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Water Potential Osmosis & Plant cells
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Plants & water potential
Plants can use the potential energy in water to perform work. Tomato plant regains turgor pressure – cell pushes against wall due to uptake of water
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Plants & water potential
The combined effects of 1.) solute concentration 2.) physical pressure (cell wall) can be measured as Water Potential = psi is measured in either kilopascals (KPa) or megapascals (MPa) *1 Mpa = 10 atmospheres of pressure
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Calculating Water Potential
= P S Or Water = pressure solute Potential potential potential
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Solute Potential S Solute potential is also called the osmotic potential because solutes affect the direction of osmosis. S of any solution at atmospheric pressure is always negative – why? Answer = less free water molecules to do work
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Solute Potential S Solutes bind water molecules reducing the number of free water molecules lowers waters ability to do work.
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P is the physical pressure on a solution.
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). *Think of suction P can be positive water in living plant cells is under positive pressure (turgid). *Think of squeezing or applying force
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Standard for measuring
Pure water is the standard. Pure water in an open container has a water potential of zero at one atmosphere (atm) or one bar of pressure.
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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 less neg to more neg) Or from hi on left to lo on right
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Water Potential: an artificial model
(b) adding pressure with plunger no net flow of water (c) applying pressure increases water potential solution now has of +0.07 Water moves right to left
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Water Potential: an artificial model
(d) negative pressure or tension using plunger decreases water potential on the left. Water moves from right to left
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Water relations in plant cells
(b) Flaccid cell in pure water Water potential is into cell cell becomes turgid
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Water relations in plant cells
(a) Flaccid cell placed in hypertonic solution Water potential is out of cell plasmolysis
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Calculating Solute potential
Need solute concentration Use the equation S = - iCRT i = # particles molecule makes in water C = Molar concentration R = pressure constant liter bar mole oK T = temperature in degrees Kelvin = oC
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Solve for water potential (literal equation)
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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Water Potential problems
When calculating ‘Solute Potential’ (-iCRT), the R value will depend on the pressure units given in the problem. If ‘bars’ or ‘atm’ is used, R= L-atm (*bars) / mol 0K. If kPa is used, R= (see below) UNIVERSAL GAS CONSTANT R= Latm/molK R=8.315 dm3kPa/molK
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A few notes: R value will depend on the units used for pressure. (see last slide) The ionization constant will vary, depending on if the solute can ionize in solvent or not. Ex- For NaCl (ionic bond), when dissolved in water it forms 2 ions (Na+ and Cl-), so the value is 2. Ex- For glucose (covalent bond), does not ionize in water, so the value is 1.
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Let’s Take a class (self graded) quiz!! (A
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Practice problem The value for Ψ in root tissue was found to be -3.3 bars. If you take the root tissue and place it in a 0.1 M solution of sucrose at 20°C in an open beaker, what is the Ψ of the solution, and in which direction would the net flow of water be?
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Solution: Ψ s= -iCRT -(1)(0.1M)(0.0831 L bars/mol K)(293 K)=
-2.43 bars Yp=0, so Y= The movement will be into the root cells. Goes from higher (less negative) to lower (more neg). *M = mol/L HW- Do the Water Pot. Prac. Prob. sheet
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Big Idea of Water Potential
So, we can now define osmosis as the movement of water molecules from a region of higher water potential (hypotonic) to a region of lower water potential (hypertonic) through a semi-permeable membrane. *Hypotonic has less neg value for solute potential; Hypertonic has more neg value
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Hints & reminders 1. Remember water always moves from [hi] to [lo]. *Hi is less neg value in calculation 2. Water moves from hypo hypertonic. 3. [Solute] is related to osmotic pressure. Pressure is related to pressure potential. 4. Pressure raises water potential. 5. When working problems, use zero for pressure potential in animal cells & open beakers. 6. 1 bar of pressure = 1 atmosphere
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