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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings PowerPoint Lectures for Biology, Seventh Edition Neil Campbell and Jane Reece Chapter 36 Transport in Vascular Plants
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Forces that drive transport in plants Physical forces drive the transport of materials in plants over a range of distances Transport in vascular plants occurs on three scales – Transport of water and solutes by individual cells, such as root hairs – Short-distance transport of substances from cell to cell at the levels of tissues and organs – Long-distance transport within xylem and phloem at the level of the whole plant Water Uptake in Plants
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Minerals H2OH2O CO 2 O2O2 O2O2 H2OH2O Sugar Light Physical Processes A variety of procceses are involved in the different types of transport Sugars are produced by photosynthesis in the leaves. 5 Sugars are transported as phloem sap to roots and other parts of the plant. 6 Through stomata, leaves take in CO 2 and expel O 2. The CO 2 provides carbon for photosynthesis. Some O 2 produced by photosynthesis is used in cellular respiration. 4 Transpiration, the loss of water from leaves (mostly through stomata), creates a force within leaves that pulls xylem sap upward. 3 Water and minerals are transported upward from roots to shoots as xylem sap. 2 Roots absorb water and dissolved minerals from the soil. 1 Figure 36.2 Roots exchange gases with the air spaces of soil, taking in O 2 and discharging CO 2. In cellular respiration, O 2 supports the breakdown of sugars. 7
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Selective Permeability of Membranes: A Review The selective permeability of a plant cell’s plasma membrane – Controls the movement of solutes into and out of the cell Specific transport proteins – Enable plant cells to maintain an internal environment different from their surroundings – Mineral Uptake Mineral Uptake
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings The Central Role of Proton Pumps Proton pumps in plant cells – Create a hydrogen ion gradient that is a form of potential energy that can be harnessed to do work – Contribute to a voltage known as a membrane potential Figure 36.3 CYTOPLASM EXTRACELLULAR FLUID ATP H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ Proton pump generates membrane potential and H + gradient. – – – – – + + + + +
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Energy for Solute Transport Plant cells use energy stored in the proton gradient and membrane potential – To drive the transport of many different solutes + CYTOPLASM EXTRACELLULAR FLUID Cations (, for example) are driven into the cell by the membrane potential. Transport protein K+K+ K+K+ K+K+ K+K+ K+K+ K+K+ K+K+ K+K+ – – – + + (a) Membrane potential and cation uptake – – + + Figure 36.4a
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Cotransport In the mechanism called cotransport – A transport protein couples the passage of one solute to the passage of another Figure 36.4b H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ NO 3 – – – – + + + – – – + + + (b) Cotransport of anions H+H+ of through a cotransporter. Cell accumulates anions (, for example) by coupling their transport to the inward diffusion
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ H+H+ S S S S S Plant cells can also accumulate a neutral solute, such as sucrose ( ), by cotransporting down the steep proton gradient. S H+H+ – – – + + + – – + + – Figure 36.4c H+H+ H+H+ S + – (c) Contransport of a neutral solute Cotransport The “coattail” effect of cotransport – Is also responsible for the uptake of the sugar sucrose by plant cells
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Effects of Differences in Water Potential To survive – Plants must balance water uptake and loss Osmosis – Determines the net uptake or water loss by a cell – Is affected by solute concentration and pressure
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Effects of Differences in Water Potential Water potential – Is a measurement that combines the effects of solute concentration and pressure – Determines the direction of movement of water Water – Flows from regions of high water potential to regions of low water potential
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Standard for measuring Standard for measuring Pure water is the standard. Pure water in an open container has a water potential of zero at one atmosphere of pressure.
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings How Solutes and Pressure Affect Water Potential Both pressure and solute concentration – Affect water potential The solute potential of a solution – Is proportional to the number of dissolved molecules Pressure potential – Is the physical pressure on a solution
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Quantitative Analysis of Water Potential The addition of solutes – Reduces water potential Figure 36.5a 0.1 M solution H2OH2O Pure water P = 0 S = 0.23 = 0.23 MPa = 0 MPa (a)
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Solute Potential Solute Potential S Solutes bind water molecules 1.reducing the number of free water molecules 2. lowers waters ability to do work. The Effect of Solutes on Water Potential
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Water Potential: an artificial model (a) addition of solutes on right side reduces water potential. S = -0.23 Water flows from “hypo” to “hyper” Or from hi on left to lo on right
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Pressure Potential Pressure Potential P P is the physical pressure on a solution. P can be negative transpiration in the xylem tissue of a plant (water tension) P can be positive water in living plant cells is under positive pressure (turgid)
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Application of physical pressure – Increases water potential H2OH2O P = 0.23 S = 0.23 = 0 MPa (b) H2OH2O P = 0.30 S = 0.23 = 0.07 MPa = 0 MPa (c) Figure 36.5b, c The Effect of Pressure on Water Potential
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Water Potential: an artificial model (b) adding +0.23 pressure with plunger no net flow of water (c) applying +0.30 pressure increases water potential solution now has of +0.07 Water moves right to left
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Negative pressure – Decreases water potential H2OH2O P = 0 S = 0.23 = 0.23 MPa (d) P = 0.30 S = 0 = 0.30 MPa Figure 36.5d The Effect of Pressure on Water Potential
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings (d) negative pressure or tension using plunger decreases water potential on the left. Water moves from right to left Water Potential: an artificial model
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings The Effect of Water Potential on Plant Cells Water potential – Affects uptake and loss of water by plant cells If a flaccid cell is placed in an environment with a higher solute concentration – The cell will lose water and become plasmolyzed Figure 36.6a 0.4 M sucrose solution: Initial flaccid cell: Plasmolyzed cell at osmotic equilibrium with its surroundings P = 0 S = 0.7 P = 0 S = 0.9 P = 0 S = 0.9 = 0.9 MPa = 0.7 MPa = 0.9 MPa
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings If the same flaccid cell is placed in a solution with a lower solute concentration – The cell will gain water and become turgid Distilled water: Initial flaccid cell: Turgid cell at osmotic equilibrium with its surroundings P = 0 S = 0.7 P = 0 S = 0 P = 0.7 S = 0.7 Figure 36.6b = 0.7 MPa = 0 MPa = 0 MPa The Effect of Water Potential on Plant Cells
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings The Effect of Water Loss Turgor loss in plants causes wilting – Which can be reversed when the plant is watered Figure 36.7
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Calculating Solute potential Need solute concentration Use the equation S = - iCRT i = # particles molecule makes in water C = Molar concentration R = pressure constant 0.0831 liter bar mole o K T = temperature in degrees Kelvin = 273 + o C
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Solve for water potential Knowing solute potential, water potential can be calculated by inserting values into the water potential equation. = P + S In an open container, P = 0
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Practice Problems
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Copyright © 2005 Pearson Education, Inc. publishing as Benjamin Cummings Aquaporin Proteins and Water Transport Aquaporins – Are transport proteins in the cell membrane that allow the passage of water – Do not affect water potential
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