Whilst water can travel across a membrane in the specific channel (referred to as an aquaporin), it does not carry ions with it via that channel because the aquaporin is only just wide enough for one water molecule at a time. Instead, separate transporter proteins or 'protein pumps' are adapted to carry individual ions across the membrane, by active transport.
Transpiration is the loss of water vapour from the leaves/stomata (and stems) of plants
A potometer does not measure the true rate of transpiration in a plant because:
water is used by plant for support/turgidity
water is used for hydrolysis reactions
water is used during photosynthesis
water is produced in condensation reactions
water is produced during respiration
The potometer only measures transpiration in one shoot/section of the plant OR transpiration rates may vary in other parts of the plant
Leaking apparatusOR apparatus not sealed properly
Plants with adaptations to conserve water, such as marram grasses or cacti, are described as xerophytic, or known as xerophytes.
Marram grass leaves are well adapted to minimise water loss in the following ways:
Leaves are rolled up to reduce the exposure of leaf surfaces to the wind and so reduce water loss by evaporation
The stomata are sunken in pits to reduce water loss by evaporation
The inner surface of the leaf possesses (a large number of) hairs which shield the stomata and trap moist air, again reducing water loss by evaporation
The exposed surface has a thick waxy cuticle to reduce evaporation
A plant replaces the water it loses via transpiration by the following mechanisms:
Transpiration/evaporation of water (at leaves) creates suction/tension
This causes water to be sucked/pulled out of the xylem (in leaves)
Water moves up xylem (in stem) due to suction/tension/pulling forces
(Pulling forces transmitted by) cohesion/hydrogen bonding between water molecules
This moves water from roots to leaves
Water enters root (cell) via osmosis due to higher solute concentration inside root (cell)
A halophyte is a plant that is adapted to saline/salty conditions/soilsOR a plant that lives in salt marshes/areas periodically flooded with sea water
Adaptations of halophytes may include:
The ability to sequester/store away salts within their cell walls/vacuoles
The ability to concentrate absorbed salts in certain leaves, which then fall off the plant
Stems that can take over the role of photosynthesis when leaves are shed
Reduced leaf surface area to reduce water loss OR sunken stomata to reduce water loss
Salt glands that actively excrete salt to stop it from building up
Deep roots to reach fresh water underground
Minerals are absorbed into the plant root by:
minerals can move into root cells by facilitated diffusion
from an area of high concentration to low concentration
root hair cell has large surface area for absorption
minerals can also move into root cells via active transport
moving against the concentration gradient, requires ATP
through protein pumps/carrier proteins
proton pumps move H+ out of root cells, allowing mineral ions to enter
Pressure changes in the xylem occurs during transpiration:
Pressure increases as water moves into the xylem at the root
Increase in active transport of mineral ions increases osmosis into the xylem and increases pressure
Pressure decreases / negative pressure occurs at the leaves as water evaporates from the spongy mesophyll cells
Increased transpiration results in a more negative pressure
(Caused by) conditions such as increased wind movement, increased temperature, increased sunlight or decreased humidity
The route of water movement can be described as follows:
Osmosis into the root from the soil; from a low to a high osmolarity
Apoplast route/pathway through the cell walls of the cells in the cortex
Symplast route/pathway through the cytoplasm of the cells in the cortex
Casparian strip is a water proof layer, so water diverts out of the cell walls into the cytoplasm / out of the apoplastic route into the symplastic route
Water moves into the xylem by osmosis
More air movement leads to increased rates of transpiration
When the air is relatively still, water molecules can accumulate just outside the stomata, creating a local area of high humidity
Less water vapour will diffuse out into the air due to the reduced concentration gradient
Air currents, or wind, can carry water molecules away from the leaf surface, increasing the concentration gradient and causing more water vapour to diffuse out
Higher temperatures lead to higher rates of transpiration, up to a point at which transpiration rates will slow
An increase in temperature results in an increase in the kinetic energy of molecules
This increases the rate of transpiration as water molecules evaporate out of the leaf at a faster rate
If the temperature gets too high the stomata close to prevent excess water loss
This dramatically reduces the rate of transpiration
Higher light intensities will increase the rate of transpiration up to a point at which transpiration rates will level off
Stomata close in the dark and their closure greatly reduces the rate of transpiration
Stomata open when it is light to enable gas exchange for photosynthesis; this increases the rate of transpiration
Once the stomata are all open any increase in light intensity has no effect on the rate of transpiration
Higher humidity levels reduce the rate of transpiration
If the humidity is high that means the air surrounding the leaf surface is saturated with water vapour
This causes the rate of transpiration to decrease as there is no concentration gradient between the inside of the leaf and the outside
At a certain level of humidity, an equilibrium is reached; water vapour levels inside and outside the leaf are the same, so there is no net loss of water vapour from the leaves
Xylem is closer to the centre of the stem, phloem is further
The amount of water lost from the leaves (transpiration rate) is regulated by the opening and closing of stomata
Guard cells flank the stomata and can occlude the opening by becoming increasingly flaccid in response to cellular signals
When a plant begins to wilt from water stress, dehydrated mesophyll cells release the plant hormone abscisic acid (ABA)
Abscisic acid triggers the efflux of potassium from guard cells, decreasing water pressure within the cells (lose turgor)
A loss of turgor makes the stomatal pore close, as the guard cells become flaccid and block the opening
The rate of phloem transport will principally be determined by the concentration of dissolved sugars in the phloem.
The concentration of dissolved sugars will be affected by:
The rate of photosynthesis (which is affected by light intensity, CO2 concentration, temperature, etc.)
The rate of cellular respiration (this may be affected by any factor which physically stresses the plant)
The rate of transpiration (this will potentially determine how much water enters the phloem)
The diameter of the sieve tubes (will affect the hydrostatic pressure and may differ between plant species)
Measuring translocation rates
A plant is grown with radioactively-labelled carbon dioxide
The leaves will convert the CO2 into radioactively-labelled sugars, which are transported by the phloem
Aphids are positioned along the plant’s length and encouraged to feed on the phloem sap
Aphid stylet is severed and sap continues to flow from the plant at the selected positions
The sap is then analysed for the presence of radioactively-labelled sugars
Translocation rate can be calculated based on the time taken for the radioisotope to be detected at different positions