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Grade 11 University Biology – Unit 5 Plants Transport in Plants Section 13.4 Pages 560-566 TRANSPIRATION Process in which water evaporates from the inside of the leaf to the outside through the stomata Every day, a growing plant takes in 10-20X more water than an animal of comparable size, BUT almost 90% pf the water is lost by TRANSPIRATION, the evaporation of water from the leaves and stems. The RATE of transpiration is affected by the relative humidity in the air (i.e., plants transpire more rapidly on hot, dry days). Water loss occurs through the STOMATA in the EPIDERMIS. At night, the stomata are closed, so water loss is reduced. At the same time, there is internal water loss as water evaporates from the wet cells walls of the MESOPHYLL into the INTERCELLULAR SPACES. The process raises the internal relative humidity of the leaf to almost 100 percent. When the sun rises, the stomata open to admit carbon dioxide. Since the relative humidity of the external air is usually lower than 100 percent, water vapour diffuses from inside the leaf to the outside through the stomata openings. The water needs to be replaced in the mesophyll cells. Most of the new water comes from the XYLEM. The water movement is fast and called BULK FLOW. ABSORPTION BY ROOTS Root cells contain a higher concentration of dissolved nutrients than the surrounding soil. Thus, water MOVES INTO the roots via osmosis. ROOT HAIRS absorb most of the water. The water in the cell walls of the roots epidermis is usually HYPOTONIC, a situation in which there is a greater concentration of water outside the cell wall. In this situation, water moves passively via osmosis into the roots. When the water reaches the cell walls of the ENDOERMIS, it reaches specialized cell wall region called the CASPARIAN BAND which is impregnated with a waxy layer similar to the cuticle. Water cannot pass through the Casparian band (i.e., it is impervious to water). The movement is controlled by active transport of salt dissolved in water. That is, the cells expend energy to take in salts against a CONCENTRATION GRADIENT. Salts are secreted from the cells on the inner side of the cell, and as a result, water moves out. Both water and salt move by OSMOSIS, the diffusion of water across a membrane in living system – osmotic pressure – the pressure created by water molecules as they attempt to reach equilibrium across a membrane. By this process, salts and water move through the cell wall into the xylem. ROOT PRESSURE When transpiration in the leaves is slow at night, salt is still secreted in the endodermis of the root. This creates an area of low water pressure in the xylem. More water moves into the xylem by osmosis. As water moves into the xylem, a positive pressure called ROOT PRESSURE is created. The osmotic pressure pushes the water up the xylem. Root pressure is the mechanism by which positive pressure in the roots moves water upward in a plant. NOTE: While root pressure might account for some of the upward movement of water in small herbaceous plants, it is insufficient to overcome the force of gravity and move water up tall plants. COHESION THEORY Cohesive forces between water molecules are very strong. Water evaporates molecule by molecule from the cell walls of the leaf mesophyll. Because of cohesiveness, a continuous chain of water molecules in pulled along. As water molecules cling to each other as they move up the stem and into the leaves, they pull the molecules up as they transpire out of the stomata. This creates a negative pressure, and the negative pressure exerts tension on the water confined in the xylem. As water molecules are stuck together by cohesion, the entire column of water in the xylem adheres to the sides of the xylem. It is said that the water in under tension as the column moves up the xylem. At the same time, the XYLEM TUBE narrows because of the tension. Water moves up from the roots to replace water lost from the leaves. Cohesiveness is shown by the RATE OF TRANSPIRATION. Transpiration begins in the morning with the opening of the stomata and reaches its peak by mid-afternoon. In contrast, water uptake in the root does not reach its peak until late-afternoon and continues throughout the night. Cohesion-Tension Model is a model of water transport that explains how water is moved from the roots to the leaves of a plant. Transpiration – The evaporation of water molecules from the shoot system becoming a force that moves water and dissolved minerals upward in the plant stem Cohesion – The force of attraction between water molecules Adhesion – The force that causes water molecules to stick together FACTORS IMPACTING TRANSPIRATION Temperature Transpiration increases when it is sunny and hot outside. This is because the holes on the leaves that the water escapes from open up wider in heat. This allows more water to be released in less time. In cold weather, the holes on the leaves close up tighter and transpiration rates decrease. Humidity At high humidity, the less transpiration will take place. High humidity means that there is a lot of water in the air. When this happens, there is not as much room in the air for new water vapour. The dryer the air is, the more plants will transpire because there is a lot of space left for new water vapour. Wind Transpiration occurs at higher levels when there is wind. Wind blows the air out from underneath the leaves and keeps the air fresh. Without much wind, the same air stays underneath the leaves where the water comes out of the holes. This old air gets filled up with water vapour and does not absorb new vapour. Soil Certain soils can affect the rate of transpiration. If the soil is not rich in moisture, the plant will dry out and lose leaves. Thus, there is less opportunity for transpiration to take place. Nutrient Transport in Phloem Photosynthesis occurs in the green parts of the plant, mainly the leaves. The product of photosynthesis is glucose. It is converted to sucrose for transport through the phloem. TRANSLOCATION is the transport of sucrose and other organic molecule through the phloem. PRESSURE-FLOW MODEL Translocation is from a source to a sink. The source is where the sucrose enters the sieve tubes. The sink is any region where the plants are stored. Pressure-Flow is the combination of osmosis and pressure dynamics that pushes materials from a source to a sink. For an experimental model of this model see Figure 13.23 on Page 564. A change in the concentration on sucrose also causes a movement of water in the same direction. Internal pressure increases at the source and pushes the sucroserich solution toward the sink. In the phloem, it is a POSTIVE PRESSURE causing the flow. HOMEWORK Page 566, Questions 1, 3, 4, 7, 11, 12, 15 Experiments to demonstrate transpiration in plants Experiment #1 Materials Potted plant Empty pot Cellophane Vaseline Glass plate Bell Jar Experiment Setup Methods Take a potted plant and cover the pot and base of stem with cellophane or rubber. Place the potted plant on a “vaselined-glass plate” Invert a bell-jar over the pot and plant and leave them outside the laboratory. Set up a control experiment with no plant. Observe after one hour After an hour, drops of colourless liquid are seen inside the bell-jar with the plant. To show that these drops are water, touch them with anhydrous copper sulphate (white) and its colour changes to blue. No drops of water should be found in the control experiment where there was no plant. Inference The presence of stomata makes the leaves suitable for exchange of gases which goes on during photosynthesis and respiration, and this makes loss of water inevitable. Stomata are tiny pores in the epidermis of leaves, each pore being surrounded by a pair of special cells called guard-cells which control the size of the stomata pores. The behaviour of the stomata and the rate of transpiration are determined by environmental factors. Transpiration exerts a force against that of gravity, and this is known as transpiration pull, enables water to be absorbed. Experiment #2 Materials 1 healthy geranium plant 2 glasses that are the same size and kind Water Vaseline Shirt cardboard box Scissors Sharpened pencil Ruler Window area Methods Use your ruler and pencil to measure and mark a rectangle from the cardboard shirt box that is four by six inches. Cut out the rectangle. With the sharp tip of the pencil, poke a little hole in the middle of the cardboard rectangle. Break off a healthy leaf and stem from the geranium plant. The leaf stem is called a petiole. Put the petiole of the leaf in the hole in the cardboard rectangle. Fill one of the glasses three-quarters full with water. Cut the cardboard on top of the glass with the water in it so the stem is down into the water and the leaf is on top of the cardboard- not in the water. Take a little bit of vaseline and put it around the hole. This is to keep evaporated water from the glass seeping up into the top glass. Put the second glass upside down over the leaf, resting against the other glass' mouth. Put the glasses on a ledge or table top near a window where there is a good source of sunlight. Observe after what happens after 3 or 4 hours. Do you see little drops of water on the inside of the top glass? Where is the water coming from? If you plugged the hole around the stem, the water from the bottom glass should not be getting up into the top glass. This is transpiration, the process whereby the leaves on green plants give off excess water. Look at the bottom of the geranimum's leaves. You will see little dots which are called stomates. The stomates give off water