduces the
    thickness of the boundary layer at the leaf
    surface
  • The size and shape of leaves influence air flow
    but the stomata itself play the most critical
    role leaf transpiration

35
Stomatal control
  • Almost all leaf transpiration results from
    diffusion of water vapor through the stomatal
    pore
  • Remember the way cuticle?
  • Provide a low resistance pathway for diffusion of
    gasses across the epidermis and cuticle
  • Regulates water loss in plants and the rate of
    CO2 uptake
  • Needed for sustained CO2 fixation during
    photosynthesis

36
Stomatal control
  • When water is abundant
  • Temporal regulation of stomata is used
  • OPEN during the day
  • CLOSED at night
  • At night there is no photosynthesis, so no demand
    for CO2 inside the leaf
  • Stomata closed to prevent water loss
  • Sunny day - demand for CO2 in leaf is high
    stomata wide open
  • As there is plenty of water, plant trades water
    loss for photosynthesis products

37
Stomatal control
  • When water is limited
  • Stomata will open less or even remain closed even
    on a sunny morning
  • Plant can avoid dehydration
  • Stomatal resistance can be controlled by opening
    and closing the stomatal pores.
  • Specialized cells The Guard cells

38
Stomatal guard cells
  • There are two main types
  • One is typical of monocots and grasses
  • Dumbbell shape with bulbous ends
  • Pore is a long slit
  • The other is typical of dicots
  • Kidney shaped - have an elliptical contour with
    pore in the center

39
Stomatal guard cells
  • Alignment of cellulose microfibrils reinforce all
    plant cell walls.
  • These play an essential role in opening and
    closing stomata
  • In monocots
  • Guard cells works like beams with inflatable
    ends.
  • Bulbous ends swell, beams separate and slit
    widens
  • In dicots
  • Cellulose microfibrils fan out radially from the
    pore
  • Cell girth is reinforced like a steel-belted
    radial tire
  • Guard cell curve outward during stomatal opening

40
Stomatal guard cells
  • Guard cells act as hydraulic valves
  • Environmental factors are sensed by guard cells
  • Light intensity, temperature, relative humidity,
    intercellular CO2 concentration
  • Integrated into well defined responses
  • Ion uptake in guard cell
  • Biosynthesis of organic molecules in guard cells
  • This alters the water potential in the guard
    cells
  • Water enders them
  • Swell up 40-100

41
Relationship between water loss and CO2 gain
  • Effectiveness of controlling water loss and
    allowing CO2 uptake for photosynthesis is called
    the transpiration ratio.
  • There is a large ratio of water efflux and CO2
    influx
  • Concentration ratio driving water loss is 50
    larger than that driving CO2 influx
  • CO2 diffuses 1.6 times slower than water
  • Due to CO2 being a larger molecule than water
  • CO2 uptake must cross the plasma membrane,
    cytoplasm, and chloroplast membrane. All add
    resistance

42
Soil to plant to atmosphere
  • Soil and Xylem
  • Water moves by bulk flow
  • In the vapor phase
  • Water moves by diffusion until it reaches out
    side air, then convection occurs
  • When water is transmitted across membranes
  • Driven by water potential differences across the
    membrane
  • Such osmotic flow due to cells absorb water and
    roots take it from soil to xylem

43
Soil to plant to atmosphere
  • In each of these three cases water moves towards
    regions of low water potential or free energy.
  • Water potential decreases from soil to the leaves
  • However, water pressure can vary between
    neighboring cells
  • Xylem negative pressure
  • Leaf cell - positive pressure
  • Also, within leaf cells water potential is
    reduced by a high concentration of dissolved
    solutes

44
Figure 11.8 (1)
Leaves that eat insects
  • Some plants obtain nitrogen from digesting
    animals (mostly insects).
  • The Pitcher plant has digestive enzymes at the
    bottom of the trap
  • This is a passive trap Insects fall in and can
    not get out
  • Pitcher plants have specialized vascular network
    to tame the amino acids from the digested insects
    to the rest of the plant

45
Figure 11.12 (2)
Leaves that eat insects
  • The Venus fly trap has an active trap
  • Good control over turgor pressure in each plant
    cell.
  • When the trap is sprung, ion channels open and
    water moves rapidly out of the cells.
  • Turgor drops and the leaves slam shut
  • Digestive enzymes take over

46
Summary
  • Water is the essential medium of life.
  • Land plants faced with dehydration by water loss
    to the atmosphere
  • There is a conflict between the need for water
    conservation and the need for CO2 assimilation
  • This determines much of the structure of land
    plants
  • 1 extensive root system to get water from soil
  • 2 low resistance path way to get water to leaves
    xylem
  • 3 leaf cuticle reduces evaporation
  • 4 stomata controls water loss and CO2 uptake
  • 5 guard cells control stomata.
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